Absorption Metric
Capillary pressure profiles that govern the rate of liquid penetration into porous media describe fluid movement through interconnected channels under laminar flow conditions. The classical lucas-washburn formulation models fluid uptake by balancing capillary driving force against viscous drag inside cylindrical pore idealisations. Applied to coated board and paper converting, it calculates penetration depth as a function of surface tension, contact angle, fluid dynamic viscosity, mean pore radius and elapsed contact time.
The model relies on the assumption that pore geometries act as straight, parallel bundles of uniform radius, ceasing to apply when fibre swelling, paper surface chemical dissolution or external mechanical pressure override natural capillary action.
Governing Equations
Mathematical derivations balance the Laplace pressure across a curved meniscus with Poiseuille resistance along a liquid column. The standard lucas-washburn relation states that penetration distance squared equals pore radius multiplied by surface tension and the cosine of contact angle, multiplied by time, all divided by twice the dynamic viscosity. Doubling the effective pore radius doubles penetration depth squared for identical fluid properties.
Tortuosity factors modify the expression in compressed fibrous sheets to reflect irregular paths between compacted cellulose strands. High-viscosity lithographic oils move sluggishly into small pigment pores, whereas low-viscosity flexographic carriers penetrate porous newsprint substrates rapidly under the same capillary gradient.
Substrate Limits
Paper webs deviate from idealised cylindrical capillary assumptions because paper surfaces consist of irregular fibre networks, binder films and mineral distributions. As polar liquids such as water-based inks enter non-sized packaging grades, cellulose fibres undergo hygroscopic expansion, altering the real void geometry during liquid transit. Internal sizing treatments introduce variable surface energies throughout the thickness, modifying the wetting angle dynamically as the fluid front advances.
The relation predicts liquid movement accurately only during initial, non-pressurised wetting stages where structural changes remain minimal.