U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
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Geophysical Investigations of Heterogeneity and Scale at the
Princeton, Minnesota, ManagementSystems Evaluation Area
by
Jeffrey E. Lucius (U.S. Geological Survey; Denver, Colo.) and
Gary R. Olhoeft (U.S. Geological Survey; Denver, Colo.)
Abstract
The U.S. Geological Survey collected more than 1 gigabyte of ground penetrating
radar (GPR) data in 1991 at the Princeton, Minnesota, Management Systems
Evaluation Area (MSEA) to generate detailed images of the subsurface and
to determine the three-dimensional spatial variability of hydrogeologic
properties. The Princeton MSEA is located on the Anoka glacial outwash sand
plain northwest of Minneapolis-St. Paul. The GPR system transmitted electromagnetic
pulses that propagated through the ground. The pulses were partially reflected
back to the GPR antennas when they encountered changes in electrical properties
(which are controlled by water content, bulk density, lithology, and porosity).
The GPR data were computer processed to produce geometrically correct images
of the subsurface. Reflector continuity, amplitude, configuration, and spatial
frequency were analyzed in the GPR images to determine lithologic structure,
depositional processes, moisture content, stratification patterns, and grain-size
distributions. Changes in water-table capillary fringe thickness, areas
of possible focused recharge, areas consisting of eolian or other fine-grained
deposition, and undulations of the till surface were identified. The GPR
images were also correlated with lithology logs from sampling wells. For
agricultural sites with very little or no clay near the surface, ground
penetrating radar offers a fast, cost-effective, high-resolution method
for extending information acquired at test wells and for presenting a comprehensive
view of subsurface structure.
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