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The classic Mandel solution associated with the well-known Mandel–Cryer effect is re-examined. Using Biot theory of poroelasticity, the solution of the Mandel problem is extended to include material transverse isotropy, as well as the compressibility of the pore fluid and the solid constituents of the soil–rock skeleton.

Le résultat classique de Mandel, associé à l'effet bien comnnu de Mandel—Cryer, est réexamineé. En utilisant la théorie poro-é1astique de Blot, la solution du probléme de Mandel est étendue afin d'introduire l'anisotropie transverse du matériau, ainsi que la compressibilité des fluides présents dans les pores et celle des constituants solides du squelette du sol ou de la roche.

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