首页> 外文期刊>Fresenius environmental bulletin >QUALITY EVALUATION AND ITS CONTROLLING FACTOR ANALYSES OF SHALLOW GROUNDWATER IN THE URBAN AREA OF SUZHOU, ANHUI PROVINCE, CHINA
【24h】

QUALITY EVALUATION AND ITS CONTROLLING FACTOR ANALYSES OF SHALLOW GROUNDWATER IN THE URBAN AREA OF SUZHOU, ANHUI PROVINCE, CHINA

机译:安徽省苏州市浅层地下水质量评价及其控制因素分析

获取原文
       

摘要

Groundwater is an important source for dinking and irrigation purposes in northern Anhui province, China, and management of this resource is significant to meet the increasing demand of water. In this study, forty-three groundwater samples collected from the First (FA, 20 samples) and Second (SA, 23 samples) loose layer aquifers in the west of Suzhou city, north Anhui Province, China, and their major ion concentrations have been analyzed by a series of chemical indexes (including the Nemerow pollution index, water quality index, sodium adsorption ratio as well as sodium percent) for the evaluation of pollution status, dinking and irrigation suitability. Then the mechanisms controlling the groundwater chemistry have been analyzed. The results indicated that the groundwater samples are neutral to slightly alkaline, 75% and 100% of the FA and SA samples have TDS contents similar to the fresh water (1000mg/L), and the hydrochemical facies of the groundwater samples are classified to be Na-HCO_3, to a lesser extent, Ca-HCO_3 and Mg- HCO_3. Based on Nemerow pollution index, 55% and 26% of samples from the FA and SA are suffered litter pollution, respectively. Water quality index indicated that all of samples can be used for dinking proposes, and approximately 40% of the samples from the two aquifers are good for irrigation according to the analysis of sodium adsorption ratio and sodium percent. Furthermore, the Gibbs diagram, chloro-alkaline indices as well as the relationships between Na~+, Ca~(2+), Mg~(2+) and HCO_3~- indicated that the weathering of silicate minerals and ion exchange are the main process controlling the groundwater chemistry.
机译:在中国安徽北部地区,地下水是用于饮食和灌溉目的的重要来源,对该资源的管理对于满足日益增长的水需求具有重要意义。在这项研究中,从安徽省北部苏州市西部的第一层(FA,20个样品)和第二层(SA,23个样品)收集的43个地下水样品中,主要离子浓度为通过一系列化学指标(包括Nemerow污染指数,水质指数,钠吸附率和钠百分比)进行分析,以评估污染状况,饮食和灌溉适宜性。然后分析了控制地下水化学的机理。结果表明,地下水样品为中性至弱碱性,FA和SA样品中的TDS含量与淡水(1000mg / L)相似,分别为75%和100%,并且地下水样品的水化学相分类为Na-HCO_3,在较小程度上为Ca-HCO_3和Mg-HCO_3。根据Nemerow污染指数,来自FA和SA的样本分别有55%和26%遭受了垃圾污染。水质指数表明,所有样品均可用于取水建议,根据钠吸附率和钠百分比的分析,两个含水层中约有40%的样品适合灌溉。此外,Gibbs图,氯碱指数以及Na〜+,Ca〜(2 +),Mg〜(2+)和HCO_3〜-之间的关系表明,硅酸盐矿物的风化和离子交换是主要的控制地下水化学的过程。

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