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이주용(Lee, J.Y.),이재형(Lee, J.H.),이대성(Lee, D.S.),이원석(Lee, W.S.),김세준(Kim, S.J.),허대기(Huh, D.G.),김현태(Kim, H.T.) 한국신재생에너지학회 2008 한국신재생에너지학회 학술대회논문집 Vol.2008 No.10
Electrical resistivity in hydrate-bearing sediments is sensitive to porosity, gas hydrate saturation, gas content, pore fluid composition, and temperature, so electrical measurements such as well logs and electromagnetic surveys have been used to explore gas hydrate-bearing formation. The high pressure tomography cell is designed considering the effect of electrode configuration and electrical shielding on tomography measurements and the safety. The evolution of electrical conductivity during CO₂ hydrate formation and dissociation reflects the combined effects of concurrent changes that include ionization of dissolved CO₂, temperature-dependent ionic mobility, changes in the degree of saturation, ion exclusion, surface conduction, and porosity changes. Measurements during hydrate formation and dissociation require careful analysis to properly interpret signatures, in particular when out-of plane conductivity anomalies prevail.