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首页> 外文期刊>Journal of the Geological Society of India >Conjunctive Use of Well-Log and Remote Sensing Data for Interpreting Shallow Aquifer Geometry in Ganga Plains
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Conjunctive Use of Well-Log and Remote Sensing Data for Interpreting Shallow Aquifer Geometry in Ganga Plains

机译:结合使用测井和遥感数据解释恒河平原浅层含水层的几何形状

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摘要

Study of aquifer geometry is essential for proper development and utilization of groundwater resources. In this study, a systematic approach has been made in the analysis of shallow aquifer geometry in the western Ganga Plains, Uttar Pradesh, by integrating the well-log and remote sensing data. The study includes mapping of neotectonic lineaments from remote sensing data, and determination of aquifer depth and lithological details from the well-log data. The well-log data indicate that the region has varying thickness of alluvium composed of alternating sand, kankar and clay strata. By integrating the remote sensing and well-log data sets, sub-surface geological sections have been developed to interpret the aquifer geometry. The aquifers are found to show significant variation in nature and geometry from place to place. At some places, the lineaments on remote sensing images are in conformity with faults interpreted from well-log data, whereas at others, buried faults have been interpreted. The aquifers formed by paleochannels is particularly striking, being unconfined in nature and mainly consisting of medium to coarse sand, along with pebbles, cobbles and kankar.
机译:研究含水层的几何形状对于正确开发和利用地下水至关重要。在这项研究中,通过整合测井和遥感数据,在北方恒河平原甘加平原西部浅层含水层的几何形状分析中已经采取了系统的方法。该研究包括根据遥感数据绘制新构造地貌,并根据测井数据确定含水层深度和岩性细节。测井资料表明,该地区的冲积层厚度各不相同,由交替的砂,坎卡岩和粘土地层组成。通过整合遥感和测井数据集,开发了地下地质剖面来解释含水层的几何形状。发现该含水层在不同地方的自然和几何形状上显示出显着变化。在某些地方,遥感影像上的线条与根据测井数据解释的断层相符,而在其他地方,已解释了隐伏的断层。由古河道形成的含水层特别引人注目,自然界无限制,主要由中等至粗砂以及卵石,鹅卵石和坎卡岩构成。

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