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Soil Microbial Composition and Nitrogen Cycling in a Disturbed Wet Prairie Restoration (Wisconsin) Jenny Kao-Kniffin and Teri C. Balser (Dept of Soil Science, University of Wisconsin–Madison, 1525 Observatory Dr, Madison, WI 53706-1299 USA, 608/345-3674, tcbalser@ wisc.edu) eplanted almost entirely by the botanist Henry RGreene in the 1940s and 1950s, Lower Greene Prai- rie is among the oldest wet-mesic prairie restoration sites in the United States. Subsequent urbanization and high- way construction since the 1970s have led to an influx of stormwater, sediments, nutrient inputs, and invasive plants. Approximately one-third of the prairie (> 3 ha) is now dominated by reed canarygrass (Phalaris arundina- cea). The historical significance of the site now extends to its present use as an adaptive restoration project that integrates research with restoration (Werner and Zedler 2002, Zedler 2005), as researchers at the University of Wisconsin (under the supervision of Joy Zedler) plan to divert stormwater around the restored prairie. Our objective was to determine differ ences in soil func- tion within the native restored prairie in comparison to the highly disturbed section dominated by reed canarygrass. Such measurements can provide a useful index to assess Figure 1.
Ecological Restoration – University of Wisconsin Press
Published: Jun 10, 2010
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