Respectively, Hydrologist, U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 413, Reston, Virginia 20192; Hydrologist, U.S. Geological Survey, P.O. Box 25046, MS 415, Denver, Colorado 80225; and Contractor, Project Resources Inc., 6820 North Broadway Unit I, Denver, Colorado 80221 (E-Mail/Apodaca: lapodaca@usgs.gov).
WATER QUALITY IN SHALLOW ALLUVIAL AQUIFERS, UPPER COLORADO RIVER BASIN, COLORADO, 1997†
Article first published online: 8 JUN 2007
DOI: 10.1111/j.1752-1688.2002.tb01541.x
Issue
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JAWRA Journal of the American Water Resources Association
Volume 38, Issue 1, pages 133–149, February 2002
Additional Information
How to Cite
Apodaca, L. E., Bails, J. B. and Smith, C. M. (2002), WATER QUALITY IN SHALLOW ALLUVIAL AQUIFERS, UPPER COLORADO RIVER BASIN, COLORADO, 1997. JAWRA Journal of the American Water Resources Association, 38: 133–149. doi: 10.1111/j.1752-1688.2002.tb01541.x
- †
Paper No. 00094 of the Journal of the American Water Resources Association.Discussions are open until October 1, 2002.
- ‡
Respectively, Hydrologist, U.S. Geological Survey, 12201 Sunrise Valley Drive, MS 413, Reston, Virginia 20192; Hydrologist, U.S. Geological Survey, P.O. Box 25046, MS 415, Denver, Colorado 80225; and Contractor, Project Resources Inc., 6820 North Broadway Unit I, Denver, Colorado 80221 (E-Mail/Apodaca: lapodaca@usgs.gov).
Publication History
- Issue published online: 8 JUN 2007
- Article first published online: 8 JUN 2007
- Abstract
- References
- Cited By
Keywords:
- water quality;
- ground water;
- land use;
- Upper Colorado River Basin;
- Colorado
ABSTRACT: Shallow ground water in areas of increasing urban development within the Upper Colorado River Basin was sampled for inorganic and organic constituents to characterize water-quality conditions and to identify potential anthropogenic effects resulting from development. In 1997, 25 shallow monitoring wells were installed and sampled in five areas of urban development in Eagle, Grand, Gunnison, and Summit Counties, Colorado. The results of this study indicate that the shallow ground water in the study area is suitable for most uses. Nonparametric statistical methods showed that constituents and parameters measured in the shallow wells were often significantly different between the five developing urban areas. Radon concentrations exceeded the proposed USEPA maximum contaminant level at all sites. The presence of nutrients, pesticides, and volatile organic compounds indicate anthropogenic activities are affecting the shallow ground-water quality in the study area. Nitrate as N concentrations greater than 2.0 mg/L were observed in ground water recharged between the 1980s and 1990s. Low concentrations of methylene blue active substances were detected at a few sites. Total coliform bacteria were detected at ten sites; however, E. coli was not detected. Continued monitoring is needed to assess the effects of increasing urban development on the shallow ground-water quality in the study area.

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