chung r song, ph.d., university of mississippi
DESCRIPTION
An Easy Method of Determining Hydraulic Conductivity of Soils using Pore Pressure Response of Piezocone Penetration Test. Chung R Song, Ph.D., University of Mississippi Sreekar Pulijala, Graduate Assistant, University of Mississippi. Overview. Hydraulic Conductivity and Piezocone - PowerPoint PPT PresentationTRANSCRIPT
An Easy Method of Determining Hydraulic Conductivity of Soils using Pore Pressure Response of Piezocone Penetration Test
Chung R Song, Ph.D., University of MississippiSreekar Pulijala, Graduate Assistant, University of
Mississippi
Overview
Hydraulic Conductivity and Piezocone Hydraulic Conductivity by Piezocone
Penetration Test Previous work Current results Conclusions
Hydraulic Conductivity
Describes the rate at which water can move through a permeable medium.
Why do we need to know hydraulic conductivity of the soil ??
However, the determination of hydraulic conductivity is time consuming and not easy.
Piezocone
Used for Site exploration Assessment of ground improvement Evaluation of contaminant transport
Measures Frictional resistance Pore Pressure End bearing
Hydraulic Conductivity by Piezocone Penetration Test
(PCPT)
Advance Piezocone to the desired depth and hold it for dissipation test.
Reliable values of Hydraulic Conductivity, compared to other field tests.
This is still time consuming and expensive (half day).
Pore pressure response for soil element during PCPT
Chung R. Song and George Z. Voyiadjis (2003)
“New Method”
To overcome the drawbacks of conventional dissipation test and provide a more realistic theoretical background.
Key idea : Pore Pressure response of saturated soils is not
only a function of stress-strain parameters but also of hydraulic conductivity.
Song.C.R and Voyiadjis.G.Z (2003) Pore pressure observed by clayey soils and
sandy soils. Clay : High PWP Sand : Low or Zero PWP
Relations between the dimensionless excess PWP during Piezocone Penetration and dimensionless Hydraulic Conductivity
Chung R. Song and George Z. Voyiadjis (2003)
Previous work
Correlates the magnitude of pore water pressure to the Hydraulic Conductivity directly.
Potential for real time process.
An axi- symmetric FE program that is capable of simulating behavior of soils with the advancement of the Piezocone tip was developed and used.
Uses the coupled theory of mixtures
Finite Element Mesh
Chung R. Song and George Z. Voyiadjis (2003)
Coupled equations
Voyiadjis and Abu-Farsakh (1997)
δ W
Stiffness matrix; Coupling matrix,
Flow matrx that incorporates the hydraulic conductivity
Incremental nodal displacement
W=Incremental excess PWP
n n n
tn n n
n n
n
U
t
U
; Flow vector,
Equilibrium force
n
n
Objective
Use of Song and Voyiadjis (2003)’s method (i.e. New method)
To perform numerical analyses for various soil conditions and provide simple design charts (monogram type) that an engineer can use without great difficulties.
Current stage
Setting up penetration depth and number of increments
By changing some material properties like κ, λ Permeability, M
Corresponding values of PWP are obtained for each varying properties when others are kept constant.
1.00E-11 1.00E-09 1.00E-07 1.00E-05 1.00E-03
k (m/sec)
PWP
(KPa
)
600
200
300
400
500
100
Permeability (k) vs. PWP
0.1,005.0,13.0 M
2.1,02.0,17.0 M
0
100
200
300
400
500
600
0.5 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3
M
PWP(
KPa
)
M vs. PWP
095.0,02.0,17.0 Ek
095.0,04.0,32.0 Ek
0
100
200
300
400
500
600
700
0 0.01 0.02 0.03 0.04 0.05 0.06 0.07 0.08 0.09
kappa
PW
P (
KPa)
vs. PWPκ
κ
095.0,24.0,2.1 EkM
0
100
200
300
400
500
600
0.15 0.2 0.25 0.3 0.35 0.4 0.45
Lambda
PW
P (
KPa)
λ vs. PWP
075.0,02.0,0.1 EkM
095.0,04.0,2.1 EkM
λ
Conclusions
The trend of PWP observed by the change of different parameters is reasonable.
Easy to use design charts : a handy tool to geotechnical engineers for the determination of hydraulic conductivity
Reduction in the computation time
Can be used in seepage analysis, soil classification, detection of underground aquifers, etc…
THANK YOU