Abstract
Seepage under a flat apron in a two-layer ground consisting of homogeneous isotropic layers of equal thickness was investigated by means of the analytic theory of linear differential equations by Polubarinova-Kochina [1]. An approximate solution of the same problem for layers of different thickness by the methods of the variational calculus was given in [2]. The solution to such a problem for homogeneous anisotropic layers of different thickness by means of a special complex variable representation and linear conjugation was given in [3] by Prusov and the author of the present paper. The method of [3] is now used to investigate two-dimensional steady seepage flow under two aprons in a multilayer ground consisting of n homogeneous anisotropic layers of different thickness, the principal directions of anistropy of each layer having an arbitrary position relative to the horizontal.
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