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Fluoride and nitrate contamination of groundwater in the Loess Plateau, China: Sources and related human health risks

机译:黄土高原地下水氟化物和硝酸盐污染中国:来源及相关人体健康风险

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摘要

Fluoride (F-) and nitrate (NO3-) in groundwater have caused serious health problems worldwide. However, in the Chinese Loess Plateau where groundwater is the primary source of drinking water, previous studies have rarely reported the health risks from fluoride and nitrate in groundwater. Therefore, we collected 105 groundwater samples (78 from shallow aquifers and 27 from deep aquifers) from the western district of the Loess Plateau for physicochemical and isotopic analysis to investigate the sources of F- and NO3- in groundwater and associated health risks. Fluoride concentration in 73.1% of shallow groundwater and 22.2% of deep groundwater exceeds 1.5 mg/L, while NO3- content in 76.3% of shallow groundwater and 51.9% of deep groundwater surpasses 50 mg/L. High-F- groundwater is associated with HCO3-Na, SO4-Na center dot Mg and Cl-Na center dot Mg types water. Fluorine bearing minerals dissolution, cation exchange, calcite precipitation, evaporation, and anthropogenic activities contribute significantly F- in groundwater. Mixing with shallow groundwater is an important source of F- in deep groundwater. The NO3- content is highest in Cl type water, followed by SO4 type and HCO3 type water. NO3- mainly originates from soil organic nitrogen (SON), chemical fertilizers (CF), and manure and sewage (M&S). Nitrification is the dominant transformation process of nitrogen nutrients in groundwater. The hazard index (HI) values for shallow groundwater are 0.203-9.232 for adults, 0.253-11.522 for teenagers, 0.359-16.322 for children, and 0.507-23.043 for infants, while those for deep groundwater are 0.713-5.813 for adults, 0.890-7.254 for teenagers, 1.261-10.277 for children, and 1.780-14.508 for infants. Approximately 96.2% of shallow groundwater poses non-carcinogenic risks to infants and children, followed by 92.3% to teenagers, and 89.7% to adults. All deep groundwater poses non-carcinogenic risks to infants and children, followed by 92.6% to teenagers, and 74.1% to adults. This study is helpful to develop strategies for the integrated management of high fluoride or nitrate groundwater in arid areas.
机译:地下水中的氟化物(F-)和硝酸盐(NO 3-)导致全世界严重的健康问题。然而,在中国黄土高原,地下水是饮用水的主要来源,之前的研究很少报道了地下水中氟化物和硝酸盐的健康风险。因此,我们从黄土高原西区收集了105个地下水样本(从深含水层和深含水层27号),用于探讨地下水和NO3-中的物理化学和同位素分析,以及相关健康风险的来源。氟化物浓度为73.1%的浅层地下水和22.2%的深层地下水超过1.5mg / L,而76.3%的浅层地下水的NO3含量和51.9%的深层地下水超过50mg / L.高F F-Troundwater与HCO3-Na,SO4-Na中心点Mg和Cl-Na中心点Mg类型水有关。氟轴承矿物溶解,阳离子交换,方解石沉淀,蒸发和人为的活性显着促进地下水的显着贡献。与浅层地下水混合是深水中的一个重要来源。 CL型水中的NO3含量最高,其次是SO4型和HCO3型水。 NO3-主要来自土壤有机氮(儿子),化肥(CF)和粪肥和污水(M&S)。硝化是地下水中氮营养成分的显性转化过程。浅层地下水的危害指数(HI)值为成人0.203-9.232,对于青少年为0.253-11.522,婴儿0.359-16.322,0.507-23.043为0.507-23.043,而Deeplindwater的成人为0.713-5.813,0.890- 7.254青少年,1.261-10.277儿童,婴儿1.780-14.508。大约96.2%的浅层地下水对婴儿和儿童带来了非致癌风险,其次为92.3%到青少年,成人89.7%。所有深层地下水都会对婴儿和儿童带来非致癌风险,其次对青少年的92.6%,成人74.1%。本研究有助于制定干旱地区综合管理的综合管理策略。

著录项

  • 来源
    《Environmental Pollution》 |2021年第10期|117287.1-117287.12|共12页
  • 作者单位

    Taiyuan Univ Technol Dept Earth Sci & Engn Taiyuan 030024 Peoples R China;

    Northwest Univ Dept Geol State Key Lab Continental Dynam Xian 710069 Peoples R China;

    Taiyuan Univ Technol Dept Earth Sci & Engn Taiyuan 030024 Peoples R China;

    Northwest A&F Univ Coll Nat Resources & Environm Yangling 712100 Shaanxi Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Fluoride; Nitrate; Source; Health risk assessment; Loess Plateau;

    机译:氟化物;硝酸盐;来源;健康风险评估;黄土高原;

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