通过水文地质化学调查和多元化学计量统计评估孟加拉国巴格哈特地区的地下水资源

IF 2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Sujan Mallik , Sukhen Goswami , Dhiman Kumer Roy , Md Jakir Hossain , Afroz Jahan , Ayon Saha , Abu Reza Md Towfiqul Islam
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引用次数: 0

摘要

地下水是饮用水和农业用水的主要淡水来源,但由于快速城市化、工业化和气候变 化,孟加拉国南部沿海地区的地下水正日益受到威胁。巴格哈特是沿海地区之一,不仅面临着频繁的热带气旋、低洼地区淹没、盐水入侵等问题,还面临着快速城市化、人口增长、对虾养殖和海产品加工业造成的污染等问题。本研究旨在评估巴格哈特地区地下水的水文地质化学性质及其对饮用水和灌溉的适用性。本研究采用水文地质化学、地理空间和多元统计等综合方法,利用现有深管井(深度约 350 米)中的 90 个地下水样本调查水文地质化学过程和地下水质量。水文地质化学分析确定了主要阳离子和阴离子的浓度,分别为 Na+>Mg2+>Ca2+>K+和 Cl->HCO3->SO42->NO3-。电导率(EC)值从勐拉乡南部的 16,260 μS/cm 到奇塔马里乡最低的 560 μS/cm。研究发现,蒸发-结晶过程是影响研究地区地下水化学性质的主要机制。多变量统计(包括皮尔逊相关矩阵、主成分分析和聚类分析)表明,地下水化学受地质作用的影响。水质指数(WQI)图的空间分布表明,中部和东部地区仅有 15%的地下水样本适合饮用,而研究区则有 85%的地下水样本不适合饮用。此外,对灌溉水水质参数,如钠百分比(Na%)、钠吸附比(SAR)、凯利比(KR)、渗透指数(PI)、镁危害(MH)和盐度危害的评估表明,大多数水井不适合灌溉。研究结果有助于深入了解含水层水文地球化学、地下水质量状况、易受污染地区以及巴格哈特地区地下水管理的可持续安全用水方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of groundwater resources through hydrogeochemical investigation and multivariate chemometric statistics in Bagerhat district, Bangladesh

Groundwater, a primary freshwater source for potable and agricultural uses, is increasingly threatened in southern coastal areas of Bangladesh because of rapid urbanization, industrialization, and climate change. Bagerhat, one of the coastal districts, faces not only frequent tropical cyclones, inundation of low-lying areas, and saline water intrusion but also rapid urbanization, population growth, and pollution from prawn culture and seafood processing industries. The study aims to assess the hydrogeochemistry and the suitability of groundwater based on its significance for potable and irrigation purposes in Bagerhat District. This research includes an integrated approach of hydrogeochemical, geospatial, and multivariate statistical methods to investigate the hydrogeochemical processes and groundwater quality using ninety groundwater samples from existing deep tube wells (around 350 m depth). The hydrogeochemical analysis determined the concentrations of major cations and anions were Na+>Mg2+> Ca2+> K+ and Cl > HCO3- > SO42− > NO3-, correspondingly. Electrical Conductivity (EC) values ranged from 16,260 μS/cm in the southern Mongla Upazila to a minimum of 560 μS/cm in Chitalmari Upazila. The evaporation–crystallization processes were found to be the primary mechanism influencing groundwater chemistry in the study area. Multivariate statistics, including Pearson correlation matrix, principal component analysis (PCA), and cluster analysis, indicated that geogenic processes govern groundwater chemistry. The spatial distribution of the water quality index (WQI) map demonstrated that only 15% of groundwater samples are suitable for drinking in the central and eastern parts, while 85% are unsuitable in the study area. Furthermore, evaluation of irrigation water quality parameters, such as sodium percentage (Na%), sodium adsorption ratio (SAR), Kelly ratio (KR), permeability index (PI), magnesium hazard (MH), and salinity hazard, indicated that most wells are unsuitable for irrigation. The results provide insights into aquifer hydrogeochemistry, groundwater quality status, vulnerable areas of pollution, and sustainable, safe water options for groundwater management in the Bagerhat district.

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