Gatica Silvina M, Cole Milton W
Department of Physics and Materials Research Institute, 104 Davey Laboratory, Pennsylvania State University, University Park, Pennsylvania 16802, USA.
Phys Rev E Stat Nonlin Soft Matter Phys. 2005 Oct;72(4 Pt 1):041602. doi: 10.1103/PhysRevE.72.041602. Epub 2005 Oct 10.
Using grand canonical Monte Carlo simulations, we have explored the phenomenon of capillary condensation (CC) of Ar at the triple temperature inside infinitely long, cylindrical pores. Pores of radius R = 1 nm, 1.7 nm, and 2.5 nm have been investigated using a gas-surface interaction potential parametrized by the well depth D of the gas on a planar surface made of the same material as that comprising the porous host. For strongly attractive situations--i.e., large D--one or more (depending on R) Ar layers adsorb successively before liquid fills the pore. For very small values of D, in contrast, negligible adsorption occurs at any pressure P below saturated vapor pressure P0; above saturation, there eventually occurs a threshold value of P at which the coverage jumps from empty to full, nearly discontinuously. Hysteresis is found to occur in the simulation data whenever abrupt CC occurs--i.e., for R > or = 1.7 nm--and for small D when R = 1 nm. Then, the pore-emptying branch of the adsorption isotherm exhibits larger coverage than the pore-filling branch, as is known from many experiments and simulation studies. The relation between CC and wetting on planar surfaces is discussed in terms of a threshold value of D, which is about one-half of the value found for the wetting threshold on a planar surface. This finding is consistent with a simple thermodynamic model of the wetting transition developed previously.
通过巨正则蒙特卡罗模拟,我们研究了在无限长圆柱形孔内,氩在三相温度下的毛细凝聚(CC)现象。使用由氩气在与构成多孔主体相同材料的平面上的阱深D参数化的气-表面相互作用势,对半径R = 1纳米、1.7纳米和2.5纳米的孔进行了研究。对于强吸引情况——即大的D——在液体填充孔之前,一个或多个(取决于R)氩层会相继吸附。相反,对于非常小的D值,在低于饱和蒸气压P0的任何压力P下,吸附都可忽略不计;高于饱和时,最终会出现一个P的阈值,此时覆盖率几乎不连续地从空跃变为满。每当发生突然的CC时——即对于R≥1.7纳米——以及当R = 1纳米且D较小时,在模拟数据中都会发现滞后现象。然后,吸附等温线的孔排空分支比孔填充分支表现出更大的覆盖率,这在许多实验和模拟研究中都是已知的。根据D的阈值讨论了CC与平面上的润湿之间的关系,该阈值约为在平面上发现的润湿阈值的一半。这一发现与先前建立的润湿转变的简单热力学模型一致。