This books presents one and two dimensional analytical solutions for
solute transport in homogeneous porous formations. The constant and time
dependent forms of input concentration are considered to predict the
contaminant concentration distribution along or against unsteady
groundwater flow in semi-infinite and finite aquifers. An exponentially
decreasing unsteady velocity distribution is considered. The sinusoidal
form of time dependent velocity distribution is also considered which
represents seasonal variation in year in tropical regions. The direct
relationship between dispersion coefficient and seepage velocity concept
is used in which dispersion coefficient is directly proportional to the
seepage velocity. When the groundwater table rises and falls, the
velocity of flow in the aquifer may be transient or unsteady which is
considered here. The Laplace Transform Technique (LTT) and the Hankel
Transform Technique (HTT) are used to derive analytical solutions which
would be useful to benchmark numerical codes and solutions.