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深圳大沙河河水与海水关系的水文化学识别 被引量:5

Hydrochemistry recognization of the relationship between seawater and Dasha river water of Shenzhen
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摘要 为了解深圳沿岸河口处海水与河水的混合关系,在大沙河下游靠近河口段密集取17件河水样,依据其水化学数据,分析了主要离子Ca、Mg、Na、K、SO4、HCO3与Cl的关系,Br与Cl的关系以及piper三线图解,在研究区河段从上游至入海口,对河水样品有如下认识:(1)上游4个样品(Cl<100mg/L)接受降水和地下水的补给;(2)4个样品(150mg/L<Cl<1500mg/L)受人类活动的污染影响;(3)橡胶坝上游3个样品(1500mg/L<Cl<4000mg/L)处于海水与污染水的过渡带;(4)橡胶坝下游6个样品(Cl浓度5000~10000mg/L左右)是海水与淡水的混合。 In order to study the mixing relationship between seawater and surface water on the coast of Shenzhen, 17 river water samples were collected near the estuary in the downstream of the Dasha river which disembogue into the sea. According to the hydrochemistry data, the relationships of major ions ( Ca^2+ ,Mg^2+ , Na^+ ,K^+ ,SO4^2- ,HCO3^- ) vs. Cl^- , Br^- vs. Cl^- and the piper diagram were analyzed. The river water data in comparison with seawater dilution lines in the scatter diagrams are divided into four groups: ( 1 ) 6 samples with salinities around 5 000 - 10 000 mg/L Cl^- , explained by the mixing of seawater with fresh water in downstream of rubber-dam; (2) 4 samples with salinities lower than 100 mg/L Cl^-, recharged by precipitation and groundwater in the upstream; (3) 4 samples with salinities around 150 - 1500mg/L Cl^- , resulted from anthropogenic contamination along the river; (4) 3 samples with salinities around 1 500 - 4 000mg/L Cl^- , characterized by the transition zone between polluted river water and seawater.
出处 《水文地质工程地质》 CAS CSCD 北大核心 2010年第2期32-35,41,共5页 Hydrogeology & Engineering Geology
基金 “深圳市海水入侵地质灾害调查与防治对策研究”项目成果
关键词 大沙河河水 海水 水文化学 海水入侵 s Dasha river water seawater hydrochemistry seawater intrusion
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参考文献8

  • 1Freeze, R A and Cherry, J A. Ground Water[ M]. Prentice - Hall, Inc, 1979 : 269 - 273.
  • 2Edmunds, W M. Bromine geochemistry of british groundwaters [ J ]. Mineralogical Magazine, 1996, 60 : 275 -284.
  • 3Alcala, F J and Custodio, E. Using the Cl/Br ratio as a tracer to identify the origin of salinity in aquifers in Spain and Portugal [ J ]. Journal of Hydrology, 2008, 359:189-207.
  • 4Vengosh, A and Ben - Zvi, A. Formation of a salt plume in the Coastal Plain aquifer of Israel: the Be' er Toviyya region [ J ]. Journal of Hydrology, 1994, 160 : 21 -52.
  • 5Yamanaka, M and Kumagai, Y. Sulfur isotope constraint on the provenance of salinity in a confined aquifer system of the southwestern Nobi Plain, central Japan[J]. Journal of Hydrology, 2005, 325: 33- 35.
  • 6Hiroshiro, Y. Jinno, K and Berndtsson, R. Hydrogeochemical properties of a salinity - affected coastal aquifer in western Japan [ J ]. Hydrological processes, 2006, 20: 1425- 1435.
  • 7Appelo, C A J and Postma, D. Geochemistry, groundwater and pollution[ M], 1993 : 22 - 24.
  • 8Salama, R B. Utto, C J and Fitzpatrick, R W. Contributions of groundwater conditions to soil and water salinization [ J ]. Hydrogeology Journal, 1999 (7) : 46 -64.

同被引文献44

  • 1张奎山,刘继先,赵欣萍.深圳市饮用水溴酸盐风险调查研究[J].给水排水,2008,34(S1):111-113. 被引量:2
  • 2李国敏,陈崇希,沈照理,蒋同根.涠洲岛海水入侵模拟[J].水文地质工程地质,1995,22(5):1-5. 被引量:25
  • 3许炼烽,林尹,仓恒瑾,杨惠宁,徐斌.雷州半岛地表水体非点源污染物时空变化特征研究[J].生态环境,2005,14(6):830-834. 被引量:3
  • 4曾黄锦.雷州半岛地下水开发利用对环境影响的分析[J].水利水电快报,2006,27(7):8-10. 被引量:5
  • 5Freeze,R A Cherry,J A.Ground Water[M].Prentice-Hall,Inc,1979:269-273.
  • 6Vengosh,A Ben-Zvi,A.Formation of a salt plume in the Coastal Plain aquifer of Israel:the Be' er Toviyya region[J].Journal of Hydrology,1994,160:21-52.
  • 7Yamanaka,M Kumagai,Y.Sulfur isotope constraint on the provenance of salinity in a confined aquifer system of the southwestern Nobi Plain,central Japan[J].Journal of Hydrology,2006,325:35-55.
  • 8Appelo C A J,Postma D.Geochemistry,groundwater and pollution[M].1993:22-24.
  • 9Rozanski,K,Araguas-Araguas,L Gonfiantini,et al.Isotopic patterns in modern global precipitation.In:Continental Isotope Indicators of Climate[J].American Geophysical Union Monograph.1993:1 -36.
  • 10Clark I D,Fritz P.Environmental isotopes in Hydrogeology[M].America:Lewis Publishers.1999.

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