5 rock%2520mass%2520damage%2520assessment final
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Rock mass damage assessmentRock mass damage assessment
Methods and applicationsMethods and applications
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Rock Mass Damage
Engineering perspective:damage is any change in
a material property which degrades the materialsperformance. (Brown et al 1994)
Geotechnical perspective:fracturing ordiscontinuity generation, extension ordegradation, or any irreversible deformation
such as the shearing and opening ofdiscontinuities, which causes deterioration ofthe rock mass strength (Li 1993).
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Large basal fault
Jointing sub-parallel to fault plane
Zone of Rock Cracking
Zone of Joint Cracking
Zone of Rock Bridge
Potential Failure Plane
80% Charge, 20% Air
Presplit
Blast Damage AssessmentOpen pits
(Bye, 2006)
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Damage assessment - Underground
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Damage assessment methods recenttechnologies
Technology Quantity observed or measured
3D Digital image mapping Excavation profile; overbreak
Ground Penetrating Radar(GPR)
Depth of damage. Non-destructive method that uses electromagneticradiation in the microwave band (UHF/VHF frequencies) of the radio
spectrum, and detects the reflected signals from subsurface structuresGround Probe Radar Measure and monitor the stability of rock walls (sub mm accuracy)
3D digital photogrammetry(SiroVision)
High-precision 3D images used for the mapping and analysis of rockmass surfaces.
Crack monitors Measures crack displacementLaser Scanner Pre and post blast wall displacement (30 mm accuracy)
Downhole imaging Pre and post blast fracture mapping
Impulse response technique(CSM)
Depth of damage
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Slope Monitoring Techniques
Technology Precision WallCoverage
Update Rate Range Deployment Allweather
SSR
Laser
(Prisms)
Laser(Prismless)
Extenso-meters
GPS ~ 10s cm DiscretePoints
~ secs n/a Difficult Yes
Photogram-metry
~ 1s cm BroadArea
~ mins < 150 m Moderate No
0.2 mm BroadArea
~ mins 450 m(1 km)
Easy Yes
~ 1s cm Discrete
Points
Twice Daily < 2 km Difficult No
~ 10s cm BroadArea
~ secs < 200 m Moderate
~ 1s mm DiscretePoints
~ secs n/a
No
YesDifficult
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Direct methods - observations
Borehole surveys
Half barrels
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Downhole imaging
(courtesy Wellfield Services Limitada)
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Subsurface damage
A B
Section A-B
9.2 m
distance f rom damage tonearest fully coupled blasthole
damage inspectionboreholes (1m apart)
1 m
Chapter 11, LOP, 2007)
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Direct methods profile measurements
Reflectorless distance measurementsystems
Desired profile
Measured profile
Major structures
Photo: LeicaTMS Total Station
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Direct method of overbreak measurement in undergroundenvironments - cavity monitoring system (CMS)
Developed by Noranda and Optechsystem s Canada.
CMS
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Direct methods profile measurements with 3Ddigital imaging
Courtesy MD Robotics
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Indirect methods - seismic tomography
Electronic Detonators Vs Pyrotechnic (After Ichijo et al, 1994)
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Seismic monitoring relative reduction in Vp
ASP Blastronics, 2006
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GPR technology - Underground
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GPR technology Open pit
Codelco IM2, 2006
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Impulse response techniquePetr, 2005
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Ground Probe Radar
(Bye, 2006)
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RIEGL Laser Scanner
(Bye, 2006)
3D di it l h t t
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3D digital photogrammetrySiroVision
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Other instrumentation - crack monitors
Addressing blasting complaints
Eight month history of displacement andcrack displacement showing greatest change
width to correlate with the most intense andlongest drop in humidity in April
Dowding and Siebert, 2000
D A t f Vib ti
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Damage Assessment from VibrationMonitoring
Uphole Geophone Schematic
Triaxial Geophone
PVC Pipe
Grout Bleeding Hose
Grout Pumping hose
Plug
Vertical
Geophone
Radial
Geophone
Transverse
Geophone
Data
Cable
Example of commercial data
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Example of commercial dataacquisition systems
Instantel
Texcel
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Terminology on vibrations
Peak particle velocity (PPV)refers to the peak
vibration velocity measured in a given transducer (e.g.radial, transverse or vertical)
Attenuationrefers to the diminishing of intensity of a
wave front as it progresses through a media
Vector sumis the resultant of the magnitude to thethree orthogonal components coincident with time
Peak vector sumis the resultant of the peakmagnitude of each orthogonal component not
coincident with time
Types of wave motion Body
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Types of wave motion Bodywaves
Compressional wave (P-wave). The particle motion is
parallel to the direction of the wave propagation
Propagationdirection
Particlemotion
Types of wave motion Body
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Types of wave motion Bodywaves
Shear waves (s-waves) the particles generally move
transversely to the direction of the wave propagation
Particlemotion
Propagationdirection
Types of wave motion surface
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Types of wave motion surfacewaves
At interfaces (Ground and air,
ground and joints) differenttype of surface waves aredeveloped. The most
important is the Rayleighwave (R-wave)
Particlemotion
Propagationdirection
Indirect methods Near field peak
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Indirect methods Near field peakparticle velocity (PPV) monitoring
Station 1
Leading TunnelLagging Tunnel
Observation Holes
(diamond drilled)
0.5-0.8m from geophone
holes
Geophone hole A
Geophone hole B
Plan View
Vibration measurements Equipment
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Vibration measurements Equipmentrequirements
Fit for use sensors
Good and consistent coupling
Data capturing and reporting
Monitoring system with auto-trigger level capabilities
Adequate calibration
Ideally, the monitoring system should be self reliant, thatis have long life battery or permanent power
Damage assessment - PPV
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Damage assessment PPVbased monitoring
Damage assessment - PPV
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Damage assessment PPVbased monitoring
Damage assessment - PPV based
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Damage assessment PPV basedmonitoring
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Best practice is to use a combination of directand indirect methods to infer damage
Combination of borehole surveys with vibrationsExtensometers with seismics
O di i i
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Open discussion session
Local experience on rock mass damage assessment
Use of PPV based criteria Can it be used for structurally controlled damage ?
Single versus a range of values
PPV relation to strain
Intact rock versus rock mass
Quantifying the impact of damage Surface stability
Rock reinforcement and support Mechanisms of damage (gas versus stress induced)