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Автор Dickens, Gerald R.
Автор Quinby‐Hunt, Mary S.
Дата выпуска 1994
dc.description Experimental data are presented for methane hydrate stability conditions in seawater (S ≈ 33.5‰). For the pressure range of 2.75–10.0 MPa, at any given pressure, the dissociation temperature of mcthane hydrate is depressed by approximately −1.1°C relative to the pure methane‐pure water system. These experimental results are consistent with previously reported thermodynamic predictions and experimental results obtained with artificial seawater. Collectively these results provide a minimum constraint concerning depth ranges over which methane hydrate is stable in the oceanic environment.
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Копирайт Copyright 1994 by the American Geophysical Union.
Тема BIOGEOSCIENCES
Тема Nutrients and nutrient cycling
Тема EXPLORATION GEOPHYSICS
Тема Seismic methods
Тема GEOCHEMISTRY
Тема Marine geochemistry
Тема MARINE GEOLOGY AND GEOPHYSICS
Тема Marine seismics
Тема Continental shelf and slope processes
Тема OCEANOGRAPHY: GENERAL
Тема Continental shelf and slope processes
Тема Oceanography: General: Physical and chemical properties of sea water
Тема OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL
Тема Marine organic chemistry
Тема SEISMOLOGY
Тема Seismic instruments and networks
Название Methane hydrate stability in seawater
Тип article
DOI 10.1029/94GL01858
Electronic ISSN 1944-8007
Print ISSN 0094-8276
Журнал Geophysical Research Letters
Том 21
Первая страница 2115
Последняя страница 2118
Выпуск 19
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