dictionary for quest4d 22 october 2008 - mumm.ac.be€¦parameter dictionary for quest4d – 22...
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Parameter Dictionary for QUEST4D – 22 October 2008
Parameter: BDENS - Bulk density
Method: 1040
Matrix: US - Unfractionated
Unit: g/cm3 Description: Determination of vertical bulk density profiles by non-intrusive gamma-
ray-attenuation measurements. The gamma-ray-densitometer moves automatically along the sediment core in 1 cm steps. The magnitude of attenuation depends on the bulk density of the exposed material and the diameter of the column. (Gerland and Villiger, 1995).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: TAU_CR_E - Critical shear stress for erosion
Method: 1041
Matrix: US - Unfractionated
Unit: Pa Description: The SETEG-System determines a depth oriented measurement of the
critical erosion shear stress (usually in depth intervals of 2-3 cm). The sediment core is mounted on the bottom of the pressure duct, exposing the sediment surface to the flow. The continuously adjustable discharge is increased, until entrainment of sediment particles from the surface can be observed. The corresponding wall shear stress can be determined by a hydraulic calibration function which describes the relationship between wall shear stress and discharge through pressure loss.
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.44 - Erosion rate at an excess shear stress of 0.44 Pa
Method: 1042
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.01 - Erosion rate at an excess shear stress of 0.01 Pa
Method: 1043
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.02 - Erosion rate at an excess shear stress of 0.02 Pa
Method: 1044
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.03 - Erosion rate at an excess shear stress of 0.03 Pa
Method: 1045
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.04 - Erosion rate at an excess shear stress of 0.04 Pa
Method: 1046
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.05 - Erosion rate at an excess shear stress of 0.05 Pa
Method: 1047
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.06 - Erosion rate at an excess shear stress of 0.06 Pa
Method: 1048
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.07 - Erosion rate at an excess shear stress of 0.07 Pa
Method: 1049
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.09 - Erosion rate at an excess shear stress of 0.09 Pa
Method: 1050
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.10 - Erosion rate at an excess shear stress of 0.1 Pa
Method: 1051
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.11 - Erosion rate at an excess shear stress of 0.11 Pa
Method: 1052
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.12 - Erosion rate at an excess shear stress of 0.12 Pa
Method: 1053
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.13 - Erosion rate at an excess shear stress of 0.13 Pa
Method: 1054
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.14 - Erosion rate at an excess shear stress of 0.14 Pa
Method: 1055
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.15 - Erosion rate at an excess shear stress of 0.15 Pa
Method: 1056
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.16 - Erosion rate at an excess shear stress of 0.16 Pa
Method: 1057
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.17 - Erosion rate at an excess shear stress of 0.17 Pa
Method: 1058
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.18 - Erosion rate at an excess shear stress of 0.18 Pa
Method: 1059
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.19 - Erosion rate at an excess shear stress of 0.19 Pa
Method: 1060
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.20 - Erosion rate at an excess shear stress of 0.2 Pa
Method: 1061
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.21 - Erosion rate at an excess shear stress of 0.21 Pa
Method: 1062
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.22 - Erosion rate at an excess shear stress of 0.22 Pa
Method: 1063
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.23 - Erosion rate at an excess shear stress of 0.23 Pa
Method: 1064
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.24 - Erosion rate at an excess shear stress of 0.24 Pa
Method: 1065
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.25 - Erosion rate at an excess shear stress of 0.25 Pa
Method: 1066
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.26 - Erosion rate at an excess shear stress of 0.26 Pa
Method: 1067
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.27 - Erosion rate at an excess shear stress of 0.27 Pa
Method: 1068
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.28 - Erosion rate at an excess shear stress of 0.28 Pa
Method: 1069
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.29 - Erosion rate at an excess shear stress of 0.29 Pa
Method: 1070
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.30 - Erosion rate at an excess shear stress of 0.3 Pa
Method: 1071
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.31 - Erosion rate at an excess shear stress of 0.31 Pa
Method: 1072
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.32 - Erosion rate at an excess shear stress of 0.32 Pa
Method: 1073
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.33 - Erosion rate at an excess shear stress of 0.33 Pa
Method: 1074
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.34 - Erosion rate at an excess shear stress of 0.34 Pa
Method: 1075
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.35 - Erosion rate at an excess shear stress of 0.35 Pa
Method: 1076
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.36 - Erosion rate at an excess shear stress of 0.36 Pa
Method: 1077
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.37 - Erosion rate at an excess shear stress of 0.37 Pa
Method: 1078
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET.378 - Erosion rate at an excess shear stress of 0.378 Pa
Method: 1079
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.38 - Erosion rate at an excess shear stress of 0.38 Pa
Method: 1080
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.39 - Erosion rate at an excess shear stress of 0.39 Pa
Method: 1081
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.40 - Erosion rate at an excess shear stress of 0.4 Pa
Method: 1082
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.41 - Erosion rate at an excess shear stress of 0.41 Pa
Method: 1083
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.43 - Erosion rate at an excess shear stress of 0.43 Pa
Method: 1084
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.45 - Erosion rate at an excess shear stress of 0.45 Pa
Method: 1085
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.46 - Erosion rate at an excess shear stress of 0.46 Pa
Method: 1086
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.47 - Erosion rate at an excess shear stress of 0.47 Pa
Method: 1087
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.48 - Erosion rate at an excess shear stress of 0.48 Pa
Method: 1088
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.49 - Erosion rate at an excess shear stress of 0.49 Pa
Method: 1089
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.50 - Erosion rate at an excess shear stress of 0.5 Pa
Method: 1090
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.51 - Erosion rate at an excess shear stress of 0.51 Pa
Method: 1091
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.54 - Erosion rate at an excess shear stress of 0.54 Pa
Method: 1092
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.55 - Erosion rate at an excess shear stress of 0.55 Pa
Method: 1093
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.56 - Erosion rate at an excess shear stress of 0.56 Pa
Method: 1094
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.57 - Erosion rate at an excess shear stress of 0.57 Pa
Method: 1095
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.58 - Erosion rate at an excess shear stress of 0.58 Pa
Method: 1096
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.59 - Erosion rate at an excess shear stress of 0.59 Pa
Method: 1097
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.61 - Erosion rate at an excess shear stress of 0.61 Pa
Method: 1098
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.62 - Erosion rate at an excess shear stress of 0.62 Pa
Method: 1099
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.63 - Erosion rate at an excess shear stress of 0.63 Pa
Method: 1100
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.64 - Erosion rate at an excess shear stress of 0.64 Pa
Method: 1101
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.66 - Erosion rate at an excess shear stress of 0.66 Pa
Method: 1102
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.67 - Erosion rate at an excess shear stress of 0.67 Pa
Method: 1103
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.68 - Erosion rate at an excess shear stress of 0.68 Pa
Method: 1104
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.69 - Erosion rate at an excess shear stress of 0.69 Pa
Method: 1105
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.72 - Erosion rate at an excess shear stress of 0.72 Pa
Method: 1106
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.73 - Erosion rate at an excess shear stress of 0.73 Pa
Method: 1107
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.74 - Erosion rate at an excess shear stress of 0.74 Pa
Method: 1108
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.75 - Erosion rate at an excess shear stress of 0.75 Pa
Method: 1109
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.77 - Erosion rate at an excess shear stress of 0.77 Pa
Method: 1110
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.78 - Erosion rate at an excess shear stress of 0.78 Pa
Method: 1111
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.80 - Erosion rate at an excess shear stress of 0.8 Pa
Method: 1112
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.81 - Erosion rate at an excess shear stress of 0.81 Pa
Method: 1113
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.82 - Erosion rate at an excess shear stress of 0.82 Pa
Method: 1114
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.83 - Erosion rate at an excess shear stress of 0.83 Pa
Method: 1115
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.84 - Erosion rate at an excess shear stress of 0.84 Pa
Method: 1116
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.85 - Erosion rate at an excess shear stress of 0.85 Pa
Method: 1117
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.88 - Erosion rate at an excess shear stress of 0.88 Pa
Method: 1118
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.89 - Erosion rate at an excess shear stress of 0.89 Pa
Method: 1119
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.90 - Erosion rate at an excess shear stress of 0.9 Pa
Method: 1120
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.92 - Erosion rate at an excess shear stress of 0.92 Pa
Method: 1121
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.94 - Erosion rate at an excess shear stress of 0.94 Pa
Method: 1122
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.97 - Erosion rate at an excess shear stress of 0.97 Pa
Method: 1123
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.99 - Erosion rate at an excess shear stress of 0.99 Pa
Method: 1124
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.00 - Erosion rate at an excess shear stress of 1 Pa
Method: 1125
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.01 - Erosion rate at an excess shear stress of 1.01 Pa
Method: 1126
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.03 - Erosion rate at an excess shear stress of 1.03 Pa
Method: 1127
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.04 - Erosion rate at an excess shear stress of 1.04 Pa
Method: 1128
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.06 - Erosion rate at an excess shear stress of 1.06 Pa
Method: 1129
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.08 - Erosion rate at an excess shear stress of 1.08 Pa
Method: 1130
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.09 - Erosion rate at an excess shear stress of 1.09 Pa
Method: 1131
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.11 - Erosion rate at an excess shear stress of 1.11 Pa
Method: 1132
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.12 - Erosion rate at an excess shear stress of 1.12 Pa
Method: 1133
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.15 - Erosion rate at an excess shear stress of 1.15 Pa
Method: 1134
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.16 - Erosion rate at an excess shear stress of 1.16 Pa
Method: 1135
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.17 - Erosion rate at an excess shear stress of 1.17 Pa
Method: 1136
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.18 - Erosion rate at an excess shear stress of 1.18 Pa
Method: 1137
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.19 - Erosion rate at an excess shear stress of 1.19 Pa
Method: 1138
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.20 - Erosion rate at an excess shear stress of 1.2 Pa
Method: 1139
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.23 - Erosion rate at an excess shear stress of 1.23 Pa
Method: 1140
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.25 - Erosion rate at an excess shear stress of 1.25 Pa
Method: 1141
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.35 - Erosion rate at an excess shear stress of 1.35 Pa
Method: 1142
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.37 - Erosion rate at an excess shear stress of 1.37 Pa
Method: 1143
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.40 - Erosion rate at an excess shear stress of 1.4 Pa
Method: 1144
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.41 - Erosion rate at an excess shear stress of 1.41 Pa
Method: 1145
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.45 - Erosion rate at an excess shear stress of 1.45 Pa
Method: 1146
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.46 - Erosion rate at an excess shear stress of 1.46 Pa
Method: 1147
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.54 - Erosion rate at an excess shear stress of 1.54 Pa
Method: 1148
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.69 - Erosion rate at an excess shear stress of 1.69 Pa
Method: 1149
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.72 - Erosion rate at an excess shear stress of 1.72 Pa
Method: 1150
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.73 - Erosion rate at an excess shear stress of 1.73 Pa
Method: 1151
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.81 - Erosion rate at an excess shear stress of 1.81 Pa
Method: 1152
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.82 - Erosion rate at an excess shear stress of 1.82 Pa
Method: 1153
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.84 - Erosion rate at an excess shear stress of 1.84 Pa
Method: 1154
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.85 - Erosion rate at an excess shear stress of 1.85 Pa
Method: 1155
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.88 - Erosion rate at an excess shear stress of 1.88 Pa
Method: 1156
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.89 - Erosion rate at an excess shear stress of 1.89 Pa
Method: 1157
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.90 - Erosion rate at an excess shear stress of 1.9 Pa
Method: 1158
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET1.98 - Erosion rate at an excess shear stress of 1.98 Pa
Method: 1159
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.00 - Erosion rate at an excess shear stress of 2 Pa
Method: 1160
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.04 - Erosion rate at an excess shear stress of 2.04 Pa
Method: 1161
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.15 - Erosion rate at an excess shear stress of 2.15 Pa
Method: 1162
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.18 - Erosion rate at an excess shear stress of 2.18 Pa
Method: 1163
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.27 - Erosion rate at an excess shear stress of 2.27 Pa
Method: 1164
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.30 - Erosion rate at an excess shear stress of 2.3 Pa
Method: 1165
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.33 - Erosion rate at an excess shear stress of 2.33 Pa
Method: 1166
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.34 - Erosion rate at an excess shear stress of 2.34 Pa
Method: 1167
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.39 - Erosion rate at an excess shear stress of 2.39 Pa
Method: 1168
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.49 - Erosion rate at an excess shear stress of 2.49 Pa
Method: 1169
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.55 - Erosion rate at an excess shear stress of 2.55 Pa
Method: 1170
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.70 - Erosion rate at an excess shear stress of 2.7 Pa
Method: 1171
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.84 - Erosion rate at an excess shear stress of 2.84 Pa
Method: 1172
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.85 - Erosion rate at an excess shear stress of 2.85 Pa
Method: 1173
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.87 - Erosion rate at an excess shear stress of 2.87 Pa
Method: 1174
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.95 - Erosion rate at an excess shear stress of 2.95 Pa
Method: 1175
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.00 - Erosion rate at an excess shear stress of 3 Pa
Method: 1176
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.10 - Erosion rate at an excess shear stress of 3.1 Pa
Method: 1177
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.14 - Erosion rate at an excess shear stress of 3.14 Pa
Method: 1178
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.15 - Erosion rate at an excess shear stress of 3.15 Pa
Method: 1179
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.25 - Erosion rate at an excess shear stress of 3.25 Pa
Method: 1180
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.33 - Erosion rate at an excess shear stress of 3.33 Pa
Method: 1181
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.50 - Erosion rate at an excess shear stress of 3.5 Pa
Method: 1182
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.74 - Erosion rate at an excess shear stress of 3.74 Pa
Method: 1183
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.75 - Erosion rate at an excess shear stress of 3.75 Pa
Method: 1184
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.84 - Erosion rate at an excess shear stress of 3.84 Pa
Method: 1185
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET3.93 - Erosion rate at an excess shear stress of 3.93 Pa
Method: 1186
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET4.05 - Erosion rate at an excess shear stress of 4.05 Pa
Method: 1187
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET4.30 - Erosion rate at an excess shear stress of 4.3 Pa
Method: 1188
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET4.40 - Erosion rate at an excess shear stress of 4.4 Pa
Method: 1189
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET4.41 - Erosion rate at an excess shear stress of 4.41 Pa
Method: 1190
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET4.45 - Erosion rate at an excess shear stress of 4.45 Pa
Method: 1191
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET5.00 - Erosion rate at an excess shear stress of 5 Pa
Method: 1192
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET5.33 - Erosion rate at an excess shear stress of 5.33 Pa
Method: 1193
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET5.90 - Erosion rate at an excess shear stress of 5.9 Pa
Method: 1194
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET0.86 - Erosion rate at an excess shear stress of 0.86 Pa
Method: 1195
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: ERET2.82 - Erosion rate at an excess shear stress of 2.82 Pa
Method: 1196
Matrix: US - Unfractionated
Unit: g/cm² s Description: Determined with the SEDCIA System that consists of a laser which
projects 30 lines onto the sediment surface. To compute the loss of sediment volume over a certain period of time, snapshots of the projected lines are taken by a CCD-camera, installed at a fixed vertical and centred position above the sediment core. Subsequent snapshots are taken at given time intervals. The sediment surface is recalculated by a bilinear interpolation between the laser lines using a special computer program. The loss of sediment volume is obtained by calculating the volume difference of subsequent snapshots. Together with the density of the eroded material the sediment erosion rates can be calculated. (Witt and Westrich, 2003).
Analytical Lab: University of Stuttgart - Institute of Hydraulic Engineering - Laboratory Significant Nrs: 2
Sample Handling
Seqno: 152 Preservation: Cooled (max. 9 C) Pretreatment: None
Separation: None Procedure description:
Parameter: BDENS - Bulk density
Method: 1197
Matrix: US - Unfractionated
Unit: g/cm3 Description: Analysed using the GEOTEK Multi Sensor Core Logger (MSCL) of the
University of Amsterdam. The density (Cs137 with energies principally at 0.662 MeV) was measured on whole-round sections.
Analytical Lab: TNO, Bouw en Ondergrond (TNO) Significant Nrs:
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSVFSAND - Grain size volume fraction range > 63 and < 2000 micron (sand)
Method: 1198
Matrix: FS - Fractionated
Unit: % Description: Sediment particle-size analyses were performed on the subsamples
using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs: 2
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSVFSAND - Grain size volume fraction range > 63 and < 2000 micron (sand)
Method: 1198
Matrix: FS - Fractionated
Unit: % Description: Sediment particle-size analyses were performed on the subsamples
using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs: 2
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSVFCLAY - Grain size volume fraction < 63 micron (silt/clay)
Method: 1199
Matrix: FS - Fractionated
Unit: % Description: Sediment particle-size analyses were performed on the subsamples
using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs: 2
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSVFCLAY - Grain size volume fraction < 63 micron (silt/clay)
Method: 1199
Matrix: FS - Fractionated
Unit: % Description: Sediment particle-size analyses were performed on the subsamples
using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs: 2
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSMEA - Mean grain size
Method: 1200
Matrix: US - Unfractionated
Unit: µm Description: Sediment particle-size analyses were performed on the subsamples
using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs: 2
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSMEA - Mean grain size
Method: 1200
Matrix: US - Unfractionated
Unit: µm Description: Sediment particle-size analyses were performed on the subsamples
using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs: 2
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSSKEW - Grain size skewness
Method: 1201
Matrix: US - Unfractionated
Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on
the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs:
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSSKEW - Grain size skewness
Method: 1201
Matrix: US - Unfractionated
Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on
the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs:
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSSORT - Grain size sorting
Method: 1202
Matrix: FS - Fractionated
Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on
the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: UGent, Vakgroep biologie - Sectie Mariene Biologie (MARBIO) Significant Nrs:
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: GSSORT - Grain size sorting
Method: 1202
Matrix: FS - Fractionated
Unit: sc Description: Calculated value. Sediment particle-size analyses were performed on
the subsamples using a Malvern Lazer Particle sizer Mastersizer 2000 (Section Marine Biology, Ghent University). This device allows measurement of particle size distributions within the range of 0.02 - 2000 microns (depending on the material). The system uses the principle of laser diffractometry and the Mie scattering model to determine the volume percentage of particles in each of the grain size classes.
Analytical Lab: Ghent University, Marine Biology Section (MARBIO) Significant Nrs:
Sample Handling
Seqno: 153 Preservation: Kept at room temperature Pretreatment: None
Separation: None Procedure description: Samples were stored vertically.
Parameter: NTRZ - Nitrate + Nitrite (-N)
Method: 1203
Matrix: DI - Dissolved
Unit: µmol/l Description: Colorimetry.
Analytical Lab: VUB, Laboratorium voor Analytische en Milieuchemie (ANCH) Significant Nrs: 2
Sample Handling
Seqno: 39 Preservation: Kept in deep-freeze (-18 C) Pretreatment: None
Separation: PC filter (0.6 µm) Procedure description:
Parameter: NTRZ - Nitrate + Nitrite (-N)
Method: 1203
Matrix: DI - Dissolved
Unit: µmol/l Description: Colorimetry.
Analytical Lab: Vrije Universiteit Brussel, Laboratory of Analytical and Environmental Chemistry (ANCH)
Significant Nrs: 2 Sample Handling
Seqno: 39 Preservation: Kept in deep-freeze (-18 C) Pretreatment: None
Separation: PC filter (0.6 µm) Procedure description:
Parameter: DENSV - Density per unit of volume
Method: 1204
Matrix: NA - Not applicable
Unit: 10e3 coc/l Description: Inverted microscopy. Cell densities of colonial cells are counted.
Analytical Lab: Université Libre de Bruxelles, Ecology of Aquatic systems (ESA) Significant Nrs: 1
Sample Handling
Seqno: 110 Preservation: Cooled (4 C), dark Pretreatment: Lugol-Glutaraldehyde (1 % final concentration)
Separation: Unfiltered Procedure description: Concentration by Utermöhl method. The samples were analysed 1-3 months after sampling.
Parameter: DENSV - Density per unit of volume
Method: 1204
Matrix: NA - Not applicable
Unit: 10e3 coc/l Description: Inverted microscopy. Cell densities of colonial cells are counted.
Analytical Lab: ULB, Ecologie des Systèmes Aquatiques (ESA) Significant Nrs: 1
Sample Handling
Seqno: 110 Preservation: Cooled (4 C), dark Pretreatment: Lugol-Glutaraldehyde (1 % final concentration)
Separation: Unfiltered Procedure description: Concentration by Utermöhl method. The samples were analysed 1-3 months after sampling.