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首页> 外文期刊>Arabian journal of geosciences >Geomorphological and geophysical information system analysis of major rainwater-harvesting basins in Al-Baha region, Saudi Arabia
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Geomorphological and geophysical information system analysis of major rainwater-harvesting basins in Al-Baha region, Saudi Arabia

机译:沙特阿拉伯巴哈地区主要雨水收集盆地的地貌和地球物理信息系统分析

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摘要

In the present study, a morphometric and geophysical analysis of three major rainwater-harvesting basins in Al-Baha province, Saudi Arabia, has been carried out using geographical information system (GIS) techniques and geophysical analysis. GIS techniques aimed to create a spatial database for three basins, and it was used to determine most of the morphometric parameters and stream attributes. The morphometric analysis revealed that the maximum elevation in the basins upper stream is about 2350, 2230, and 2450 m above sea level for Al-aqiq, Medhas, and Mathalmat basin, respectively. The maximum elevation decreases with steep slopes in the three basins toward the dams' site. The general flow direction of the streams in Al-aqiq basin goes from southwest to northeast following the main direction of the Arabian Shield structure; in Medhas basin, flow goes from south to north with wide flat areas in the downstream portion of the basin and near dam site and from southeast to west for Mathalamt basin. The morphometric parameters of Al-aqiq basin imply that the basin has the largest area with about 309 km(2); the perimeter is about 119 km and the total stream length is about 533 km. Medhas basin comes as a second largest area with 278 km(2); the perimeter is about 110 km and the total stream length is about 477 km. While Mathalamt basin has an area of about 220 km(2), the perimeter is about 104 km and the total stream length is about 374 km. The three basins have medium drainage density with a value of 1.72 km(-1) for Al-aqiq and 1.7 km(-1) for Medhas and Mathalamat basins. A relief ratio of 0.1 in Al-aqiq basin, 0.08 in Medhas basin, and 0.12 in Mathalamt basin was noticed. These ratios indicate a high permeable landscape in Al-aqiq and Mathalamt basins while there is a medium permeable landscape in Medhas basin. Al-aqiq and Mathalamt basins have a similar elongation and circularity of 0.73 and 1.85, and 0.73 and 1.8, respectively, which indicates that the two basins have fairly elongated shape, while elongation and circularity is estimated at 0.62 and 2.56 for Medhas basin, respectively. Drainage pattern of Al-aqiq and Medhas basins has a high dendritic shape, while Mathalamt basin has a simple dendritic shape. The geophysical survey was performed using vertical electrical sounding (VES) resistivity. The geophysical analysis reflected the presence of several different layers of resistance. High resistance was more than 2000 a"broken vertical bar at a 2-m depth due to dry river sediments in the dams' location while in other areas because of the presence of the basement rocks and climatic change. These results confirm the output of the geological study and give an indication of the state of recharge and rainwater harvesting in the three basins.
机译:在本研究中,已使用地理信息系统(GIS)技术和地球物理分析方法对沙特阿拉伯Al-Baha省的三个主要雨水收集盆地进行了形态学和地球物理分析。 GIS技术旨在为三个盆地创建一个空间数据库,并用于确定大多数形态参数和河流属性。形态分析表明,Al-aqiq,Medhas和Mathalmat盆地的盆地上游最高海拔分别为2350、2230和2450 m。在三个盆地中,向坝址倾斜的最大坡度使最高海拔降低。 Al-aqiq盆地的水流一般沿阿拉伯盾构架的主要方向从西南向东北方向流动。在Medhas盆地,水流从南向北流动,流域下游,坝址附近平坦区域宽广,Mathalamt盆地从东南向西流动。 Al-aqiq盆地的形态参数表明该盆地面积最大,约为309 km(2)。周长约119公里,溪流总长约533公里。 Medhas盆地面积278 km(2),位居第二。周长约110公里,总流长约477公里。 Mathalamt盆地的面积约为220 km(2),而周长约为104 km,总河流长度约为374 km。这三个盆地的排水密度中等,Al-aqiq盆地的排水密度为1.72 km(-1),Medhas和Mathalamat盆地的排水密度为1.7 km(-1)。 Al-aqiq盆地的浮雕比率为0.1,Medhas盆地的浮雕比率为0.08,Mathalamt盆地的浮雕比率为0.12。这些比率表明Al-aqiq和Mathalamt盆地具有高渗透性景观,而Medhas盆地则具有中等渗透性景观。 Al-aqiq和Mathalamt盆地的伸长率和圆形度分别相似,分别为0.73和1.85,以及0.73和1.8,这表明两个盆地具有相当长的形状,而Medhas盆地的伸长率和圆形度分别为0.62和2.56。 。 Al-aqiq和Medhas盆地的排水模式具有较高的树枝状形状,而Mathalamt盆地具有简单的树枝状形状。地球物理调查是使用垂直电声(VES)电阻率进行的。地球物理分析反映了几个不同电阻层的存在。由于坝体位置河干沉积物的干燥,而在其他地区则由于基底岩的存在和气候变化,因此在2 m深度处2000英寸高的“垂直竖条断裂”。这些结果证实了该坝的产出。地质研究,并指出这三个盆地的补给和雨水收集状态。

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