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A Process-Based Experimental Framework for Simulating Soil Organic Carbon Dynamics and Evaluating the Sustainability of Land Management Practices in Intensively Managed Landscapes

机译:基于过程的实验框架,用于模拟土壤有机碳动态并评估集约化景观中土地管理实践的可持续性

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Changes in land cover can significantly affect the spatial and temporal heterogeneity of water-driven soil erosion and deposition in Intensively Managed Landscapes (IMLs), and hence the redistribution of soil organic carbon (SOC) along a hillslope. In IMLs, erosion and deposition are typically more prominent than in grassland and forested ecosystems, while exhibiting higher spatial heterogeneity and temporal variability due to the intensive management. However, the degree to which erosion and deposition affect the carbon budget is not fully understood, and in many cases, it is unclear whether or not these processes lead to net carbon emissions or sequestration. This is, in part, due to the lack of a comprehensive model that accounts for many key processes at the landscape scale. A framework that adequately accounts for such landscape processes would significantly improve model predictions of carbon fluxes and lead to a better understanding of the role of soil redistribution on carbon fluxes. Such a framework would also produce comprehensive carbon budgets that shed light on the sustainability of different management practices in IMLs. Initial steps have been taken to account for the increased role of erosion and deposition on SOC redistribution through the coupling of soil biogeochemical models, like CENTURY, and process-based, upland erosion models, like the Water Erosion Prediction Project (WEPP). The coupled WEPP-CENTURY model will serve as an effective tool for managing and evaluating best management practices that can conserve and replenish SOC. One limitation of this model, however, is the inability to determine the fate of SOC during transport. In this study, changes in SOC in soil aggregates were explored through their interaction with rainfall and runoff and quantified via enrichment ratio and aggregate stability experiments. Soil aggregates encapsulate SOC and act as either sinks of carbon or sources to the atmopshere, so the fate of aggregates during transport greatly impacts the SOC budget. These experiments were performed under different management practices in the Clear Creek, IA watershed, an intensively managed landscape of the U.S. Midwest. The results herein show differences in the stability of aggregates and enrichment ratios for the different management practices in Clear Creek.
机译:在集约化管理景观(IMLs)中,土地覆盖的变化会严重影响水驱动的土壤侵蚀和沉积的时空异质性,因此会影响坡地上土壤有机碳(SOC)的重新分布。在IML中,侵蚀和沉积通常比草地和森林生态系统更为突出,而由于集约化管理,其表现出更高的空间异质性和时间变异性。然而,侵蚀和沉积影响碳收支的程度尚不完全清楚,在许多情况下,还不清楚这些过程是否导致净碳排放或碳固存。这在一定程度上是由于缺乏全面的模型,该模型无法解释景观范围内的许多关键过程。一个充分考虑到此类景观过程的框架将大大改善碳通量的模型预测,并使人们对土壤再分配对碳通量的作用有更好的了解。这样的框架还将产生全面的碳预算,从而阐明IML中不同管理实践的可持续性。已经采取了初步步骤来考虑侵蚀和沉积在土壤重塑过程中的作用,这是通过土壤生物地球化学模型(如​​CENTURY)和基于过程的旱地侵蚀模型(如水蚀预测项目(WEPP))的耦合来实现的。耦合的WEPP-CENTURY模型将成为管理和评估可节省和补充SOC的最佳管理实践的有效工具。但是,该模型的局限性在于无法确定运输过程中SOC的命运。在这项研究中,通过与降雨和径流的相互作用探讨了土壤团聚体中SOC的变化,并通过富集比和团聚体稳定性实验对其进行了量化。土壤团聚体包裹了SOC,并充当了碳汇或汇入大气的来源,因此运输过程中团聚体的命运极大地影响了SOC预算。这些实验是在爱荷华州分水岭(美国中西部一个集约化管理景观)的不同管理实践下进行的。本文的结果显示了Clear Creek不同管理实践的骨料稳定性和富集率的差异。

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