首页> 外文期刊>Journal of earth system science >Identification of groundwater prospective zones by using remote sensing and geoelectrical methods in Jharia and Raniganj coalfields, Dhanbad district, Jharkhand state
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Identification of groundwater prospective zones by using remote sensing and geoelectrical methods in Jharia and Raniganj coalfields, Dhanbad district, Jharkhand state

机译:贾坎德邦(Jhankhand)州贾巴德(Jhanaria)贾哈里亚(Jharia)和拉尼甘杰(Raniganj)煤田的遥感和地电方法识别地下水潜在区域

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The Dhanbad district in Jharkhand faces acute water scarcity and is chronically drought-prone. The groundwater resources in the area have not been fully exploited.The present study was undertaken to evaluate the groundwater prospective zones.Landsat-5 Multi Spectral Scanner (MSS)data of band 2 and band 4 and false colour composite (FCC)of band 2,3,4 were interpreted visually to differentiate different hydromorphogeological units and to delineate the major trends of lineaments.The different geomorphic features identi???ed are linear ridges, residual hills,and pediplain,buried pediment and dissected pediplain,besides lineaments.The study shows that the pediplain and buried pediments are promising zones for groundwater prospecting.The occurrence and movement of groundwater is restricted to the unconsolidated material, weathered and fractured rocks.For the selection of tube well sites,geoelectrical resistivity investigations have been carried out at the sites,which were found suitable based on hydro-geomorphological and hydrogeological studies.Twenty-six Vertical Electrical Soundings (VES) have been carried out by using Schlumberger electrode con ???guration,which have brought out 3 to 7 layered sub-surface layers.The resistivity of water-bearing weathered/fractured rocks varies from 120 a€“150 ohmm.The integrated studies have revealed that the blue colour zones are most promising for groundwater exploration and dug wells may be dug up to depths of 30 ?± 5m.
机译:贾坎德邦(Jharkhand)的丹巴德(Dhanbad)地区面临严重的缺水问题,长期干旱多发。该地区的地下水资源尚未得到充分开发。本研究旨在评估地下水的潜在区域。Landsat-5波段2和波段4的多光谱扫描仪(MSS)数据以及波段2的假色合成(FCC)直观地解释了3,4,以区分不同的水文形态学单元并描绘出线状体的主要趋势。确定的不同地貌特征是线性脊,残余丘陵和山地平原,埋山下山岩和解剖的山地平原以及线状体。研究表明,三角洲平原和埋藏的三角洲是有希望的地下水勘探区。地下水的发生和运动仅限于松散的材料,风化和破裂的岩石。为选择管井地点,在该地区进行了地电电阻率研究。根据水文地貌学和水文地质研究,发现了合适的地点。26垂直电测深s(VES)是通过使用斯伦贝谢电极配置进行的,它产生了3至7层次表层。含水的风化/破裂岩石的电阻率在120至150欧姆之间。综合研究表明,蓝色地带最有可能用于地下水勘探,而挖水井的深度可达30±5m。

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