Abstract

A finite element model was developed in order to solve for both regional groundwater flow and conservative solute transport in porous medium. The model was applied to a 55-sq-km groundwater basin in the Ruehen region of Germany using a network of 1450 elements and 780 nodes. This model was used in simulating a contaminant plume done through injection. Similarly, the model was applied to a 4750-sq-km portion in the eastern Nile Delta aquifer in Egypt. The model was applied to this portion of the delta using a network of 543 elements and 310 nodes with the main objective of simulating the problem of salt water intrusion.

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