...
首页> 外文期刊>Environmental earth sciences >Isotopic and geochemical studies of groundwater from the Ramganga basin and the middle Ganga Plains: implication for pollution and metal contamination
【24h】

Isotopic and geochemical studies of groundwater from the Ramganga basin and the middle Ganga Plains: implication for pollution and metal contamination

机译:Ramganga盆地和Ganga中部平原的地下水的同位素和地球化学研究:对污染和金属污染的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Hydrochemical and isotopic studies in groundwater were carried out along the entire Ramganga Basin and parts of middle Ganga Plain to examine the quality of shallow groundwater accessed by hand pumps. The aim of the study was to determine the spatial distribution of arsenic (As) in groundwater of the Middle Ganga (Haridwar-Banaras-Saidpur region) and of the Ramganga (Ramnagar-Kannauj) basins. Groundwater samples were collected from a shallow depth because most of the population in the study area use locally drilled hand pumps for obtaining drinking water. A large area encompassing the Rampur, Bareilly, Bilsi, Faridpur, Badaun, Farrukhabad and Varanasi districts were found to have levels of arsenic above the drinking water criterion of 10 ppb. Sampling has indicated that arsenic (As) and nitrate (NO3) present in groundwater in elevated levels are the chemical constituents of most health concern in the shallow alluvial aquifers of Ramnagar, Bareilly, Badaun and Jaunpur districts of Uttar Pradesh in the middle Ganga Plain. These chemical constituents in groundwater are likely to have been derived from both geogenic and anthropogenic sources. The geochemical characteristics of groundwater may be influenced by factors like changes in climatic conditions, mineral weathering (silicate, carbonate), mixing of polluted surface water at shallow depths, ion exchange and anthropogenic activities. Stable isotopes of oxygen (delta O-18), hydrogen (delta D) and carbon (delta C-13(DIC)) suggest that the process of carbonate weathering during the post-monsoon season has increased the input of chemical constituents into shallow groundwater. A shift in delta O-18 suggests soil-water interaction at shallow depths, which is reflected in elevated metal concentrations. The results indicate that arsenic concentrations in groundwater increase in the dry season and are decreased by recharge during the monsoon season.
机译:在整个Ramganga盆地和中部Ganga平原的部分地区进行了地下水的水化学和同位素研究,以检查手动泵进入的浅层地下水的质量。该研究的目的是确定中部恒河(Haridwar-Banaras-Saidpur地区)和Ramganga(Ramnagar-Kannauj)盆地地下水中砷(As)的空间分布。由于研究区域的大多数人口都使用本地钻孔的手动泵来获取饮用水,因此从浅深度收集了地下水样本。发现包括Rampur,Bareilly,Bilsi,Faridpur,Badaun,Farrukhabad和Varanasi地区的大部分地区的砷含量都超过饮用水标准10 ppb。采样表明,在恒河平原中部的北方邦拉姆纳加尔,巴里利,巴丹和贾恩布尔地区的浅冲积含水层中,地下水中砷(As)和硝酸盐(NO3)含量升高是最关注健康的化学成分。地下水中的这些化学成分很可能来自地源和人为来源。地下水的地球化学特征可能受气候条件变化,矿物风化(硅酸盐,碳酸盐),浅层受污染地表水混合,离子交换和人为活动等因素影响。氧(δO-18),氢(δD)和碳(δC-13(DIC))的稳定同位素表明,季风后季节碳酸盐岩风化的过程增加了化学成分向浅层地下水的输入。 O-18的变化表明土壤与水之间的相互作用在较浅的深度,这反映在金属浓度升高的情况下。结果表明,地下水中的砷浓度在干旱季节增加,而在季风季节通过补给而降低。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号