孙宝元, 王永才, 侯彦珍, 张根深. 冀中深部热水溶解无机碳的分布及其来源[J]. 华北地震科学, 1992, 10(3): 75-82.
引用本文: 孙宝元, 王永才, 侯彦珍, 张根深. 冀中深部热水溶解无机碳的分布及其来源[J]. 华北地震科学, 1992, 10(3): 75-82.
Sun Baoyuan, Wang Yongcai, Hou Yanzhen, Zhang Genshen. THE DISTRIBUTION OF THE INORGANIC CARBON DISSOLVED IN DEEP HOT WATER IN CENTRAL HEBEI PROVINCE AND ITS SOURCE[J]. North China Earthquake Sciences, 1992, 10(3): 75-82.
Citation: Sun Baoyuan, Wang Yongcai, Hou Yanzhen, Zhang Genshen. THE DISTRIBUTION OF THE INORGANIC CARBON DISSOLVED IN DEEP HOT WATER IN CENTRAL HEBEI PROVINCE AND ITS SOURCE[J]. North China Earthquake Sciences, 1992, 10(3): 75-82.

冀中深部热水溶解无机碳的分布及其来源

THE DISTRIBUTION OF THE INORGANIC CARBON DISSOLVED IN DEEP HOT WATER IN CENTRAL HEBEI PROVINCE AND ITS SOURCE

  • 摘要: 本文叙述了冀中地区深井热水中CO2、HCO3-及其碳同位素分布特征。并根据其δ13C值分析了地下水中溶解无机碳化合物的来源,结果表明,冀中拗陷内基岩地下水溶解无机碳主要来自碳酸盐的变质作用,其次来自土壤和大气CO2随地下水的渗入;而沧县隆起的济1井,黄骅拗陷内的孔20和徐7井除上述来源外,还有生物化学作用产生的CO2。冀中拗陷变质生成的无机碳化合物,可能是映震的灵敏组分,在地震地球化学监测中可优先选择。

     

    Abstract: The distribution characteristics of CO2,HCO3 and their carbonisotope in the hot water of the deep well in central Hebei area have been presented.Therefore,the sources of the inorganic carbon chemicals dissolved in the ground water has been analyzed by their δ13C value.The results have shown that the dissolved inorganic carbon in the ground water in the base rock in central Hebei depression are mainly from metamorphic action of the carbonate secondly from imbibing of CO2 in the soil and the air following the ground water.Otherwise, No.20 well in Huanghua depression in Changxian rise and XU No.7 welJ have,except above sources,CO2 causing from bio-chemical action.The inorganic carbon chemicals from metamorphic action in central Hebei is possibly sensitive factor for earthquake precursor and priority to the selection in the geochemical surveilance.

     

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