Inhaltszusammenfassung

Methane (CH4) formation under aerobic conditions has been intensely debated, especially since the discovery of CH4 generation by both dried plant material and living plants. In this study we test the hypothesis that non-microbial CH4 formation also occurs in soils. All lyophilised soil samples investigated under aerobic conditions released CH4 at temperatures ranging from 30 to 70 degrees C exceeding that allowing normal enzymatic activity to proceed. No emissions were observed for single min...Methane (CH4) formation under aerobic conditions has been intensely debated, especially since the discovery of CH4 generation by both dried plant material and living plants. In this study we test the hypothesis that non-microbial CH4 formation also occurs in soils. All lyophilised soil samples investigated under aerobic conditions released CH4 at temperatures ranging from 30 to 70 degrees C exceeding that allowing normal enzymatic activity to proceed. No emissions were observed for single mineral soil components such as quartz sand, clay mineral and iron oxide. Methane release rates from the soils investigated were found to increase both with increasing temperature and higher organic carbon content. Addition of water to dried soils increased CH4 release rates up to 8-fold those observed with the dried material. Our results suggest the existence of a chemical process in soils that produces CH4 under aerobic conditions, a finding which has not been hitherto reported. (C) 2011 Elsevier Ltd. All rights reserved. » weiterlesen» einklappen

Autoren