Geochemical assessment of fluoride enriched groundwater and health implications from a part of Yavtmal District, India

A comprehensive study was conducted from a semi-arid part of Yavtmal District, Maharashtra, India through combination approaches of geochemical modeling and its health consequences. The groundwater quality assessment shows that 55% of groundwater samples have the concentration of fluoride above the...

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Published inHuman and ecological risk assessment Vol. 26; no. 3; pp. 673 - 694
Main Authors Marghade, Deepali, Malpe, Deepak B., Subba Rao, N., Sunitha, B.
Format Journal Article
LanguageEnglish
Published Boca Raton Taylor & Francis 15.03.2020
Taylor & Francis Ltd
Subjects
Aridity
Calcite
calcium
Calcium carbonate
Cation exchange
Cation exchanging
Chemical precipitation
Computer simulation
Cooking
Dental fluorosis
Dolomite
drinking
feldspar
Fluoride
Fluorides
Fluorite
Fluorosis
geochemical modeling
Geochemistry
Groundwater
Groundwater chemistry
Groundwater quality
Gypsum
Halites
health assessment
hydrochemistry
India
Modelling
monitoring
pollution
Pollution index
pollution index of groundwater
public health
Quality assessment
Quality control
Simulation analysis
simulation models
sodium
Water analysis
Water pollution
Water quality
Water sampling
India
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Abstract A comprehensive study was conducted from a semi-arid part of Yavtmal District, Maharashtra, India through combination approaches of geochemical modeling and its health consequences. The groundwater quality assessment shows that 55% of groundwater samples have the concentration of fluoride above the desirable limit. The high Na + /Ca + ratio (>1.0) suggest the occurrence of cation exchange, which is further supported by Scholler' chloro-alkaline indices. The geochemical modeling reveals that the existence of CaCO 3 precipitation and CaF 2 in groundwater. Simulation analysis indicates the dissolution of calcite, gypsum, and albite and precipitation of dolomite, fluorite, halite, and K-feldspar along with cation exchange as the main water-rock interactions influencing the groundwater chemistry. This is further significantly supported by pollution index of groundwater (PIG). PIG indicates about 18% of total samples fall in very high pollution zone, 3% in high pollution zone, 8% in moderate pollution zone, 24% in low pollution zone, and remaining (47%) express insignificant pollution. The 28% of subject studied have skeletal fluorosis varying from mild to severe type. In different pollution zones, the affected persons by dental fluorosis are varying from 15% to 41%. A proper monitoring and treatment are required for high fluoride water before its use for drinking and cooking.
AbstractList A comprehensive study was conducted from a semi-arid part of Yavtmal District, Maharashtra, India through combination approaches of geochemical modeling and its health consequences. The groundwater quality assessment shows that 55% of groundwater samples have the concentration of fluoride above the desirable limit. The high Na⁺/Ca⁺ ratio (>1.0) suggest the occurrence of cation exchange, which is further supported by Scholler’ chloro-alkaline indices. The geochemical modeling reveals that the existence of CaCO₃ precipitation and CaF₂ in groundwater. Simulation analysis indicates the dissolution of calcite, gypsum, and albite and precipitation of dolomite, fluorite, halite, and K-feldspar along with cation exchange as the main water–rock interactions influencing the groundwater chemistry. This is further significantly supported by pollution index of groundwater (PIG). PIG indicates about 18% of total samples fall in very high pollution zone, 3% in high pollution zone, 8% in moderate pollution zone, 24% in low pollution zone, and remaining (47%) express insignificant pollution. The 28% of subject studied have skeletal fluorosis varying from mild to severe type. In different pollution zones, the affected persons by dental fluorosis are varying from 15% to 41%. A proper monitoring and treatment are required for high fluoride water before its use for drinking and cooking.
A comprehensive study was conducted from a semi-arid part of Yavtmal District, Maharashtra, India through combination approaches of geochemical modeling and its health consequences. The groundwater quality assessment shows that 55% of groundwater samples have the concentration of fluoride above the desirable limit. The high Na + /Ca + ratio (>1.0) suggest the occurrence of cation exchange, which is further supported by Scholler' chloro-alkaline indices. The geochemical modeling reveals that the existence of CaCO 3 precipitation and CaF 2 in groundwater. Simulation analysis indicates the dissolution of calcite, gypsum, and albite and precipitation of dolomite, fluorite, halite, and K-feldspar along with cation exchange as the main water-rock interactions influencing the groundwater chemistry. This is further significantly supported by pollution index of groundwater (PIG). PIG indicates about 18% of total samples fall in very high pollution zone, 3% in high pollution zone, 8% in moderate pollution zone, 24% in low pollution zone, and remaining (47%) express insignificant pollution. The 28% of subject studied have skeletal fluorosis varying from mild to severe type. In different pollution zones, the affected persons by dental fluorosis are varying from 15% to 41%. A proper monitoring and treatment are required for high fluoride water before its use for drinking and cooking.
A comprehensive study was conducted from a semi-arid part of Yavtmal District, Maharashtra, India through combination approaches of geochemical modeling and its health consequences. The groundwater quality assessment shows that 55% of groundwater samples have the concentration of fluoride above the desirable limit. The high Na+/Ca+ ratio (>1.0) suggest the occurrence of cation exchange, which is further supported by Scholler’ chloro-alkaline indices. The geochemical modeling reveals that the existence of CaCO3 precipitation and CaF2 in groundwater. Simulation analysis indicates the dissolution of calcite, gypsum, and albite and precipitation of dolomite, fluorite, halite, and K-feldspar along with cation exchange as the main water–rock interactions influencing the groundwater chemistry. This is further significantly supported by pollution index of groundwater (PIG). PIG indicates about 18% of total samples fall in very high pollution zone, 3% in high pollution zone, 8% in moderate pollution zone, 24% in low pollution zone, and remaining (47%) express insignificant pollution. The 28% of subject studied have skeletal fluorosis varying from mild to severe type. In different pollution zones, the affected persons by dental fluorosis are varying from 15% to 41%. A proper monitoring and treatment are required for high fluoride water before its use for drinking and cooking.
Author Sunitha, B.
Subba Rao, N.
Marghade, Deepali
Malpe, Deepak B.
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  fullname: Marghade, Deepali
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  organization: Department of Applied Chemistry, Priyadarshini Institute of Engineering and Technology
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  givenname: Deepak B.
  surname: Malpe
  fullname: Malpe, Deepak B.
  organization: Department of Geology, R.T.M. Nagpur University
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  surname: Subba Rao
  fullname: Subba Rao, N.
  organization: Department of Geology, Andhra University
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  surname: Sunitha
  fullname: Sunitha, B.
  organization: Department of Civil Engineering, JNT University
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Snippet A comprehensive study was conducted from a semi-arid part of Yavtmal District, Maharashtra, India through combination approaches of geochemical modeling and...
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StartPage 673
SubjectTerms Aridity
Calcite
calcium
Calcium carbonate
Cation exchange
Cation exchanging
Chemical precipitation
Computer simulation
Cooking
Dental fluorosis
Dolomite
drinking
feldspar
Fluoride
Fluorides
Fluorite
Fluorosis
geochemical modeling
Geochemistry
Groundwater
Groundwater chemistry
Groundwater quality
Gypsum
Halites
health assessment
hydrochemistry
India
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Title Geochemical assessment of fluoride enriched groundwater and health implications from a part of Yavtmal District, India
URI https://www.tandfonline.com/doi/abs/10.1080/10807039.2018.1528862
https://www.proquest.com/docview/2375515658
https://www.proquest.com/docview/2431854132
Volume 26
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