Integrated approach to hydrogeochemical appraisal of groundwater quality concerning arsenic contamination and its suitability analysis for drinking purposes using water quality index

• Published in: Scientific reports 2023-11, Vol.13 (1), p.20455-20455, Article 20455
• Main Authors: Ullah, Zahid, Zeng, Xian-Chun, Rashid, Abdur, Ghani, Junaid, Ali, Asmat, Shah, Muddaser, Zainab, Rimsha, Almutairi, Mikhlid H., Sayed, Amany A., Aleya, Lotfi
• Format: Article
• Language: English
• Subjects: 704/172; 704/242; Anions; Anthropogenic factors; Arsenic; Arsenic - analysis; Calcite; Calcium chloride; Cations; Child; Contamination; Developing countries; Dolomite; Drinking water; Drinking Water - analysis; Environmental Monitoring; Evaporation; Groundwater; Groundwater - analysis; Gypsum; Health risk assessment; Health risks; Humanities and Social Sciences; Humans; LDCs; Magnesium; multidisciplinary; Physicochemical properties; Principal components analysis; Public health; Quality control; Saturation index; Science; Science (multidisciplinary); Sodium chloride; Statistical analysis; Water analysis; Water Pollutants, Chemical - analysis; Water Quality; Water quality assessments; Water resources; Water sampling
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/s41598-023-40105-9

Arsenic (As), contamination in drinking groundwater resources is commonly environmental problem in many developing countries including Pakistan, with significant human health risk reports. In order to examine the groundwater quality concerning As contamination, its geochemical behavior along with physicochemical parameters, 42 samples were collected from community tube wells from District Bahawalpur, Punjab, Pakistan. The results showed the concentration of elevated As, its source of mobilization, and associated public health risk. The As concentration detected in groundwater samples varied from 0.12 to 104 µg/L with an average value of 34.7 µg/L. Among 42 groundwater samples, 27 samples were beyond the permitted limit of 10 µg/L recommended by World Health Organization (WHO), for drinking purposes. Statistical analysis result show that the groundwater cations values are in decreasing order such as: Na +  > Mg 2+  > Ca 2+  > K + , while anions were HCO 3 –  > SO 4 2–  > Cl –  > NO 3 – . Hydrochemical facies result depict that the groundwater samples of the study area, 14 samples belong to CaHCO 3 type, 5 samples belong to NaCl type, 20 samples belong to Mixed CaMgCl type, and 3 samples belong to CaCl 2 type. It can be accredited due to weathering and recharge mechanism, evaporation processes, and reverse ion exchange. Gibbs diagram shows that rock water interaction controls the hydrochemistry of groundwater resources of the study area. Saturation Index (SI) result indicated the saturation of calcite, dolomite, gypsum, geothite, and hematite mineral due their positive SI values. The principal component analysis (PCA) results possess a total variability of 80.69% signifying the anthropogenic and geogenic source of contamination. The results of the exposure-health-risk-assessment method for measuring As reveal significant potential non-carcinogenic risk (HQ), exceeding the threshold level of (> 1) for children in the study area. Water quality assessment results shows that 24 samples were not suitable for drinking purposes.