<?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>C. L. Thomas</dc:contributor>
  <dc:creator>Cynthia G. Abeyta</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>The Chromic Acid Pit site is an inactive waste disposal site &#13;
that is regulated by the Resource Conservation and Recovery Act of &#13;
1976. The 2.2-cubic-yard cement-lined pit was operated from 1980 &#13;
to 1983 by a contractor to the U.S. Army Air Defense Artillery &#13;
Center and Fort Bliss. The pit, located on the Fort Bliss military &#13;
reservation, in El Paso, Texas, was used for disposal and &#13;
evaporation of chromic acid waste generated from chrome plating &#13;
operations. The site was certified closed in 1989 and the Texas &#13;
Natural Resources Conservation Commission issued Permit Number &#13;
HW-50296 (U.S. Environmental Protection Agency Permit Number &#13;
TX4213720101), which approved and implemented post-closure care &#13;
for the Chromic Acid Pit site. In accordance with an approved &#13;
post-closure plan, the U.S. Geological Survey is cooperating with &#13;
the U.S. Army in evaluating hydrogeologic conditions and ground-&#13;
water quality at the site. One upgradient and two downgradient &#13;
ground-water monitoring wells were installed adjacent to the &#13;
chromic acid pit by a private contractor. Quarterly ground-water &#13;
sampling of these wells by the U.S. Geological Survey began in &#13;
December 1993.&#13;
&#13;
     The Chromic Acid Pit site is situated in the Hueco Bolson &#13;
intermontane valley. The Hueco Bolson is a primary source of &#13;
ground water in the El Paso area. City of El Paso and U.S. Army &#13;
water-supply wells are located on all sides of the study area and &#13;
are completed 600 to more than 1,200 feet below land surface. The &#13;
ground-water level in the area of the Chromic Acid Pit site has &#13;
declined about 25 feet from 1982 to 1993. Depth to water at the &#13;
Chromic Acid Pit site in September 1994 was about 284 feet below &#13;
land surface; ground-water flow is to the southeast.&#13;
&#13;
     Ground-water samples collected from monitoring wells at the &#13;
Chromic Acid Pit site contained dissolved-solids concentrations &#13;
of 442 to 564 milligrams per liter. Nitrate as nitrogen &#13;
concentrations ranged from 2.1 to 2.7 milligrams per liter; &#13;
nitrite plus nitrate as nitrogen concentrations ranged from 2.3 &#13;
to 3.0 milligrams per liter. Nitrate concentrations are &#13;
abnormally high in the Old Mesa well field located about 5,000 &#13;
feet southwest of the Chromic Acid Pit site. Volatile and &#13;
semivolatile organic compounds in water samples were analyzed for &#13;
the first sampling round; no confirmed volatile or semivolatile &#13;
organic compounds were detected above the laboratory reporting &#13;
limits. Total chromium concentrations ranged from 0.0099 to 0.092 &#13;
milligram per liter; dissolved chromium concentrations ranged &#13;
from 0.0068 to 0.0094 milligram per liter. Overall, water-quality &#13;
characteristics in water from the chromic acid pit ground-water &#13;
monitoring wells are similar to those in the surrounding area. &#13;
Detected chemical concentrations in water from the chromic acid &#13;
pit monitoring wells during the four sampling periods were below &#13;
U.S. Environmental Protection Agency-established maximum &#13;
contaminant levels for public drinking water supplies.&#13;
&#13;
     Statistical analyses were performed on 39 of the chemical &#13;
constituents analyzed for in ground water from the chromic acid &#13;
pit monitoring wells. Concentrations of chloride and fluoride &#13;
were significantly less in water from the downgradient wells than &#13;
in water from the upgradient well, whereas concentrations of &#13;
nitrate as nitrogen, nitrite plus nitrate as nitrogen, and &#13;
dissolved solids were significantly greater in water from the &#13;
downgradient wells than in water from the upgradient well. &#13;
Concentrations of nitrate as nitrogen were significantly &#13;
different in water from the two downgradient wells. Differences &#13;
detected through statistical analysis of chemical constituents of &#13;
water in the chromic acid pit monitoring wells did not appear to &#13;
indicate a release of hazardous chemicals from the chromic acid &#13;
pit. There was no indication of ground-water contamination in &#13;
either downgradient well.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/wri964035</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Hydrogeology and ground-water quality of the chromic acid pit site, U.S. Army Air Defense Artillery Center and Fort Bliss, El Paso, Texas</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>