| 海康盐场井水化离子与地震关系初探 |
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| 引用本文： | 吴运恒. 海康盐场井水化离子与地震关系初探[J]. 华南地震, 1991, 11(3): 75-79 |
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| 作者姓名： | 吴运恒 |
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| 作者单位： | 湛江市地震局 |
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| 摘 要： | 本文对广东省海康盐场339^#深井8年来的水化观测资料进行了初步分析，认为该井Cl^-含量和Ca^ Mg^ 合量的下尝稳定型的，它们与气象等外界因素影响无明显关系，对一定范围内的地震活动具有震兆显示能力。
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| 关 键 词： | 氯 钙 镁离子 地下水化学 水化离子异常 地震前兆 |
PRELIMINARY STUDY ON THE RELATIONSBETWEEN SEISMICITY AND CHEMICAL ION INTHE WELL WATER AT THE SALT FIELDOF HAIKANG AREA |
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| Wu Yunheng. PRELIMINARY STUDY ON THE RELATIONSBETWEEN SEISMICITY AND CHEMICAL ION INTHE WELL WATER AT THE SALT FIELDOF HAIKANG AREA[J]. South China Journal of Seismology, 1991, 11(3): 75-79 |
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| Authors: | Wu Yunheng |
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| Affiliation: | Seismological Bureau of Zhanjiang City |
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| Abstract: | By analysing the observated data of hydration at the well of No. 339 in the salt field of Haikang, Guangdong Province, it thinks that the content of C1 and the mixed contents of Ca + + Mg++ are in the normal behaviour of stable. They bear no distinct relation to the infl ence of outside factor (such as climate, meteorology and so on) and have the ability to indicate earthquake precursor in the certain range of seismicity. |
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| Keywords: | Hydrochemical observation in the deep well The relations between seismicity and the ion content of C1 Ca and Ng |
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