Date of Award
Master of Science (MS)
Mathematics and Statistics
Joseph V. Koebbe
The purpose of this report is to investigate the behavior of a nonreactive contaminant in a perfectly stratified aquifer under uniform, steady-state flow. The design and the implementation of a solute transport model which characterizes the heterogeneities of the aquifer properties in a stochastic framework is reviewed. The model closely examines the advection and dispersion of the plume. The advection is the process by which the plume is transported in the aquifer by the bulk average motion of the groundwater whereas the dispersion refers to the spreading of the plume about its mean displacement position. The relationship between the fractally distributed hydraulic conductivity and the extent of spreading is the focus of investigation.
Oana, Joan Leilani, "Numerical Simulation of Saturated Flow with Fractal Analysis of the Hydraulic Conductivity Distribution" (1991). All Graduate Plan B and other Reports. 1295.
Copyright for this work is retained by the student. If you have any questions regarding the inclusion of this work in the Digital Commons, please email us at .