Appraisal of groundwater suitability for drinking and irrigation utilities in the Cooum River basin, South India: Implications from uranium, nitrate, and fluoride health risks

IF 3 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
M. Sivakumar , T. Subramani , V.N. Prapanchan , D. Karunanidhi
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引用次数: 0

Abstract

The study reveals that 6% of groundwater samples exceed the WHO's recommended fluoride limit of 1.5 mg/L, and 15% surpass the nitrate standard of 45 mg/L, rendering the water unsuitable for drinking. Gibbs plot analysis identifies evaporation as the dominant factor affecting groundwater chemistry, while the Piper diagram classifies the water into mixed Ca–Mg–Cl and NaCl types, indicating natural processes and potential seawater intrusion. Cation exchange processes are observed in 75.5% of samples, as shown by Schoeller's indices. The hydrochemical facies evolution suggests freshening from recharge in most samples, with signs of salinity intrusion in others. Between 2010 and 2023, land use and land cover (LULC) changes show a significant increase in built-up areas, resulting in reduced groundwater recharge and heightened pollution risks. The classification accuracy is high, with an overall accuracy of 82.20% and a Kappa coefficient of 83.06%. Water Quality Index (WQI) assessment reveals that 47% of the groundwater samples are excellent for drinking, while 20.6% are suitable. Although 80% of the groundwater remains appropriate for agriculture, the study highlights the need for targeted groundwater management to address urbanization impacts and mitigate health risks from elevated nitrate ingestion, particularly for vulnerable populations such as children.
印度南部库姆河流域地下水饮用和灌溉适宜性评估:铀、硝酸盐和氟化物对健康的影响
研究显示,6% 的地下水样本超过了世界卫生组织建议的 1.5 毫克/升的氟含量限值,15% 的地下水样本超过了 45 毫克/升的硝酸盐含量标准,因此不适合饮用。吉布斯图分析表明,蒸发是影响地下水化学性质的主要因素,而皮珀图则将地下水分为 Ca-Mg-Cl 和 NaCl 混合型,这表明了地下水的自然过程和潜在的海水入侵。根据 Schoeller 指数,75.5% 的样本观察到阳离子交换过程。水化学面貌的演变表明,大多数样本中的水是由补给水形成的,而其他样本中的水则有盐分侵入的迹象。从 2010 年到 2023 年,土地利用和土地覆盖(LULC)的变化表明,建筑密集区显著增加,导致地下水补给减少,污染风险增加。分类准确率很高,总体准确率为 82.20%,卡帕系数为 83.06%。水质指数(WQI)评估显示,47% 的地下水样本为优良饮用水质,20.6% 为适宜饮用水质。虽然 80% 的地下水仍然适合农业用水,但这项研究强调有必要对地下水进行有针对性的管理,以应对城市化带来的影响,并降低因摄入硝酸盐过高而带来的健康风险,尤其是对儿童等弱势群体而言。
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来源期刊
Physics and Chemistry of the Earth
Physics and Chemistry of the Earth 地学-地球科学综合
CiteScore
5.40
自引率
2.70%
发文量
176
审稿时长
31.6 weeks
期刊介绍: Physics and Chemistry of the Earth is an international interdisciplinary journal for the rapid publication of collections of refereed communications in separate thematic issues, either stemming from scientific meetings, or, especially compiled for the occasion. There is no restriction on the length of articles published in the journal. Physics and Chemistry of the Earth incorporates the separate Parts A, B and C which existed until the end of 2001. Please note: the Editors are unable to consider submissions that are not invited or linked to a thematic issue. Please do not submit unsolicited papers. The journal covers the following subject areas: -Solid Earth and Geodesy: (geology, geochemistry, tectonophysics, seismology, volcanology, palaeomagnetism and rock magnetism, electromagnetism and potential fields, marine and environmental geosciences as well as geodesy). -Hydrology, Oceans and Atmosphere: (hydrology and water resources research, engineering and management, oceanography and oceanic chemistry, shelf, sea, lake and river sciences, meteorology and atmospheric sciences incl. chemistry as well as climatology and glaciology). -Solar-Terrestrial and Planetary Science: (solar, heliospheric and solar-planetary sciences, geology, geophysics and atmospheric sciences of planets, satellites and small bodies as well as cosmochemistry and exobiology).
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