Soil Organic Carbon Mineralization as Affected by Cyclical Temperature Fluctuations in a Karst Region of Southwestern China
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Deep tillage enhanced soil organic carbon sequestration in China: A meta-analysis
2023, Journal of Cleaner ProductionPriming of soil organic carbon mineralization and its temperature sensitivity in response to vegetation restoration in a karst area of Southwest China
2022, Science of the Total EnvironmentCitation Excerpt :Overall, strong linkages were detected between the changes in soil properties of different vegetation types and the response to cumulative SOC mineralization and Cm/SOC. Our results are in accordance with other studies (Ci et al., 2015; Fanin et al., 2020; Guttières et al., 2021), highlighting the importance of vegetation succession in C sequestration in this karst region. A previous study showed that vegetation restoration accelerated SOC accumulation and increased the C/N ratio, which may account for the lower magnitude of SOC decomposition (Zhang et al., 2021b), which is in agreement with our results (Table 1; Fig. 1E, F).
The effects of shallow flooding on carbon mineralization in a paddy soil: Constraints observed with the addition of straw
2022, Applied Soil EcologyCitation Excerpt :Many previous research studies have confirmed that temperature and moisture levels are important environmental factors affecting soil C mineralization (Li et al., 2005; Conant et al., 2008; Arnold et al., 2015). Many studies have shown that a significant positive correlation exists between soil temperature and soil C mineralization (Kirschbaum, 1995; Ci et al., 2015; Hou et al., 2016), yet the relationship between soil moisture levels and soil C mineralization remains unclear (Craine and Gelderman, 2011; Ge et al., 2012; von Haden and Dornbush, 2014). Some studies have shown the role of physical processes (transport, aggregate dynamics), microbial physiological processes (osmoregulation, dormancy), and community dynamics etc., as drivers of mineralization under different soil moistures (Rabbi et al., 2014; Jones et al., 2019; Yu et al., 2020).
Modelling dynamic soil organic carbon flows of annual and perennial energy crops to inform energy-transport policy scenarios in France
2020, Science of the Total EnvironmentCitation Excerpt :Several physical and biochemical mechanisms may influence the decomposition rate, and these mechanisms can be in turn influenced by management (e.g. to increase C sequestration) (Wiesmeier et al., 2019; Zomer et al., 2017). In general, SOC models take into consideration soil temperature, water, and clay content; as main drivers for changes in C stocks (Bockstaller and Girardin, 2010; Ci et al., 2015; FAO, 2017; Han et al., 2018; Zhong et al., 2018). They are usually based on the assumption that SOM decomposes following first order kinetics (Luo et al., 2016; Smith et al., 2012), initially proposed in the 1945 pioneering model from Hénin and Dupuis (Hénin and Dupuis, 1945; Shibu et al., 2006), where the decomposition rate constant corresponds to the pedoclimatic condition-dependent annual mineralisation rate.
Root litter diversity and functional identity regulate soil carbon and nitrogen cycling in a typical steppe
2020, Soil Biology and Biochemistry