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首页> 外文期刊>Journal of African earth sciences >Groundwater potential zones identification using geoelectrical sounding and remote sensing in Wadi Touil plain, Northwestern Algeria
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Groundwater potential zones identification using geoelectrical sounding and remote sensing in Wadi Touil plain, Northwestern Algeria

机译:地下水潜在地区使用地电气探测和遥感在阿尔及利亚西北部的瓦迪瓦尔平原遥感

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The Wadi Touil plain is situated southwest of Tiaret city; it contains two important localities, Ksar Chellala (Reibell) and Zemalet El Amir Abdelkader (Taguine). This semi-arid region belongs to the western high plains and is characterized by scarce and irregular rainfall. The lack of surface water and the agricultural activities of this region increase the demand for groundwater. Several water boreholes were installed to meet the large water needs; however, these boreholes no longer cover the high demand for water due to the increase in population, increase in irrigated areas, and wear and tear on pumps. Therefore, in order to better define the catchment area and find new sites that meet the water quality and quantity requirements, a geoelectrical survey using the electrical resistivity method was carried out in the Wadi Touil large plain South of Tiaret to investigate the electrical characteristics of sub-surface layering and evaluate the aquifer potentials. Using the Schlumberger array, a total of 127 vertical electrical soundings were conducted along 16 profiles. The recorded data were interpreted quantitatively and qualitatively through the use of isoapparent resistivity maps, geoelectrical pseudosections analysis, and the established geoelectric sections. The results show the presence of three very promising levels; the surface aquifer formed by the Mio-plio-Quaternary terrain (rho = 55 Omega m), the Barremian-Albian-Aptian complex (rho = 300 Omega m), and the Jurassic aquifer (rho = 1200 Omega m). In this study, we determined the extent of these aquifers, their depth and their thickness. These results provide a better understanding of the geology and the deep geo-structure of the region. The remote sensing observations using Sentinel 2A images located the wet lands and provided visual evidence of the evolution of the irrigated areas over time. Finally, according to the study results, the most favorable sites for the establishment of water exploitation boreholes are proposed.
机译:Wadi Touil Plane位于Tiaret City的西南部;它包含两个重要的地方,Ksar Chellala(Reibell)和Zemalet El Amir Abdelkader(Taguine)。该半干旱地区属于西部高平原,其特点是稀缺和不规则的降雨。缺乏地表水和该地区的农业活动增加了对地下水的需求。安装了几个水钻孔以满足大型水需求;然而,由于人口增加,灌溉区域增加,这些钻孔不再覆盖对水的高需求,以及泵上的磨损和撕裂。因此,为了更好地定义集水区,并找到满足水质和数量要求的新网站,使用电阻率法的电气测量在割礼南部的南部南部南部进行了探讨了子的电气特性-surface分层并评估含水层电位。使用Schlumberger阵列,总共127个垂直电探测沿16个型材进行。通过使用异形电阻率图,地电压伪分析和建立的电气切片,定量和定性地解释记录的数据。结果表明存在三个非常有前途的水平;由Mio-Plio-armaternary地区(Rho = 55 omega M)形成的表面含水层,Barremian-Albian-Aptian Complex(Rho = 300 omomega m)和侏罗纪含水层(rho = 1200 omega m)。在这项研究中,我们确定了这些含水层的程度,深度和厚度。这些结果更好地了解该地区的地质和深层地质结构。使用Sentinel 2A图像定位的遥感观察,并提供了随时间灌溉区域演变的视觉证据。最后,根据研究结果,提出了建立水剥削孔的最有利地点。

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