Arid
DOI10.1007/s11356-019-06610-z
High levels of fluoride contamination in groundwater of the semi-arid alluvial aquifers, Pakistan: evaluating the recharge sources and geochemical identification via stable isotopes and other major elemental data
Younas, Ayesha1; Mushtaq, Nisbah1; Khattak, Junaid Ali1; Javed, Tariq2; Rehman, Hafiz Ur3; Farooqi, Abida1
通讯作者Farooqi, Abida
来源期刊ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
ISSN0944-1344
EISSN1614-7499
出版年2019
卷号26期号:35页码:35728-35741
英文摘要Hydrogeochemical methods were integrated to delineate the geochemical factors controlling fluoride (F-) contamination in groundwater at four sites in the districts of Lahore (Samada) and Kasur (Sari Chimba, Kot Maiga, and Chah Fatehwala) in Panjab province of Pakistan. Hydrochemical data and stoichiometric ratios indicate Na-Cl and Na-HCO3 as the dominant water types with silicate weathering influencing overall hydrogeochemistry of the study area. The groundwater F- concentrations ranged between 0.54 mg/L and 17.5 mg/L, with more than 70% samples having F- concentrations above the World Health Organization (WHO) provisional drinking water guideline (1.5 mg/L). Saturation indices determined that 100% samples were saturated with respect to calcite and 96% samples were undersaturated with respect to fluorite, indicating the influence of calcite precipitation on fluoride enrichment. A positive correlation was observed between fluoride with pH, Na+, and HCO3-, confirming that high fluoride concentrations were the result of weathering of silicate minerals and the exchange of OH- on clay surface under the alkaline pH conditions. The isotopic values of delta O-18 and delta H-2 in groundwater ranged from 9.14 to - 5.51 parts per thousand and 56.57 to - 39.5 parts per thousand, respectively. The stable isotope data indicated the meteoric origin of groundwater with some evaporative effect, which is partly influencing groundwater quality such as high pH and salinity, as a result facilitating anion exchange (OH- for F-) on clays surface. The research indicates that the groundwater quality of the study area is not recommendable for drinking due to its high total dissolved solids (TDS) and elevated fluoride concentrations.
英文关键词Fluoride (F-) Geochemistry Saturation indices Stable isotopes Silicate weathering Evaporation
类型Article
语种英语
国家Pakistan ; Japan
收录类别SCI-E
WOS记录号WOS:000507276300040
WOS关键词BEDROCK GROUNDWATER ; ETHIOPIAN RIFT ; THAR DESERT ; RIVER-BASIN ; TAMIL-NADU ; WATER ; AREA ; HYDROGEOCHEMISTRY ; DISTRICT ; PROVINCE
WOS类目Environmental Sciences
WOS研究方向Environmental Sciences & Ecology
EI主题词2019-12-01
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/311259
作者单位1.Quaid I Azam Univ, Fac Biol Sci, Dept Environm Sci, Environm Geochem Lab, Islamabad, Pakistan;
2.Pakistan Inst Nucl Sci & Technol PINSTECH, Isotope Applicat Div, Islamabad, Pakistan;
3.Kagoshima Univ, Grad Sch Sci & Engn, Kagoshima 8900065, Japan
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Younas, Ayesha,Mushtaq, Nisbah,Khattak, Junaid Ali,et al. High levels of fluoride contamination in groundwater of the semi-arid alluvial aquifers, Pakistan: evaluating the recharge sources and geochemical identification via stable isotopes and other major elemental data[J],2019,26(35):35728-35741.
APA Younas, Ayesha,Mushtaq, Nisbah,Khattak, Junaid Ali,Javed, Tariq,Rehman, Hafiz Ur,&Farooqi, Abida.(2019).High levels of fluoride contamination in groundwater of the semi-arid alluvial aquifers, Pakistan: evaluating the recharge sources and geochemical identification via stable isotopes and other major elemental data.ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH,26(35),35728-35741.
MLA Younas, Ayesha,et al."High levels of fluoride contamination in groundwater of the semi-arid alluvial aquifers, Pakistan: evaluating the recharge sources and geochemical identification via stable isotopes and other major elemental data".ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH 26.35(2019):35728-35741.
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