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Organic and inorganic sulfur constituents of a forest soil and their relationship to microbial activity

Journal Article · · Soil Sci. Soc. Am. J.; (United States)
Sulfur (S) constituents, microbial biomass, and sulfohydrolase activity were determined for each soil horizon at both hardwood and conifer sites in a Becket soil (Adirondack Mountains, New York). Drying of soil before analysis altered the S constituents. There was a threefold increase (p<0.05) in sulfate in the organic horizons. Total S was greatest in the O horizons with 2,010 and 1,690 ..mu..g S/g in conifer and hardwood solums, respectively. Mineral soil had a maximum S concentration in the B21h horizon. Sulfate concentrations were a small proportion (<15%) of total S in B horizons. Organic S was dominant (93% of total S) in all horizons. Carbon-bonded S and ester sulfate were 74 and 18% of total S, respectively. Microbial biomass was greatest in the O1 horizon of both hardwood and conifer solums (59 and 70 mg biomass C per 100 g/sup -1/ dry mass, respectively). The B21h horizon contained the greatest biomass in the mineral soil. Sulfohydrolase activity exhibited the same distribution. Total S, carbon-bonded S, and ester sulfate were all positively correlated (p<0.05) to percent organic matter in the soil horizons. Correlations between microbial biomass and sulfohydrolase activity with organic S indicate the potential for microbial S transformations. Sulfate formation by mineralization may be more important than exogenous inputs. This has major implications for assessing the impact of atmospheric S deposition on soils.
Research Organization:
S.U.NY, Syracuse, NY
OSTI ID:
5822128
Journal Information:
Soil Sci. Soc. Am. J.; (United States), Journal Name: Soil Sci. Soc. Am. J.; (United States) Vol. 46:4; ISSN SSSJD
Country of Publication:
United States
Language:
English