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Radiocarbon and Soil Carbon Dynamics

机译:放射性碳和土壤碳动力学

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Research over the past several decades has clarified the mechanisms and timescales involved in stabilizing organic matter ill Soils, but We Still lack process-based understanding sufficient for predicting how vulnerable soil carbon (C) is, given climatic or environmental change across a range of soil types and landscapes. Part of the problem is the emphasis oil short-term studies and processes that dominate C balance at the point or soil profile scale, whereas other processes that dominate over longer timescales and larger spatial scales may actually be more important for determining the carbon balance of soils in a region. Radiocarbon is one of the only tools to study the dynamics of C in soils oil decadal to millennial timescales. It provides a means for directly testing models of organic matter dynamics in ecosystems and, when measured in respired CO2 or dissolved organic carbon (DOC), provides evidence of shifts in microbial metabolism. This review explores the application of this underutilized tool, with an emphasis on conceptual advances made using the state-factor approach mid oil detecting processes causing abrupt change in soil C stores.
机译:过去几十年的研究澄清了稳定病态有机土壤的机制和时间表,但是鉴于整个土壤的气候或环境变化,我们仍然缺乏基于过程的理解足以预测脆弱的土壤碳(C)。类型和风景。问题的一部分是强调油的短期研究和在点或土壤剖面尺度上主导碳平衡的过程,而在更长的时间尺度和更大的空间尺度上主导的其他过程实际上可能对于确定土壤的碳平衡更为重要。在一个地区。放射性碳是研究年代际至千禧年尺度的土壤中碳的动力学的仅有工具之一。它提供了一种直接测试生态系统中有机物动力学模型的方法,并且当以呼吸的CO2或溶解的有机碳(DOC)进行测量时,它提供了微生物代谢变化的证据。这篇综述探索了这种未充分利用的工具的应用,重点是在状态检测油过程中使用状态因子方法引起土壤C储量突然变化的概念性进展。

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