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评估孟加拉国西北部的砷污染:基于地理信息系统的地下水脆弱性及对人类健康影响的评估

Evaluating arsenic contamination in northwestern Bangladesh: A GIS-Based assessment of groundwater vulnerability and human health impacts.

作者信息

Habib Md Ahsan, Reza A H M Selim, Hasan Md Irfanul, Ahsan Md Aminul, Moniruzzaman Md, Hasan Asma Binta, Shofi Shofiul Islam, Hridoy Kayesh Mahmud

机构信息

Department of Geology and Mining, University of Rajshahi, Bangladesh.

Institute of National Analytical Research and Service (INARS), Bangladesh Council of Scientific and Industrial Research (BCSIR), Dhanmondi, Dhaka, 1205, Bangladesh.

出版信息

Heliyon. 2024 Mar 16;10(6):e27917. doi: 10.1016/j.heliyon.2024.e27917. eCollection 2024 Mar 30.

Abstract

One of the biggest environmental worries in the world today is the risk of arsenic (As) contamination in groundwater. The Atomic Absorption Spectrometer (AAS) was used in this work to assess the As content in groundwater samples from 38 shallow (27 m) tubewells in northwest Bangladesh to determine the existing situation, potential source(s), and likely health risk of As and other important water quality parameters. The range of arsenic concentrations (μgL) was troublesome and greater than the WHO recommended level for drinking water, ranging from 0.50 to 164 (mean ± SD: 20.22 ± 36.46). In groundwater, the concentrations of Fe, and Mn vary from 0.04 to 52.75 mgL (mean ± SD: 4.23 ± 9.68), and 0.23 to 3.27 mgL (mean ± SD: 1.10 ± 0.67). The obtained groundwater samples have pH values ranging from 5.9 to 7.1, which indicates a somewhat acidic to neutral character. Major cations have an average abundance that is as follows: Ca > Mg > Na > K, while major anions have an average abundance that is as follows: HCO > Cl > SO > NO; Ca and HCO are the main cation and anion, respectively. The groundwater in the Rajarampur village was deemed unfit for drinking or irrigation based on analyses of water quality performed using the entropy water quality index. The Ca-HCO type of water, in which Ca and HCO are the main positive ions and negative ions, is suggested by the Piper tri-linear diagram. It was discovered that silicate weathering regulates the hydro-geochemical activities in groundwater using a bi-variate examination of several hydro-chemical variables. Four major clusters were observed for the water sample. According to reductive dissolution processes and principal component analysis, the arsenic in groundwater is geogenic in origin. Arsenic is discharged from sediment to groundwater by reductive dissolution of FeOOH and MnOOH, as shown by the modest connection between As, Fe, and Mn. The United Nations Environmental Protection Agency's (USEPA) suggested value for probable cancer risk assessment was 10, however the probable cancer risk assessment found a higher value, indicating that the population in the study region was at high risk for cancer. Remedial measures for arsenic mitigation include removing arsenic from groundwater after it is extracted, searching for alternative aquifers, and implementing various water-supply technologies such as dugwells, deep tubewells, pond-sand filters, and rainwater harvesting systems.

摘要

当今世界最大的环境问题之一是地下水中砷污染的风险。本研究使用原子吸收光谱仪(AAS)评估了孟加拉国西北部38口浅(27米)管井的地下水样本中的砷含量,以确定砷及其他重要水质参数的现状、潜在来源和可能的健康风险。砷浓度范围(μg/L)令人担忧,高于世界卫生组织推荐的饮用水水平,范围为0.50至164(平均值±标准差:20.22±36.46)。地下水中铁和锰的浓度分别为0.04至52.75mg/L(平均值±标准差:4.23±9.68)和0.23至3.27mg/L(平均值±标准差:1.10±0.67)。所采集的地下水样本pH值在5.9至7.1之间,呈弱酸性至中性。主要阳离子的平均丰度顺序为:Ca>Mg>Na>K,主要阴离子的平均丰度顺序为:HCO>Cl>SO>NO;Ca和HCO分别是主要阳离子和阴离子。根据熵水质指数对水质进行分析,拉贾兰布尔村的地下水被认为不适合饮用或灌溉。派珀三线图显示,水的类型为Ca-HCO型,其中Ca和HCO分别是主要的阳离子和阴离子。通过对多个水化学变量的双变量分析发现,硅酸盐风化作用控制着地下水中的水文地球化学活动。水样观察到四个主要聚类。根据还原溶解过程和主成分分析,地下水中的砷源于地质成因。砷通过FeOOH和MnOOH的还原溶解从沉积物中释放到地下水中,这从砷、铁和锰之间的适度相关性可以看出。联合国环境保护局(USEPA)建议的可能癌症风险评估值为10,但实际可能癌症风险评估得出了更高的值,这表明研究区域的人群面临较高的癌症风险。减轻砷污染的补救措施包括在抽取地下水后去除砷、寻找替代含水层以及采用各种供水技术,如挖掘井、深管井、池塘砂滤器和雨水收集系统。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4dba/10963321/8705d4ea11f7/gr1.jpg

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