THE RELATIONSHIP BETWEEN SOLUTIONS OF FLOW PROBLEMS IN ISOTROPIC AND ANISOTROPIC SOILS

摘要: Abstract Problems of flow through a given region nonisotropic porous medium may be solved by means an equivalent isotropic obtained from the appropriate scale change. The derivation these scales is based on similarity between equations describing in both systems. Several special cases single liquid and two liquids under confined phreatic conditions are considered. derived this way most useful model investigations.