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Rainwater and throughfall chemistry in a terra firme rain forest: Central Amazonia

Journal Article · · Journal of Geophysical Research; (United States)
DOI:https://doi.org/10.1029/90JD02170· OSTI ID:5400698
;  [1]
  1. Instituto Nacional de Pesquisas Espaciais Sao Jose dos Campos, Sao Paulo (Brazil)
During the Global Tropospheric Experiment (GTE)-Amazon Boundary Layer Experiment (ABLE) 2B campaign in the Amazon basin, samples of rainwater and throughfall were obtained in a terra firme (nonflooded forest) rain forest at the Ducke Reserve (2{degree}57{prime}S, 59{degree}58{prime}W). The samples were collected during one wet period (April 1 to May 13, 1987) and one dry period (August 1 to October 1, 1987). All samples were analyzed for Na{sup +}, K{sup +}, Mg{sup 2+}, Ca{sup 2+}, NH{sub 4}{sup +}, Cl{sup {minus}} and SO{sub 4}{sup 2{minus}}, and pH. The rainwater was acidic, with a volume-weighted mean pH of 4.6 for two periods. Rainwater input from the dry period was 2 times greater for Na{sup +}, Mg{sup 2+}, NH{sub 4}{sup +}and SO{sub 4}{sup 2{minus}} and about 4 times greater for K{sup +} than from the wet period. The ionic concentrations in throughfall were higher than those in rainwater, except for NH{sub 4}{sup +} during the dry period. This enrichment of throughfall is attributed to the interaction of precipitation with the forest canopy.
OSTI ID:
5400698
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 96:D4; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English