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Regional patterns of soil sulfate accumulation: relevance to ecosystem sulfur budgets

Conference ·
OSTI ID:5390760
Analysis of soils from Walker Branch, Camp Branch, and Cross Creek, Tennessee, Coweeta, North Caroline, and Hubbard Brook, New Hamsphire support the hypothesis that watershed sulfur accumulation is due to inorganic sulfate adsorption in soils. Analysis of soils from lysimeter study sites at La Selva, Costa Rico, and Thompson Site, Washington produced similar results. In laboratory adsorption studies, only soils from Coweeta retained substantial (50 to 100%) additional amounts of sulfate in insoluble forms. Soil adsorbed sulfate content and sulfate adsorption capacity were positively correlated with sesquioxide content but negatively correlated with organic matter content. Organic matter apparently blocks sesquioxide adsorption sites, preventing sulfate adsorption in sesquioxide-rich A horizons and Spodosol B/sub 2/ir horizons. This blockage may account for the accummulation of adsorbed sulfate in B horizons in temperate and tropical soils and the susceptibility of New England Spodosols to leaching by H/sub 2/SO/sub 4/.
Research Organization:
Oak Ridge National Lab., TN (USA)
Sponsoring Organization:
USDOE Office of Environment, Safety and Health (EH)
DOE Contract Number:
W-7405-ENG-26
OSTI ID:
5390760
Report Number(s):
CONF-791090--6
Country of Publication:
United States
Language:
English