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Soil emissions of Nd2O, NO, and COd2 in Brazilian Savannas: Effects of vegetation type, seasonality, and prescribed fires

Using closed chamber techniques, soil fluxes of NO, Nd2O, and COd2 were measured from September 1999 to November 2000 in savanna areas of central Brazil (cerrado) subjected to prescribed fires. Our studies focused on two vegetation types, cerrado stricto sensu (20-50 percent canopy cover) and campo...

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Bibliographic Details
Published in:Journal of Geophysical Research. D. Atmospheres 2002-10, Vol.107 (D20)
Main Authors: De Siqueira Pinto, A, Bustamante, M.M.C., Kisselle, K, Burke, R, Zepp, R, Viana, L T, Varella, R F, Molina, M
Format: Article
Language:English
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Summary:Using closed chamber techniques, soil fluxes of NO, Nd2O, and COd2 were measured from September 1999 to November 2000 in savanna areas of central Brazil (cerrado) subjected to prescribed fires. Our studies focused on two vegetation types, cerrado stricto sensu (20-50 percent canopy cover) and campo sujo (open, grass dominated), which were either burned every 2 years or protected from fire. Soil moisture and vegetation type were more important in controlling NO and COd2 fluxes than fire regime (early dry season, middle dry season or late dry season burning). Nd2O fluxes, however, were very low and below detection limit in any of the vegetation-fire treatments. NO emissions increased after burning (1.0 ng NO-N cm super -2 h super -1), but flux returned quickly to prefire levels and even lower. In comparison, NO emissions increased 100-fold (to 10.5 ng NO-N cm super -2 h super -1) during a water-addition experiment in unburned campo sujo, and to 1.0 ng NO-N cm super -2 h super -1 in unburned cerrado and 1.9 ng NO-N cm super -2 h super -1 in burned cerrado with the first rains. Low NO and Nd2O emissions, low nitrification rates, and the majority of inorganic N in the form of NHd4 beta u+ all indicate a conservative N cycle in the cerrado. COd2 fluxes increased with the onset of the rainy season and after artificial water addition. The highest COd2 measured in the wet season was 6.3 micro mol COd2 m super -2 s super -1 in burned campo sujo. During the dry season, soil respiration in burned and unburned treatments were similar (average flux = 1.6-2.3 micro mol COd2 m super -2 s super -1). Differences between fire treatments of cerrado and campo sujo COd2 fluxes are attributed to differences in relative litter production and root activity.
ISSN:0148-0227
DOI:10.1029/2001JD000342