Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data

Standard

Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data. / Hachikubo, Akihiro; Khlystov, Oleg; Manakov, Andrey; Kida, Masato; Krylov, Alexey; Sakagami, Hirotoshi; Minami, Hirotsugu; Takahashi, Nobuo; Shoji, Hitoshi; Kalmychkov, Gennadiy; Poort, Jeffrey.

в: Geophysical Research Letters, Том 36, № 18, L18504, 01.09.2009.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Hachikubo, A, Khlystov, O, Manakov, A, Kida, M, Krylov, A, Sakagami, H, Minami, H, Takahashi, N, Shoji, H, Kalmychkov, G & Poort, J 2009, 'Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data', Geophysical Research Letters, Том. 36, № 18, L18504. https://doi.org/10.1029/2009GL039805, https://doi.org/doi:10.1029/2009GL039805

APA

Hachikubo, A., Khlystov, O., Manakov, A., Kida, M., Krylov, A., Sakagami, H., Minami, H., Takahashi, N., Shoji, H., Kalmychkov, G., & Poort, J. (2009). Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data. Geophysical Research Letters, 36(18), [L18504]. https://doi.org/10.1029/2009GL039805, https://doi.org/doi:10.1029/2009GL039805

Vancouver

Hachikubo A, Khlystov O, Manakov A, Kida M, Krylov A, Sakagami H и пр. Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data. Geophysical Research Letters. 2009 Сент. 1;36(18). L18504. https://doi.org/10.1029/2009GL039805, https://doi.org/doi:10.1029/2009GL039805

Author

Hachikubo, Akihiro ; Khlystov, Oleg ; Manakov, Andrey ; Kida, Masato ; Krylov, Alexey ; Sakagami, Hirotoshi ; Minami, Hirotsugu ; Takahashi, Nobuo ; Shoji, Hitoshi ; Kalmychkov, Gennadiy ; Poort, Jeffrey. / Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data. в: Geophysical Research Letters. 2009 ; Том 36, № 18.

BibTeX

@article{41635d372be94efb9af9a5ca679a2478,

title = "Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data",

abstract = "We measured the isotopic compositions of methane (C1) and ethane (C2) of hydrate-bound gas and of dissolved gas in pore water retrieved from bottom sediments in Lake Baikal. Both structure I (sI:3%C 2) and II (sII:14%C2) gas hydrates are observed in the same sediment cores in Kukuy K-2 mud volcano. We found that C2 δD of sI gas hydrate is larger than that of sII, whereas C1 δ13C, C1 δD and C2 δ13C values are practically the same in both hydrate structures. δ13C Of C1 and C2 of hydrate-bound gas are several permil smaller than those in pore water, showing that the current pore water is not the source of gas hydrates. These findings lead to a new model where the sII gas hydrates were formed prior to the si hydrates.",

author = "Akihiro Hachikubo and Oleg Khlystov and Andrey Manakov and Masato Kida and Alexey Krylov and Hirotoshi Sakagami and Hirotsugu Minami and Nobuo Takahashi and Hitoshi Shoji and Gennadiy Kalmychkov and Jeffrey Poort",

year = "2009",

month = sep,

day = "1",

doi = "10.1029/2009GL039805",

language = "English",

volume = "36",

journal = "Geophysical Research Letters",

issn = "0094-8276",

publisher = "American Geophysical Union",

number = "18",

}

RIS

TY - JOUR

T1 - Model of formation of double structure gas hydrates in Lake Baikal based on isotopic data

AU - Hachikubo, Akihiro

AU - Khlystov, Oleg

AU - Manakov, Andrey

AU - Kida, Masato

AU - Krylov, Alexey

AU - Sakagami, Hirotoshi

AU - Minami, Hirotsugu

AU - Takahashi, Nobuo

AU - Shoji, Hitoshi

AU - Kalmychkov, Gennadiy

AU - Poort, Jeffrey

PY - 2009/9/1

Y1 - 2009/9/1

N2 - We measured the isotopic compositions of methane (C1) and ethane (C2) of hydrate-bound gas and of dissolved gas in pore water retrieved from bottom sediments in Lake Baikal. Both structure I (sI:3%C 2) and II (sII:14%C2) gas hydrates are observed in the same sediment cores in Kukuy K-2 mud volcano. We found that C2 δD of sI gas hydrate is larger than that of sII, whereas C1 δ13C, C1 δD and C2 δ13C values are practically the same in both hydrate structures. δ13C Of C1 and C2 of hydrate-bound gas are several permil smaller than those in pore water, showing that the current pore water is not the source of gas hydrates. These findings lead to a new model where the sII gas hydrates were formed prior to the si hydrates.

AB - We measured the isotopic compositions of methane (C1) and ethane (C2) of hydrate-bound gas and of dissolved gas in pore water retrieved from bottom sediments in Lake Baikal. Both structure I (sI:3%C 2) and II (sII:14%C2) gas hydrates are observed in the same sediment cores in Kukuy K-2 mud volcano. We found that C2 δD of sI gas hydrate is larger than that of sII, whereas C1 δ13C, C1 δD and C2 δ13C values are practically the same in both hydrate structures. δ13C Of C1 and C2 of hydrate-bound gas are several permil smaller than those in pore water, showing that the current pore water is not the source of gas hydrates. These findings lead to a new model where the sII gas hydrates were formed prior to the si hydrates.

UR - http://www.scopus.com/inward/record.url?scp=72149083565&partnerID=8YFLogxK

U2 - 10.1029/2009GL039805

DO - 10.1029/2009GL039805

M3 - Article

VL - 36

JO - Geophysical Research Letters

JF - Geophysical Research Letters

SN - 0094-8276

IS - 18

M1 - L18504

ER -

ID: 5477579