Abstract
In this chapter, we present the constitutive equations of the Biot model. The main difficulties of this model are the coupling of the equations and the application of the superposition principle. We present the general solution of the coupled problem resulting from the Biot model. This solution is based on a new method for decoupling the equations. This decoupling approach permits to derive a superposition principle of the loadings. Several types of loadings and boundary conditions for the water pressure and the displacement field are discussed. Analytical solutions are also derived and discussed.
Also, the problem of the computation of the different causes and their relative contribution to the total subsidence and/or settlement is analyzed in terms of two main principles of the partial differential equations, as follows:
-
the coupling/decoupling of the system of equations; and
-
the principle of superposition of loadings.
For soft clays and/or loose sand, the ratio between the maximum vertical displacements using the coupled model may be 170 times larger than the maximum vertical displacement computed with the decoupled model.
Also, for large values of the shear modulus and a standard value of the Young modulus (gravel sand), the consolidation ratio of the coupled solution and the decoupled solution are similar. This ratio deceases rapidly with the radial distance to the pumping well. However, for small values of the shear modulus, the consolidation ratio is decreasing slowly with the radial distance to the pumping well.
Eliyahu Wakshal (Deceased)
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Bear J (1972) Dynamics of fluids in porous media. Dover, New York
Belotserkovets A, Prevost JH (2011) Thermoporoelastic response of a fluid-saturated porous sphere: an analytical solution. Int J Eng Sci 49:1415–1423
Biot MA (1941) General theory of three-dimensional consolidation. J Appl Phys 12:155–164
Biot MA (1955) Theory of elasticity and consolidation for a porous anisotropic solid. J Appl Phys 26:182–185
Booker JR, Carter JP (1986a) Analysis of a point sink embedded in a porous elastic half space. Int J Numer Anal Method Geomech 10:137–150
Booker JR, Carter JP (1987a) Elastic consolidation around a point sink embedded in a half-space with anisotropic permeability. Int J Numer Anal Method Geomech 11:61–77
Booker JR, Carter JP (1986b) Long term subsidence due to fluid extraction from a saturated, anisotropic, elastic soil mass. Q J Mech Appl Math 39:85–98
Booker JR, Carter JP (1987b) Withdrawal of a compressible pore fluid from a point sink in an isotropic elastic half space with anisotropic permeability. Int J Solids Struct 23:369–385
Carslaw HS, Jaeger JC (1959) Conduction of heat in solids, 2nd edn. Oxford University Press, London
Castelletto N, Ferronato M. Gambolati G, Janna C, Teatini P (2010a) Thermo-poro-elastic effects in the anthropogenic uplift of Venice by deep seawater injection. In: Proceedings of the EISOLS 2010, Queretaro, Mexico, 17–22 Oct 2010. IAHS Publication 339
Castelletto N, Ferronato M, Gambolati G, Teatini P (2010b) An analytical solution of plane-strain consolidation due to a point sink within a fluid-saturated porous elastic media. In: Proceedings of the EISOLS 2010, Queretaro, Mexico, 17–22 Oct 2010. IAHS Publication 339
Chen GJ (2002) Analysis of pumping in multilayered and poroelastic half space. Comput Geotech 30:1–26
Chen GJ (2005) Steady-state solutions of multilayered and cross-anisotropic poroelastic half-space due to a point sink. Int J Geomech 5:45–57
Cours de mecanique des sols (1980) – enseignement specialise – Ecole des Ponts et Chaussees – Les fondations
Detournay E, Cheng AH-D (1993) Fundamentals of poroelasticity, Chapter 5. In: Fairhurst C (ed) Comprehensive rock engineering: principle, practice and projects, vol II, Analysis and design method. Pergamon Press, Oxford, pp 113–171
Ferronato M, Pini G, Gambolati G (2009) The role of preconditioning in the solution to FE coupled consolidation equations by Krylov subspace methods. Int J Numer Anal Method Geomech 33:405–423
Geertsma J (1973) Land subsidence above compacting oil and gas reservoirs. J Petrol Technol 25:734–744
Gui YF, Dou WB (2007) A rigorous and completed statement on Helmhotz theorem. In: Progress in electromagnetics research, PIER 69, pp 287–307
Gui YF, Li P (2011) On the uniqueness theorem of time-harmonic electromagnetic fields. J Electromagn Anal Appl 3:13–21
Harbaugh AW (2005) MODFLOW-2005, the US Geological Survey modular ground-water model – the ground-water flow process techniques and methods 6-A16. US Geological Survey, Reston
Harbaugh AW, Banta ER, Hill MC, McDonald MG (2000) MODFLOW-2000, the US Geological Survey modular ground-water model – user guide to modularization concepts and the ground-water flow process. US Geological Survey Open-File-Report 00–92
Hsieh PA (1996) Deformation-induced changes in hydraulic head during ground-water withdrawal. Ground Water 34:1082–1089
Jian-Fei Lu F, Sheng-Leng D (2006) A semi-analytical solution of a circular tunnel surrounded by a poroelastic medium and subjected to a moving load. Research report no R857. University of Civil Engineering- Sydney NSW 2006 Australia
Kaynia AM, Banerjee P (1993) Fundamental solutions of Biot’s equations of dynamic poroelasticity. Int J Eng Sci 31:817–830
Lu J C-C, Lin F-T (2005) Analysis of transient ground surface displacements due to a point sink in a porous elastic half-space. In: Proceedings of the 10th conference of Advanced Technology Council in Mathematics, Cheong-Ju, Korea, 12–16 December, pp 135–144
Lu J C-C, Lin F-T (2006) The transient ground surface displacements due to a point sink/heat source in an elastic half-space. In: ASCE, Proceedings of GeoShanghai international conference, Shanghai, China, Geotechnical special publication no. 148, pp 210–218
Lu J C-C, Lin F-T (2007) Analysis of the transient ground surface displacements subject to a point sink in a poroelastic half space. Chung Hua J Sci Eng 5(1):77–86
Magnan J-P (2001) Cours de mécanique des sols et des roches. Ecole Nationale des Ponts et Chaussées, 2 vols
Mandel AH, Zeitoun DG, Dagan G (2003) Salinity sources of Kfar Uria wells in the Judea group aquifer of Israel. Quantitative identification model. J Hydol 270:39–48
Morse PM, Feshbach H (1953) Methods of theoretical physics, vol II. Mc Graw Hill Company, New York
Poland JF, Davis GH (1969) Land subsidence due to withdrawal of fluids. In Varnes DJ, Kiersch G (eds) Reviews in engineering geology II. Geological Society of America Inc., Boulder
Poland GF (1976) Land subsidence stopped by artesian- head recovery- San Joaquim Valley. In: Proceedings of the second international symposium land subsidence held at Anaheim, California, December 1976
Poulos HG, Davis EH (1974) Elastic solutions for soil and rock mechanics. John Wiley & sons Inc., New York
Phienwej N, Giao PH, Nutalaya P (2006) Land subsidence in Bangkok, Thailand. Eng Geol 82:187–201
Shan C, Falta RW, Javandel I (1992) Analytical solutions for steady state gas flow to a soil vapor extraction well. Water Resour Res 28:1105–1120
Slough KJ, Sudicky EA, Forsyth PA (1999) Numerical simulation of multiphase flow and phase partitioning in discretely fractured geologic media. J Contam Hydrol 40(2):107–136
Sneddon IN (1951) Fourier transforms. McGraw-Hill, New York, pp 48–70
Tarn J-Q, Lu C-C (1991) Analysis of subsidence due to a point sink in an anisotropic porous elastic half space. Int J Numer Anal Method Geomech 15:573–592
Vardoulakis I (2009) Lecture notes on Cosserat continuum mechanics with application to the mechanics of granular media. N.T.U. Athens, Greece, P.O. box 144, Paiania Gr-19002, http://geolab.mechan.ntua.gr/
Wang HF (2000) Theory of linear poroelasticity. Princeton University press, Princeton
Wilson AM, Gorelick S (1996) The effects of pulsed pumping on land subsidence in the Santa Clara valley, California. J Hydrol 174:375–396
Zhang C, Guo H (2006) Time-space coupled predicting model of land subsidence caused by groundwater exploitation based on stochastic medium theory. International conference on safety science and technology, Shanghai
Zhang H, Baray DA, Hocking GC (1999) Analysis of continuous and pulsed pumping of a phreatic aquifer. Adv Water Res 22:623–632
Zhou XL (2006) On uniqueness theorem of a vector function. In: Progress in Electromagnetics research, PIER 65, pp 93–102
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 2013 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Zeitoun, D.G., Wakshal, E. (2013). Biot’s Theory of Consolidation. In: Land Subsidence Analysis in Urban Areas. Springer Environmental Science and Engineering. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-5506-2_5
Download citation
DOI: https://doi.org/10.1007/978-94-007-5506-2_5
Published:
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-007-5505-5
Online ISBN: 978-94-007-5506-2
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)