Show simple item record

contributor authorH. M. Selim
date accessioned2017-05-08T20:46:56Z
date available2017-05-08T20:46:56Z
date copyrightAugust 1988
date issued1988
identifier other%28asce%290733-9437%281988%29114%3A3%28442%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/26982
description abstractAn analytical solution is derived for a two‐dimensional soil with a sloping surface under steady and water‐saturated flow conditions. The soil was assumed to consist of several layers, each horizontally stratified. The lower layer was assumed to extend to a great depth. Each layer was considered anisotropic in nature where the hydraulic conductivity in the vertical (κ) and the horizontal (ξ) directions are dissimilar. Potential and stream functions are obtained and several flow nets are presented for two‐layered soils with varying degrees of anisotropy. The range of values chosen was
publisherAmerican Society of Civil Engineers
titleWater Flow in Layered Soils With Sloping Surface
typeJournal Paper
journal volume114
journal issue3
journal titleJournal of Irrigation and Drainage Engineering
identifier doi10.1061/(ASCE)0733-9437(1988)114:3(442)
treeJournal of Irrigation and Drainage Engineering:;1988:;Volume ( 114 ):;issue: 003
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record