Open AccessNatural gas hydrates with locally different cage occupancies and hydration numbers in Lake Baikal
Author(s) -
Kida Masato,
Hachikubo Akihiro,
Sakagami Hirotoshi,
Minami Hirotsugu,
Krylov Alexey,
Yamashita Satoshi,
Takahashi Nobuo,
Shoji Hitoshi,
Khlystov Oleg,
Poort Jeffrey,
Narita Hideo
Publication year - 2009
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1029/2009gc002473
Subject(s) - clathrate hydrate , hydrate , natural gas , volcano , geology , mineralogy , mud volcano , cage , geochemistry , chemistry , organic chemistry , combinatorics , mathematics
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 CH 4 to mixed gas hydrate containing up to 15% C 2 H 6 are compared. The average hydration numbers are n = 6.1 for the sI CH 4 hydrates recovered from the Malenky and Bolshoy mud volcanoes, n = 6.2 for the sI hydrates, containing 3–4% C 2 H 6 recovered from the K‐2 mud volcano, and n = 6.9 for the sII hydrate containing about 15% C 2 H 6 recovered from the K‐2 mud volcano. The differences in hydration number are due to the differences in the small cage occupancy of CH 4 among the samples studied.