IGN 15-9
Why lime Adirondack forests and streams?

Thursday, August 8, 2013
101H, Minneapolis Convention Center
Randall Fuller, Department of Biology, Colgate University, Hamilton, NY
Gregory B. Lawrence, U.S. Geological Survey, Troy, NY
Barry Baldigo, USGS, Troy, NY
Clifford E. Kraft, Department of Natural Resources, Cornell University, Ithaca, NY
Dan Josephson, Department of Natural Resources, Cornell University, Ithaca, NY
Heather A. Bechtold, Cary Institute of Ecosystem Studies, Millbrook, NY
Emma Rosi-Marshall, Cary Institute of Ecosystem Studies, Millbrook, NY
Colin M. Beier, College of Environmental Science and Forestry, State University of New York, Syracuse, NY
Clean Air Act Amendments have reduced acid deposition across the northeastern US, but recovery of surface waters has lagged because of calcium depletion in Adirondack forest soils. Current estimates suggest that 65% of headwater streams are episodically or chronically acidified.   To date, calcium availability in soil has not increased so remediation may be the only way to achieve desired levels of recovery at some high value sites within a reasonable length of time.  Our research is investigating different remediation strategies to determine best practices to protect species, the first being one of 7 heritage brook trout strains in New York.