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Effects of free‐air CO 2 enrichment (FACE) on CH 4 emission from a rice paddy field
Author(s) -
Inubushi Kazuyuki,
Cheng Weiguo,
Aonuma Shinichi,
Hoque M.M.,
Kobayashi Kazuhiko,
Miura Shu,
Kim Han Yong,
Okada Masumi
Publication year - 2003
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 - 10.1046/j.1365-2486.2003.00665.x
Subject(s) - paddy field , methane , tiller (botany) , greenhouse gas , environmental science , agronomy , biomass (ecology) , nitrogen , growing season , field experiment , environmental chemistry , soil water , carbon dioxide , chemistry , soil science , biology , ecology , organic chemistry
Methane (CH 4 ) is a particularly potent greenhouse gas with a radiative forcing 23 times that of CO 2 on a per mass basis. Flooded rice paddies are a major source of CH 4 emissions to the Earth's atmosphere. A free‐air CO 2 enrichment (FACE) experiment was conducted to evaluate changes in crop productivity and the crop ecosystem under enriched CO 2 conditions during three rice growth seasons from 1998 to 2000 in a rice paddy at Shizukuishi, Iwate, Japan. To understand the influence of elevated atmospheric CO 2 concentrations on CH 4 emission, we measured methane flux from FACE rice fields and rice fields with ambient levels of CO 2 during the 1999 and 2000 growing seasons. Methane production and oxidation potentials of soil samples collected when the rice was at the tillering and flowering stages in 2000 were measured in the laboratory by the anaerobic incubation and alternative propylene substrates methods, respectively. The average tiller number and root dry biomass were clearly larger in the plots with elevated CO 2 during all rice growth stages. No difference in methane oxidation potential between FACE and ambient treatments was found, but the methane production potential of soils during the flowering stage was significantly greater under FACE than under ambient conditions. When free‐air CO 2 was enriched to 550 ppmv, the CH 4 emissions from the rice paddy field increased significantly, by 38% in 1999 and 51% in 2000. The increased CH 4 emissions were attributed to accelerated CH 4 production potential as a result of more root exudates and root autolysis products and to increased plant‐mediated CH 4 emissions because of the larger rice tiller numbers under FACE conditions.