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Research about Anoka Sand Plain aquifer

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Effects of agricultural and residential land use on ground-water quality, Anoka Sand Plain Aquifer, east-central Minnesota

Water quality in the 1,700-square-mile Anoka Sand Plain aquifer is affected by irrigated and nonirrigated agriculture and by residential land use. Concentrations of sulfate, chloride, nitrite plus nitrate nitrogen, and pesticides in ground water are related to human activities; nitrite plus nitrate nitrogen concentrations are affected more than concentrations of other chemical constituents. Of the water samples collected from 100 wells during this study, samples from 30 wells had concentrations of nitrite plus nitrate nitrogen greater than 10 mg/L (milligrams per liter), which is the limit recommended for drinking water by the Minnesota Pollution Control Agency. Analysis of 360 water samples indicated that the median concentrations of nitrite plus nitrate nitrogen for undeveloped, nonirrigated-cultivated, irrigated, and residential lands were 0.22,2.0,5.3, and 4.2 mg/L, respectively. Differences in nitrite plus nitrate nitrogen concentrations at various depths below the water table were statistically significant. Median concentrations of nitrite plus nitrate nitrogen in groundwater samples less than 10 feet, 10 to 20 feet, and more than 20 feet below the water table were 5.1 mg/L, 2.7 mg/L, and less than 0.1 mg/L, respectively. Seasonal fluctuations in nitrite plus nitrate nitrogen concentrations at many wells were as great or greater than long-term change; however, the springtime median concentration of nitrite plus nitrate nitrogen increased steadily from 1984 (4.8 mg/L) through 1987 (5.5 mg/L). Triazine herbicides were detected in 11 of 18 samples analyzed for pesticides. Concentrations of atrazine were less than the 3 (J-g/L maximum contaminant level set for atrazine by the Minnesota Department of Health and by the U.S. Environmental Protection Agency.

Minnesota

Geology and water-supply potential of the Anoka Sand Plain aquifer, Minnesota

Intensified land development on the Anoka sand plain necessitates a better understanding of the hydrogeology of the surficial outwash deposits of the area. The Anoka sand-plain aquifer consists of outwash attributable to two different ice lobes. Predominant grain size of the upper outwash decreases and sorting coefficient increases from west to east. Till or lake deposits underlie most of the surficial outwash. In some areas, these deposits are absent and the aquifer is directly underlain by bedrock, mainly sandstone. Preliminary study indicates that parts of the aquifer may yield several hundred to more than 1,000 gallons of water per minute to properly developed large-diameter wells. Storage in the aquifer is estimated to be 2,000 billion gallons and annual withdrawals approaching 250 billion gallons may be sustained. More detailed analysis is essential for proper management and optimum use of the resource.

Minnesota