利用AHP和WIO分析结合地电测量在印度安得拉邦东戈达瓦里地区硬岩地形进行地下水勘探

IF 0.9 Q4 GEOSCIENCES, MULTIDISCIPLINARY
P. V. Rao, M. Subrahmanyam, B. A. Raju
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引用次数: 5

摘要

由于对现有水资源的非司法利用,印度对地下水勘探的需求大大增加。本研究区位于东哥达瓦里地区东高止山脉活动带东经81°52′20.293”~ 82°29′32.058”、北纬17°01′6.71”~ 17°38′12.906”之间。研究区地质背景多样,地形高低不规则。该地区被政府认定为高度落后地区,部落居民居住在这里。为了在研究区寻找良好的含水层,收集了10个参数信息和地电阻率数据。采用层次分析法(AHP)作为决策方法,利用有利于地下水补给、储存和选址的不同主题层(参数)的权重。该分析考虑了地质、地貌、土壤、坡度、线状密度、排水密度、地下水位、土地利用/土地覆盖、降雨量和电性各向异性系数等各主题层(参数)。利用地电资料分析得到的含水层厚度图,编制了地下水综合勘探图,并进行了验证。将整个研究区划分为地下水勘探好、中、差潜力区。地下水良好潜势区面积为750.91平方公里(28.4%),含水层厚度在40 ~ 140 m之间;中等潜势区面积为1220.33平方公里,占研究区总面积的46.1%,含水层厚度约为20 ~ 40 m。其余24.5%的面积为厚度小于20 m的不良含水层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Groundwater exploration in hard rock terrains of East Godavari district, Andhra Pradesh, India using AHP and WIO analyses together with geoelectrical surveys
The need for groundwater exploration in India has been increasing enormously, due to the non-judicial use of available water resources. The present study area is located between longitudes from 81°52′20.293′′ to 82°29′32.058′′ E and latitudes from 17°01′6.71′′ to 17°38′ 12.906′′ N in the Eastern Ghats mobile belt region of East Godavari district. The study area is characterized by a wide range of geological settings and high and irregular topographic features. The area is identified by Government as highly backward and Tribal people dwell here. For exploring good aquifer in the study area, the information of ten parameters together with geoelectrical resistivity data has been collected. Analytical Hierarchy Process (AHP) is used as the decision-making technique which uses the weights of different thematic layers (parameters) favorable for groundwater recharge, storage and location. Various thematic layers (parameters) of geology, geomorphology, soil, slope, lineament density, drainage density, groundwater level, Land use/Land cover, rainfall and coefficient of electrical anisotropy were considered in this analysis. A comprehensive groundwater prospect map has been prepared and validated with aquifer thickness map derived from the analysis of geoelectrical data. The entire study area has been classified into different potential zones of good, moderate and poor for groundwater exploration. The good groundwater potential zone is covering an area of 750.91 sqkm (28.4%) with aquifer thickness varying in the range 40–140 m, moderate potential zone encompasses 46.1% of the study area with an areal extent of 1220.33 sqkm and aquifer thickness is about 20–40 m. The remaining area of 24.5% is poor aquifer zone with thickness less than 20 m.
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来源期刊
AIMS Geosciences
AIMS Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
自引率
7.70%
发文量
31
审稿时长
8 weeks
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