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Chemical Equilibrium

  • Naotatsu Shikazono
Chapter

Abstract

Using chemica l equilibrium model, stability fields of common silicate minerals are shown on activity diagram and solubilities of minerals as functions of pH , gaseous fugacity and oxidation -reduction potential. It is shown that the chemical composition of ground water reacting with silicates are interpreted based on inverse mass balance model and natural aqueous solutions (ground water, hydrothermal solution) are also controlled by the partitioning of elements between aqueous solution and surface of mineral (Rayleigh fractionation ).

Keywords

Geothermal Water Reaction Reaction Argillic Alteration Concentration Concentration Shallow Ground Water 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Further Reading

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Copyright information

© Springer Japan 2015

Authors and Affiliations

  • Naotatsu Shikazono
    • 1
  1. 1.Keio UniversityTokyoJapan

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