利用基于 GIS 的模糊化 AHP 进行多标准地下水潜力分区:尼日利亚西南部翁多市案例研究

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Olumuyiwa Olusola Falowo , Olajumoke Ojo
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引用次数: 0

摘要

该研究利用模糊分析层次过程(F-AHP)对与地下水潜力/产量相关的七个重要水文地质参数进行了多标准决策分析。目的是利用地下水潜能指数值 (GWPIV) 绘制尼日利亚西南部翁多市的地下水潜能图。利用 F-AHP,对水文地质参数进行了优先排序,并根据其重要程度分层赋予不同权重,如含水层厚度(0.05)、含水层电阻率(0.04)、覆盖层厚度(0.12)、横向阻力(0.18)、渗透率(0.32)、各向异性系数(0.25)和形成系数(0.03)。从区域角度看,根据排水流域和河网,该区域被归类为地下水产量低/中等,水流连通性中等到高。一般来说,北部和南部地区海拔较高,海拔较低,因此水流有可能流向南部,北部形成分水岭。此外,纵向单元电导率的区域平均值为 1.168,而花岗岩、片麻岩和辉绿岩的电导率分别为 1.20、1.16 和 1.10,这表明该地区易受污染的程度为中等。覆盖层厚度、导水率、透射率、横向阻力、成岩系数、各向异性系数、断裂对比度和反射系数的平均值分别为 22.5 米、0.33 米/天、5.56 平方米/天、4966 欧姆-平方米、2.42、1.17、15.3 和 0.66。地下水位含水层和断裂基底是该地区的主要含水单元,而各地质单元显示出重叠的水文地质特性。获得的全球升温潜能值从 1.21 到 3.55 不等,区域平均值为 1.86,表明潜力适中。然而,南部地区比北部地区显示出更大的潜力/产量。这项研究表明,涉及模糊分析层次过程的地理空间制图技术在地下水评价中非常重要,因为它能够解决和获得不同的水文地质参数,并将这些参数综合起来,优先考虑和确定该地区的地下水丰度,以改善、扩大和管理研究地区的现有供水计划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multi-criteria groundwater potential zonation using GIS-based fuzzified AHP: Case study of Ondo metropolis Southwestern Nigeria

The study utilized the fuzzy analytical hierarchical process (F-AHP) in the multicriteria decision analysis of seven important hydrogeologic parameters associated with groundwater potentiality/yield. The purpose was to develop groundwater potential map using groundwater potential index values (GWPIV) for Ondo metropolis, Southwestern Nigeria. The hydrogeologic parameters were prioritize and assigned different weights hierarchically according to their level of importance using F-AHP, as aquifer layer thickness (0.05), aquifer layer resistivity (0.04), overburden thickness (0.12), transverse resistance (0.18), transmissivity (0.32), coefficient of anisotropy (0.25), and formation factor (0.03). From regional perspective, based on drainage basin, and river network, the region was categorized to be of low/moderate groundwater yield, with moderate to high flow connectivity. The higher and lower elevations are generally remarkable in the northern and southern areas respectively, hence possibility of movement of water towards the southern part with the northern forming the watershed. Furthermore, the longitudinal unit conductance recorded regional average value of 1.168, while 1.20, 1.16, and 1.10 were recorded for granite, gneiss and migmatite, which suggests moderate vulnerability to contamination. The average values recorded for overburden thickness, hydraulic conductivity, transmissivity, transverse resistance, formation factor, coefficient of anisotropy, fracture contrast, and reflection coefficient are 22.5 m, 0.33 m/d, 5.56 m2/d, 4966 ohm-m2, 2.42, 1.17, 15.3, and 0.66 respectively. The water table aquifer and the fractured basement are the major water bearing units in the area; while the geological units showed overlapping hydrogeologic properties. The obtained GWPIV ranged from 1.21 to 3.55 with regional average of 1.86, suggesting a moderate potential. Nevertheless, the southern part showed more propensity/yield than the northern area. The study showed the importance of geospatial mapping technique, involving fuzzy analytical hierarchical process, in groundwater evaluation, as it was able to solve and obtain different hydrogeological parameters, which were integrated to prioritize and define the area's groundwater prolificacy for the purpose of improving, expanding, and management of the existing water scheme in the study area.

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来源期刊
Solid Earth Sciences
Solid Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
5.00%
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20
审稿时长
103 days
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