Decomposition pattern of 14C-labeled rice straw in aerobic and submerged rice soils of the Philippines
References (4)
- et al.
Tubificial role in soil mineralization and recovery of algal nitrogen by lowland rice
Soil Biol. Biochem
(1985) - et al.
Use of isotopes in studying the dynamics of organic matter in soils
Cited by (36)
Soil bacterial community mediates the effect of plant material on methanogenic decomposition of soil organic matter
2018, Soil Biology and BiochemistryCitation Excerpt :Consequently, an effect of rice straw on rice field SOM degradation could influence the global budgets not only of CO2, but also CH4. While 80–90% of the RS is decomposed within the first year (Neue and Scharpenseel, 1987), the SOM in rice field soils is rather refractory, and was found to decrease only little (6–17%) within 120 days of anoxic incubation (Yao et al., 1999). The RS applied might be of significance for the decomposition rate of SOM in rice field soils exerting either a positive or negative PE.
The effect of rice straw on the priming of soil organic matter and methane production in peat soils
2015, Soil Biology and BiochemistryCitation Excerpt :The decomposition of more recalcitrant components of rice straws may continue to stimulate SOM decomposing microorganisms and lead to even more CH4 production from SOM (Fontaine et al., 2003). The average half-life of rice straw in a rice field was estimated to be about 2 years (Neue and Scharpenseel, 1987). It is therefore reasonable to postulate that the PE of anaerobic decomposition and CH4 production influenced by straw incorporation may persist for long periods in rice fields.
Biogeochemistry of paddy soils
2010, GeodermaRole of Alternative Electron Acceptors (AEA) to control methane flux from waterlogged paddy fields: Case studies in the southern part of West Bengal, India
2009, International Journal of Greenhouse Gas ControlGlobal warming potential of manure amended soils under rice-wheat system in the Indo-Gangetic plains
2005, Atmospheric Environment