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Dynamics of poro-viscoelastic wetting with large swelling

  • Bo Xue Zheng (Corresponding author)
  • , Tak Shing Chan (Corresponding author)
  • , Harald Van Brummelen (Corresponding author)
  • , Jacco H. Snoeijer (Corresponding author)

Onderzoeksoutput: Bijdrage aan tijdschriftTijdschriftartikelAcademicpeer review

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The deposition of droplets onto a swollen polymer network induces the formation of a wetting ridge at the contact line. Current models typically consider either viscoelastic effects or poroelastic effects, while polymeric gels often exhibit both properties. In this study, we investigate the growth of the wetting ridge using a comprehensive large-deformation theory that integrates both dissipative mechanisms-viscoelasticity and poroelasticity. In the purely poroelastic case, following an initial instantaneous incompressible deformation, the growth dynamics exhibits scale-free behaviour, independent of the elastocapillary length or system size. A boundary layer of solvent imbibition between the solid surface (in contact with the reservoir) and the region of minimal chemical potential is created. At later times, the ridge equilibrates on the diffusion time scale given by the elastocapillary length. When viscoelastic properties are incorporated, our findings show that, during the early stages (prior to the viscoelastic relaxation time scale), viscoelastic effects dominate the growth dynamics of the ridge and solvent transport is significantly suppressed. Beyond the relaxation time, the late-time dynamics closely resembles that of the purely poroelastic case. These findings are discussed in light of recent experiments, showing how our approach offers a new interpretation framework for wetting of polymer networks of increasing complexity.

Originele taal-2Engels
ArtikelnummerA58
Aantal pagina's23
TijdschriftJournal of Fluid Mechanics
Volume1025
Vroegere onlinedatum19 dec. 2025
DOI's
StatusGepubliceerd - 25 dec. 2025

Bibliografische nota

Publisher Copyright:
© The Author(s), 2025. Published by Cambridge University Press.

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