| 600-acre, 174-lot Subdivision.
A hydrogeologic study utilizing conductivity, seismic, and
very
low frequency geophysical investigations characterized
fracture patterns and groundwater flow in a shale bedrock
aquifer. Monitoring wells indicated elevated nitrates in several
of the fracture systems. The contaminated fracture systems
were identified by the geophysical surveys. The geophysical
data identified another pattern of fractures that appeared
separate from the contaminated fractures. This integrated
interpretation of geological and geophysical data resulted
in three additional proposed drilling locations that were
tested. The second set of wells produced 20 to 100 gallons
per minute of uncontaminated water and resulted in development
approval.
50-acre, 15-lot Subdivision. Managed hydrogeologic
study that utilized geophysical investigations to locate bedrock
fractures and identify proposed well locations for a water
supply/on-lot disposal impact study. 3,500 feet of very low
frequency and seismic survey resulted in three proposed drilling
locations. These locations were drilled and encountered 25
to 120 gallon per minute flows with good water quality.
Residual Waste Landfill - Conducted the
geologic and hydrogeologic portions of the expansion permit
application for a 117-acre landfill. Directed and managed
all field investigations conducted for the permit application.
Groundwater investigation consisted of the installation, pump,
and permeability testing of numerous wells. Geophysical investigations
were conducted to high-grade well locations, and consisted
of 18,500 feet of VLF EM profiling, 14,100 feet of EM profiling,
6,000 feet of seismic refraction profiles and 600 feet of
resistivity profiles and soundings to locate water-bearing
fractures in the bedrock aquifer. Geophysical features indicating
potential fractures in the bedrock were tested by forty-one
(41) test wells, indicating a good correlation with geophysical
anomalies, and a poor correlation with aerial fracture traces.
Captive Landfill - Conducted a closure
investigation to determine the nature and extent of foundry
sand fill on the site and its potential on and off-site environmental
impact. During the groundwater assessment phase of this project,
geophysical
surveys and aerial photographs were used to locate a fracture
system in the bedrock for optimum monitoring well placement.
Monitoring wells encountered the fracture and produced 10
to 15 gallons per minute of groundwater. Well testing indicated
minor groundwater degradation of the type associated with
municipal waste. Review of historic aerial photographs showed
that an abandoned township landfill, adjacent to the subject
property, was the cause of groundwater contamination at the
site.
Based on this information, the economics of alternative
closure and beneficial use permits were determined and a state
approved closure plan was implemented.
Industrial Park - Conducted geophysical
surveys and test borings for the site evaluation of a 25-acre
property located in limestone terrain. Used geophysical surveys
to provide economical site coverage between boring locations.
Provided depth to bedrock map across the site and preliminary
engineering data for foundation design. Final report outlined
areas of high sinkhole and solution zone potential for planning
consideration.
Interstate Highway - Used aerial photographs,
conductivity, resistivity, and seismic methods to optimally
locate five groundwater-monitoring wells in an environmentally
sensitive area underlain by limestone bedrock. The impact
study delineated sensitive environmental areas, located areas
of particularly troublesome bedrock characteristics, and assisted
in establishing a groundwater monitoring network to provide
baseline data for on-going monitoring or environmental impact.
Groundwater Modeling- Constructed a groundwater
model covering a twelve (12) square mile area around the Buzby
Brothers Landfill as part of the site development requirements
for an adjacent residential development proposal. Shallow
groundwater required a subdrain system for the development
that had the potential to alter the geometry of the contaminant
plume associated with the aquifer. The model was calibrated
to match surrounding well data, nearby water bodies, and the
recharge/discharge budget for the basin. The hydrogeologic
model was relatively complex and included several geologic
formations and the affect of streams in the basin.

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