Abstract
Moderate high-pressure condition less than several tens MPa can be very useful for reproduction of deep underground environments to be utilized for waste disposal of CO2. Recent development in the feasibility test of CO2 sequestration has been achieved by phase-shift interference microscopy, laboratory in-situ measurement of calcite growth rate in the high-temperature and high-pressure cell and ex-situ measurement of calcite reacted in the crystal growth sonde diving into natural geothermal underground. These two approaches enable precise validation of safety storage of CO2 and its life-time.