4.7 Article

Changes in the chemistry of acidified Adirondack streams from the early 1980s to 2008

Journal

ENVIRONMENTAL POLLUTION
Volume 159, Issue 10, Pages 2750-2758

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2011.05.016

Keywords

Acidic deposition; Stream chemistry; Dissolved organic carbon; Calcium leaching; Base cation surplus

Funding

  1. New York State Energy Research and Development Authority (NYSERDA)
  2. Adirondack Long Term Monitoring Program
  3. U.S. Geological Survey (USGS)
  4. New York State Department of Environmental Conservation, Air Resources Division, and Fish, Wildlife and Marine Resources Division
  5. Adirondack Effects Assessment Program (AEAP)
  6. U.S. Environmental Protection Agency [68D20171]
  7. U.S. Environmental Protection Agency

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Lakes in the Adirondack region of New York have partially recovered in response to declining deposition, but information on stream recovery is limited. Here we report results of Adirondack stream monitoring from the early 1980s to 2008. Despite a 50% reduction in atmospheric deposition of sulfur, overall increases in pH of only 0.28 and ANC of 13 mu eq L-1 were observed in 12 streams over 23 years, although greater changes did occur in streams with lower initial ANC, as expected. In the North Tributary of Buck Creek with high dissolved organic carbon (DOC) concentrations, SO42- concentrations decreased from 1999 to 2008 at a rate of 2.0 mu mol L-1 y(-1), whereas in the neighboring South Tributary with low DOC concentrations, the decrease was only 0.73 mu mol L-1 y(-1). Ca2+ leaching decreased in the North Tributary due to the SO42- decrease, but this was partially offset by an increase in Ca2+ leaching from increased DOC concentrations. Published by Elsevier Ltd.

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