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From soilscapes to landscapes: A landscape-oriented approach to simulate soil organic carbon dynamics in intensively managed landscapes

机译:从土壤景观到景观:以景观为导向 模拟土壤有机碳动态的方法 在密集管理的景观

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摘要

Most available biogeochemical models focus within a soil profile and cannot adequately resolve contributions of the lighter size fractions of organic rich soils for enrichment ratio (ER) estimates, thereby causing unintended errors in soil organic carbon (SOC) storage predictions. These models set ER as constant, usually equal to unity. The goal of this study is to provide spatiotemporal predictions of SOC stocks at the hillslope scale that account for the selective entrainment and deposition of lighter size fractions. It is hypothesized herein that ER values may vary depending on hillslope location, Land Use/Land Cover (LULC) conditions, and magnitude of the hydrologic event. An ER module interlinked with two established models, CENTURY and Watershed Erosion Prediction Project, is developed that considers the effects of changing runoff coefficients, bare soil coverage, tillage depth, fertilization, and soil roughness on SOC redistribution and storage. In this study, a representative hillslope is partitioned into two control volumes (CVs): a net erosional upslope zone and a net depositional downslope zone. We first estimate ER values for both CVs I and II for different hydrologic and LULC conditions. Second, using the improved ER estimates for the two CVs, we evaluate the effects that management practices have on SOC redistribution during different crop rotations. Overall, LULC promoting less runoff generally yielded higher ER values, which ranged between 0.97 and 3.25. Eroded soils in the upland CV were up to 4% more enriched in SOC than eroded soils in the downslope CV due to larger interrill contributions, which were found to be of equal importance to rill contributions. The chronosequence in SOC storage for the erosional zone revealed that conservation tillage and enhanced crop yields begun in the 1980s reversed the downward trend in SOC losses, causing nearly 26% of the lost SOC to be regained.
机译:大多数可用的生物地球化学模型都集中在土壤剖面内,无法充分解析富含有机物的土壤的较轻尺寸部分对富集比(ER)的贡献,从而在土壤有机碳(SOC)储存预测中引起意外错误。这些模型将ER设置为常数,通常等于1。这项研究的目的是提供在坡度规模上的SOC储量的时空预测,以解释较轻尺寸馏分的选择性夹带和沉积。本文假设ER值可能根据山坡位置,土地利用/土地覆盖(LULC)条件和水文事件的大小而变化。开发了一个与两个已建立的模型CENTURY和分水岭侵蚀预测项目链接的ER模块,该模型考虑了径流系数变化,裸土覆盖,耕作深度,施肥和土壤粗糙度对SOC重新分配和存储的影响。在这项研究中,代表性的山坡被分为两个控制体积(CV):净侵蚀性上坡带和净沉积性下坡带。我们首先估算不同水文和LULC条件下CV I和II的ER值。其次,使用针对两个CV的改进的ER估算,我们评估了管理实践对不同轮作期间SOC重新分配的影响。总体而言,LULC促进减少径流一般会产生较高的ER值,介于0.97和3.25之间。由于中间钻具的贡献较大,发现高地CV上的侵蚀土壤的SOC含量比下坡CV上的侵蚀土壤的SOC高出4%,这与钻探的贡献同等重要。侵蚀带的SOC储存的时间序列显示,从1980年代开始的保护性耕作和提高的农作物产量扭转了SOC损失的下降趋势,使近26%的SOC损失得以恢复。

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