刘建刚, 吴顺华, 郑克勋. 基于活度计算的碳酸平衡研究[J]. 水科学进展, 2004, 15(5): 640-642.
引用本文: 刘建刚, 吴顺华, 郑克勋. 基于活度计算的碳酸平衡研究[J]. 水科学进展, 2004, 15(5): 640-642.
LIU Jian-gang, WU Shun-hua, ZHENG Ke-xun. Study of carbonate equilibrium based on activity[J]. Advances in Water Science, 2004, 15(5): 640-642.
Citation: LIU Jian-gang, WU Shun-hua, ZHENG Ke-xun. Study of carbonate equilibrium based on activity[J]. Advances in Water Science, 2004, 15(5): 640-642.

基于活度计算的碳酸平衡研究

Study of carbonate equilibrium based on activity

  • 摘要: 研究考虑活度情况下地下水开放系统在不同温度和CO2分压下碳酸的3种存在形式与pH值之间的关系.分析地下水中CO2分压为10~105Pa,温度为0~30℃变化时pH0的变化情况,发现在一定CO2分压下,pH0值随温度的升高而降低并趋于一个稳定的值.在一定温度下,pH0值随CO2分压的升高而降低.但不论地下水的温度和CO2分压如何变化,pH0=7.92~8.60.这些结论更符合地下水实际情况,更有利于对水分析资料的审查.

     

    Abstract: In this article,the relationship between the three existing forms of carbonate and pH value is studied at different temperatures and CO2 pressures in an open underground water system while activity is taken into consideration.We find that the value of pH0 decreases with the increase of temperature and tends to a stable value at a given CO2 pressure and the value of pH0 decreases with the increase of the CO2 pressure at a given temperature when CO2 pressure changes in the range of 10~105Pa and the temperature changes in the range of 0~30℃.However,no matter how the temperature and CO2 pressure of the underground water change,pH0=7.92~8.60.These conclusions reflects the actual conditions of the underground water and can be better used for the review of water analysis data.

     

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