地下水潜力带的勘探:以芬措林为例

Monika Thapa, Kezang Yuden, S. Acharya
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引用次数: 0

摘要

在地表水不足饮用的地方,地下水可以作为替代水源。本报告重点介绍了所有可用于地下水勘探的不同方法,并考虑到各种参数,如经济性,适用性,准确性等,分析了这种不同的勘探方法,从而为个人提供了在地下水潜在带勘探过程中选择特定方法的各种选择。考虑到该仪器在地质和矿业部(DGM)的可用性以及我们项目中的经济因素,我们使用地震折射层析成像(SRT)和地理信息系统(GIS)来划定不丹Phuentsholing地下水的潜在区域。GIS侧重于地表特征作为地下水指标,SRT侧重于地下水次表层和深度的识别。还收集了研究区域现有井的各种信息,以验证通过地面和地下方法开发的潜在层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Exploration of Groundwater Potential Zones: A Case Study In Phuentsholing
In places where surface water sources are insufficient for drinking purpose, groundwater serves as an alternative source. This report highlights all the different methods that can be used for exploration of the groundwater and to analyse this different exploration methods considering various parameters such as economy, suitability, accuracy, etc, hence providing an individual with various choices regarding the selection of particular method during the exploration of groundwater potential zone. Considering the availability of the instrument in Department of Geology and Mines (DGM) and the economic factor in our project, seismic refraction Tomography (SRT) and Geographical Information System (GIS) was used to delineate the potential zones of groundwater in Phuentsholing, Bhutan. GIS focuses on the surface features for groundwater indicator while SRT identify the subsurface layers and the depth of groundwater. The various information regarding existing bore well in the study area were also collected to validate the potential zones developed both by surface and subsurface method.
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