『Abstract
　The effects of CO2 on water-basaltic glass interaction have been simulated at 25℃. The calculations indicate that addition of CO2 (2-30 bar) to water significantly changes the reaction path. Initially, the pH is buffered between 4 and 6 by CO2 ionization, with dissolution of basaltic glass and the formation of secondary minerals with SiO2, Mg-Fe carbonates and dolomite predominating. Upon the dissolution of additional basaltic glass and mineral fixation of CO2, the pH increases to ＞8 and (Ca)-Fe-Mg smectites, SiO2, Ca-Na zeolites and calcite become the dominant secondary minerals forming. The overall reaction path depends on the initial water composition, reactive surface area, and the composition of the phyllosilicates and carbonates forming. The key factors are the mobility of Mg²⁺, Fe²⁺ and Ca²⁺ and the competing reactions for these solutes among secondary minerals.』

Introduction
Methods
Results and discussion
　Low CO2 systems
　Elevated CO2 systems
　Reaction path
Conclusions
Acknowledgements
References