2023
DOI: 10.1021/acs.jced.2c00568
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Stable Isotope Fractionation of Nitrogen between Gas and Hydrate Phases

Abstract: Stable isotope ratios of nitrogen gas in ice core air samples represent a valuable tool for studying the past climate change. In this study, we investigated the stable isotope fractionation of nitrogen between the gas and hydrate phases during nitrogen hydrate formation. Nitrogen hydrate samples were formed in the temperature range of 225–271 K and pressure range of 13–19 MPa. The isotopic compositions of the original, residual (unreacted), and hydrate-bound gases were measured. The nitrogen isotope ratio of t… Show more

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Cited by 2 publications
(2 citation statements)
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“…Researchgrade methane (99.99% purity; Takachiho Chemical Industrial, Tokyo, Japan) was used as the guest gas. In the synthesis process, fine ice powder (0.1 g), with a specific surface area of 350−450 m 2 kg −1 , 34 was placed in the cell, and the air within the cell was evacuated at 77 K. Methane was then introduced into the cell, which was either placed in a cold room (226, 246, and 255 K) or immersed in a temperature-controlled liquid bath (273 K). Methane hydrate formation occurred with approximate formation times of 1 day (246, 255, and 273 K) and 1 week (226 K).…”
Section: ■ Experimental Methodsmentioning
confidence: 99%
“…Researchgrade methane (99.99% purity; Takachiho Chemical Industrial, Tokyo, Japan) was used as the guest gas. In the synthesis process, fine ice powder (0.1 g), with a specific surface area of 350−450 m 2 kg −1 , 34 was placed in the cell, and the air within the cell was evacuated at 77 K. Methane was then introduced into the cell, which was either placed in a cold room (226, 246, and 255 K) or immersed in a temperature-controlled liquid bath (273 K). Methane hydrate formation occurred with approximate formation times of 1 day (246, 255, and 273 K) and 1 week (226 K).…”
Section: ■ Experimental Methodsmentioning
confidence: 99%
“…The hydrogen isotope ratio of the hydrate-bound gas is several ‰ lower than that of the residual gas [9], whereas stable isotope fractionation is negligible in terms of carbon isotope ratios [9,10]. Such stable isotope fractionation of guest gases during gas hydrate formation has been similarly investigated for ethane [9], carbon dioxide [11,12], hydrogen sulfide [13], and nitrogen [14].…”
Section: Introductionmentioning
confidence: 99%