2008
DOI: 10.3133/sir20085050
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Hydrogeology, Chemical Characteristics, and Transport Processes in the Zone of Contribution of a Public-Supply Well in York, Nebraska

Abstract: The U.S. Geological Survey (USGS) is committed to providing the Nation with credible scientific information that helps to enhance and protect the overall quality of life and that facilitates effective management of water, biological, energy, and mineral resources (http://www.usgs.gov/). Information on the Nation's water resources is critical to ensuring long-term availability of water that is safe for drinking and recreation and is suitable for industry, irrigation, and fish and wildlife. Population growth and… Show more

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Cited by 21 publications
(14 citation statements)
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“…Multiple investigations have sought to characterize sources of contaminants to public-supply wells by studying observations of groundwater chemistry and age ( Aeschbach-Hertig et al 1998 ; Manning et al 2005 ; Katz et al 2007 ; Jurgens et al 2008 ; Landon et al 2008 ; McMahon et al 2008 ; Plummer et al 2008 ; Brown et al 2009 ; Hinkle et al 2009 ; Katz et al 2009 ; Landon et al 2010b ; Ayotte et al 2011 ; Musgrove et al 2011 ; Bexfield et al 2012 ; Eberts et al 2012 ); however, few studies appear to have used these observational data to explore whether seasonal variability in well operations can have important effects on water quality. Seasonal to multi-year variability has been described for public-supply wells in karst systems dominated by relatively young water (commonly less than about 50 years) ( Katz et al 2007 ; Musgrove et al 2011 ), where the quality of water from supply wells could be expected to respond to even short-term changes in hydrologic conditions.…”
Section: Introductionmentioning
confidence: 99%
“…Multiple investigations have sought to characterize sources of contaminants to public-supply wells by studying observations of groundwater chemistry and age ( Aeschbach-Hertig et al 1998 ; Manning et al 2005 ; Katz et al 2007 ; Jurgens et al 2008 ; Landon et al 2008 ; McMahon et al 2008 ; Plummer et al 2008 ; Brown et al 2009 ; Hinkle et al 2009 ; Katz et al 2009 ; Landon et al 2010b ; Ayotte et al 2011 ; Musgrove et al 2011 ; Bexfield et al 2012 ; Eberts et al 2012 ); however, few studies appear to have used these observational data to explore whether seasonal variability in well operations can have important effects on water quality. Seasonal to multi-year variability has been described for public-supply wells in karst systems dominated by relatively young water (commonly less than about 50 years) ( Katz et al 2007 ; Musgrove et al 2011 ), where the quality of water from supply wells could be expected to respond to even short-term changes in hydrologic conditions.…”
Section: Introductionmentioning
confidence: 99%
“…To demonstrate that simple models can be used to assess the potential impact of multi‐aquifer wells on confined‐aquifer PWS wells, we use a well‐studied example from York, Nebraska (Clark et al. , 2008; Landon et al. , 2008).…”
Section: Introductionmentioning
confidence: 99%
“…The higher number of pesticide detections in a developed area could originate from their use for weed control along rights-of-way in urban areas in the study area. Well SPRT-26 is a relatively high capacity supply well, and the land use inventory for the 500-m buffer area may not reflect land uses in the contributing area of this well, as has been shown for public-supply wells in other areas (Landon et al 2008). Agricultural land use in the 500-m buffer areas for the other five wells ranged from 31-75%.…”
Section: Geochemical Reactions Along Groundwater Flow Pathsmentioning
confidence: 96%
“…Well SPRT-26 is located in the east part of the study area in the outcrop area of the MCA where the aquifer is unconfined and this well is relatively shallow with a screened interval from 61 to 91 m. The relatively high pumping rate for this publicsupply well (about 3,800 L/min) likely induces the movement of groundwater from shallow zones into the screen. A similar pumping rate for a public supply well in the northern High Plains aquifer (an aquifer with similar lithology to the MCA) drew contaminants from shallow unconfined parts into the deeper confined parts of the aquifer (Landon et al 2008). Two other wells, SPRT-14 (domestic well) and SPRT-24 (public supply well) also are located in the east part of the study area where the MCA crops out (Fig.…”
Section: Geochemical Reactions Along Groundwater Flow Pathsmentioning
confidence: 98%