Nitrogen Transformations Following Tropical Forest Felling and Burning on a Volcanic Soil

Abstract

We measured nitrogen transformations and loss following forest clearing in a relatively fertile tropical forest site. Nitrogen mineralization, nitrification, and amounts of ammonium and nitrate increased substantially in surface soils during the 6 mo following burning, then returned to background levels. The nitrogen content of microbial biomass declined to half its original value 6 mo after clearing and remained low in the cleared sites. Plant uptake of nitrogen was substantial on cleared plots (50 g/m 2 ), but it accounted for only 18% of 1 5 N label added to field plots. Microbial immobilization of 1 5 N was small relative to that in a cleared temperate site, and measurements of denitrification potentials suggested that relatively little mineralized nitrogen was lost to the atmosphere. Substantial amounts of nitrogen (40—70 g/m 2 ) were retained as exchangeable bound nitrate deep in the soils of a cleared plot on which revegetation was prevented; this process accounted for 12% of the 1 5 N label added to field plots.