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Conservation Practice Effects On Sediment Load In The Goodwin Creek Experimental Watershed

机译:保护实践对古德温河实验流域泥沙负荷的影响

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Water quality and aquatic habitat due to unstable stream channels and high sediment concentrations during storm runoff events are major environmental concerns on the 2,132 ha (5,266 ac) Goodwin Creek Experimental Watershed in north Mississippi. Effects of enrolling erodible lands in the Conservation Reserve Program (CRP) and instream grade stabilization structures were evaluated using measured rainfall, runoff, and sediment concentration data and model simulations. Signatures of naturally occurring radionuclides indicated that 78% of the total sediment load originated from channel sources. The change of land to a CRP-like state (reducing cultivated land from 26% to 8%) reduced erosion and runoff from fields and thus decreased total sediment concentration by 63% between 1982 to 1990. Simulations using the Fluvial Routing Analysis and Modeling Environment model indicated that mean sediment yields would increase from 15% to over 200%, depending upon location in the watershed, if in-channel structures were not present.The combined effect of the grade control structures and the change of lands to a CRP-state was to reduce sediment yields by 78% near the outlet of the watershed.
机译:在密西西比州北部的2,132公顷(5,266 ac)Goodwin Creek实验流域,由于降雨径流过程中不稳定的河道和高沉积物浓度而导致的水质和水生生境是主要的环境问题。使用测得的降雨,径流和沉积物浓度数据以及模型模拟,评估了将易蚀土地纳入保护区计划(CRP)和河流级稳定结构的影响。天然放射性核素的特征表明,总沉积物负荷的78%来自通道源。从1982年到1990年,土地变为CRP状状态(耕地从26%减少到8%)减少了田间的侵蚀和径流,从而使总泥沙浓度降低了63%。使用河流路径分析和建模环境进行模拟模型表明,如果不存在河道内结构,取决于流域中的位置,平均沉积物产量将从15%增加到200%以上。坡度控制结构和土地变为CRP状态的综合影响是为了使流域出口附近的沉积物产量减少78%。

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