Su Huan, Wang Wen-Long, Kang Hong-Liang, Bai Yun, Guo Ming-Ming, Chen Zhuo-Xin
State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, Shaanxi, China.
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, Shaanxi, China.
Ying Yong Sheng Tai Xue Bao. 2020 Sep 15;31(9):3194-3206. doi: 10.13287/j.1001-9332.202009.018.
In the open pit, runoff from the platform is large discharge and rapid afflux, which often results in serious gully erosion of dump slope. The study of erosion process under catchment conditions of the platform-slope system is still backward. In this study, field scouring experiments were conducted to investigate runoff characteristics and sediment yield processes of the platform-slope system under different flow discharges (48, 60, 72 and 84 L·min). Our results showed that rill erosion dominated the platform-slope system under the flow discharge of 48 L·min, and gully was formed under 60-84 L·min. The flow velocity of the platform and the slope showed an abrupting-fluctuating-stable trend with the duration of discharge. The flow velocity of the platform was smaller than that of the slope, with the magnitude of reduction at 8.3%-67.1%. The highest flow velocity appeared on the up-slop/down-slope, being 18.5%-44.6% higher than that of the middle-slope. In general, the sediment yield rate of the platform and the slope varied with the duration of discharge, with the sediment yield rate of the slope being 17.4 times as that of the platform. The ratio of gully width to depth showed substantial difference between the platform and slope. The platform generally had the largest ratio than the slope. For the slope, the largest ratio appeared on the middle-slop/down-slope, being 1.36-1.93 times as that of the up-slope. The morphology of rill and gully along the platform to down-slope presented in the form of "wide and shallow-narrow and deep-wide and shallow". Rill erosion mainly concentrated in the platform and the middle slope under the flow discharge of 48 L·min, contributed 29.9% and 26.8% of the total erosion volume, respectively. When the flow discharge increased to 60-84 L·min, the largest average across-section areas (1083.25-1737.86 cm) formed on the up-slope accounted for 36.1%-44.7% of the total erosion volume. Our results provided evidence for modelling soil and water erosion of the platform-slope system in opencast coal mine.
在露天矿中,平台径流流量大、汇入快,常导致排土场边坡严重的沟蚀。目前关于平台 - 边坡系统集水条件下侵蚀过程的研究仍较为滞后。本研究通过野外冲刷试验,探究了不同流量(48、60、72 和 84 L·min)下平台 - 边坡系统的径流特征和产沙过程。结果表明,在流量为 48 L·min 时,细沟侵蚀主导平台 - 边坡系统,而在 60 - 84 L·min 时会形成沟壑。平台和边坡的流速随放水历时呈突增 - 波动 - 稳定趋势。平台流速小于边坡,减小幅度为 8.3% - 67.1%。最高流速出现在上坡/下坡,比中坡高 18.5% - 44.6%。总体而言,平台和边坡的产沙率随放水历时变化,边坡产沙率是平台的 17.4 倍。平台和边坡的沟宽与沟深之比存在显著差异。平台的该比值通常大于边坡。对于边坡,最大比值出现在中坡/下坡,是上坡的 1.36 - 1.93 倍。沿平台至下坡方向,细沟和沟壑形态呈现“宽浅 - 窄深 - 宽浅”的形式。在流量为 48 L·min 时,细沟侵蚀主要集中在平台和中坡,分别占总侵蚀量的 29.9%和 26.8%。当流量增至 60 - 84 L·min 时,上坡形成的最大平均横截面积(1083.25 - 1737.86 cm)占总侵蚀量的 36.1% - 44.7%。本研究结果为露天煤矿平台 - 边坡系统土壤侵蚀和水土流失建模提供了依据。