Scaling of solvation force in 2D Ising strip
arXiv:0808.3350 · doi:10.1103/PhysRevE.78.060602
Abstract
The solvation force for the 2D Ising strip is calculated via exact diagonalization of the transfer matrix in two cases: the symmetric case corresponds to identical surface fields, and the antisymmetric case to exactly opposite surface fields. In the symmetric case the solvation force is always negative (attractive) while in the antisymmetric case the solvation force is positive (repulsive) at high temperatures and negative at low temperatures. It changes sign close to the critical wetting temperature characterizing the semi--infinite system. The properties of the solvation force are discussed and the scaling function describing its dependence on temperature, surface field, and strip's width is proposed.
References in corpus (2)
Cited by in corpus (14)
- Casimir interactions in Ising strips with boundary fields: exact results
- Crossover of Critical Casimir forces between different surface universality classes
- Critical Casimir Effect: Exact Results
- The imperfect Bose gas in d dimensions: critical behavior and Casimir forces
- The phase behaviour and structure of a fluid confined between competing (solvophobic and solvophilic) walls
- Casimir force in the O(n -> infinity) model with free boundary conditions
- Thermodynamic Casimir Effect in Films: the Exchange Cluster Algorithm
- Properties of the solvation force of a two-dimensional Ising strip in scaling regimes
- Critical Casimir forces between defects in the 2D Ising model
- Critical and near critical phase behaviour and interplay between the thermodynamic Casimir and van der Waals forces in confined non-polar fluid medium with competing surface and substrate potentials
- Probing interface localization-delocalization transitions by colloids
- Thermodynamic Casimir forces in strongly anisotropic systems within the class
- Casimir Force in a Model with Strongly Adsorbing Competing Walls: Analytical Results
- Manipulation and amplification of the Casimir force through surface fields using helicity