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Identifying Dominant Runoff Processes at a Regional Scale – A GIS - Based Approach

机译:在区域范围内确定主要径流过程–基于GIS的方法

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Identifying landscapes with similar hydrological characteristics is useful for the determination of dominant runoff process (DRP) and flood prediction. Several approaches used for DRP-mapping differ in respect to time and data requirement. Manual approaches based on field investigation and expert knowledge are time consuming and difficult to implement at regional scale. Automatic GIS-based approach on the other hand require simplification of data but are easier to implement and it is applicable on regional scale. In this study, GIS-based automated approach was used to identify the DRPs in Anambra area. The result showed that Hortonian Overland Flow (HOF) has the highest coverage of 1508.3 Km2 (33.5%) followed by Deep Percolation (DP) with coverage of 1455.3 Km2 (32.3%). Subsurface Flow (SSF) is the third dominant runoff process covering 920.6 Km2 (20.4%) while Saturated Overland Flow (SOF) covers the least area of 618.4 Km2 (13.7%) of the study area. The result reveal that considerable amount of precipitated water would be infiltrated into the subsurface through deep percolation process contributing to groundwater recharge in the study area. However, it is envisaged that HOF and SOF will continue to increase due to the continuous expansion of built-up area. With the expected increase in HOF and SOF and the change in rainfall pattern associated with perpetual problem of climate change, it is paramount that groundwater conservation practices be considered to ensure continued sustainable utilization of groundwater in the study area.
机译:识别具有相似水文特征的景观对于确定主要径流过程(DRP)和洪水预报很有用。用于DRP映射的几种方法在时间和数据要求方面有所不同。基于现场调查和专家知识的手动方法非常耗时,并且难以在区域范围内实施。另一方面,基于GIS的自动方法需要简化数据,但易于实现,并且适用于区域规模。在这项研究中,基于GIS的自动方法用于识别Anambra地区的DRP。结果表明,霍顿溢流(HOF)的最高覆盖率为1508.3 Km 2 (33.5%),其次是深层渗滤(DP),覆盖率为1455.3 Km 2 ( 32.3%)。地表下径流(SSF)是第三大径流过程,覆盖面积920.6 Km 2 (20.4%),而饱和陆上径流(SOF)覆盖的面积最小,为618.4 Km 2 (13.7 %)的研究区域。结果表明,大量的沉淀水将通过深层渗滤过程渗入地下,从而有助于研究区域的地下水补给。但是,可以预见,由于建筑面积的不断扩大,HOF和SOF将继续增加。随着HOF和SOF的预期增加以及与气候变化的永久性问题相关的降雨模式的变化,考虑地下水保护措施以确保研究区域对地下水的持续可持续利用至关重要。

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