Chromium deposition pressured by degree of saturation were monitored applying deterministic modelling techniques, the study express the rate of saturation effect on the migration process of chromium, the developed model were subjected to simulations, the results express various rate of chromium concentration under the influences of various degree of saturation in silty and clay formation, the behaviour of water penetration into soil and its volume content has been describes by experts in various dimensions under the deposition of water content base on several factors, the mechanic of soil has express degree of saturation to affect the rate of chromium concentration when water has filled up the void ratio of the soil, the degree of saturation is one of the formation characteristics which also includes porosity and permeability, these variables also influences where found as determinant of the migration concentration between silty and clay formation in the study area. Gradual and rapid processes of chromium concentration were as a result of these factors deposited in the study as it expressed from the simulation values. Experts will definitely apply these concepts in monitoring this contaminant in such deposited formations.
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