2022
DOI: 10.3390/geosciences12070261
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Temperature Variation during Salt Migration in Frozen Hydrate-Bearing Sediments: Experimental Modeling

Abstract: Salt migration may be another reason why pore-gas hydrates dissociate in permafrost, besides pressure and temperature changes. Temperature variations in frozen hydrate-saturated sediments interacting with a NaCl solution have been studied experimentally at a constant temperature, ~−6 °C typical for permafrost. The experiments with frozen sandy samples containing metastable methane hydrate show that the migration of Na+ ions in the NaCl solution and their accumulation in the sediments can induce heat-consuming … Show more

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Cited by 5 publications
(6 citation statements)
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“…It can be seen that the curve Frontiers in Energy Research frontiersin.org shape of position 1A and 2A has similar "well" shape. The temperature decreased firstly because of the intense endothermic process of hydrate dissociation promoted by the salt effect of the self-heating solution, which phenomenon had been reported widely in other studies (Yuan et al, 2013a;Chuvilin et al, 2022). And then, the temperature increased to the highest temperature point 60 °C, which is because of the continuous heat supply from the chemical reaction between NaNO 2 and NH 4 Cl.…”
Section: Temperature Variation Characteristics During the Self-heatin...mentioning
confidence: 79%
“…It can be seen that the curve Frontiers in Energy Research frontiersin.org shape of position 1A and 2A has similar "well" shape. The temperature decreased firstly because of the intense endothermic process of hydrate dissociation promoted by the salt effect of the self-heating solution, which phenomenon had been reported widely in other studies (Yuan et al, 2013a;Chuvilin et al, 2022). And then, the temperature increased to the highest temperature point 60 °C, which is because of the continuous heat supply from the chemical reaction between NaNO 2 and NH 4 Cl.…”
Section: Temperature Variation Characteristics During the Self-heatin...mentioning
confidence: 79%
“…Equilibrium disturbance is essential for CH 4 production through carbon dioxide injection/mixed gas injection, thermal stimulation, ,, depressurization, chemical inhibitor injection, or a combination of these. , The advantages and disadvantages of these methods are listed in Table . However, the depressurization method is the best reported through experiments with low operation costs, having been tested successfully in the United States, Japan, China, Russia, and Canada. There are around 230 natural gas hydrate deposits worldwide, with at least 1.5 × 10 15 m 3 of natural gas deposits . Natural gas hydrates are formed in the continental margins (∼97%) at a sea bed in the depth ranges of 800–4000 m and permafrost regions (∼3%) (polar areas) characterized by low temperature .…”
Section: Theorymentioning
confidence: 99%
“…In addition to the temperature and pressure changes, destabilization of gas hydrates can result from reactions with various organic or inorganic chemical agents that inhibit hydrate formation: salts, acids, and other compounds [21][22][23][24][25][26][27][28]. The effect of dissolved salts on the pressure and temperature limits of hydrate stability has received much attention [21,23,[29][30][31][32][33].…”
Section: Introductionmentioning
confidence: 99%