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Impact of road-generated storm runoff on a small catchment response

机译:道路暴雨径流对小流域响应的影响

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摘要

The impact of road-generated runoff on the hydrological response of a zero-order basin was monitored for a sequence of 24 storm events. The study was conducted in a zero-order basin (C1; 0.5ha) with an unpaved mountain road; an adjacent unroaded zero-order basin (C2; 0.2 ha) with similar topography and lithology was used to evaluate the hydrological behaviour of the affected zero-order basin prior to construction of the road. The impact of the road at the zero-order basin scale was highly dependent on the antecedent soil-moisture conditions, total storm precipitation, and to some extent rainfall intensity. At the beginning of the monitoring period, during dry antecedent conditions, road runoff contributed 50% of the total runoff and 70% of the peak flow from the affected catchment (C1). The response from the unroaded catchment was almost insignificant during dry antecedent conditions. As soil moisture increased, the road exerted less influence on the total runoff from the roaded catchment. For very wet conditions, the influence of road-generated runoff on total outflow from the roaded catchment diminished to only 5.4%). Both catchments, roaded and unroaded, produced equivalent amount of outflow during very wet antecedent conditions on a unit area basis. The lag time between the rainfall and runoff peaks observed in the unroaded catchment during the monitoring period ranged from 0 to 4 h depending on the amount of precipitation and antecedent conditions, owing mainly to much slower subsurface flow pathways in the unroaded zero-order basin. In contrast, the lag time in the roaded zero-order basin was virtually nil during all storms.
机译:监测了道路产生的径流对零级流域水文响应的影响,涉及24个暴风雨事件。这项研究是在零阶盆地(C1; 0.5ha)和未铺山路的地方进行的;在修筑道路之前,使用一个具有相似地形和岩性的相邻未修整零阶盆地(C2; 0.2公顷)来评估受影响的零阶盆地的水文行为。道路在零阶流域尺度上的影响在很大程度上取决于先前的土壤湿度条件,总的暴雨降水以及某种程度上的降雨强度。在监测期开始时,在干旱的前期条件下,道路径流贡献了总径流的50%,受影响流域(C1)的洪峰流量占70%。在干旱的前期条件下,未铺路的集水区的响应几乎没有意义。随着土壤水分的增加,道路对道路集水区总径流量的影响较小。对于非常潮湿的条件,道路产生的径流对道路集水区总流出量的影响减少到仅5.4%。在非常潮湿的前期条件下,无论是集水区还是非集水区,在单位面积上都产生了同等的流出量。在监测期内,在非道路集水区观测到的降雨与径流峰值之间的滞后时间介于0至4小时之间,具体取决于降水量和前期条件,这主要是由于非道路零阶流域的地下流动路径要慢得多。相反,在所有暴风雨期间,行进零阶流域的滞后时间几乎为零。

著录项

  • 来源
    《Hydrological Processes》 |2009年第25期|3631-3638|共8页
  • 作者单位

    Department of Geophysics,Graduate School of Science, Kyoto University, DPRI, Gokasho 611-0011,Uji, Kyoto, Japan;

    Department of Geology, Environmental Science Program, Appalachian State University, Boone, NC, USA;

    Tokyo University of Agriculture and Technology International Environmental and Agricultural Science 3-5-8 Saiwai-cho, Fuchu Tokyo, Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    zero-order basin; forest road; road-runoff; peak flow; antecedent moisture;

    机译:零阶盆地林道径流峰值流量前期水分;

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