2000
DOI: 10.1007/s003740000214
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Wetland rice soils as sources and sinks of methane: a review and prospects for research

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Cited by 60 publications
(45 citation statements)
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“…At the same time, methane can also be oxidized by methanotrophs that settled in the rhizosphere of rice plants and at the surface of flooded rice soils (Kumaraswamy et al, 2000). Transport through rice plants, diffusion and ebullition serve as three vehicles for transport of methane from the sites of production in the soil to the atmosphere (Wassmann et al, 1993).…”
Section: Introductionmentioning
confidence: 99%
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“…At the same time, methane can also be oxidized by methanotrophs that settled in the rhizosphere of rice plants and at the surface of flooded rice soils (Kumaraswamy et al, 2000). Transport through rice plants, diffusion and ebullition serve as three vehicles for transport of methane from the sites of production in the soil to the atmosphere (Wassmann et al, 1993).…”
Section: Introductionmentioning
confidence: 99%
“…Transport through rice plants, diffusion and ebullition serve as three vehicles for transport of methane from the sites of production in the soil to the atmosphere (Wassmann et al, 1993). Therefore, the entire process of methane emission from rice fields, including production, oxidation and transport to the atmosphere is affected by biotic and abiotic factors, such as growth status of rice, temperature, soil characteristics (Conrad and Rothfuss, 1991;Masscheleyn et al, 1993;Neue, 1993;Sass et al, 1994;Yang et al, 1994;Denier et al, 1996;Hanson and Hanson, 1996;Chang, 1997, 1998;Rath et al, 1999;Kumaraswamy et al, 2000). In addition, under dif- ferent exploitation methods, the amounts of methane emission from wetland ecosystem are also different, usually varying from 0.47 to 171.12 mg m −2 h −1 (Wei, 2000).…”
Section: Introductionmentioning
confidence: 99%
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“…In paddy soils, CH 4 is produced by methanogenic archaea when soils turn anoxic after flooding (e.g., Kumaraswamy et al 2000). Generated CH 4 may be released to the atmosphere by (1) diffusional transport through the rice plants' aerenchyma, (2) aqueous diffusion to the water table and subsequent partitioning across the air/water interface, and (3) gas-bubble ebullition.…”
Section: Introductionmentioning
confidence: 99%