Abstract
It is sshown that the stresses and the pore pressure in porous elastic media through which a liquid is diffusing can be expressed in terms of two displacement functions. These functions are particularly useful in problems relating to a semi-infinite body or infinite layer when the stresses or displacements are prescribed on the surface. Problems of plane or axially symmetric strain are closely related when expressed in terms of these functions and the introduction of suitable repeated transforms (Fourier or Hankel followed by a Laplace transform) permits a parallel development of solutions for these two types of strain.

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