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- W4283640641 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 hydrate dissociation and ice melting. The hydrate-saturated frozen soils cool down at higher rates than their hydrate-free counterparts and require more time to recover their initial temperature. The temperature effects in hydrate-saturated frozen sediments exposed to contact with NaCl solutions depend strongly on salt concentration. The experimental results are used to model phase changes in the pore space associated with salt-ions transport and provide insights into the reasons for temperature changes." @default.
- W4283640641 created "2022-06-29" @default.
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- W4283640641 date "2022-06-27" @default.
- W4283640641 modified "2023-10-14" @default.
- W4283640641 title "Temperature Variation during Salt Migration in Frozen Hydrate-Bearing Sediments: Experimental Modeling" @default.
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- W4283640641 doi "https://doi.org/10.3390/geosciences12070261" @default.
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