The Effect of Temperature Gradient on the Interaction between Geothermal Water and Rock—An Approach by Numerical Simulation

1989 Mining Geology  
Reaction between rhyolitic welded tuff and geothermal solution cooled or heated from the temperature in equilibrium with alteration minerals is numerically examined by the geochemical simulation code. Six varieties of the initial solutions are calculated assuming that total chloride concentrations are 0.01, 0.05 and 0.1 mole/kg and
doi:10.11456/shigenchishitsu1951.39.217_295 fatcat:pq5kc7crcfbpvbopqwtkwyowsm