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Sulfur cycling in Douglas-fir on a glacial outwash terrace

Journal Article · · J. Environ. Qual.; (United States)
OSTI ID:5546362
In a study to determine if a temperate forest site would exhibit accelerated nutrient cycling or increased sulfur accumulation with an increased precipitation input of S, a second-growth Douglas-fir ecosystem (Pseudotsuge menziesii (Mirb) Franco) on a glacial outwash terrace accumulated 2.2 kg ha/sup -1/ year/sup -1/ of S. Prior to Mount St. Helen's activity, an atmospheric input as precipitation of 8.9 kg ha/sup -1/ year/sup -1/ of sulfate-S was augmented by an additional 8.1 kg ha/sup -1/ year/sup -1/ in throughfall. Sulfate-sulfur leaching decreased with increased soil depth: 8.4 kg ha/sup -1/ year/sup -1/ leached through the forest floor, 10.5 through the A horizon, 6.7 through the B horizon, and 3.2 at 1.5 m in the C horizon. This S budget was not complete, since gaseous forms and movements were not monitored. Sulfate-sulfur mobility accounted for an average 25% of the cation leaching through the soil profile. Sulfur utilization did not measurably change from a similar stand with lower S inputs. The increased SO/sub 4/-S input did not accelerate nutrient cycling, rather SO/sub 4/-S accumulated in the soil, presumably by sorption. Sulfate-sulfur mobility is defined by the sorption mechanism within the soil.
Research Organization:
Colorado State Univ., Fort Collins
OSTI ID:
5546362
Journal Information:
J. Environ. Qual.; (United States), Journal Name: J. Environ. Qual.; (United States) Vol. 11:1; ISSN JEVQA
Country of Publication:
United States
Language:
English