Reconstructing the hydraulic conductivity model of freezing soils based on lubrication theory
Abstract
Accurate characterization of hydraulic conductivity is essential for understanding coupled heat and water transport during soil freezing and thawing. However, conventional models can produce a nonphysical conductivity cutoff under strong supercooling because they oversimplify film-driven transport. Here, an existing combined capillary-film framework is extended by deriving a physically based expression for film flow conductivity. Using established film-thickness relationships to define the geometry, classical lubrication theory is applied to quantify flow velocity and hydraulic conductivity within thin adsorbed water films. Integrating this lubrication-based expression with the capillary flow equation yields a continuous hydraulic conductivity model without an artificial dry-end cutoff. Validation against diverse unfrozen and frozen soil datasets shows that the model performs consistently across the full moisture range and avoids the dry-end failure of the Campbell and van Genuchten models. Parameter sensitivity analyses further clarify how film flow responds to particle radius and porosity. Smaller particles provide greater specific surface area to sustain film flow at low-water contents, whereas lower porosity delays the transition from capillary-dominated to film-dominated transport. The model therefore provides a physically interpretable basis for representing continuous unfrozen-water migration in frozen soils.
Document Type: Original article
Cited as: Yu, C., Wang, F., Hui, C., Li, L., Zhang, S., Li, S. Reconstructing the hydraulic conductivity model of freezing soils based on lubrication theory. Capillarity, 2026, 19(3): 75-85. https://doi.org/10.46690/capi.2026.06.02
DOI:
https://doi.org/10.46690/capi.2026.06.02Keywords:
Frozen soil, hydraulic conductivity, lubrication theory, film flowReferences
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Copyright (c) 2026 Ceting Yu, Fugang Wang, Hui Cheng, Longxuan Li, Yinteng Li, Zhaohui Peng

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