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Hydrogeochemistry in regional aquifer systems supports agricultural water quality investigations in Iowa

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5815701
; ;  [1]
  1. Iowa State Univ., Ames, IA (United States). Dept. of Geological and Atmospheric Sciences

In this study, the authors demonstrate conjunctive use of traditional water quality data with environmental isotopes and geochemistry to determine whether present or future application of chemicals at the land surface will affect water quality in deep aquifers. The study area is located in central Iowa in the Walnut Creek Basin, one of three USDA-CSRS Management System Evaluation Area (MSEA) sites in Iowa. Pre-Illinoian gravel, Pennsylvanian sandstone, and Mississippian limestone comprise the major aquifers in this area and they are overlain by at least 50 m of late Wisconsin and Pre-Illinoian glacial sediments. Well depths, water levels, and aquifer units were identified by well construction logs followed by a house-to-house survey of residents. A subset of 125 total wells was sampled for major ions, trace metals, H-3, delta O-18, delta H-2, delta C-13, and C-14-DIC. Results suggest that contamination of deep aquifers from agricultural practices in the basin is unlikely. First, data from this study and the Till Hydrology Site to the northwest suggest that vertical groundwater velocities through the Pre-Illinoian till are too low for recent vertical recharge to reach the aquifers. Second, H-3 and corrected C-14 dates suggest that groundwater recharged both vertically and at outcrop is at least 13,000 years old and may be > 40,000 years old. Third, the groundwater in these aquifers is anaerobic and contains high Fe concentrations, SO[sub 4] concentrations < 1 mmol/L, CH[sub 4] gas, and delta C-13 DIC values between 0.0 and [minus]21.9 [per thousand]. The processes involved suggest a geochemical environment unfavorable for persistence of NO[sub 3]. In contrast, water samples from some wells suggest that some contamination may occur through poorly-constructed wells or deteriorating well casing.

OSTI ID:
5815701
Report Number(s):
CONF-921058--
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Journal Name: Geological Society of America, Abstracts with Programs; (United States) Vol. 24:7; ISSN GAAPBC; ISSN 0016-7592
Country of Publication:
United States
Language:
English

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