The eastern Amazon Basin may become drier as a result of less regional recirculation of water in a largely deforested landscape and because of increased frequency and intensity of El Niño events induced by global warming. Drier conditions may affect several plant and soil microbial processes, including soil emissions of CO2, CH4, NO, and N2O. We report here unanticipated results of a pilot study that was initiated to test the feasibility of a larger-scale throughfall exclusion experiment. In particular, soil drying caused a switch from net consumption of atmospheric CH4 by soils in the control plot to net CH4 emission from soils in the experimentally dried plot.
Amazônia em Chamas nº 12 – entendendo a relação entre o fogo e desmatamento em 2023
Amazônia em Chamas nº 12 – entendendo a relação entre o fogo e desmatamento em 2023
Apesar da redução de 50% no desmatamento na Amazônia, a pior seca em 125 anos aumentou o fogo em outras áreas do bioma, elevando a área queimada total para 10 milhões de hectares, 36% a mais do que em 2022. Dados foram publicados Nota Técnica Amazônia em Chamas nº...