Skip to main content
Log in

Effects of body force on transient poroelastic consolidation due to groundwater pumping

  • Original Article
  • Published:
Environmental Geology

Abstract

By applying linear poro-elasticity theory, the body force effect on steady soil consolidation, i.e., settlement, caused by constant water table depression due to groundwater pumping was investigated. The result shows that when the soil is soft or thick, or both, neglecting the body force effect can lead to severe underestimation of soil displacement and incremental effective stress. However, the transient response of soil consolidation was not analyzed. In addition, the water table depression due to groundwater pumping in fact varies with time. In this study, the body force effect on transient consolidation of soil subjected to variable water table depression is further examined. A poroelastic consolidation numerical model is developed herein to conduct this examination.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9

Similar content being viewed by others

Abbreviations

B :

thickness of clay

C d :

the average degree of consolidation

f :

body force

f 0 :

initial steady value of body force

f e :

consolidation-producing incremental value of body force

g :

gravitational acceleration

G :

Lame constant

h :

water table depression

h**:

effective water table depression

K :

hydraulic conductivity

M :

body force number

n :

porosity

n 0 :

initial steady value of porosity

n e :

consolidation-producing incremental value of porosity

P :

pore water pressure

P 0 :

initial steady value of pore water pressure

P e :

consolidation-producing incremental value of pore water pressure

P e* :

nondimensionalized pore water pressure

q r :

Darcy’s velocity

q 0 r :

initial steady value of Darcy’s velocity

q e r :

consolidation-producing incremental value of Darcy’s velocity

S 1 :

the integration of transient pore water pressure with respect to z* at time t*

S 2 :

the integration of pore water pressure difference between the steady state and time t*

t :

time

t * :

nondimensionalized time

u :

displacement of solid

u z :

soil displacement in z direction

u * z :

nondimensionalized soil displacement

z :

co-ordinate

z * :

nondimensionalized coordinate

ρ w :

density of fluid

ρs :

density of solid

Δρ:

difference in density between solid and fluid

\(\sigma_{i,j}^{\prime}\) :

effective stress tensor

\({\sigma_{i,j}^{\prime}}^{0}\) :

initial steady value of effective stress tensor

\({\sigma_{i,j}^{\prime}}^{\rm e}\) :

consolidation-producing incremental value of effective stress tensor

λ:

Lame constant

Δt :

time step

Δt*:

nondimensionalized time step

Δz :

grid space

Δz*:

nondimensionalized grid space

References

  • Bear J, Corapcioglu MY (1981) Mathematical model for regional land subsidence due to pumping. 2. Integrated aquifer subsidence equations for vertical and horizontal displacements. Water Resour Res 17(3):947–958

    Article  Google Scholar 

  • Biot MA (1941) General theory of three-dimensional consolidation. J Appl Phys 12(2):155–164

    Article  Google Scholar 

  • Corapcioglu MA, Bear J (1983) A mathematical model for regional land subsidence due to pumping. 3. Integrated equations for a phreatic aquifer. Water Resour Res 19(4):895–908

    Article  Google Scholar 

  • Das BM (1990) Principles of geotechnical engineering. PWS-KENT, Boston

    Google Scholar 

  • Fallou SN, Mei CC, Lee CK (1992) Subsidence due to pumping from layered soil—a perturbation theory. Int J Numer Anal Meth Geomech 16(2):157–187

    Article  Google Scholar 

  • Gambolati G, Freeze RA (1973) Mathematical simulation of the subsidence of Venice 1 theory. Water Resour Res 9(3):721–732

    Article  Google Scholar 

  • Gambolati G, Ricceri G, Bertoni W, Brighenti G, Vuillermin E (1991) Mathematical simulation of the subsidence of ravenna. Water Resour Res 27(9):2899–2918

    Article  Google Scholar 

  • Gibson RE, England GL, Hussey MJL (1967) The theory of one-dimensional consolidation of saturated clays. I. Finite non-linear consolidation of thick homogeneous layers. Geotechnique 17(1):1–273

    Article  Google Scholar 

  • Gibson RE, Schiffman RL, Cargill KW (1981) The theory of one-dimensional consolidation of saturated clays. II. Finite non-linear consolidation of thick homogeneous layers. Can Geotech J 18(3):280–293

    Article  Google Scholar 

  • Gutierrez MS, Lewis RW (2002) Coupling fluid flow and deformation in underground formations. J Eng Mech 128(5):779–787

    Article  Google Scholar 

  • Helm DC (1975) One-dimensional simulation of aquifer system compaction near Pixley, California. 1. Constant parameters. Water Resour Res 11(3):465–477

    Article  Google Scholar 

  • Helm DC (1987) Three-dimensional consolidation theory in terms of the velocity of soil. Geotechnique 37(2):369–392

    Google Scholar 

  • Lambe TW, Whitman RV (1979) Soil mechanics. Wiley, New York

    Google Scholar 

  • Larson KJ, Basagaoglu H, Marino MA (2001) Prediction of optimal safe ground water yield and land subsidence in Los Banos-Kettlenman City area, California, using a calibrated numerical simulation model. J Hydrol 242(1):79–102

    Article  Google Scholar 

  • Lewis RW, Schrefler B (1978) A fully coupled consolidation model of the subsidence of Venice. Water Resour Res 14(2):223–229

    Article  Google Scholar 

  • Mei CC (1985) Gravity effects in consolidation of layer of soft soil. J Eng Mech 111(8):1038–1047

    Article  Google Scholar 

  • Ng CO, Mei CC (1995) Ground subsidence of finite amplitude due to pumping and surface loading. Water Resour Res 31(8):1953–1968

    Article  Google Scholar 

  • Onta PR, Gupta AD (1995) Regional management modeling of a complex groundwater system for land subsidence control. Water Resour Manag 9(1):1–25

    Article  Google Scholar 

  • Terzaghi K (1954) Theoretical soil mechanics. Wiley, New York

    Google Scholar 

  • Thomas LH (1949) Elliptic problems in linear difference equations over a network. Waston Scientific Computing Laboratory, Columbia

    Google Scholar 

  • Tsai TL, Chang KC, Huang LH (2006) Body force effect on consolidation of porous elastic media due to pumping. J Chin Inst Eng 29(1):75–82

    Google Scholar 

  • Verrujit A (1969) Elastic storage of aquifers. Flow through porous media, Academic, Dublin, pp 331–376

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Tung-Lin Tsai.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Tseng, CM., Tsai, TL. & Huang, LH. Effects of body force on transient poroelastic consolidation due to groundwater pumping. Environ Geol 54, 1507–1516 (2008). https://doi.org/10.1007/s00254-007-0932-2

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00254-007-0932-2

Keywords

Navigation