Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics

Jiang Xueyan; Yu Zhigang; Ning Jinsong; Chen Hongtao; Mi Tiezhu

doi:10.1007/BF02842861

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Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics

OriginalPaper | Updated：2023-05-16

- Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics
- Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics
- 海洋湖沼学报（英文） 2006年24卷第4期页码：435-442
- Affiliations：
  
  1. Chemistry and Chemical Engineering College Ocean University of China
  2. Environmental Science and Engineering College Ocean University of China
- Author bio：
- Funds：
  
  Supported by NSFC (No. 40276026), and the Key Science and Technology Plan of The Ministry of Education of China ([2000]156-00079)
- DOI：10.1007/BF02842861
  中图分类号：
- 网络首发：2013-01-31，
  
  纸质出版：2006
- Accepted：
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Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics[J]. 海洋湖沼学报（英文）, 2006,24(4):435-442.

Xueyan, J., Zhigang, Y., Jinsong, N. et al. Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics., Chin. J. Ocean. Limnol. 24, 435–442 (2006). https://doi.org/10.1007/BF02842861
Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics[J]. 海洋湖沼学报（英文）, 2006,24(4):435-442. DOI： 10.1007/BF02842861.

Xueyan, J., Zhigang, Y., Jinsong, N. et al. Genesis of underground brine along south coast of Laizhou Bay: hydrochemical characteristics., Chin. J. Ocean. Limnol. 24, 435–442 (2006). https://doi.org/10.1007/BF02842861 DOI：

摘要

Abstract

Hydrochemistry of underground brines along south coast of Laizhou Bay

Shandong

China has been analyzed. Brine samples were collected from 43 wells in this area. It was considered that the brines were originated from seawater. However

whether they were formed by seawater evaporation or seawater freezing was not fully sure. We created a simple method by plotting Na/Clvs. seawater concentration factor (SCF) and Ca/Mgvs. SCF to determine the brine formation geochemically. Comparison of our results to previous seawater freezing and evaporation experiments indicated that the brines were formed by seawater evaporation. The ratios of HCO3/Cl of some low salinity brines in the study area were relatively higher

indicating that the brines may have mixed with other waters after the generation. The Br/Cl ratios of the brines decreased annually in the past 20 to 30 years of exploitation

indicating downward permeation of the brine from which bromine was extracted.

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references

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