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Afforestation stimulates soil organic carbon decomposition but suppresses its temperature sensitivity by altering microbial co-occurrence network topology and mineral protection in a subtropical karst region

xinyu Hou (21988862) · figshare

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造林被广泛认为是基于自然的气候解决方案。 H然而，它对土壤有机碳（SOC）动力学的影响涉及复杂的生物-非生物反馈，这些反馈在区域性上具有变异性和机制上的难以捉摸性。一个关键的不确定性在于林如何同时调节SOC分解的基础速率和温度敏感度（Q10），这两个参数共同决定了变暖时微生物驱动的碳流失大小。本研究SOC分解与Q10造林西南亚热带喀斯特地区配对方法比较次生林与耕地造林显著提高了SOC分解速率205.56%，但同期使2010作者了27.60%。结构方程建模显示，SOC分解速率的显著提升是由生物与非生物途径协同驱动的：造林降低了SOC的相对矿物保护（证据为Fe/Al氧化

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<b>Afforestation stimulates soil</b><b> </b><b>organic carbon decomposition but suppresses its temperature sensitivity</b> <b>by altering microbial</b><b> </b><b>co-occurrence network topology</b><b> and mineral protection in a subtropical karst region</b>

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