Journal
CHEMOSPHERE
Volume 59, Issue 11, Pages 1697-1702Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.chemosphere.2004.12.011
Keywords
Amazon; hydroelectric reservoirs; methane emission; isotope analysis
Categories
Ask authors/readers for more resources
Biogeochemical distinction of methane emissions to the atmosphere may essentially rely on the surface area and morphometry of Amazon hydroreservoirs. Tucurui (deep) and Samuel (shallow) reservoirs released in average 13.82 +/- 22.94 and 71.19 +/- 107.4 mg CH4 m(-2) d(-1), respectively. delta C-13-CH4 values from the sediments to the atmosphere indicate that the deep reservoir has extended methanotrophic layer, oxidizing large quantities of light isotope methane coming from the sediments, while sediment-generated methane can easily evade the shallow reservoir. (c) 2005 Elsevier Ltd. All rights reserved.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available