The experience of mapping of Baikal subsurface gas hydrates and gas recovery |
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| Institution: | 1. Limnological Institute, Siberian Branch of the Russian Academy of Sciences, ul. Ulan-Batorskaya 3, Irkutsk, 664033, Russia;2. Institute of Technology, Shimizu Corporation, 4-17, Etchujima 3-chome, Koto-ku, Tokyo 135-8530, Japan;3. A.V. Nikolaev Institute of Inorganic Chemistry, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Lavrent’eva 3, Novosibirsk, 630090, Russia;4. Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia;1. Institute of the Earth’s Crust, Siberian Branch of the RAS, ul. Lermontova 128, Irkutsk, 664033, Russia;2. Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and the Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, GPO Box U1987, Perth, WA 6845, Australia;3. School of Earth and Environment, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia;4. Department of Earth Sciences, Carleton University, 1125 Colonel By Drive, Ottawa, ON K1S 5B6, Canada;5. Tomsk State University, pr. Lenina 36, Tomsk, 634050, Russia;6. Ernst Geosciences, 43 Margrave Ave., Ottawa, ON K1T 3Y2, Canada |
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| Abstract: | Lake Baikal is the only fresh-water lake where natural gas hydrate accumulations were found in sediments. For the recent decade, Baikal has become a natural laboratory for investigation of the properties of gas hydrates, their indicators, and recovery of gas from subsurface (subbottom) gas hydrates. We present the main results of subsurface gas hydrate mapping and gas recovery test near the delta of the Goloustnaya River. |
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