<?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:creator>Roy C. Bartholomay</dc:creator>
  <dc:date>1998</dc:date>
  <dc:description>Radiochemical and chemical constituents in wastewater 
generated at facilities of the Idaho National Engineering 
and Environmental Laboratory (INEEL) (figure 1) have 
been discharged to waste-disposal ponds and wells since 
the early 1950 s. Public concern has been expressed that 
some of these constituents could migrate through the 
Snake River Plain aquifer to the Snake River in the Twin 
Falls-Hagerman area Because of these concerns the 
U.S. Department of Energy (DOE) requested that the U.S. 
Geological Survey (USGS) conduct three studies to gain a 
greater understanding of the chemical quality of water in 
the aquifer. One study described a one-time sampling 
effort for radionuclides, trace elements, and organic 
compounds in the eastern part of the A&amp;B Irrigation 
District in Minidoka County (Mann and Knobel, 1990). 
Another ongoing study involves sampling for tritium from 
19 springs on the north side of the Snake River in the 
Twin Falls-Hagerman area (Mann, 1989; Mann and Low, 
1994). A third study an ongoing annual sampling effort 
in the area between the southern boundary of the INEEL 
and Hagerman (figure 1) (hereafter referred to as the 
Magic Valley study area), is being conducted with the 
Idaho Department of Water Resources in cooperation with 
the DOE. Data for a variety of radiochemical and 
chemical constituents from this study have been published 
by Wegner and Campbell (1991); Bartholomay, Edwards, 
and Campbell (1992, 1993, 1994a, 1994b); and 
Bartholomay, Williams, and Campbell (1995, 1996, 
1997b). Data discussed in this fact sheet were taken from 
these reports. An evaluation of data collected during the 
first four years of this study (Bartholomay Williams, and 
Campbell, 1997a) showed no pattern of water-quality 
change for radionuclide data as concentrations randomly 
increased or decreased. The inorganic constituent data 
showed no statistical change between sample rounds.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/fs05298</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Effect of activities at the Idaho National Engineering and Environmental Laboratory on the water quality of the Snake River Plain aquifer in the Magic Valley study</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>