The phase behaviour of a simple fluid or Ising magnet (at temperatures above its roughening transition) confined between parallel walls that exert opposing surface fields h 2 = - h 1 is found to be markedly different from that which arises for h 2 = h 1. Whereas critical wetting plays little role for confinement by identical walls, it is of crucial importance for opposing surface fields. Analysis of a Landau functional and other mean-field treatments show that if h 1 is such that critical wetting occurs at a single wall ( L = ∞) at a transition temperature T w , then phase coexistence, for finite wall separation L, is restricted to temperatures T < T c , L, where the critical temperature T c, L lies below T w . In the temperature range T c, b > T > T w there is a single soft mode phase that is characterized, for zero bulk field and large L, by a +- interface located at the centre of the slit, a transverse correlation length ξ ∼≈ e L and a solvation force that is repulsive. For large h 1, T w can lie arbitrarily far below the bulk critical temperature T c, b . Scaling arguments, whose validity we have confirmed in two dimensions by comparison with exact solutions for interfacial Hamiltonians, predict that such behaviour persists beyond mean-field for systems with short-ranged forces. They also predict similar phase behaviour for long-ranged forces, but with ξ ξ ∼ increasing algebraically with L in the soft mode phase. The solvation force t̃f s changes from repulsive to attractive (at large L) as the temperature is reduced below T w , i.e. the sign of t̃f s reflects wetting characteristics.
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