Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Transformations of organic and inorganic sulfur: importance to sulfate flux in an adirondack forest soil

Journal Article · · J. Air Pollut. Control Assoc.; (United States)
Sulfate flux from forest soils as a result of inputs from acidic deposition is thought to be a critical process in regulating acidification of surface waters. The purpose of this study was to evaluate biotic transformations of sulfur in an Adirondack Mountain forest soil by adding /sup 35/S-sulfate to the forest floor. In September 1983 to each of two 0.5 m/sup 2/ plots, 2.22 x 10/sub 10/ dpm of /sup 35/S-sulfate was added in 4 liters of solution. Analysis of soil horizons from the plot at the end of the six week incubation indicated that 70 and 99 percent of the added /sup 35/S was retained in the soil at plots 1 and 2, respectively. More than 70 percent of the /sup 35/S was found in Oa, Bh, and Bs1 horizons. In O horizons greater than 80 percent of the /sup 35/S was found as organic sulfur, whereas in mineral horizons most was found as adsorbed sulfate. These findings indicated that a portion of the sulfate moving through the soil is both rapidly immobilized in the forest floor and adsorbed in the mineral horizons. On a net basis, however, the soil is not accumulating sulfur so that mineralization and desorption must equal immobilization and adsorption.
Research Organization:
State Univ. of New York, Syracuse
OSTI ID:
6939587
Journal Information:
J. Air Pollut. Control Assoc.; (United States), Journal Name: J. Air Pollut. Control Assoc.; (United States) Vol. 37:1; ISSN JPCAA
Country of Publication:
United States
Language:
English