Assessment of methane gas production from Indian gas hydrate petroleum systems. (15th April 2016)

• Record Type: Journal Article
• Authors: Vedachalam, N.; Ramesh, S.; Srinivasalu, S.; Rajendran, G.; Ramadass, G.A.; Atmanand, M.A.
• Is Part Of: Applied energy. Volume 168(2016)
• Page Start: 649
• Page End: 660
• Publication Date: 2016-04-15
• Subjects: Depressurization -- Gas hydrate -- Marine settings -- Methane -- Thermal -- TOUGH + HYDRAT; Power (Mechanics) -- Periodicals; Energy conservation -- Periodicals; Energy conversion -- Periodicals; 621.042
• DOI: 10.1016/j.apenergy.2016.01.117
• Languages: English
• ISSNs: 0306-2619

Abstract

Highlights: Methane gas extraction methodology studied for Indian gas hydrate reservoirs. Effectiveness of in-situ electro-thermal stimulation and depressurization techniques analyzed. Results from modeling and simulation with MATLAB and TOUGH + HYDRATE presented. Depressurization technique could dissociate laterally up to 145 m from well bore in KG basin. In-situ electro-thermal stimulation found to be economical in KG and Andaman reservoirs. Abstract: The effectiveness of the electro-thermal and depressurisation based techniques applied to three marine gas hydrate reservoir settings of India is modeled and simulated using MATLAB and TOUGH + HYDRATE reservoir modeling software. The results indicate that the depressurisation technique (with an achievable Δ P of >90 bar) will be effective in dissociating gas hydrates up to 145 m from a well bore in the Krishna Godavari (KG) reservoir. The technique when applied to the Andaman and Mahanadi reservoirs is found to produce a maximum Δ P of 64 and 70 bar against the minimum required threshold of 134 and 152 bar, and hence, found to be less effective for hydrate dissociation. The in-situ electro-thermal technique will be effective in the KG and Andaman reservoirs; and in the Mahanadi reservoir, if the gas hydrate saturations are >17%. The depressurization technique when applied to a hypothetical sandy reservoir in the KG basin shows that the spatial pressure drop is nearly double that in a clayey setting, which is conducive for hydrate dissociation.