Critical point shift in a fluid confined between opposing walls

被引:32
作者
Carlon, E
Drzewinski, A
机构
[1] Katholieke Univ Leuven, Inst Theoret Phys, B-3001 Louvain, Belgium
[2] Polish Acad Sci, Inst Low Temp & Struct Res, PL-50950 Wroclaw 2, Poland
来源
PHYSICAL REVIEW E | 1998年 / 57卷 / 03期
关键词
D O I
10.1103/PhysRevE.57.2626
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
The properties of a fluid, or Ising magnet, confined in an LX infinity geometry with opposing surface fields at the walls, is studied by density matrix renormalization techniques. In particular we focus on the effect of gravity on the system, which is modeled by a bulk field whose strength varies linearly with the distance from the walls. It is well known that, in the absence of gravity, phase coexistence is restricted to temperatures below the wetting temperature. We find that gravity restores phase coexistence up to the bulk critical temperature, in agreement with previous mean field results. A detailed study of the scaling to the critical point, as L-->infinity, is performed. The temperature shift scales as 1/L-yT, while the gravitational constant scales as 1/L1+yH, with y(T) and y(H) the bulk thermal and magnetic exponents, respectively. For weak surface fields and L not too large, we also observe a regime where the gravitational constant scales as 1/L1+yH-Delta tyr (Delta 1 is the surface gap exponent), with a crossover, for sufficiently large L, to a scaling of type 1/L1+yH.
引用
收藏
页码:2626 / 2633
页数:8
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