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Acidification sources in red alder and Douglas fir soils - importance of nitrification

Conference · · Soil Sci. Soc. Am. J.; (United States)
OSTI ID:6294116

Precipitation, throughfall, forest floor, and soil leachate samples were monitored continuously in 1981 and 1982 in a N-poor douglas fir (Pseudotsuga menziesii (Mirb.) Franco) forest and a red alder (Alnus rubra Bong.) forest growing adjacently on a glacial soil in western Washington. The purpose of the study was to quantify the relative importance of atmospheric vs. natural sources of H input to forest soil acidification, and to determine the role of N transformation processes in the overall H balance of soils with different N status. Rainwater samples had an avg pH of 4.7 and annual H deposition via precipitation averaged 320 mol H ha yr . This was modest compared to internal H production associated with HCO3 and NO3 formation. In the soil under alder cover, which was naturally enriched in N through symbiotic N2-fixation, nitrification released up to 4500 mol H ha annually to the solution percolating through the upper part of the soil profile. In the N-poor soil no nitrification could be observed and N transformation processes had a minor influence on the soil H balance. The main internal acidification source in this case was H2CO3 dissociation releasing 420 mol H ha yr . In both instances, soil solutions appeared well buffered against these external and internal acidification sources, and few H leached below the 40-cm soil depth.

Research Organization:
Univ. of Washington, Seattle
OSTI ID:
6294116
Journal Information:
Soil Sci. Soc. Am. J.; (United States), Journal Name: Soil Sci. Soc. Am. J.; (United States) Vol. 49:5; ISSN SSSJD
Country of Publication:
United States
Language:
English