Determination of the Diffusion Coefficient for Sands for the Prediction of Enhanced Scour on Beaches - PowerPoint PPT Presentation

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Determination of the Diffusion Coefficient for Sands for the Prediction of Enhanced Scour on Beaches

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Title: Determination of the Diffusion Coefficient for Sands for the Prediction of Enhanced Scour on Beaches


1
Determination of the Diffusion Coefficient for
Sands for the Prediction of Enhanced Scour on
Beaches due to Tsunamis
  • Eric Heller
  • University of Washington
  • Department of Civil Engineering

2
Introduction
  • Tonkin-de Vries (2001) performed scale model
    scour tests in wave tank
  • Traditional scour model uses only shear stress,
    scour not correctly predicted
  • Account for effective stresses in new model,
    scour more accurately predicted
  • Effective stresses controlled by rate of
    diffusion
  • Conclusion diffusion coefficient has effect in
    scour

3
Objectives
  • Determine Cv (diffusion coefficient) in sands
  • Develop procedure and apparatus for determination
    of Cv in sands
  • Find factors that influence Cv in sands
  • Validate values of Cv estimated by Tonkin-de
    Vries (2001)

4
Literature Review
  • Most research considers wave induced liquefaction
  • Cv an input parameter in several models
    (Zen Yamazaki, 1990b Nago Maeno, 1986
    Madsen, 1978 Okusa, 1985)
  • Cv determined by standard lab procedure
  • standard method assumed to be oedometer test

5
Field Conditions
  • Pressure increases under wave peak
  • Pressure decreases as wave passes
  • Applied (wave) pressure decreases faster than
    pressure in pores can dissipate
  • Pressure dissipation described by Cv

6
Scour Enhancement Parameter
  • Quantify effect of effective stresses in scour
  • L Scour enhancement parameter
  • r density of water
  • rsat saturated density of soil
  • DP Change in pore pressure
  • DT time for DP to occur
  • Cv diffusion coefficient

7
Diffusion Coefficient
  • Need to quantify Cv in sands for use in L
  • Natural phenomenon, occurs in many situations
  • Cv relates change in pressure over time with
    change in pressure over space
  • P pressure
  • t time
  • z vertical distance

8
Estimation of Cv
  • Current laboratory methods estimate av
  • related to Cv by
  • k and e can be accurately estimated in sands

9
Estimation of Cv
  • Current lab methods designed for clays
  • Oedometer
  • Isometric consolidation
  • Not suitable for sands
  • May be adapted for use in sands

10
Values of Cv
  • Few studies for Cv of Sands, mainly used for
    clays
  • SANDS (cm2 / s) CLAYS (cm2 / s )
  • 12 ( Zen Yamazaki, 1990b) 0.000018
    (Mitchell, 1992)
  • 80 (Tonkin Yeh 2002) 0.000115
    (Al-Dahir Tan, 1968)
  • 800 (Tonkin Yeh 2002) 0.00044
    (Sridharan et al, 1995)
  • 11520 (Zen Yamazaki, 1991) 0.505
    (Sridharan prakash, 2001)
  • Analytical methods estimate modulus ? av k e
    ? Cv

11
Finite Difference Estimation of Diffusion Equation
12
Test Apparatus
13
Test Apparatus
  • Pressure Control
  • Bottom Lower head pipe
  • Top Upper head pipe orifice
  • Pore Pressure Transducers
  • Pore pressures measured temporally spatially
  • Data Acquisition
  • Labtech

14
(No Transcript)
15
Transducer Probes
16
  • Photos by Eric Heller

17
  • Photo by Eric
    Heller
  • Photo by Brian Bennetts

18
Sample Preparation
  • 4 methods considered
  • Dry pluviation
  • Wet pluviation
  • Moist tamping
  • Slurry method (Kuebris Vaid, 1988)
  • Wet pluviation used
  • Ensure saturation
  • Model depositional environment

19
Test Procedure
  • Sediment sample
  • Attach cap assembly and lower head pipe
  • Equilibrate head pipes
  • Open valve and record data
  • Close valve when done

20
Analysis Methods
  • Data filtered
  • Data analyzed
  • Manual analysis
  • Point estimate analysis
  • Linear regression analysis
  • Quadratic

21
Raw Data
22
Filtered Data w/ Time Window
23
Manual analysis
  • Mean value

24
Point estimate analysis
  • Initial, average, and final values

25
Linear regression analysis
  • Initial, mean, and final values

26
Quadratic approximation analysis
  • Initial, average, and final values

27
Initial Cv vs. void ratio
28
Mean Cv vs. void ratio
29
Final Cv vs. void ratio
30
Trends
31
Results
  • gt100 values estimated

32
Comparison with other values
33
Estimate Scour Depth
  • Estimate DP DT
  • Estimate critical gradient g
  • Satisfy
  • Calculate G
  • Estimate z from plot
  • Estimate ds,

34
Estimate of Scour Depth
  • Drawdown velocity vs. depth of scour. g0.5.
    Cv800cm2/s for Tonkin-de Vries, Cv 812cm2/s
    for Heller1, and Cv 447cm2/s for Heller2.

35
Estimate Enhanced Scour
  • Estimate L,

36
Conclusions
  • The design of the testing apparatus has performed
    adequately
  • The test method seems to be suitable to determine
    the coefficient of diffusion, Cv
  • An experimental estimate of the diffusion
    coefficient, Cv, of 812cm2/s for a particular
    sand was obtained
  • The Cv for sand decreases with increasing void
    ratio
  • The values of Cv determined in this study
    correlate well with values determined by
    Tonkin-de Vries (2001)
  • Cv decreases as the head falls ending at a nearly
    constant value for all tests
  • The values of Cv are within one order of
    magnitude of other published values

37
Further Research
  • Investigate and ensure that void ratio is
    constant throughout sample.
  • The effect of the aspect ratio of the test cell
    must be investigated.
  • The effect of other soil properties besides void
    ratio on Cv must be investigated
  • The effect of different sizes of orifices should
    also be investigated
  • It is recommended that field research also be
    done
  • Use other methods to find Cv such as the modified
    permeability test proposed by Al-Dhahir Tan
    (1968)
  • Other models that use Cv to predict liquefaction
    besides Tonkin-de Vries (2001) and Tonkin et al
    (2002) should be considered.

38
  • Questions
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