Thermal Conductivity of Frozen and Unfrozen Gas-Saturated Soils

Arctic permafrost often contains gas-saturated horizons. The gas component in freezing and frozen soils can exist under different pressures, which are expected to affect their properties and behavior. The effect of pore gas pressure on the thermal conductivity of frozen and unfrozen silt loam satura...

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Main Authors: Evgeny Chuvilin, Dinara Davletshina, Boris Bukhanov, Sergey Grebenkin
Format: Article
Language:English
Published: MDPI AG 2023-11-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/13/11/347
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author Evgeny Chuvilin
Dinara Davletshina
Boris Bukhanov
Sergey Grebenkin
author_facet Evgeny Chuvilin
Dinara Davletshina
Boris Bukhanov
Sergey Grebenkin
author_sort Evgeny Chuvilin
collection DOAJ
description Arctic permafrost often contains gas-saturated horizons. The gas component in freezing and frozen soils can exist under different pressures, which are expected to affect their properties and behavior. The effect of pore gas pressure on the thermal conductivity of frozen and unfrozen silt loam saturated with methane or carbon dioxide at pressures below the hydrate formation conditions is observed in the current study. The variable gas pressure and temperature conditions are simulated in a specially designed pressure cell, which allows thermal conductivity measuring in pressurized samples at positive and negative temperatures. The experiments using natural samples collected near the gas emission crater (Yamal Peninsula) show that thermal conductivity is sensitive to pore gas pressure even at high moisture contents. The thermal conductivity of methane-saturated soil becomes 4% and 6% higher in frozen and unfrozen samples, respectively, as the gas pressure increases from 0.1 MPa to 2 MPa. In the case of CO<sub>2</sub> saturation, the respective thermal conductivity increase in frozen and unfrozen samples reaches 25% and 15% upon pressure change from 0.1 to 0.9 MPa. The results stimulate further special studies of the effects of gas type and pressure on the thermal properties of closed gas-saturated taliks, of which the pore pressure is increasing during freezing up.
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spelling doaj.art-a3298dfaff2645afb6d7fcf87c73867a2023-11-24T14:44:30ZengMDPI AGGeosciences2076-32632023-11-01131134710.3390/geosciences13110347Thermal Conductivity of Frozen and Unfrozen Gas-Saturated SoilsEvgeny Chuvilin0Dinara Davletshina1Boris Bukhanov2Sergey Grebenkin3Center for Petroleum Science and Engineering, Skolkovo Institute of Science and Technology (Skoltech), Skolkovo Innovation Center, 121205 Moscow, RussiaCenter for Petroleum Science and Engineering, Skolkovo Institute of Science and Technology (Skoltech), Skolkovo Innovation Center, 121205 Moscow, RussiaCenter for Petroleum Science and Engineering, Skolkovo Institute of Science and Technology (Skoltech), Skolkovo Innovation Center, 121205 Moscow, RussiaCenter for Petroleum Science and Engineering, Skolkovo Institute of Science and Technology (Skoltech), Skolkovo Innovation Center, 121205 Moscow, RussiaArctic permafrost often contains gas-saturated horizons. The gas component in freezing and frozen soils can exist under different pressures, which are expected to affect their properties and behavior. The effect of pore gas pressure on the thermal conductivity of frozen and unfrozen silt loam saturated with methane or carbon dioxide at pressures below the hydrate formation conditions is observed in the current study. The variable gas pressure and temperature conditions are simulated in a specially designed pressure cell, which allows thermal conductivity measuring in pressurized samples at positive and negative temperatures. The experiments using natural samples collected near the gas emission crater (Yamal Peninsula) show that thermal conductivity is sensitive to pore gas pressure even at high moisture contents. The thermal conductivity of methane-saturated soil becomes 4% and 6% higher in frozen and unfrozen samples, respectively, as the gas pressure increases from 0.1 MPa to 2 MPa. In the case of CO<sub>2</sub> saturation, the respective thermal conductivity increase in frozen and unfrozen samples reaches 25% and 15% upon pressure change from 0.1 to 0.9 MPa. The results stimulate further special studies of the effects of gas type and pressure on the thermal properties of closed gas-saturated taliks, of which the pore pressure is increasing during freezing up.https://www.mdpi.com/2076-3263/13/11/347permafrostgas-saturated sedimentsthermal propertyexperimental modellingfreezing under gas pressurethermal conductivity
spellingShingle Evgeny Chuvilin
Dinara Davletshina
Boris Bukhanov
Sergey Grebenkin
Thermal Conductivity of Frozen and Unfrozen Gas-Saturated Soils
Geosciences
permafrost
gas-saturated sediments
thermal property
experimental modelling
freezing under gas pressure
thermal conductivity
title Thermal Conductivity of Frozen and Unfrozen Gas-Saturated Soils
title_full Thermal Conductivity of Frozen and Unfrozen Gas-Saturated Soils
title_fullStr Thermal Conductivity of Frozen and Unfrozen Gas-Saturated Soils
title_full_unstemmed Thermal Conductivity of Frozen and Unfrozen Gas-Saturated Soils
title_short Thermal Conductivity of Frozen and Unfrozen Gas-Saturated Soils
title_sort thermal conductivity of frozen and unfrozen gas saturated soils
topic permafrost
gas-saturated sediments
thermal property
experimental modelling
freezing under gas pressure
thermal conductivity
url https://www.mdpi.com/2076-3263/13/11/347
work_keys_str_mv AT evgenychuvilin thermalconductivityoffrozenandunfrozengassaturatedsoils
AT dinaradavletshina thermalconductivityoffrozenandunfrozengassaturatedsoils
AT borisbukhanov thermalconductivityoffrozenandunfrozengassaturatedsoils
AT sergeygrebenkin thermalconductivityoffrozenandunfrozengassaturatedsoils