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Investigating spatial distribution of fluoride in groundwater with respect to hydro-geochemical characteristics and associated probabilistic health risk in Baruipur block of West Bengal, India.

Authors :
De A
Das A
Joardar M
Mridha D
Majumdar A
Das J
Roychowdhury T
Source :
The Science of the total environment [Sci Total Environ] 2023 Aug 15; Vol. 886, pp. 163877. Date of Electronic Publication: 2023 May 06.
Publication Year :
2023

Abstract

Fluoride (F <superscript>-</superscript> ) enrichment in groundwater of the lower Gangetic plain in West Bengal, India is a major concern. Fluoride contamination and its toxicity were reported earlier in this region; however, limited evidence was available on the precise site of contamination, hydro-geochemical attributions of F <superscript>-</superscript> mobilization and probabilistic health risk caused by fluoridated groundwater. The present study addresses the research gap by exploring the spatial distribution and physico-chemical parameters of fluoridated groundwater along with the depth-wise sedimental distribution of F <superscript>-</superscript> . Approximately, 10 % of the groundwater samples (n = 824) exhibited high F <superscript>-</superscript>  ≥ 1.5 mg/l from 5, out of 19 gram-panchayats and Baruipur municipality area and the maximum F <superscript>-</superscript> was observed in Dhapdhapi-II gram-panchayat with 43.7 % of samples showed ≥1.5 mg/l (n = 167). The distribution patterns of cations and anions in fluoridated groundwater were Na <superscript>+</superscript>  > Ca <superscript>2+</superscript>  > Mg <superscript>2+</superscript>  > Fe > K <superscript>+</superscript> and Cl <superscript>-</superscript>  > HCO <subscript>3</subscript> <superscript>-</superscript>  > SO <subscript>4</subscript> <superscript>2-</superscript>  > CO <subscript>3</subscript> <superscript>2-</superscript>  > NO <subscript>3</subscript> <superscript>-</superscript>  > F <superscript>-</superscript> . Different statistical models like Piper and Gibbs diagram, Chloro Alkaline plot, Saturation index were applied to better understand the hydro-geochemical characteristics for F <superscript>-</superscript> leaching in groundwater. Fluoridated groundwater is of Na-Cl type which implies strong saline character. The intermediate zone between evaporation and rock dominance area controls F <superscript>-</superscript> mobilization along with ion-exchange process occurring between groundwater and host silicate mineral. Furthermore, saturation index proves geogenic activities related to groundwater F <superscript>-</superscript> mobilization. All cations present in sediment samples are closely interlinked with F <superscript>-</superscript> in the depth range of 0-18.3 m. Mineralogical analyses revealed that muscovite is the most responsible mineral for F <superscript>-</superscript> mobilization. The probabilistic health risk assessment disclosed severe health hazard in the order of infants > adults > children > teenagers through F <superscript>-</superscript> tainted groundwater. At P95 percentile dose, all the studied age groups showed THQ >1 from Dhapdhapi-II gram-panchayat. Supply of F <superscript>-</superscript> safe drinking water is required through reliable water supply strategies in the studied area.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2023 Elsevier B.V. All rights reserved.)

Details

Language :
English
ISSN :
1879-1026
Volume :
886
Database :
MEDLINE
Journal :
The Science of the total environment
Publication Type :
Academic Journal
Accession number :
37156382
Full Text :
https://doi.org/10.1016/j.scitotenv.2023.163877