Land use change and biogeochemical controls of nitrogen oxide emissions from soils in eastern Amazonia

作者：Louis Vincent Verchot, Eric A. Davidson, Henrique Cattânio, Ilse L. Ackerman, Heather E. Erickson, Michael Keller · 发表于：Global Biogeochemical Cycles · 年份：1999 · DOI：10.1029/1998gb900019 · 被引用次数：349 · 研究领域：Soil Carbon and Nitrogen Dynamics、Groundwater and Isotope Geochemistry、Soil and Water Nutrient Dynamics

The objectives of this study were (1) to determine the effects of land use change on N oxide fluxes from soil in seasonally dry, eastern Amazonia and (2) evaluate the “hole‐in‐the‐pipe” model in a field setting where N availability varies among land uses and soil moisture varies among seasons. We measured N oxide flux from an old‐growth forest, a 20‐year‐old secondary forest, an active pasture, and a degraded pasture. We also measured soil water content, soil inorganic N stocks, net N mineralization and nitrification potential. To determine the effects of pasture age on N oxide flux, we measured gas fluxes at a chronosequence of pastures (0‐13 years). In the land use study, N2O fluxes followed the order: primary forest (2.4 kg N ha−1 yr−1) > secondary forest (0.9 kg N ha−1 yr−1) > active pasture (0.3 kg N ha−1 yr−1) ≥ degraded pasture (0.1 kg N ha−1 yr−1), and NO fluxes followed the order: primary forest (1.5 kg N ha y−11) > degraded pasture (0.7 kg N ha−1 yr−1) > active pasture (0.5 kg N ha−1 yr−1) ≥ secondary forest (0.3 kg N ha−1 yr−1). In the chronosequence study, no trend in N oxide emissions with pasture age was apparent, but emissions from pastures were lower than from the forest.Total N oxide flux correlated with a laboratory measure of nitrification potential (r2 = 0.85).The ratio N2O:NO correlated with soil water content (r2 = 0.56). Parameterization of the model accounted for variability in N oxide emissions across land uses and seasons and the model application re...