4.3 Article

Geochemical Modeling Source Provenance, Public Health Exposure, and Evaluating Potentially Harmful Elements in Groundwater: Statistical and Human Health Risk Assessment (HHRA)

出版社

MDPI
DOI: 10.3390/ijerph19116472

关键词

groundwater contamination; carcinogenic; noncarcinogenic risk; spatial distribution; geochemical speciation; mineral phases

资金

  1. King Saud University, Riyadh, Saudi Arabia [RSP-2021/19]
  2. National Natural Science Foundation of China [41521001, 41877204]
  3. 111 Program State Administration of Foreign Experts Affairs and Ministry of Education of China [B18049]
  4. China Postdoctoral Science Foundation [2018M642944]

向作者/读者索取更多资源

Contamination of groundwater by potentially harmful elements (PHEs), originating from the weathering of rock, poses a global public health concern. This study investigated the distribution, source, speciation, and health hazard of PHEs in the groundwater system and mine water of the Adenzai flood plain region in Pakistan, using the human health risk assessment (HHRA) model. The findings suggest that remedial measures are needed to ensure health safety and address public health concerns regarding groundwater sources.
Groundwater contamination by potentially harmful elements (PHEs) originating from the weathering of granitic and gneissic rock dissolution poses a public health concern worldwide. This study investigated physicochemical variables and PHEs in the groundwater system and mine water of the Adenzai flood plain region, in Pakistan, emphasizing the fate distribution, source provenance, chemical speciation, and health hazard using the human health risk assessment HHRA-model. The average concentrations of the PHEs, viz., Ni, Mn, Cr, Cu, Cd, Pb, Co, Fe, and Zn 0.23, were 0.27, 0.07, 0.30, 0.07, 0.06, 0.08, 0.68, and 0.23 mg/L, respectively. The average values of chemical species in the groundwater system, viz., H+, OH-, Ni2+, Mn2+, Mn3+, Cr3+, Cr6+, Cu+, Cu2+, Cd2+, Pb2+, Pb4+, Co2+, Co3+, Fe2+, Fe3+, and Zn2+, were 1.0 x 10(-4) +/- 1.0 x 10(-6), 1.0 x 10(-4) +/- 9.0 x 10(-7), 2.0 x 10(-1) +/- 1.0 x 10(-3), 3.0 x 10(-1) +/- 1.0 x 10(-3), 1.0 x 10(-22) +/- 1.0 x 10(-23), 4.0 x 10(-6) +/- 2.0 x 10(-6), 4.0 x 10(-11) +/- 2.0 x 10(-11), 9.0 x 10(-3) +/- 1.0 x 10(-2), 2.0 x 10(-1) +/- 2.0 x 10(-3), 7.0 x 10(-2) +/- 6.0 x 10(-2), 5.0 x 10(-2) +/- 5.0 x 10(-2), 2.0 x 10(-2) +/- 1.5 x 10(-2), 6.0 x 10(-2) +/- 4.0 x 10(-2), 8.0 x 10(-31) +/- 6.0 x 10(-31), 3.0 x 10(-1) +/- 2.0 x 10(-4), 4.0 x 10(-10) +/- 3.0 x 10(-10), and 2.0 x 10(-1) +/- 1.0 x 10(-1). The mineral compositions of PHEs, viz. Ni, were bunsenite, Ni(OH)(2), and trevorite; Mn viz., birnessite, bixbyite, hausmannite, manganite, manganosite, pyrolusite, and todorokite; Cr viz., chromite and eskolaite; Cu viz., CuCr2O4, cuprite, delafossite, ferrite-Cu, and tenorite; Cd viz., monteponite; Pb viz, crocoite, litharge, massicot, minium, plattnerite, Co viz., spinel-Co; Fe viz., goethite, hematite, magnetite, wustite, and ferrite-Zn; and Zn viz., zincite, and ZnCr2O4 demarcated undersaturation and supersaturation. However, EC, Ca2+, K+, Na+, HCO3-, Cr, Cd, Pb, Co, and Fe had exceeded the WHO guideline. The Nemerow's pollution index (NPI) showed that EC, Ca2+, K+, Na+, HCO3-, Mn, Cd, Pb, Co, and Fe had worse water quality. Principal component analysis multilinear regression (PCAMLR) and cluster analysis (CA) revealed that 75% of the groundwater contamination originated from geogenic inputs and 18% mixed geogenic-anthropogenic and 7% anthropogenic sources. The HHRA-model suggested potential non-carcinogenic risks, except for Fe, and substantial carcinogenic risks for evaluated PHEs. The women and infants are extremely exposed to PHEs hazards. The non-carcinogenic and carcinogenic risks in children, males, and females had exceeded their desired level. The HHRA values of PHEs exhibited the following increasing pattern: Co > Cu > Mn > Zn > Fe, and Cd > Pb > Ni > Cr. The higher THI values of PHEs in children and adults suggested that the groundwater consumption in the entire region is unfit for drinking, domestic, and agricultural purposes. Thus, all groundwater sources need immediate remedial measures to secure health safety and public health concerns.

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