A preliminary study on the distribution and genesis of underground brine in the littoral plain of Laizhou Bay in the Bohai Sea

Han Yousong; Meng Guanglan; Wang Shaoqing

doi:10.1007/BF02850727

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A preliminary study on the distribution and genesis of underground brine in the littoral plain of Laizhou Bay in the Bohai Sea

Updated：2023-05-16

- A preliminary study on the distribution and genesis of underground brine in the littoral plain of Laizhou Bay in the Bohai Sea
- Journal of Oceanology and Limnology Vol. 11, Issue 1, Pages: 46-56(1993)
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
- DOI：10.1007/BF02850727
  CLC：
- Published：1993
- Accepted：
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Yousong, H., Guanglan, M. & Shaoqing, W. A preliminary study on the distribution and genesis of underground brine in the littoral plain of Laizhou Bay in the Bohai Sea., Chin. J. Ocean. Limnol. 11, 46–56 (1993). https://doi.org/10.1007/BF02850727
DOI：

Yousong, H., Guanglan, M. & Shaoqing, W. A preliminary study on the distribution and genesis of underground brine in the littoral plain of Laizhou Bay in the Bohai Sea., Chin. J. Ocean. Limnol. 11, 46–56 (1993). https://doi.org/10.1007/BF02850727 DOI：

摘要

Abstract

Quaternary underground brine in the littoral plain region of the Bohai coast is new type littoral facies evaporation ore deposit in liquid state. This model of “littorally-forming brine” is based on study of the distribution

depositional environment

forming/storing process

and genesis of underground brine in the coast of Laizhou Bay. Essential conditions for genesis of brine are arid and semiarid climate

abundant sources of ancient seawater

and geological and geomorphological environment of wide tidal beach along a coast. The process of underground brine genesis may be: seawater/tidal beach » evaporation and concentration » seeping and accumulation » brine/tidal beach » burial (evolution of the sea-land)» underground brine. Underground brine is characterized by high content of chemical elements

shallow burial depth and easy exploitation. The process of extracting salt from underground brine present in the tidal flat is incomparably superior to that of producing salt from seawater

and has brough great economic benefits to the coastal areas of Laizhou Bay

Shandong Province.

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Keywords

references

Ovchinikov, A. M., 1960. General Hydrogeology. Geological Press, Beijing, pp. 183–184. (Chinese translation)

Han Yousong and Wu Hongfa, 1982. The origin of underground brine in the coastal plain of Laizhou Bay.Geological Review 28(2): 126–131. (in Chinese with English abstract)

Han Yousong, Meng Guanglan and Wang Shaoqing, 1986. A study of the marine strata, the ancient coastline and the sea level changes in the Shandong Peninsula coastal areas during late Quaternary.In: China Sea Level Changes. Ocean Press, Beijing pp. 98–104. (in Chinese with English abstract)

Meng Guanglan and Wang Shaoqing, 1986. Studies on Quaternary sporo-pollen assemblage and paleoclimate based on Bohai Sea Core Bc-1.Oceanologia et Limnologia Sinica 18(3): 253–263. (in Chinese with English abstract)

Xu Keqin, Hu Shouxi and Yu Shouyun, 1964. Mineral Deposit. Peopl'es Education Press, Beijing, pp. 377–393. (in Chinese)

Yuan Jianqi, Zhu Changqing and Zhai Yusheng, 1979. Mineral Deposit. Geological Press, Beijing, pp. 240–263. (in Chinese)

Zhou Zhonghuai, Xu Lijun and Liu Xingjun, 1989. The discovery of high concentration uranium in the concentrated underground seawater and the geochemical anomaly in Laizhou Bay.Oceanologia et Limnologia Sinica 20(1): 52–57. (in Chinese with English abstract)

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