Shamim Ahmed , Khondaker Emamul Haque , Md. Moniruzzaman , Most. Afroza Khatun Suborna , Tasnim Abdary Anonna , Md. Abdul Quaiyum Bhuyian , Md. Ariful Ahsan , Abdul Hadi Al Nafi Khan , Md. Masud Karim , M.A. Kasem
{"title":"孟加拉国干旱易发地区地下水的水文地球化学、水质和潜在人类健康风险评估","authors":"Shamim Ahmed , Khondaker Emamul Haque , Md. Moniruzzaman , Most. Afroza Khatun Suborna , Tasnim Abdary Anonna , Md. Abdul Quaiyum Bhuyian , Md. Ariful Ahsan , Abdul Hadi Al Nafi Khan , Md. Masud Karim , M.A. Kasem","doi":"10.1016/j.gsd.2025.101450","DOIUrl":null,"url":null,"abstract":"<div><div>The intensifying issue of water contamination poses a growing threat in developing, industrialized, and agricultural regions, endangering the environment, human health, and economic development. Therefore, understanding the recharge mechanisms, hydrogeochemistry, water quality, and groundwater risk assessment is crucial for effective water resource management. Forty-five water samples were analyzed for their isotopic and chemical compositions to evaluate the sources of recharge and suitability. The study area is divided into the Younger Ganges Floodplain (YGF), Older Mahananda Floodplain (OMF), and Pleistocene Barind Tract (BT), which exhibit heterogeneous aquifer thicknesses, subsurface geology, and varying recharge dynamics. Cation concentrations followed the order of Ca<sup>2+</sup>>Na<sup>+</sup>>Mg<sup>2+</sup>>K<sup>+</sup>, while the dominant anions were HCO<sub>3</sub><sup>−</sup> > Cl<sup>−</sup> > SO<sub>4</sub><sup>2−</sup> > NO<sub>3</sub><sup>−</sup> > NO<sub>2</sub><sup>−</sup>. Most parameters were within standard limits, where elevated concentrations were attributed to <strong>natural processes (e.g., silicate weathering, cation exchange, and carbonate dissolution)</strong> and <strong>anthropogenic sources (e.g., fertilizer use and sewage leakage).</strong> Isotopic analysis revealed active rainfall recharge in the YGF aquifer, while the BT demonstrated no recent recharge, likely due to the presence of a thick, impermeable clay layer. The OMF, on the other hand, exhibited both recently recharged and stagnant water, reflecting spatial heterogeneity in aquifer characteristics. Piper and Chadha diagrams classified the groundwater as Ca<sup>2+</sup>–Mg<sup>2+</sup>–HCO<sub>3</sub><sup>-</sup> type, indicating temporary hardness. Hydrogeochemistry was predominantly influenced by ion exchange, rock-water interactions, and the dissolution of calcite and dolomite. The Entropy Water Quality Index (EWQI) values revealed good water quality in BT, unsuitability in YGF, and good to poor quality in OMF. Non-carcinogenic health risk assessments revealed arsenic as the highest risk, followed by NO<sub>2</sub><sup>−</sup>, NO<sub>3</sub><sup>−</sup>, Mn, and Fe, with children facing greater exposure than other groups. Non-carcinogenic risk limits were exceeded in 53.33 % of samples for both children and females and in 33.33 % for males. To mitigate these risks, strategies should focus on improved agricultural practices, reduced fertilizer application, modified irrigation methods, and public awareness campaigns. This study provides valuable insights into groundwater conditions in Chapai Nawabganj, contributing to sustainable water resource management and the protection of public health.</div></div>","PeriodicalId":37879,"journal":{"name":"Groundwater for Sustainable Development","volume":"29 ","pages":"Article 101450"},"PeriodicalIF":4.9000,"publicationDate":"2025-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Hydrogeochemistry, water quality, and potential human health risk assessment of groundwater in a drought-prone area, Bangladesh\",\"authors\":\"Shamim Ahmed , Khondaker Emamul Haque , Md. Moniruzzaman , Most. Afroza Khatun Suborna , Tasnim Abdary Anonna , Md. Abdul Quaiyum Bhuyian , Md. Ariful Ahsan , Abdul Hadi Al Nafi Khan , Md. Masud Karim , M.A. Kasem\",\"doi\":\"10.1016/j.gsd.2025.101450\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The intensifying issue of water contamination poses a growing threat in developing, industrialized, and agricultural regions, endangering the environment, human health, and economic development. Therefore, understanding the recharge mechanisms, hydrogeochemistry, water quality, and groundwater risk assessment is crucial for effective water resource management. Forty-five water samples were analyzed for their isotopic and chemical compositions to evaluate the sources of recharge and suitability. The study area is divided into the Younger Ganges Floodplain (YGF), Older Mahananda Floodplain (OMF), and Pleistocene Barind Tract (BT), which exhibit heterogeneous aquifer thicknesses, subsurface geology, and varying recharge dynamics. Cation concentrations followed the order of Ca<sup>2+</sup>>Na<sup>+</sup>>Mg<sup>2+</sup>>K<sup>+</sup>, while the dominant anions were HCO<sub>3</sub><sup>−</sup> > Cl<sup>−</sup> > SO<sub>4</sub><sup>2−</sup> > NO<sub>3</sub><sup>−</sup> > NO<sub>2</sub><sup>−</sup>. Most parameters were within standard limits, where elevated concentrations were attributed to <strong>natural processes (e.g., silicate weathering, cation exchange, and carbonate dissolution)</strong> and <strong>anthropogenic sources (e.g., fertilizer use and sewage leakage).</strong> Isotopic analysis revealed active rainfall recharge in the YGF aquifer, while the BT demonstrated no recent recharge, likely due to the presence of a thick, impermeable clay layer. The OMF, on the other hand, exhibited both recently recharged and stagnant water, reflecting spatial heterogeneity in aquifer characteristics. Piper and Chadha diagrams classified the groundwater as Ca<sup>2+</sup>–Mg<sup>2+</sup>–HCO<sub>3</sub><sup>-</sup> type, indicating temporary hardness. Hydrogeochemistry was predominantly influenced by ion exchange, rock-water interactions, and the dissolution of calcite and dolomite. The Entropy Water Quality Index (EWQI) values revealed good water quality in BT, unsuitability in YGF, and good to poor quality in OMF. Non-carcinogenic health risk assessments revealed arsenic as the highest risk, followed by NO<sub>2</sub><sup>−</sup>, NO<sub>3</sub><sup>−</sup>, Mn, and Fe, with children facing greater exposure than other groups. Non-carcinogenic risk limits were exceeded in 53.33 % of samples for both children and females and in 33.33 % for males. To mitigate these risks, strategies should focus on improved agricultural practices, reduced fertilizer application, modified irrigation methods, and public awareness campaigns. 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Hydrogeochemistry, water quality, and potential human health risk assessment of groundwater in a drought-prone area, Bangladesh
The intensifying issue of water contamination poses a growing threat in developing, industrialized, and agricultural regions, endangering the environment, human health, and economic development. Therefore, understanding the recharge mechanisms, hydrogeochemistry, water quality, and groundwater risk assessment is crucial for effective water resource management. Forty-five water samples were analyzed for their isotopic and chemical compositions to evaluate the sources of recharge and suitability. The study area is divided into the Younger Ganges Floodplain (YGF), Older Mahananda Floodplain (OMF), and Pleistocene Barind Tract (BT), which exhibit heterogeneous aquifer thicknesses, subsurface geology, and varying recharge dynamics. Cation concentrations followed the order of Ca2+>Na+>Mg2+>K+, while the dominant anions were HCO3− > Cl− > SO42− > NO3− > NO2−. Most parameters were within standard limits, where elevated concentrations were attributed to natural processes (e.g., silicate weathering, cation exchange, and carbonate dissolution) and anthropogenic sources (e.g., fertilizer use and sewage leakage). Isotopic analysis revealed active rainfall recharge in the YGF aquifer, while the BT demonstrated no recent recharge, likely due to the presence of a thick, impermeable clay layer. The OMF, on the other hand, exhibited both recently recharged and stagnant water, reflecting spatial heterogeneity in aquifer characteristics. Piper and Chadha diagrams classified the groundwater as Ca2+–Mg2+–HCO3- type, indicating temporary hardness. Hydrogeochemistry was predominantly influenced by ion exchange, rock-water interactions, and the dissolution of calcite and dolomite. The Entropy Water Quality Index (EWQI) values revealed good water quality in BT, unsuitability in YGF, and good to poor quality in OMF. Non-carcinogenic health risk assessments revealed arsenic as the highest risk, followed by NO2−, NO3−, Mn, and Fe, with children facing greater exposure than other groups. Non-carcinogenic risk limits were exceeded in 53.33 % of samples for both children and females and in 33.33 % for males. To mitigate these risks, strategies should focus on improved agricultural practices, reduced fertilizer application, modified irrigation methods, and public awareness campaigns. This study provides valuable insights into groundwater conditions in Chapai Nawabganj, contributing to sustainable water resource management and the protection of public health.
期刊介绍:
Groundwater for Sustainable Development is directed to different stakeholders and professionals, including government and non-governmental organizations, international funding agencies, universities, public water institutions, public health and other public/private sector professionals, and other relevant institutions. It is aimed at professionals, academics and students in the fields of disciplines such as: groundwater and its connection to surface hydrology and environment, soil sciences, engineering, ecology, microbiology, atmospheric sciences, analytical chemistry, hydro-engineering, water technology, environmental ethics, economics, public health, policy, as well as social sciences, legal disciplines, or any other area connected with water issues. The objectives of this journal are to facilitate: • The improvement of effective and sustainable management of water resources across the globe. • The improvement of human access to groundwater resources in adequate quantity and good quality. • The meeting of the increasing demand for drinking and irrigation water needed for food security to contribute to a social and economically sound human development. • The creation of a global inter- and multidisciplinary platform and forum to improve our understanding of groundwater resources and to advocate their effective and sustainable management and protection against contamination. • Interdisciplinary information exchange and to stimulate scientific research in the fields of groundwater related sciences and social and health sciences required to achieve the United Nations Millennium Development Goals for sustainable development.