Technical Papers
Oct 4, 2023

Large-Strain Radial Consolidation Analysis Incorporating Soil Smear and Well Resistance Effect

Publication: International Journal of Geomechanics
Volume 23, Issue 12

Abstract

A mathematical model was developed to investigate the consolidation behavior of soft soil deposits improved by prefabricated vertical drains. The smear effect caused by drain installation was incorporated into the model by assuming a parabolic variation of permeability and compressibility with radius. The non-Darcian flow of pore water in the soil and the well resistance effect caused by the limited discharge capacity of drain were also incorporated in the model. The void ratio dependence of permeability and compressibility was taken into consideration to account for their variation with time. The proposed model was validated by comparing the predicted results with experimental data and with existing analytical models. A parametric study was performed to evaluate the influence of various parameters such as non-Darcian flow, permeability ratio, and discharge capacity on the consolidation of the soil deposit. The average effective stress decreased by approximately 20% when the ratio of permeability in the undisturbed zone to the smear zone was increased from 1.5 to 5. The average excess pore-water pressure at the soil–drain interface reduced by approximately 80% when the discharge capacity was increased from 20 to 100 m3/year. The well resistance effect was more significant for non-Darcian flow as compared to Darcian flow. The rate of dissipation of average excess pore-water pressure increased by approximately 75% when the non-Darcian parameter n was increased from 1 to 2. However, the average excess pore-water pressure became independent of the non-Darcian parameter (n) for n greater than 2.5.

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Data Availability Statement

All data, models, and code that support the findings of this study are available from the corresponding author upon reasonable request.

Notation

The following symbols are used in this paper:
A
total area of the influence zone of the drain;
As
area of smear zone;
Au
area of undisturbed zone;
a
Lagrangian coordinate;
ac
compressibility ratio;
b
function of r;
bs
ratio of area of smear zone to the total area of influence zone;
Cc
compression index;
Chi
initial coefficient of radial consolidation;
Ck
permeability index;
Cr
recompression index;
EPWP
excess pore-water pressure;
e
average void ratio at any time t and depth z;
e0
average initial void ratio at any depth z;
FDM
finite difference method;
f(r)
function of radial distance r;
fj
value of function f(r) at the jth node of radial distance;
g(r)
function of radial distance r;
gj
value of function g(r) at the jth node of radial distance;
ih
hydraulic gradient in the horizontal direction;
k~
permeability at any time t and depth z for non-Darcian flow;
k~¯
average permeability at any time t and depth z;
k~¯0
average initial permeability at any depth z;
k~0
initial permeability at any depth z for non-Darcian flow;
k~h
permeability soil in horizontal direction for non-Darcian flow;
k~hs
horizontal permeability in smear zone at a radial distance r from the center of the drain;
k~s
horizontal permeability in smear zone at the soil–drain interface under non-Darcian flow;
k~u
horizontal permeability in the undisturbed zone under non-Darcian flow;
k~u0
initial horizontal permeability in the undisturbed zone under non-Darcian flow;
L
initial height of the soil deposit;
mvs
volume compressibility in the smear zone at the soil–drain interface;
mvu
volume compressibility in the undisturbed zone;
mvu0
initial volume compressibility in the undisturbed zone;
μ
ratio of constant B to A;
N
constant, function of re, rw, qw, and θ;
n
non-Darcian parameter;
Q
surcharge load on the soil deposit;
Qin(t)
total flow entering the drain from the surrounding soil at any time t;
qw
discharge capacity of the drain;
q¯
total stress at any time t and depth z in the soil sample;
r
radial distance measured from the center of the drain;
re
radius of influence zone measured from the center of the drain;
rj
radial distance of the jth node from the center of the drain;
rs
radius of smear zone measured from the center of the drain;
rw
equivalent radius of the vertical drain;
S
ratio of radius of smear zone to the radius of drain;
S(t)
settlement of soil deposit at any time t;
Sf
final settlement of the soil deposit;
Thu
time factor;
U¯p
average degree of consolidation at any time t based on EPWP dissipation;
U¯s
average degree of consolidation at any time t based on settlement of the soil deposit;
u
EPWP at a radial distance r;
usj
EPWP in the smear zone at the jth node of the radial distance;
usj+1
EPWP in the smear zone at the (j + 1)th node of the radial distance;
uuj
EPWP in the undisturbed zone at the jth node of the radial distance;
uuj+1
EPWP in the undisturbed zone at the (j + 1)th node of the radial distance;
ui,j
EPWP corresponding to the ith node of the radial distance grid and the jth node of the time grid;
ui+1,j
EPWP corresponding to the (i + 1)th node of the radial distance grid and the jth node of the time grid;
us
EPWP in the smear zone at any radial distance r and time t;
uu
EPWP in the undisturbed zone at any radial distance r and time t;
u¯rj
average EPWP at the jth node of the time grid;
u¯rj+1
average EPWP at the (j + 1)th node of the time grid;
u¯rj1
average EPWP at the (j − 1)th node of the time grid;
u¯r
radial average of EPWP over the entire influence zone at any depth z and time t;
u¯s
average EPWP in the smear zone;
u¯u
average EPWP in the undisturbed zone;
u¯w
average EPWP at the soil–drain interface in the smear zone;
vr(r)
radial flow velocity at any radial distance r from the center of the drain and time t;
xj
function of fj, gj, and β(t);
Yi
function of fi and gi;
β(t)
function of time;
Δr
small interval of radial distance;
Δt
small interval of time;
φ
constant obtained while determining the radial average of EPWP;
γw
unit weight of water;
κ
permeability ratio;
λ
constant, function of the compressibility ratio;
θ
constant, function of λ and bs;
σ¯
radial average of effective stress over the entire influence zone at any time t and depth z;
σ0¯
radial average initial effective stress over the entire influence zone at any depth z;
σp¯
average preconsolidation pressure for the entire influence zone;
σps¯
average preconsolidation pressure for the smear zone;
σpu¯
average preconsolidation pressure for the undisturbed zone;
σs¯
average effective stress in the smear zone;
σs0¯
initial average effective stress in the smear zone;
σu¯
average effective stress in the undisturbed zone;
σu0¯
initial average effective stress in the undisturbed zone;
ω
constant;
ξ
convective coordinate;
ξ0(t)
height of the sample at any time t in the convective coordinate;
ζ
constant, function of mvu, k~u, and θ; and
ζ0
constant, a function of mvu0, k~u0, and θ.

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International Journal of Geomechanics
Volume 23Issue 12December 2023

History

Received: Oct 15, 2022
Accepted: Jun 26, 2023
Published online: Oct 4, 2023
Published in print: Dec 1, 2023
Discussion open until: Mar 4, 2024

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Dept. of Civil Engineering, National Institute of Technology Rourkela, Rourkela, Orissa 769008, India. ORCID: https://orcid.org/0009-0005-9176-3058. Email: [email protected]
Assistant Professor, Dept. of Civil Engineering, Indian Institute of Technology Roorkee, Roorkee, Uttarakhand 247667, India (corresponding author). ORCID: https://orcid.org/0000-0003-0739-6610. Email: [email protected]

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ASCE Library Cards let you download journal articles, proceedings papers, and available book chapters across the entire ASCE Library platform. ASCE Library Cards remain active for 24 months or until all downloads are used. Note: This content will be debited as one download at time of checkout.

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Save for later Information on ASCE Library Cards
ASCE Library Cards let you download journal articles, proceedings papers, and available book chapters across the entire ASCE Library platform. ASCE Library Cards remain active for 24 months or until all downloads are used. Note: This content will be debited as one download at time of checkout.

Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
ASCE Library Card (5 downloads)
$105.00
Add to cart
ASCE Library Card (20 downloads)
$280.00
Add to cart
Buy Single Article
$35.00
Add to cart

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