Pay and Download

Mathematics

FINITE DIFFERENCE APPROXIMATIONS OF CONFINED AQUIFER FLOW EQUATIONS

Manyonge Alfred Wanyama & Bitok Jacob K. and Nyambane Haron

Manyonge Alfred Wanyama & Bitok Jacob K. and Nyambane Haron

In general, groundwater flow in porous media on microscopic level is three dimensional (3-D). However, when considering regional problems.

$70

6 Pages