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Effects of an experimental drought on soil emissions of carbon dioxide, methane, nitrous oxide, and nitric oxide in a moist tropical forest
Author(s) -
Davidson Eric A.,
Ishida Françoise Yoko,
Nepstad Daniel C.
Publication year - 2004
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2004.00762.x
Subject(s) - nitrous oxide , environmental science , soil water , denitrification , carbon dioxide , methanogenesis , methane , environmental chemistry , chemistry , agronomy , nitrogen , soil science , biology , organic chemistry
Changes in precipitation in the Amazon Basin resulting from regional deforestation, global warming, and El Niño events may affect emissions of carbon dioxide (CO 2 ), methane (CH 4 ), nitrous oxide (N 2 O), and nitric oxide (NO) from soils. Changes in soil emissions of radiatively important gases could have feedback implications for regional and global climates. Here we report results of a large‐scale (1 ha) throughfall exclusion experiment conducted in a mature evergreen forest near Santarém, Brazil. The exclusion manipulation lowered annual N 2 O emissions by >40% and increased rates of consumption of atmospheric CH 4 by a factor of >4. No treatment effect has yet been detected for NO and CO 2 fluxes. The responses of these microbial processes after three rainy seasons of the exclusion treatment are characteristic of a direct effect of soil aeration on denitrification, methanogenesis, and methanotrophy. An anticipated second phase response, in which drought‐induced plant mortality is followed by increased mineralization of C and N substrates from dead fine roots and by increased foraging of termites on dead coarse roots, has not yet been detected. Analyses of depth profiles of N 2 O and CO 2 concentrations with a diffusivity model revealed that the top 25 cm soil is the site of most of the wet season production of N 2 O, whereas significant CO 2 production occurs down to 100 cm in both seasons, and small production of CO 2 occurs to at least 1100 cm depth. The diffusivity‐based estimates of CO 2 production as a function of depth were strongly correlated with fine root biomass, indicating that trends in belowground C allocation may be inferred from monitoring and modeling profiles of H 2 O and CO 2 .