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首页> 外文期刊>Sustainable Water Resources Management >A GIS-based approach in drainage morphometric analysis of Rihand River Basin, Central India
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A GIS-based approach in drainage morphometric analysis of Rihand River Basin, Central India

机译:基于GIS的印度中部Rihand流域排水形态分析方法。

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AbstractThe study on morphometric attributes of the Rihand River Basin (RRB) in Central India was carried out for characterizing the hydrological response behavior using geographic information system (GIS). The RRB supports production of more than 20,000 MW electricity from coal-based thermal power plants. In light of this the management of RRB becomes paramount to sustain the industrial needs and livelihood of more than two million people in the study area. The Rihand River Basin comprises a dendritic drainage pattern where the maximum number of streams was found in the first order and the stream order increased with decrease in stream number. The mean bifurcation ratio was 1.57 which indicates that the drainage pattern is not affected by structural disturbances. The mean value of stream frequency, drainage density and drainage texture was 0.60 km/km2, 0.06 and 0.03, respectively. These characteristics showed dominance of coarse drainage texture, low runoff, low erosional potential, permeable subsurface material, high vegetation cover and low relief. The elongation ratio and form factor were 0.25 and 0.30, respectively, which suggest elongated shape of the basin having a flatter peak of flow for longer duration. Flood flows of such elongated basin are easier to manage and would be helpful in determining the effect of the catchment characteristics on hydrological assessment of the study area. The dominant slopes were east facing indicating high moisture content and low evaporation in the study area. The slope map revealed gentle and moderate nature which are excellent for groundwater recharge in the RRB.
机译: Abstract 印度中部Rihand流域(RRB)的形态特征研究使用地理信息系统(GIS)对水文响应行为进行了表征。 RRB支持从燃煤热电厂生产超过20,000兆瓦的电力。有鉴于此,RRB的管理对于维持研究区域内超过200万人的工业需求和生计至关重要。里汉德河流域包括一个树突状的排水模式,在该树状排水模式中,一线河道的最大数量被发现,并且随着河道数的减少,河道的次序增加。平均分叉率为1.57,表明排水方式不受结构扰动的影响。水流频率,排水密度和排水质地的平均值分别为0.60 km / km <上标> 2 ,0.06和0.03。这些特征显示出主要的排水结构,低径流量,低侵蚀潜力,可渗透的地下物质,高植被覆盖率和低浮雕。伸长率和形状因子分别为0.25和0.30,这表明盆地的拉长形状具有更长的持续时间的较平坦的流量峰值。这种细长盆地的洪水流量易于管理,有助于确定集水特征对研究区水文评估的影响。主坡向东,表明研究区域含水量高,蒸发量低。坡度图显示出温和适中的性质,非常适合RRB中的地下水补给。

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