Slip and friction at fluid-solid interfaces: Concept of adsorption layer
Haodong Zhang, Fei Wang, Britta Nestler
TL;DR
The paper introduces the adsorption layer (AL) as a finite-thickness interfacial region $\delta l$ in which solid–fluid interactions simultaneously drive adsorption/depletion and interfacial slip. By constructing a total energy functional $\mathcal{L}_{T}=\mathcal{F}+\mathcal{P}+\mathcal{K}+\mathcal{K}_{\text{w}}$ for the AL and applying an energy-minimization principle, the authors derive coupled interfacial equations that account for chemical diffusion, viscous stresses, and solid–fluid friction, with explicit pressure coupling across the interface. This framework recovers and generalizes the generalized Navier boundary condition (GNBC) while highlighting the role of normal pressure gradients $\nabla P_{\text{s}}$ and surface chemical potential gradients $\nabla\mu_{\text{s}}$ in determining slip. The model successfully explains confinement-enhanced water slippage in carbon nanotubes and captures spatial slip variations near moving contact lines in binary fluids, demonstrating that the slip length is an emergent, geometry- and composition-dependent quantity rather than a fixed material constant. Overall, the AL approach provides a physically grounded link between molecular-scale interfacial physics and continuum hydrodynamics with strong implications for microfluidics and surface engineering.
Abstract
When a fluid flows past a solid surface, its macroscopic motion arises from a subtle interplay between microscopic hydrodynamic and thermodynamic effects at the fluid-solid interface. Classical hydrodynamic models often rely on an unphysical no-slip boundary condition or an arbitrarily prescribed slip length, yet both approaches lack a rigorous physical foundation. This work introduces the concept of an Adsorption Layer (AL), an interfacial region of thickness delta l, where fluid-solid molecular interactions regulate both surface adsorption/depletion and interfacial slip. By applying the energy minimization principle, we derive balance equations within the AL that couple fluid-solid friction, viscous stresses, and surface adsorption dynamics. This framework establishes a self-consistent thermodynamic coupling between the AL and the bulk fluid, unlike conventional sharp-interface models. A key finding is the often-overlooked role and coupling of pressure and chemical potential gradients in the direction normal to the interface. This theoretical advance successfully explains the confinement-induced enhancement of water slippage in carbon nanotubes, quantitatively agreeing with molecular dynamics and experimental data -- an effect classical slip models fail to reproduce. Furthermore, when extended to binary liquids, the theory captures spatial variations in slip velocity near moving contact lines, highlighting the role of interfacial friction in shaping local flow. Our results demonstrate that the slip length is not a fixed material constant but rather an emergent, geometry- and composition-dependent property arising from coupled interfacial thermodynamics and hydrodynamics. This framework provides a physically grounded description of interfacial momentum transfer, with significant implications for microfluidics and surface engineering.
