Methane Emissions From Major Rice Ecosystems in Asia 2000
DOI: 10.1007/978-94-010-0898-3_30
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Differences among rice cultivars in root exudation, methane oxidation, and populations of methanogenic and methanotrophic bacteria in relation to methane emission

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Cited by 24 publications
(31 citation statements)
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“…Different rates of soil gaseous emissions have been related to specific cultivars, crop growth and developmental stage (Wang et al 1997;Wang and Adachi 2000;Das and Baruah 2008). Methane emission of rice cultivars was related to higher root biomass, root exudates, and number of tillers because the plant acts as a conduit for methane transport (Wang et al 1997;Wang and Adachi 2000).…”
Section: Cultivar Mixturesmentioning
confidence: 99%
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“…Different rates of soil gaseous emissions have been related to specific cultivars, crop growth and developmental stage (Wang et al 1997;Wang and Adachi 2000;Das and Baruah 2008). Methane emission of rice cultivars was related to higher root biomass, root exudates, and number of tillers because the plant acts as a conduit for methane transport (Wang et al 1997;Wang and Adachi 2000).…”
Section: Cultivar Mixturesmentioning
confidence: 99%
“…Methane emission of rice cultivars was related to higher root biomass, root exudates, and number of tillers because the plant acts as a conduit for methane transport (Wang et al 1997;Wang and Adachi 2000). Gaseous emissions of 3-cv and 5-cv mixtures differed from the monoculture at some spot samplings under the fallow treatment.…”
Section: Cultivar Mixturesmentioning
confidence: 99%
“…5). Based on these ideas, Wang and Adachi 56) studied the effect of rice cultivars on the CH 4 -oxidizing activity and the population of methanotrophic bacteria in rice Fig. 4.…”
Section: Effect Of Rice Cultivars On Ch 4 Emission From the Paddy Fiementioning
confidence: 99%
“…Figure 1 57) shows a sketch of a flooded rice field in relation to CH 4 production, oxidation, and emission, along with CH4 diffusion, ebullition, and leaching from the paddy soil. Rice plants play the key role in CH 4 emission from paddy fields: (1) they supply root exudate and detritus which are substrates for CH4 production 56) ; (2) the rice aerenchyma system is a major pathway of CH 4 from paddy soil to atmosphere 13,42,46) ; (3) the aerenchyma system is also a pathway of O 2 supply to the rice rhizosphere by downward transportation, thus rice plants support CH4 oxidation in the rhizosphere; and (4) the rice rhizosphere itself is an important niche for methanotrophic bacteria which oxidize CH 4 to CO 2 56,63) . Methanogenic archaea (methanogens) are strictly anaerobic microbes belonging to the Archaea domain, and play an important role in anoxic environments by performing the last step of the anaerobic decomposition of organic matter: mineralization into CH 4 and CO 2 27) .…”
mentioning
confidence: 99%
“…Butterbach-Bahl et al [23] attributed a difference in CH 4 fluxes among cultivars to differences in CH 4 transport capacity, as no differences were measured between potential CH 4 productions or oxidations among the cultivars. While several studies suggested differences in gas transport capacity or microbial community structure are the major influencing factors on differences in CH 4 fluxes among cultivars, additional studies have consistently suggested that differences in root exudation rates among cultivars are the primary factors that influence differences in CH 4 fluxes among cultivars [26,27,28,57,58].…”
mentioning
confidence: 99%