<?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>G. F. Huff</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>Ground-water-level, ground-water-withdrawal, and ground-&#13;
water-quality data were evaluated for trends. Holloman Air Force &#13;
Base is located in the west-central part of Otero County, New &#13;
Mexico. Ground-water-data analyses include assembly and &#13;
inspection of U.S. Geological Survey and Holloman Air Force Base &#13;
data, including ground-water-level data for public-supply and &#13;
observation wells and withdrawal and water-quality data for &#13;
public-supply wells in the area.&#13;
&#13;
     Well Douglas 4 shows a statistically significant decreasing &#13;
trend in water levels for 1972-86 and a statistically significant &#13;
increasing trend in water levels for 1986-90. Water levels in &#13;
wells San Andres 5 and San Andres 6 show statistically significant &#13;
decreasing trends for 1972-93 and 1981-89, respectively. A &#13;
mixture of statistically significant increasing trends, &#13;
statistically significant decreasing trends, and lack of &#13;
statistically significant trends over periods ranging from the &#13;
early 1970's to the early 1990's are indicated for the Boles wells &#13;
and wells near the Boles wells. Well Boles 5 shows a &#13;
statistically significant increasing trend in water levels for &#13;
1981-90. Well Boles 5 and well 17S.09E.25.343 show no &#13;
statistically significant trends in water levels for 1990-93 and &#13;
1988-93, respectively. For 1986-93, well Frenchy 1 shows a &#13;
statistically significant decreasing trend in water levels.&#13;
&#13;
     Ground-water withdrawal from the San Andres and Douglas wells &#13;
regularly exceeded estimated ground-water recharge from San &#13;
Andres Canyon for 1963-87. For 1951-57 and 1960-86, ground-water &#13;
withdrawal from the Boles wells regularly exceeded total &#13;
estimated ground-water recharge from Mule, Arrow, and Lead &#13;
Canyons. Ground-water withdrawal from the San Andres and Douglas &#13;
wells and from the Boles wells nearly equaled estimated ground-&#13;
water recharge for 1989-93 and 1986-93, respectively. For 1987-&#13;
93, ground-water withdrawal from the Escondido well regularly &#13;
exceeded estimated ground-water recharge from Escondido Canyon, &#13;
and ground-water withdrawal from the Frenchy wells regularly &#13;
exceeded total estimated ground-water recharge from Dog and &#13;
Deadman Canyons.&#13;
&#13;
     Water-quality samples were collected from selected Douglas, &#13;
San Andres, and Boles public-supply wells from December 1994 to &#13;
February 1995. Concentrations of dissolved nitrate show the most &#13;
consistent increases between current and historical data. Current &#13;
concentrations of dissolved nitrate are greater than historical &#13;
concentrations in 7 of 10 wells.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/wri964116</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey ;&#13;
Branch of Information Services [distributor],</dc:publisher>
  <dc:title>Analysis of ground-water data for selected wells near Holloman Air Force Base, New Mexico, 1950-95</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>