Abstract
Methane hydrate (MH) in Nankai-trough is expected as a Japanese domestic future energy resource of natural gases. It is mainly condensed in the pores of unconsolidated oceanic sedimentary layers. CO2 hydrate that formed from CO2 and water shows functions of exothermic heat and phase equilibrium in the same environment under the sea bottom. The functions of CO2 hydrate could be used for enhanced recovery of methane hydrate. We had shown experimental validations that warming ability of the layer sediments by using exothermic heat of CO2 hydrate and CO2 injection method using the phase equilibrium of CO2 hydrate. In this paper, we show experimental validation about the phenomena about the exothermic heat of CO2 hydrate formation and CO2 permeation when CO2 is injected into super cooling layer sediments, which temperature is lower than phase equilibrium temperature by few degrees Celsius. We think that this validation made higher adaptability of CO2 for enhanced recovery of methane hydrate.