<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>L. J. Kauffman</dc:contributor>
  <dc:contributor>A. L. Baehr</dc:contributor>
  <dc:contributor>M. A. Ayers</dc:contributor>
  <dc:creator>Paul E. Stackelberg</dc:creator>
  <dc:date>2000</dc:date>
  <dc:description>The number and total concentration of&#13;
volatile organic compounds (VOCs) per&#13;
sample were significantly greater in water from&#13;
public-supply wells than in water from shallow&#13;
and moderate-depth monitoring wells in the&#13;
surficial Kirkwood-Cohansey aquifer system in&#13;
the Glassboro area of southern New Jersey. In&#13;
contrast, concentrations of nitrate (as nitrogen)&#13;
and the number and total concentration of&#13;
pesticides per sample were statistically similar&#13;
in samples from shallow and moderate-depth&#13;
monitoring wells and those from public-supply&#13;
wells.&#13;
VOCs in ground water typically are&#13;
derived from point sources, which commonly&#13;
exist in urban areas and which result in&#13;
spatially variable contaminant concentrations&#13;
near the water table. Because larger volumes of&#13;
water are withdrawn from public-supply wells&#13;
than from monitoring wells, their contributing&#13;
areas are larger and, therefore, they are more&#13;
likely to intercept water flowing from VOC&#13;
point sources. Additionally, public-supply&#13;
wells intercept flow paths that span a large&#13;
temporal interval. Public-supply wells in the&#13;
Glassboro study area withdraw water flowing&#13;
along short paths, which contains VOCs that&#13;
recently entered the aquifer system, and water&#13;
flowing along relatively long paths, which&#13;
contains VOCs that originated from the&#13;
degradation of parent compounds or that are&#13;
associated with past land uses. Because the&#13;
volume of water withdrawn from monitoring&#13;
wells is small and because shallow monitoring&#13;
wells are screened near the water table, they&#13;
generally intercept only relatively short flow&#13;
paths. Therefore, samples from these wells&#13;
represent relatively recent, discrete time&#13;
intervals and contain both fewer VOCs and a&#13;
lower total VOC concentration than samples&#13;
from public-supply wells.&#13;
Nitrate and pesticides in ground water&#13;
typically are derived from nonpoint sources,&#13;
which commonly are found in both agricultural&#13;
and urban areas and typically result in lowlevel,&#13;
relatively uniform concentrations near&#13;
the water table. Because nonpoint sources are&#13;
diffuse and because processes such as&#13;
degradation or sorption/dispersion do not occur&#13;
at rates sufficient to prevent detection of these&#13;
constituents in parts of the aquifer used for&#13;
domestic and public supply in the study area,&#13;
concentrations of nitrate and pesticides and&#13;
numbers of pesticide compounds are likely to&#13;
be similar in samples from shallow monitoring&#13;
wells and samples from public-supply wells.&#13;
Results of a comparison of (1) the general&#13;
characteristics of, and water-quality data from,&#13;
public-supply wells in the Glassboro study area&#13;
to available data from public-supply wells&#13;
screened in the Kirkwood-Cohansey aquifer&#13;
system outside the study area, and (2) land-use&#13;
settings, soil characteristics, and aquifer&#13;
properties in and outside the study area indicate&#13;
that the findings of this study likely are&#13;
applicable to the entire extent of the Kirkwood-&#13;
Cohansey aquifer system in southern New&#13;
Jersey.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/wri004123</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Comparison of nitrate, pesticides, and volatile organic compounds in samples from monitoring and public-supply wells, Kirkwood-Cohansey aquifer system, southern New Jersey</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>