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江苏南通地下水补给源、水化学特征及形成机理
引用本文:周慧芳,谭红兵,张西营,张文杰,孙雪.江苏南通地下水补给源、水化学特征及形成机理[J].地球化学,2011(6):566-576.
作者姓名:周慧芳  谭红兵  张西营  张文杰  孙雪
作者单位:[1]河海大学地球科学与工程学院,江苏南京210098 [2]中国科学院青海盐湖研究所,青海西宁810008
基金项目:国家自然科学基金(41073034),在野外调查采样过程中,南通市水文水资源勘测局于成主任等给予了很多支持和帮助,在此谨表谢意.
摘    要:在地下水的大规模开采条件下,江苏沿海一带,特别是南通许多地区的地下水一度出现咸化趋势,对区域水资源及环境产生了极大的影响,已成为制约生态环境建设和经济社会发展的重要因素.为查明地下水的补给来源、水化学特征和矿化度增高的机理,对南通地区深浅层地下水开展了野外调查取样.通过对各种水化学参数的讨论分析,系统地研究了该区地下水...

关 键 词:地下水  水化学特征  形成机理  南通地区

Recharge source, hydrochemical characteristics and formation mechanism of groundwater in Nantong, Jiangsu Province
ZHOU Hui-fang,TAN Hong-bing,ZHANG Xi-ying,ZHANG Wen-jie,SUN Xue.Recharge source, hydrochemical characteristics and formation mechanism of groundwater in Nantong, Jiangsu Province[J].Geochimica,2011(6):566-576.
Authors:ZHOU Hui-fang  TAN Hong-bing  ZHANG Xi-ying  ZHANG Wen-jie  SUN Xue
Institution:1. School of Earth Sciences arid Engineering, Hohai University, Nanjing 210098, China; 2. Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China)
Abstract:Salinity of groundwater in the coastal aquifers of Jiangsu Province becomes high, especially in some areas of Nantong because of the heavy usage due to economic development. This problem has great impact on the regional water resources and it potentially has high negative effects on the ecological environment, economic and social development. Groundwater samples were collected from the superficial and deep confined aquifers of Nantong to identify the water recharge source, hydrochemical characteristics and evolution mechanism of water chemistry. The total dissolved solids (TDS) of the superficial aquifer is higher than the deep aquifer in most areas, and it is higher in the coastal areas than in inland areas; groundwater of the superficial aquifer in the central and western areas has a low TDS, but the TDS shows very high in some special areas near the coastal region. Oxygen and hydrogen isotopes (D, O) and hydrochemical coefficients indicate that the local precipitation is the recharge source of superficial and deep aquifers. Dissolving salts of ancient marine strata is the major cause that increases the TDS of the deep confined groundwater in eastern coastal areas. The water quality of the deep aquifer in central and western areas is good as a whole, and the hydrochemical evolution is the natural water-rock interaction. The superficial aquifer water in Yinyang, Haiyan areas in southeastern coastal areas shows a very high TDS, to some extend due to seawater intrusion. In other areas, evapor-concentration and dissolving the salts of strata are the dominated hydrochemical evolution patterns of the superficial aquifer. Hence, the deep aquifer groundwater in eastern coastal areas where TDS is high should be protected effectively, especially the salified areas such as Yinyang and Haiyan.
Keywords:groundwater  hydrochemical characteristics  formation mechanism  Nantong area
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