Technical Papers
Dec 1, 2023

Analysis on Large-Strain Nonlinear Consolidation of PVD-Improved Soft Soils with Non-Darcian Flow Considering Variable Well Resistance and Vacuum Pressure

Publication: International Journal of Geomechanics
Volume 24, Issue 2

Abstract

The deviation of water seepage from Darcy’s law has been verified in soft soils with high compressibility. Consolidation behaviors of prefabricated vertical drains (PVD)-improved soft soils caused by non-Darcian flow have been extensively studied, but most of them are based on small-strain consolidation theory, and it is generally assumed that the discharge capacity of vertical drains keeps constant during the process of consolidation. Considering the large-strain characteristic of the soft soils with high compressibility, the consolidation model of soft soils with non-Darcian flow is established in the Lagrange coordinate system. Meanwhile, considering the poor stages of drainages such as bending and silting caused by the deformation of soil layers, the discharge capacity of vertical drains in the proposed model is regarded as changing with time and depth. The feasibility of the solution is verified by comparing the proposed results with existing solutions, and consolidation behaviors under different conditions are investigated. The results show that the influence of non-Darcian flow cannot be ignored when the ratio of the influential zone radius to the radius of vertical drains reaches 15. The common surcharge loading applied to the PVD-improved soft soils has to consider the influence of consolidation results by non-Darcian flow. The difference of vacuum pressure distribution between Darcy’s flow and non-Darcian flow mainly exists in the middle and late period of consolidation. Finally, the proposed consolidation model is applied to the consolidation calculation of Brisbane Port, and the calculation results by the proposed model coincide with the field measurement.

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Data Availability Statement

Some or all data, models, or code generated or used during the study are available in a repository online in accordance with funder data retention policies.

Acknowledgments

This research is supported by the National Natural Science Foundation of China (Grant No. 51878320).

Notation

The following symbols are used in this paper:
a
vertical coordinate in Lagrangian coordinate system;
b
coefficient of the decrease of the PVD discharge capacity with time;
Cc
compressibility index;
Ckh
radial permeability index;
Ckv
vertical permeability index;
c
coefficient of the decrease of the PVD discharge capacity with depth;
e
void ratio;
e0
initial void ratio;
eref
reference void ratio;
H
initial thickness of soft soil layer;
i
hydraulic gradient;
i0
i1(m − 1)/i;
i1
critical hydraulic gradient value in Hansbo’s flow model;
ia
vertical hydraulic gradient;
ir
radial hydraulic gradient;
k
permeability coefficient;
kh
radial permeability coefficient of the undisturbed soil;
khref
reference value of kh;
kv
vertical permeability coefficient of the undisturbed soil;
kvref
reference value of kv;
kw
permeability coefficient of the PVD;
kw0
initial value of kw;
m
index of exponential function in Hansbo’s flow model;
n
drain spacing ratio;
p
vacuum pressure;
q
surcharge loading;
qa
discharge of vertical flow in Lagrangian coordinate;
qr
discharge of radial flow;
qξ
discharge of vertical flow in convective coordinate;
r
radial coordinate;
re
radius of the effect zone;
rs
radius of the smear zone;
rw
radius of the PVD;
S
settlement;
St
settlement at the top surface of soils at time t;
S
final settlement at the surface of soils;
t
time;
Up
average degree of consolidation defined by stress;
Ust
average degree of consolidation defined by strain;
us
excess pore-water pressure in soils;
u¯s
average value of us at depth a;
uw
excess pore-water pressure in the PVD;
V
volume of soil element;
vs
velocity of soil particles;
vw
velocity of the flow in the PVD;
vwa
velocity of flow in vertical direction;
vwr
velocity of flow in radial direction;
β
ratio of final discharge capacity to initial discharge capacity;
γsat
unit weight of saturated soils;
γw
unit weight of water;
κ
k/(mi1m1);
ξ
vertical coordinate in convective coordinate system;
ξ0
thickness of soil layers at time t in the convective coordinate;
σ
effective stress;
σ¯
average value of σ′ at depth a;
σ0
initial effective stress; and
σ¯ref
reference value of σ¯.

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 24Issue 2February 2024

History

Received: Jan 27, 2023
Accepted: Jul 16, 2023
Published online: Dec 1, 2023
Published in print: Feb 1, 2024
Discussion open until: May 1, 2024

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Dept. of Civil Engineering, Jiangsu Univ., Zhenjiang, Jiangsu 212013, P. R. China (corresponding author). ORCID: https://orcid.org/0000-0002-2811-5497. Email: [email protected]
Dept. of Civil Engineering, Jiangsu Univ., Zhenjiang, Jiangsu 212013, P. R. China. Email: [email protected]

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