通过形态计量分析研究 Hadejia 河子流域的流域特征:对地下水补给的影响

Mudassir H., Murtala M. R.
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摘要

了解流域的地质水文特性与地形特征及其流动模式的关系,在很大程度上取决于形态计量分析。估算流域的入渗和径流频率及其他水文特征也很有帮助。本研究采用地理信息系统 (GIS) 技术,旨在确定地表形态、地下地质和地下水补给之间的关系。为了进行详细的测量和分析,采用了数字高程模型(DEM)和高分辨率图像进行盆地划分、坡度特征描述、河道网络提取和溪流排序,以得出形态参数的线性、面积和地形。研究结果表明,共有 116 条溪流加入了 4 级溪流,其中 83 条为 1 级溪流,25 条为 2 级溪流,7 条为 3 级溪流,主要干流为 4 级溪流,占地面积为 1486.86 平方公里。溪流网络的排水系统呈树枝状设计。结果进一步表明,溪流频率、渗透数、排水密度、排水质地、过流长度、伸长比和流域起伏值分别为 0.08、0.032、0.41km/km2、0.023、1.22km、0.54 和 28.59m。观测到的线性参数、面积比参数和地形起伏参数值普遍较低。面积和起伏标准值较低,表明该子盆地正处于开发的青年阶段,具有很好的渗透性地下岩层和前景,地下水资源潜力很大。研究结果有助于我们了解水文变量与地貌参数之间的联系,并将其作为指导和/或决策工具,供有关部门制定哈德嘉河子流域内环境友好型增长、供水规划、水资源预算和减灾决策。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Investigation of the Basin Characteristics through Morphometric Analysis of Hadejia River Sub-Basin: Implications for Groundwater Recharge
Understanding the geohydrological properties of a drainage basin in relation to the topographical feature and its flow patterns depends heavily on morphometric analysis. Estimating a watershed's frequency of infiltration and runoff as well as its other hydrological characteristics is also helpful. The study was conducted using Geographical Information System (GIS) techniques with the aim of establishing relationship between surface morphometry, underlying geology and groundwater recharge. For detailed measurement and analysis, Digital Elevation Model (DEM) and high resolution imageries were employed for basin delineation, slope characterization, channel network extraction and stream ordering in order to derive the linear, areal, and relief aspects of morphometric parameters. The findings showed that a total number of 116 streams joined the 4th order stream in which 83 streams were 1st order, 25 streams were 2nd order, 7 streams were 3rd order and the major trunk was 4th order stream, occupied an area of 1486.86km2. The stream network's drainage system exhibits dendritic design. The results further indicate that the values for stream frequency, infiltration number, drainage density, drainage texture, length of overland flow, elongation ratio and basin relief are 0.08, 0.032, 0.41km/km2, 0.023, 1.22km, 0.54 and 28.59m respectively. The observed values of both linear, areal and relief parameters were generally low. Low values for the areal and relief criteria indicates that the sub-basin is at its youthful stage of development and possesses very good permeable subsurface formation and prospect with the possibility of high potential groundwater resources. The result help us understand the connections between hydrological variables and geomorphological parameters as guidance and/or decision-making instruments for the authorities to develop decisions for the environmentally friendly growth of the basin, water supply planning, water budgeting, and disaster mitigation within the Hadejia river sub-basin.
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