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Contributions of acid deposition and natural processes to cation leaching from forest soils: a review

Conference ·
OSTI ID:6088686

Methods of quantifying the roles of atmospheric acid inputs and internal acid generation by carbonic, organic, and nitric acids are illustrated by reviewing data sets from several intensively studied sites in North America. Some of the sites (tropical, Costa Rica (La Selva); temperate deciduous, Tennessee (Walker Branch); and temperate coniferous, Washington (Thompson)) received acid precipitation whereas others (northern, southeast Alaska (Petersburg); and subalpine, Washington Cascades (Findley Lake)) did not. Natural leaching by carbonic acid dominated soil leaching in the tropical and temperate coniferous sites, nitric acid (caused by nitrification) dominated leaching in an N-fixing temperate deciduous site (red alder in Washington), and organic acids dominated surface soil leaching in the subalpine site and contributed to leaching of surface soils in several other sites. Only at the temperate deciduous sites in eastern Tennessee did atmospheric acid input play a major role in soil leaching. In no case, however, are the annual net losses of cations regarded as alarming as compared to soil exchangeable cation capital.

Research Organization:
Oak Ridge National Lab., TN (USA); Washington Univ., Seattle (USA). Coll. of Forest Resources
DOE Contract Number:
W-7405-ENG-26
OSTI ID:
6088686
Report Number(s):
CONF-830617-11; ON: DE83014027
Country of Publication:
United States
Language:
English