<?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>David P. Krabbenhoft</dc:contributor>
  <dc:contributor>Robert G. Striegl</dc:contributor>
  <dc:creator>David M. Lodge</dc:creator>
  <dc:date>1989</dc:date>
  <dc:description>&lt;p&gt;We measured groundwater velocity and submersed macrophyte biomass at 52 shal- low (0.4-6.6 m) sites in mesotrophic Sparkling Lake, Vilas County, Wisconsin, during May-Au- gust 1985. Seventeen percent of variation in macrophyte biomass was explained by a signifi- cant (P &amp;lt; 0.005) relation with depth [log(biomass + 1) = 0.49 depth - 0.08 (depth)2 + 0.121. Some of the remaining variation in macrophyte bio- mass was explained by a significant rank corre- lation of biomass-on-depth residuals with groundwater velocity (rs = 0.46, P &amp;lt; 0.0 1). These results suggest that water movement through the sediment-water interface may be a determinant of macrophyte abundance and distribution.&amp;nbsp;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.4319/lo.1989.34.1.0235</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Society of Limnology and Oceanography, Inc.</dc:publisher>
  <dc:title>A positive relationship between groundwater velocity and submersed macrophyte biomass in Sparkling Lake, Wisconsin</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>