The solution of the Zhukovskii problem of the flow around a sheet pile is g
iven using the principles of two-dimensional steady-state seepage in the ca
se when, accompanying the motion of the seeping water, there is a layer of
saline ground waters at a certain depth under the sheet pile and this layer
is located above an impermeable thickness of rock salt. The mixed boundary
-value problem of the theory of analytic functions which arises is solved u
sing Polubarinova-Kochina's method, which is based on the application of th
e analytical theory of linear differential equations and, also, the method,
developed by us, of the conformal mappings of circular polygons in polar m
eshes, which are extremely typical for the velocity hodograph domains of su
ch flows. While reflecting the specific details and individual properties o
f such flows, the solution constructed below turns out to be expressed in c
losed form in terms of elementary functions and, consequently, it is the si
mplest and most convenient solution. In addition, it is the most general so
lution for the class of problems being considered. The well known results Z
hukovskii, Vedernikov and others are obtained from it as special and limiti
ng cases. A detailed hydrodynamic analysis and the specific features of the
seepage process being considered, as well as the effects of all the physic
al parameters of the model on the pattern of the phenomenon, are presented
using this solution and by numerical calculations. (C) 1999 Elsevier Scienc
e Ltd. All rights reserved.