том 368 страницы 125694

Hydrochemical facies distribution, controlling mechanisms and Natural background concentrations of major pollutants in Ganga-Yamuna Interfluve Aquifer, India

Тип публикацииJournal Article
Дата публикации2025-03-01
scimago Q1
wos Q1
БС1
SJR2.205
CiteScore16.0
Impact factor7.3
ISSN02697491, 18736424
Краткое описание
Evolution of groundwater genesis in Central Ganga Plain (CGP) is scrutinized with due consideration of hydrochemical and hydrodynamic environment within Quaternary alluviums. Wide variation in hydrochemical facies in CGP indicates a dynamic hydro-geochemical environment influenced from the seasonal rainfall, return flows, canal seepages, and anthropogenic activities. The Ca-HCO3 facies retaining meteoric nature is characterized by shallow water levels, high recharge rate, high hydraulic conductivity, low salinity and trace elemental load. A noticeable increase in salinity and trace elemental load is reported as groundwater evolved from Ca-HCO3 to Ca-Mg-HCO3, Ca-Mg-Cl-SO4, Ca-Na-HCO3 type and Na-Cl-SO4 types. The hydrochemical facies and bivariate plots infer Silicate and Carbonate weathering in a redox-ion exchange environment. The varying concentrations of radio-nuclides like U and Th in different hydrochemical facies depicts the migration attributed to oxidizing-reducing environment and acid-alkaline conditions. Aquifer heterogeneity and spatial variability of groundwater recharge sources including rainfall, return flows, canal seepages imparts changes that make it difficult to appoint sources. The shallow groundwater recharge zones are depleted in heavier isotopes (δ1⁸O: 12‰ to −7‰) advocating recharge primarily from precipitation and surface water. The concomitant occurrences of HCO3, Sr, and SiO2 ascribe genesis from geogenic source more precisely the silicate weathering. Reverse geochemical modelling shows that groundwater is saturated with chalcedony, quartz, barite, talc and under-saturated with anhydrite, gypsum, halite, and sylvite. Analyses including contamination evolution and PPI, point that NO3, Cl, SO4, Sr, As, Mn are common pollutants stemming particularly from agricultural activities and industrial effluents pose a serious threat to groundwater sustainability.
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Ahmad I. et al. Hydrochemical facies distribution, controlling mechanisms and Natural background concentrations of major pollutants in Ganga-Yamuna Interfluve Aquifer, India // Environmental Pollution. 2025. Vol. 368. p. 125694.
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Ahmad I., Khan S. A., Shoeb M., Islam S., Khan M. A. Hydrochemical facies distribution, controlling mechanisms and Natural background concentrations of major pollutants in Ganga-Yamuna Interfluve Aquifer, India // Environmental Pollution. 2025. Vol. 368. p. 125694.
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TY - JOUR
DO - 10.1016/j.envpol.2025.125694
UR - https://linkinghub.elsevier.com/retrieve/pii/S0269749125000673
TI - Hydrochemical facies distribution, controlling mechanisms and Natural background concentrations of major pollutants in Ganga-Yamuna Interfluve Aquifer, India
T2 - Environmental Pollution
AU - Ahmad, Izrar
AU - Khan, Saif Ahmad
AU - Shoeb, Mohd
AU - Islam, Saiful
AU - Khan, Md. Afzal
PY - 2025
DA - 2025/03/01
PB - Elsevier
SP - 125694
VL - 368
SN - 0269-7491
SN - 1873-6424
ER -
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@article{2025_Ahmad,
author = {Izrar Ahmad and Saif Ahmad Khan and Mohd Shoeb and Saiful Islam and Md. Afzal Khan},
title = {Hydrochemical facies distribution, controlling mechanisms and Natural background concentrations of major pollutants in Ganga-Yamuna Interfluve Aquifer, India},
journal = {Environmental Pollution},
year = {2025},
volume = {368},
publisher = {Elsevier},
month = {mar},
url = {https://linkinghub.elsevier.com/retrieve/pii/S0269749125000673},
pages = {125694},
doi = {10.1016/j.envpol.2025.125694}
}
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