Methane Emission from Natural Wetlands in China: Summary of Years 1995–2004 Studies*
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2022, Agriculture, Ecosystems and EnvironmentMethane emissions and methanogenic community investigation from constructed wetlands in Chengdu City
2021, Urban ClimateCitation Excerpt :With few exceptions (Søvik and Kløve, 2007), CH4 fluxes increase with increasing temperature (Zhu et al., 2008), and the problem arises in part from the greater sensitivity of methanogenesis to temperature (Inglett et al., 2012). Moreover, it has been reported that both reduced CH4 production and stimulated CH4 oxidation are impacted by temperature by lowering the activity of other aerobic microbes in which more O2 can stay in the rhizosphere for methanotrophs (Ding and Cai, 2007). Some studies report the relevance between temperature and CH4 emissions from CWs (Hargreaves and Fowler, 1998; Macdonald et al., 1998; Venkiteswaran and Schiff, 2005), which is exemplified by the optimum temperature for CH4 oxidation being approximately 25 °C, but CH4 can be oxidized at both extremely low (−2 °C) and high (30 °C) temperatures (King and Adamsen, 1992; Sitaula et al., 1995).
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Project supported by the National Natural Science Foundation of China (No. 40471121) and the Field Station Foundation of the Chinese Academy of Science