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Spatio-temporal variations of Uranium in groundwater: Implication to the environment and human health

机译:地下水中铀的时空变化:对环境与人体健康的影响

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摘要

Groundwater overexploitation has resulted in huge scarcity and increase in the demand for water and food security in India. Groundwater in India has been observed to have experienced various water quality issues like arsenic, fluoride, and Uranium (U) contamination, leading to risk in human health. Markedly, the health risk of higher U in drinking water, as well as its chemical toxicity in groundwater have adverse effects on human. This study has reported occurrence of U as an emerging and widespread phenomenon in South Indian groundwater. Data on U in ground-water were generated from 284 samples along the Cretaceous Tertiary boundary within 4 seasons viz. pre-monsoon (PRM), southwest monsoon (SWM), northeast monsoon (NEM), and post-monsoon (POM). High U concentrations (74 ugL~') showed to be above the World Health Organization's provisional guideline value of 30 ugL~(-1). The geo-chemical, stable isotope and geophysical studies suggested that U in groundwater could vary with respect to season and was noted to be highest during NEM. The bicarbonate (HCO_3) released by weathering process during monsoon could affect the saturation index (SI)_(Caicite) and carbonate species of U. However, the primary source of U was found to be due to geogenic factors, like weathering, dissolution, and groundwater level fluctuation, and that, U mobilization could be enhanced due to anthropogenic activities. The findings further indicated that groundwater in the study area has reached the alarming stage of chemical toxicity. Hence, it is urgent and imperative that workable management strategies for sustainable drinking water source be developed and preventive measures be undertaken, relative to these water quality concerns to mitigate their disconcerting effect on human health.
机译:地下水过度引发了印度水和粮食安全需求巨大稀缺和增加。印度地下水已被观察到经历了砷,氟化物和铀(U)污染物等各种水质问题,导致人类健康风险。显着,饮用水中较高的健康风险,以及地下水中的化学毒性对人体产生不利影响。本研究报告南印度地下水中作为新兴和广泛现象的发生。在沿着白垩纪的三级边界内的284个样品中产生了u的u u的数据,在4个赛季viz。季风前(PRM),西南季风(SWM),东北季风(NEM)和后季风(POM)。高U浓度(74 UGL〜')表明,高于世界卫生组织的临时准则价值30 ugl〜(-1)。地理化学,稳定的同位素和地球物理研究表明,地下水中的u可能会因季节而变化,并且在NEM期间被认为是最高的。在季风的耐候过程中释放的碳酸氢盐(HCO_3)可能影响U的饱和指数(Si)和碳酸盐物种。然而,发现U的主要来源是由于造成造成造成造型因素,如风化,溶解,和地下水位波动,而且,由于人为活动,可以提高动员。结果进一步表明研究区域的地下水已达到化学毒性的令人震惊的阶段。因此,采取可持续饮用水源的可行管理策略紧急,需要采取预防措施,相对于这些水质担忧,以减轻对人体健康的令人难以置信的影响。

著录项

  • 来源
    《Science of the total environment》 |2021年第25期|145787.1-145787.17|共17页
  • 作者单位

    Department of Earth Sciences Annamalai University Tamil Nadu 608002 India;

    Department of Earth Sciences Annamalai University Tamil Nadu 608002 India;

    Department of Earth Sciences Annamalai University Tamil Nadu 608002 India Research Scientist Water Research Centre Kuwait Institute for Scientific Research Safat Kuwait;

    Department of Applied Geology Faculty of Engineering and Science Curtin University Malaysia CDT 250 98009 Miri Sarawak Malaysia;

    Crass Roots Research and Creation India (P) Ltd India;

    School of Environmental Sciences JNU New Delhi India;

    Health Physics Division BARC Mumbai India;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Uranium; Groundwater; Statistics; Stable isotopes; Speciation; Health risk;

    机译:铀;地下水;统计数据;稳定同位素;形态;健康风险;

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