The mechanisms of soil organic carbon (SOC) loss and its modeling
水力侵蚀造成的土壤有机碳(SOC)流失不仅会导致土壤退化、土地生产力下降,还会在一定程度上加剧全球变暖。因此,侵蚀导致的SOC流失成为全世界关注的重要环境问题。在以往的研究中,虽然SOC流失特征及规律已经得到了广泛研究,但是较少涉及其与径流水力特性的内在联系。水力学模拟一直是土壤侵蚀建模的经典方法。因此,充分了解不同侵蚀环境下SOC流失的径流水动力学机制,建立基于径流水力因子的SOC流失模型具有重要意义。本研究按照土壤黏粒含量依次递减的规律,选取了黄土高原四种典型的坡耕地土壤:塿土(杨凌)、黑垆土(长武)
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