effect of subsurface barrier on seismic waves

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Effects Of Subsurface Barriers On Seismic Waves Group Members •Akshay M. Krishnan •Ashwitha Reddy •Haseeb Tahir •Rohith Grandhi •Sagar Shah Cee - 5464

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Effects Of Subsurface Barriers On Seismic Waves

Group Members• Akshay M.

Krishnan• Ashwitha Reddy• Haseeb Tahir• Rohith Grandhi• Sagar Shah

Cee - 5464

Overview• Objectives• Background• Experiment• Theoretical Model• Results• Errors• Conclusion

Objectives

Study effects of change in subsurface conditions on wave propagation.

Develop an experiment to compare different subsurface conditions

Prepare a STRATA model for theoretical modeling

Compare results

Background

Waves

Compressional Waves• Sound waves• Seismic Waves

Longitudinal waves• Light waves

Experiment

1. Only Sand Sand layer

7” thick

2. Sand with wood layer Sand layer 3” thick Wood 0.75” thick Sand layer 3” thick

• 2’x1’ box of ply wood• Subjected to ground motion by the shake table• Ground Motion: Sine wave

Amplitude= 5cm Frequency 2 Hz.

• Used 2 Accelerometers to measure the Accelerations

Theoretical Model

StrataFree Software

Shear Velocity Velocity that relates shear between layers of flow.

Unit WeightWeight of Material

Shear Velocity

Theoretical Model Contd.

Damping Inelastic Darendeli & Stokoe Model

Shear Modulus Inelastic Darendeli & Stokoe Model

0.00E+00 1.00E+00 2.00E+00 3.00E+00 4.00E+000

0.20.40.60.8

11.2

Darendeli & Stokoe G/Gmax Model

StrainG

/Gm

ax

0.00E+00 1.00E+00 2.00E+00 3.00E+00 4.00E+000

5

10

15

20

25

Darendeli & Stokoe damping Model

Strain

Dam

ping

, %

Results

0 1 2 3 4 5-0.8

-0.6

-0.4

-0.2

0

0.2

0.4

0.6

0.8

Sand-only : surface acc. (in "g") - actual vs strata

Actual StrataTime (sec)

Acce

lera

tion

(g)

Results Contd.

0 1 2 3 4 5-0.8

-0.6

-0.4

-0.2

0

0.2

0.4

0.6

0.8

Sand-Wood : surface acc. (in "g") - actual vs strata

Actual Strata

Time (sec)

Acce

lera

tion

(g)

Results Contd.

0 0.5 1 1.5 2 2.5 3 3.5 4 4.5 5-0.8

-0.6

-0.4

-0.2

0

0.2

0.4

0.6

0.8

Strata outputs : Sand-only vs. Sand-Wood

Sand-only : surface acc. (g) - output Strata Sand-Wood : surface acc. (g) - output Strata

Time (sec)

Acce

lera

tion

(g)

Errors Experiment was extremely scaled down Soil Properties depend on pressure

Centrifuges are used to conduct tests on soils The whole assembly acted as one rigid body Vibrations from the table movement affected the

readings Assumption of that waves will travel vertically

Conclusion