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Sediment Fingerprinting for Calibrating a Soil Erosion and Sediment-Yield Model in Mixed Land-Use Watersheds

机译:泥沙指纹图谱用于混合土地利用流域的土壤侵蚀和产沙量模型的校准

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This research estimates sediment yield contributed from surface mining soils, stream banks, and forest soils using sediment fingerprinting with isotope tracers coupled with soil erosion and sediment yield modeling in mixed land use watersheds. New δ~(13)C and δ~(15)N tracer results from sediment sources and transported sediments are collected and explained; sediment fingerprinting, including uncertainty analyses, is performed; and soil erosion and sediment yield modeling is applied through calibration with sediment fingerprinting as well as sediment concentration measurements. The δ~(13)C and δ~(15)N tracers successfully separated the forest, reclaimed mine, and stream bank sources in Island Branch and Whitaker Branch watersheds located in the Appalachian region of Kentucky, and the results expand the literature database for the usefulness of δ~(13)C and δ~(15)N tracers to separate end-member sources. A significant difference was measured for the values of δ~(13)C and δ~(15)N of the forest sediment source when comparing data results collected in 2007 and 2009/2010, highlighting the nonconstant nature of the source. The results from the sediment fingerprinting allowed for further calibration of the transport capacity coefficient, sediment delivery ratio for reclaimed mining soils, and stream bank erosion parameters. Sediment yield from reclaimed surface mining sites showed a decrease over time including 4.4, 2.1, and 0.8 t • year~(-1) • ha~(-1) for 1 1/2, 4, and 6 1/2, respectively, years after mining. A severe ice storm and rainstorms increased forest sediment production by 3.5 times from 2007 to 2009/2010, and sediment yield increased from 0.08 to 0.29 t • year~(-1) • ha~(-1). Change in the stream bank sediment yield over time was not pronounced. Whitaker Branch bank sediment production was five times higher than Island Branch, which was attributable to the larger susceptible bank area and driving logging trucks across the stream. It is expected that soil erosion and sediment yield modeling in mixed land use watersheds will be coupled with sediment fingerprinting in future studies.
机译:这项研究使用混合同位素土地利用流域中的同位素示踪剂结合泥沙指纹和土壤侵蚀和泥沙产量模型,估计了地表采矿土壤,溪流和森林土壤的泥沙产量。沉积物来源产生了新的δ〜(13)C和δ〜(15)N示踪剂,并收集并解释了所输送的沉积物。进行沉积物指纹分析,包括不确定性分析;通过对泥沙指纹进行校准以及对泥沙浓度进行测量,应用土壤侵蚀和泥沙产量建模。 δ〜(13)C和δ〜(15)N示踪剂成功地分离了位于肯塔基州阿巴拉契亚地区的Island Branch和Whitaker Branch流域中的森林,开垦的矿山和溪流源,结果扩展了文献数据库。 δ〜(13)C和δ〜(15)N示踪剂对分离末端成员源的有用性。当比较2007年和2009/2010年收集的数据结果时,测得的森林沉积物来源的δ〜(13)C和δ〜(15)N值存在显着差异,突显了来源的非恒定性。沉积物指纹图谱的结果可用于进一步校准运输能力系数,填海采矿土壤的沉积物输送比以及河岸侵蚀参数。再生露天采矿场的沉积物产量随时间下降,分别为4.4、2.1和0.8 t•年〜(-1)•ha〜(-1)分别为1 1 / 2、4和6 1/2。开采多年后。从2007年到2009/2010年,一场严重的冰暴和暴雨使森林沉积物产量增加了3.5倍,沉积物产量从0.08 t•year〜(-1)•ha〜(-1)增加到0.29 t•年〜(-1)•ha〜(-1)。河岸沉积物产量随时间的变化没有明显变化。惠特克(Whitaker)分行河岸的沉积物产量比岛分行高五倍,这归因于较大的易感河岸面积和横穿溪流的伐木卡车。预计在未来的研究中,混合土地利用流域的土壤侵蚀和沉积物产量模型将与沉积物指纹图谱结合。

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