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. CO
2 hydrate that formed from CO
2 and water shows functions of exothermic heat and phase equilibrium in the same environment under the sea bottom. The functions of CO
2 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 CO
2 hydrate and CO
2 injection method using the phase equilibrium of CO
2 hydrate. In this paper, we show experimental validation about the phenomena about the exothermic heat of CO
2 hydrate formation and CO
2 permeation when CO
2 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 CO
2 for enhanced recovery of methane hydrate.
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