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<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>Robert B. Fendick Jr.</dc:contributor>
  <dc:contributor>Lane B. Simmons</dc:contributor>
  <dc:creator>Roland W. Tollett</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description>In 2000-2001, water-quality data were collected from 60 randomly selected domestic wells in the 

Acadian-Pontchartrain Study Unit, as part of the National Water-Quality Assessment Program.  The 

data were collected from wells screened in shallow sands (less than 350 feet below land surface) 

in two major aquifer systems--the Chicot aquifer system in southwestern Louisiana and the Chicot 

equivalent aquifer system in southeastern Louisiana and southwestern Mississippi.  The Chicot 

equivalent aquifer system is part of the Southern Hills regional aquifer system, and both the 

Chicot aquifer system and the Southern Hills regional aquifer systems are designated as 

sole-source aquifers by the U.S. Environmental Protection Agency (USEPA).

The well depths ranged from 40 to 340 feet below land surface with a median depth of 120 feet.  

The ground-water-quality data included 5 physiochemical properties, dissolved solids, 9 major 

inorganic ions, 24 trace elements, 6 nutrients, dissolved organic carbon, 109 pesticides and 

degradation products, and 85 volatile organic compounds (VOC's); and a subset of the wells were 

sampled for radon, chlorofluorocarbons, and stable isotopes.

Water from 35 of the 60 domestic wells sampled had pH values less than the USEPA Seconday 

Maximum Contaminant Level (SMCL) range of 6.5 to 8.5 standard units.  Specific conductance 

ranged from 17 to 1,420 microsiemens per centimeter at 25 degrees Celsius.  Dissolved-solids 

concentrations in water from two wells exceeded the SMCL of 500 mg/L (milligrams per liter); the 

maximum concentration was 858 mg/L.  Sodium and calcium were the dominant cations, and 

bicarbonate and chloride were the dominant anions.  One chloride concentration (264 mg/L) 

exceeded the SMCL of 250 mg/L.  One arsenic concentration (55.3 micrograms per liter) exceeded 

the USEPA Maximum Contaminant Level (MCL) of 10 micrograms per liter.  Iron concentrations in 

water from 22 wells exceeded the SMCL of 300 micrograms per liter; the maximum concentration was 

8,670 micrograms per liter.  Manganese concentrations in water from 26 wells exceeded the SMCL 

of 50 micrograms per liter; the maximum concentration was 481 micrograms per liter.  Health 

Advisories have been established for six of the trace elements analyzed; no concentrations were 

greater than these nonenforceable standards.  Radon concentrations in water from 9 of 50 wells 

sampled were greater thanthe proposed USEPA MCL of 300 picocuries per liter.

Concentrations of ammonia, ammonia plus organic nitrogen, and nitrite plus nitrate in water from 

four wells were greater than 2 mg/L, a level that might indicate anthropogenic influences.  The 

median dissolved organic carbon concentration was an estimated 0.30 mg/L, which indicated 

naturally occurring dissolved organic carbon conditions in the study area.  Eight pesticides and 

two degradation products were detected in water from five wells.  Twenty-four VOC's were 

detected in water from 44 wells.  All concentrations of pesticides and VOC's were less than 

USEPA drinking-water standards.

Quality-control samples, which included field-blank samples, replicates, and field and 

laboratory spikes, indicated no bias in ground-water data from collection procedures or 

analyses.  VAriance between the environmental sampls and he corresponding replicate samples was 

typically less than 5 percent, indicating and acceptable degree of laboratory precision and data 

collection reproducibility.

The Mann-Whitney rank-sum test was used to compare depth to top of screen and selected physicochemical properties and chemical constituents between six groups of wells.  Values for selected physicochemical and chemical constituents were typically greater in wells located in the Chicot aquifer system than in the Chicot equivalent aquifer system.  Values for specific conductance, pH, calcium, sodium, bicarbonate, chloride, dis</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/wri034122</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Quality of water in domestic wells in the Chicot and Chicot equivalent aquifer systems, southern Louisiana and southwestern Mississippi, 2000-2001</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>