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The effect of different flooding duration on soil organic carbon and its labile fraction in the riparian zone of Three Gorges Reservoir Area

机译:不同洪水持续时间对三峡库区河岸区土壤有机碳及其不稳定性分数的影响

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The labile fractions of organic carbon (OC) in soil can respond rapidly to changes in C supply and have been suggested as a sensitive indicator of soil quality. The object is to determine soil organic C and its labile fractions at the duration of different flooding. Three elevation gradient sites were chose: below 145m (permanently flooding site), 145-175m (seasonal flooding site), and above 175m (never flooding site) in the riparian zone of Three Gorges reservoir Area. The results showed that soil OC, dissolved organic C (DOC) and water-soluble carbohydrate (WSCh) were lower under seasonal flooding sites than those of never flooding upland and permanently flooding sites, whereas microbial biomass C (MBC) decreased with the flooding duration. Correlation analysis showed that soil OC and MBC had significantly positive relationship with DOC. The results suggested that seasonal flooding significantly affected soil OC and its labile fractions in the riparian zone of Three Gorges reservoir Area.
机译:土壤中有机碳(OC)的不稳定级分可以迅速响应C供应的变化,并被建议作为土壤质量的敏感指标。目的是在不同洪水持续时间内测定土壤有机C及其不稳定的级分。选择了三个海拔梯度网站:在三峡库区河岸区的145亿(永久洪水型位点),145-175米(季节性洪水型),高于175米(从不泛滥的地方)。结果表明,在季节性洪水场地下,土壤OC,溶解的有机C(DOC)和水溶性碳水化合物(WSCH)低于永不洪水的普通和永久性洪水位点,而微生物生物量C(MBC)随着洪水持续时间而降低。相关分析表明,土壤OC和MBC与DOC有明显的阳性关系。结果表明,三峡库区河岸区季节性洪水显着影响土壤OC及其不稳定馏分。

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