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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:一种基于过程的实验框架,用于模拟土壤有机碳动力学,评价集中管理景观的土地管理实践可持续性

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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:陆地覆盖的变化可以显着影响水驱动土壤侵蚀和沉积的空间和时间异质性,并在集中管理的景观(IML)中,因此沿着山坡的土壤有机碳(SoC)的再分配。在IMLS中,侵蚀和沉积通常比草原和森林生态系统更突出,而由于密集的管理,呈现出更高的空间异质性和时间可变性。然而,侵蚀和沉积影响碳预算的程度尚未完全理解,并且在许多情况下,目前尚不清楚这些过程是否导致净碳排放或封存。部分原因是由于缺乏综合模型,这些模型占横向规模的许多关键过程。一种框架,即适当占这种景观过程的框架将显着改善碳通量的模型预测,并更好地了解土壤再分配对碳通量的作用。这样的框架还将产生综合碳预算,阐明了IML中不同管理实践的可持续性。通过耦合土壤生物地球化学模型,诸如基于流程预测项目(WEPP),已经考虑了通过土壤生物地球化学模型的耦合来再分配的初步步骤来解释侵蚀和沉积对SOC再分配的增加。耦合的WEPP世纪模型将作为管理和评估最佳管理实践的有效工具,可以保护和补充SOC。然而,这种模型的一个限制是在运输过程中无法确定SOC的命运。在这项研究中,通过与降雨和径流的相互作用来探讨了土壤聚集体中SOC的变化,并通过富集率和聚集稳定性实验进行量化。土壤聚集体包封了SOC,并充当碳或源的沉积物,因此运输过程中的集合命运极大地影响了SOC预算。这些实验在透明溪流,IA流域的不同管理实践下进行,是美国中西部的一个集中管理的景观。本文的结果显示了透明溪流中不同管理实践的聚集体和富集比稳定性的差异。

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