421506088550001 BOONE COUNTY, IL, LOCAL NUMBER 44N3E-32.7G1
LOCATION.--
Lat 42°15'06", long 88°54'59", in SE1/4NW1/4NW1/4 sec. 32 T.44N., R.3E,
Hydrologic Unit 07090006, about 3 miles west of Belvidere. Owner: U.S.
Environmental Protection Agency.
AQUIFER.--
Glacial drift of the Quaternary age.
WELL CHARACTERISTICS.--
Diameter 2.0 inches, depth 22.6 feet, cased to 17.6 feet, slotted screen,
drilled, observation.
PERIOD OF RECORD.--
GROUND-WATER QUALITY:
September 2001.
REMARKS FOR CURRENT YEAR.--
During 1990-2000, the U.S. Geological Survey (USGS), in cooperation with the
U.S. Environmental Protection Agency, conducted a study of hydrogeology and water quality
in the aquifers underlying Belvidere, Ill. and vicinity (Mills and others, 1998; Mills and
others, 1999; Mills and others, 1999; Mills and others, in press). For this study, water-quality
samples were collected from about 100 private water-supply wells, 8 public water-supply
wells, and 25 monitoring wells. All samples were analyzed for volatile organic
compounds; samples were analyzed selectively for major ions, trace elements, tritium and other
radionuclides, and semi-volatile organic compounds. Details regarding well location/construction,
sampling methodology and analytical results are given in the reports referenced
above. During May 2000, a monitoring well open to the water table in the glacial drift aquifer
was installed about 1.5 miles west of Belvidere. This well is intended to provide long-term
(years and decades) water-level and water-quality data from the vicinity of the Troy Bedrock
Valley--an area that is expected to undergo future changes in land and increased usage as a
ground-water source. Analytical results from the initial sampling of the well in September
2001 are given below.
Water samples were collected using field-parameter stabilization and volumetric purge
criteria to ensure samples were representative of the aquifer water quality. Samples for
analysis of inorganic constituents were filtered through a 0.45 micron acetate filter.
Samples collected for analysis of herbicides and their transformation products were filtered
through a 0.7 micron backed glass-fiber filter. All samples were chilled immediately to
4 degrees Centigrade for handling and shipment. Laboratories received the samples within
1-4 days of sample collection. Inorganic samples were analyzed by the USGS National Water-Quality
Laboratory in Lakewood, Col. using automated colorimetric procedures described by
Fishman and Friedman (1989). Analyses for herbicides and their transformation products were
made at the USGS Organic Geochemistry Research Laboratory in Lawrence, Kans. Using solid-phase
extraction techniques, parent herbicides, the atrazine products deethylatrazine and deisopropylatrazine,
and the cyanazine product cyanazine-amide were analyzed by gas chromatography/mass
spectrometry (GC/MS)(Zimmerman and Thurman, 1999; Kish and others, 2000). Chloroacetanilide
herbicide products (ethanesulfonic (ESA) and oxanilic acid (OXA) compounds) were analyzed by liquid
chromatography/mass spectrometry (LC/MS) (Zimmerman and others, 2000; Lee and others, 2001).
Glyphosate was analyzed by immunoassay using a proprietary method (Elizabeth Scribner,
U.S. Geological Survey, oral communications, 2001).