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Changes of soil microbial biomass carbon and organic carbon with sea level elevation increasing in soils of mountainous areas, Southwest China

机译:西南山区土壤微生物量碳和有机碳随海拔升高的变化

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Soil organic matter, a major factor affecting agroecosystem stability, is controlled by many parameters. It is well understood that cultivation practive would lead to a decrease in organic matter content of soils. However, small gradual changes in total soil organic matter may be difficult to monitor and detect in the short term because of generally high background carbon levels and natural variability of soils. On a short-term scale the measurement of the living fraction of soil organic matter, i.e. microbial biomass C, can reveal early changes in soil organic matter. Our work is to identify the relationship of soil organic C and changes in microbial biomass C with sea-level elevation increasing.
机译:土壤有机质是影响农业生态系统稳定性的主要因素,受许多参数控制。众所周知,积极种植会导致土壤有机质含量下降。但是,由于总体上本底碳水平较高和土壤的自然变异性,短期内总土壤有机质的缓慢变化可能难以监测和检测。在短期尺度上,对土壤有机质(即微生物生物量C)的活度分数的测量可以揭示土壤有机质的早期变化。我们的工作是确定土壤有机碳与微生物生物量碳变化与海平面升高之间的关系。

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