Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Natural gas hydrates with locally different cage occupancies and hydration numbers in Lake Baikal. / Kida, Masato; Hachikubo, Akihiro; Sakagami, Hirotoshi; Minami, Hirotsugu; Krylov, Alexey; Yamashita, Satoshi; Takahashi, Nobuo; Shoji, Hitoshi; Khlystov, Oleg; Poort, Jeffrey; Narita, Hideo.
в: Geochemistry, Geophysics, Geosystems, Том 10, № 5, Q05003, 01.05.2009.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
}
TY - JOUR
T1 - Natural gas hydrates with locally different cage occupancies and hydration numbers in Lake Baikal
AU - Kida, Masato
AU - Hachikubo, Akihiro
AU - Sakagami, Hirotoshi
AU - Minami, Hirotsugu
AU - Krylov, Alexey
AU - Yamashita, Satoshi
AU - Takahashi, Nobuo
AU - Shoji, Hitoshi
AU - Khlystov, Oleg
AU - Poort, Jeffrey
AU - Narita, Hideo
PY - 2009/5/1
Y1 - 2009/5/1
N2 - [1] Knowledge of cage occupancies and hydration numbers (n) of naturally occurring gas hydrate in a local environment is important for the improvement in global estimates of hydrate-bound natural gas. We report on local differences in cage occupancies and hydration number of gas hydrates from Lake Baikal. Natural gas hydrates of both structures I and II (sI and sII) and ranging in composition from pure CH4 to mixed gas hydrate containing up to 15% C2H6 are compared. The average hydration numbers are n = 6.1 for the sI CH4 hydrates recovered from the Malenky and Bolshoy mud volcanoes, n = 6.2 for the sI hydrates, containing 3-4% C2 H 6 recovered from the K-2 mud volcano, and n = 6.9 for the sII hydrate containing about 15% C2H6 recovered from the K-2 mud volcano. The differences in hydration number are due to the differences in the small cage occupancy of CH4 among the samples studied.
AB - [1] Knowledge of cage occupancies and hydration numbers (n) of naturally occurring gas hydrate in a local environment is important for the improvement in global estimates of hydrate-bound natural gas. We report on local differences in cage occupancies and hydration number of gas hydrates from Lake Baikal. Natural gas hydrates of both structures I and II (sI and sII) and ranging in composition from pure CH4 to mixed gas hydrate containing up to 15% C2H6 are compared. The average hydration numbers are n = 6.1 for the sI CH4 hydrates recovered from the Malenky and Bolshoy mud volcanoes, n = 6.2 for the sI hydrates, containing 3-4% C2 H 6 recovered from the K-2 mud volcano, and n = 6.9 for the sII hydrate containing about 15% C2H6 recovered from the K-2 mud volcano. The differences in hydration number are due to the differences in the small cage occupancy of CH4 among the samples studied.
KW - Cage occupancy
KW - Ethane
KW - Hydration number
KW - Lake Baikal
KW - Methane
KW - Natural gas hydrate
UR - http://www.scopus.com/inward/record.url?scp=72749124274&partnerID=8YFLogxK
U2 - 10.1029/2009GC002473
DO - 10.1029/2009GC002473
M3 - Article
AN - SCOPUS:72749124274
VL - 10
JO - Geochemistry, Geophysics, Geosystems
JF - Geochemistry, Geophysics, Geosystems
SN - 1525-2027
IS - 5
M1 - Q05003
ER -
ID: 47749973