Document Type
Thesis
Degree
Master of Science (MS)
Major/Program
Geosciences
First Advisor's Name
David Genereux
First Advisor's Committee Title
Committee Chair
Second Advisor's Name
Grenville Draper
Third Advisor's Name
James Saiers
Date of Defense
7-11-1996
Abstract
Hydrogeologic variables controlling groundwater exchange with inflow and flow-through lakes were simulated using a three-dimensional numerical model (MODFLOW) to investigate and quantify spatial patterns of lake bed seepage and hydraulic head distributions in the porous medium surrounding the lakes. Also, the total annual inflow and outflow were calculated as a percentage of lake volume for flow-through lake simulations. The general exponential decline of seepage rates with distance offshore was best demonstrated at lower anisotropy ratio (i.e., Kh/Kv = 1, 10), with increasing deviation from the exponential pattern as anisotropy was increased to 100 and 1000. 2-D vertical section models constructed for comparison with 3-D models showed that groundwater heads and seepages were higher in 3-D simulations. Addition of low conductivity lake sediments decreased seepage rates nearshore and increased seepage rates offshore in inflow lakes, and increased the area of groundwater inseepage on the beds of flow-through lakes. Introduction of heterogeneity into the medium decreased the water table and seepage rates
nearshore, and increased seepage rates offshore in inflow lakes. A laterally restricted aquifer located at the downgradient side of the flow-through lake increased the area of outseepage. Recharge rate, lake depth and lake bed slope had relatively little effect on the spatial patterns of seepage rates and groundwater exchange with lakes.
Identifier
FI14050421
Recommended Citation
Bandopadhyay, Indranil, "Investigation of spatial patterns of ground-water exchange with lakes, using a three-dimensional numerical model" (1996). FIU Electronic Theses and Dissertations. 1384.
https://digitalcommons.fiu.edu/etd/1384
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