Temperature Variation during Salt Migration in Frozen Hydrate-Bearing Sediments: Experimental Modeling
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...
I tiakina i:
| Ngā kaituhi matua: | , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
MDPI AG
2022-06-01
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| Rangatū: | Geosciences |
| Ngā marau: | |
| Urunga tuihono: | https://www.mdpi.com/2076-3263/12/7/261 |
| Ngā Tūtohu: |
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