<?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>Richard P. Hooper</dc:contributor>
  <dc:contributor>Thomas G. Huntington</dc:contributor>
  <dc:contributor>Brent T. Aulenback</dc:contributor>
  <dc:creator>Norman E. Peters</dc:creator>
  <dc:date>2000</dc:date>
  <dc:description>&lt;p&gt;The Panola Mountain Research Watershed (PMRW) is a 41-hectare forested&amp;nbsp;watershed in the southern Piedmont physiographic province near Atlanta,&amp;nbsp;Georgia. The watershed contains a naturally regenerated second-growth&amp;nbsp;forest on abandoned agricultural land, typical of the Piedmont. Research at&amp;nbsp;PMRW has focused on how streamflow is generated, and in particular, on how&amp;nbsp;water and solutes move from hillslopes to the stream. The research shows&amp;nbsp;that streamflow and solute concentrations of precipitation, throughfall, soil&amp;nbsp;water and streamwater change rapidly during rainstorms. Furthermore,&amp;nbsp;these variations are strongly associated with the soil-moisture conditions,&amp;nbsp;the soil type and thickness, and the rainfall intensity, all of which effect&amp;nbsp;the chemical interactions and mixing of water traveling along hydrological&amp;nbsp;pathways over and through the bedrock and soils. &lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/fs16299</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey,</dc:publisher>
  <dc:title>Panola Mountain, Georgia: A Water, Energy, and Biogeochemical Budgets Program Site</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>