Assessing the water quantities required for leaching salt-affected soi
l is an important task in a reclamation programme. In Iraq, evaluation
of leaching processes, in most reclamation projects, is achieved usin
g empirical equations or by carrying out simple laboratory tests which
can lead to error in estimating leaching requirements. In this study,
five well-known mathematical models, each with a different theoretica
l background, are chosen for evaluation against measured salt concentr
ations within four test sites located in four major reclamation projec
ts of different locations within the Mesopotamian Plain. The verificat
ion of the single reservoir model with bypass, the theoretical plate t
hickness scheme. the hydrodynamic convection-dispersion model and the
transfer function models used against field data revealed significant
agreement between the observed and predicted values of salinity during
the leaching process within a certain depth of soil below surface. Bu
t the model comprising a series of reservoirs provided a high degree o
f correlation with the observed salinity within the whole profile of s
oil. It was concluded that the selected mathematical models used for s
tudying the leaching process lead to good correlations between predict
ed and observed salinity values and these tend to improve with the inc
rease of leaching water amounts.