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5 - Radially Symmetric Thermo-Poroelasticity Problems for a Solid Cylinder

Published online by Cambridge University Press:  10 November 2016

A. P. S. Selvadurai
Affiliation:
McGill University, Montréal
A. P. Suvorov
Affiliation:
McGill University, Montréal
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Summary

Many standard mathematical techniques for solving partial differential equations in applied mathematics can be used to explain at least the simplest experimental results pertaining to geomechanics and to test the accuracy of the computational techniques used in poroelasticity. Thus, it is often possible to solve poroelasticity problems for geometries more complex than a one-dimensional column, examples of which can include a sphere, a cylinder or an ellipsoid. A limitation of the one-dimensional formulation also stems from the fact that manifestations of effects that are particular to poroelasticity cannot be observed unless a two- or three-dimensional formulation is used. Such an example is the Mandel–Cryer effect of amplification of the pore fluid pressure in a radially loaded sphere or a cylinder (Cryer, 1963; Mason et al., 1991; Detournay and Cheng, 1993), or in a poroelastic parallelepiped compressed between two rigid plates (Mandel, 1950; Abousleiman et al., 1996).

In this chapter, we examine the thermo-hydro-mechanical problem related to a poroelastic cylinder on the lateral surface of which a non-zero temperature change is prescribed while the fluid pressure and the radial stress are kept at zero. The end faces of the cylinder remain insulated for axial fluid flow and heat transfer. Thus, the fluid flow and heat transfer in such a cylinder occur only in the radial direction. The effect of the mechanical loading of this cylinder can also be considered – it can include, for example, applied axial strain/stress and radial stress applied to the lateral surface. Taking advantage of the linearity of the problem, for the sake of brevity, it is sufficient at first to prescribe zero values for the mechanical loading; for example, zero radial stress on the lateral surface and zero axial strain. It will be shown how the solution of the given thermo-hydro-mechanical problem, with specified non-zero temperature change on the boundary, can be reduced to a problem of prescribed uniform temperature change that does not vary over time. In turn, the last problem can be reduced to a hydro-mechanical problem of the applied radial stress and applied axial strain (or applied axial stress) if certain replacements in coefficients of the solution are performed.

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Publisher: Cambridge University Press
Print publication year: 2016

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References

Abousleiman, Y., Cheng, A.H.-D., Cui, L., Detournay, E. and Roegiers, J.-C. (1996) Mandel problem revisited, Géotechnique, 46, 187–195.Google Scholar
Belotserkovets, A. and Prevost, J.H. (2011) Thermo-poroelastic response of a fluid-saturated porous sphere: an analytical solution, International Journal of Engineering Science, 49, 1415–1423.Google Scholar
Carslaw, H.S. and Jaeger, J.C. (1959) Conduction of Heat in Solids. Oxford, UK: Oxford University Press.
Cryer, C.W. (1963) A comparison of the three-dimensional consolidation theories of Biot and Terzaghi, Quarterly Journal of Mechanics and Applied Mathematics, 16, 401–412.Google Scholar
Detournay, E. and Cheng, A.H.-D. (1993) Fundamentals of poroelasticity. In Comprehensive Rock Engineering, Vol. 2 (Ed. Hudson, J.). Oxford, UK: Pergamon Press, pp. 113–171.
Mandel, J. (1950) Etude mathematique de la consolidation des sols, Actes du Colloque International de Mécanique, Poitiers, 4, 9–19.Google Scholar
Mason, D.P., Solomon, A. and Nicolaysen, L.O. (1991) Evolution of stress and strain during the consolidation of a fluid-saturated porous elastic sphere, Journal of Applied Physics, 70, 4724–4740.Google Scholar
Selvadurai, A.P.S. (2000) Partial Differential Equations in Mechanics, Vol. 1, Fundamentals, Laplace's Equation, the Diffusion Equation, the Wave Equation. Berlin, Germany: Springer.
Selvadurai, A.P.S. and Shirazi, A. (2004) Mandel–Cryer effects in fluid inclusions in damage susceptible poroelastic media, Computers and Geotechnics, 37, 285–300.Google Scholar
Selvadurai, A.P.S. and Suvorov, A.P. (2012) Boundary heating of poroelastic and poro-elastoplastic spheres, Proceedings of the Royal Society, A, 468, 2779–2806.Google Scholar
Selvadurai, A.P.S. and Suvorov, A.P. (2014) Thermo-poromechanics of a fluid-filled cavity in a fluid-saturated porous geomaterial, Proceedings of the Royal Society, A, 470, 20130634.Google Scholar
Sneddon, I.N. (1950) Fourier Transforms. New York, NY: McGraw-Hill.
Sneddon, I.N. (1972) The Applications of Integral Transforms. New York, NY: McGraw-Hill.

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