Moisture migration within the melting laps during construction controls frost heaving damage of lining in permafrost tunnels

Frost heaving damage is a typical hazard in tunnels constructed in cold regions, among which frost heave induced by the freezing expansion of surrounding rock stands as one of the primary factors leading to stress concentration and even cracking failure in lining structures. Under the influence of construction thermal disturbances, the thawing of surrounding rock is accompanied by moisture redistribution, where the characteristics of water distribution play a critical role in governing frost heave. This study establishes a thermal-hydro-mechanical (THM) coupled model for melting laps, validated through the Jiangluling Tunnel case. Integrating laboratory freezing tests on gravel soils with numerical simulations, we investigate moisture migration impacts on lining frost heaving damage under construction thermal disturbance and operational refreezing. The results indicate: (1) The numerical simulations align closely with field monitoring data, validating the accuracy of the model for this project. (2) Pore ice formation without moisture migration generates negligible frost heave pressure. (3) Moisture redistribution during construction creates water-enriched zones at tunnel flanks, causing tensile stress concentration (peak 6.008 MPa) at lining sidewalls. (4) The tensile stress at the inner walls of the lining initially increases gradually, then rises rapidly, and finally stabilizes. Mechanistic analysis reveals that moisture redistribution within the melting laps under construction thermal disturbance establishes essential material precondition for frost heave. During operational phases, initial frost heave develops in surrounding rocks, which subsequently subjected to seasonal freeze–thaw cycles triggers cumulative frost heave effects. Consequently, maximum tensile stress in lining structures demonstrates progressive annual escalation. This research provides theoretical basis for frost-resistant lining design in permafrost tunnels.

Institutions

Publication Details

Journal
Tunnelling and Underground Space Technology
Published
2025-09-22
DOI
https://doi.org/10.1016/j.tust.2025.107107
Citations
5
Primary Topic
Bioenergy crop production and management
Type
article
Field-Weighted Citation Impact
9.51
Controls
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article

Moisture migration within the melting laps during construction controls frost heaving damage of lining in permafrost tunnels

5 citations
Tunnelling and Underground Space Technology
Bioenergy crop production and management
9.51
article

Moisture migration within the melting laps during construction controls frost heaving damage of lining in permafrost tunnels

article en
5 citations

Abstract

Frost heaving damage is a typical hazard in tunnels constructed in cold regions, among which frost heave induced by the freezing expansion of surrounding rock stands as one of the primary factors leading to stress concentration and even cracking failure in lining structures. Under the influence of construction thermal disturbances, the thawing of surrounding rock is accompanied by moisture redistribution, where the characteristics of water distribution play a critical role in governing frost heave. This study establishes a thermal-hydro-mechanical (THM) coupled model for melting laps, validated through the Jiangluling Tunnel case. Integrating laboratory freezing tests on gravel soils with numerical simulations, we investigate moisture migration impacts on lining frost heaving damage under construction thermal disturbance and operational refreezing. The results indicate: (1) The numerical simulations align closely with field monitoring data, validating the accuracy of the model for this project. (2) Pore ice formation without moisture migration generates negligible frost heave pressure. (3) Moisture redistribution during construction creates water-enriched zones at tunnel flanks, causing tensile stress concentration (peak 6.008 MPa) at lining sidewalls. (4) The tensile stress at the inner walls of the lining initially increases gradually, then rises rapidly, and finally stabilizes. Mechanistic analysis reveals that moisture redistribution within the melting laps under construction thermal disturbance establishes essential material precondition for frost heave. During operational phases, initial frost heave develops in surrounding rocks, which subsequently subjected to seasonal freeze–thaw cycles triggers cumulative frost heave effects. Consequently, maximum tensile stress in lining structures demonstrates progressive annual escalation. This research provides theoretical basis for frost-resistant lining design in permafrost tunnels.

Tunnelling and Underground Space TechnologyVol. 167
Xi'an University of Science and Technology (CN), CCCC Highway Consultants (China) (CN), Institute of Rock and Soil Mechanics (CN)
Climate action
Openalex Percentile: Top 2%
Bioenergy crop production and management
9.51
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