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ATMOSPHERIC CONTRIBUTIONS TO FOREST NUTRIENT CYCLING 1
Author(s) -
Swank Wayne T.
Publication year - 1984
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/j.1752-1688.1984.tb04710.x
Subject(s) - nutrient , environmental science , temperate climate , temperate rainforest , precipitation , nitrogen , deposition (geology) , phosphorus , ecosystem , hydrology (agriculture) , agronomy , ecology , chemistry , biology , geology , geography , meteorology , paleontology , geotechnical engineering , organic chemistry , sediment
The atmosphere is a significant source of plant nutrients that partially replenishes losses due to timber harvesting. The relative importance of wet and dry deposition depends upon the specific nutrient and site. Nitrogen in bulk precipitation (wetfall and dryfall) is equivalent to at least 70 percent of the nitrogen incorporated annually in above‐ground woody tissues of some temperate hardwood forests. Atmospheric sources of calcium and potassium supply between 20 and 40 percent of the nutrients sequestered in woody increments. Annual nutrient inputs in bulk precipitation can exceed removals associated with sawiog harvest over a rotation period. Atmospheric inputs of nitrogen are only slightly less than hydrologic losses immediately after timber harvesting. The deposition of nutrients is highly variable in both time and space; interpretations of nutrient inputs and forest management impacts require quantification of inputs for a variety of ecosystems over long periods of time.