Evaporation and transport of non-dilute, multi-component liquid mixtures in porous wicks: Simulation and experimental validation

被引:6
作者
Beyhaghi, Saman [1 ]
Pillai, Krishna M. [1 ]
Qadah, Diab T. [2 ]
Dietz, Mark L. [2 ]
机构
[1] Univ Wisconsin, Lab Flow & Transport Studies Porous Media, Dept Mech Engn, Milwaukee, WI 53211 USA
[2] Univ Wisconsin, Dept Chem & Biochem, Milwaukee, WI 53211 USA
关键词
Evaporation; Mass transfer; Porous media; Polymer wick; Multicomponent mixture; Gas chromatography; MASS-TRANSFER; ORGANIC-COMPOUNDS; SOLUTE TRANSPORT; PHASE-CHANGE; MEDIA; HEAT; FLOW; DIFFUSION; MODEL; SOIL;
D O I
10.1016/j.ijheatmasstransfer.2011.08.022
中图分类号
O414.1 [热力学];
学科分类号
摘要
Modeling the transport and evaporation of multi-component liquids remains one of the most challenging problems in porous media studies. In this paper, slow isothermal evaporation of a non-dilute multi-component liquid mixture from a cylindrical porous wick made of sintered polymer beads is studied numerically and experimentally. Such wicks are used in several consumer products, such as air-fresheners and insect repellants, for dispensing volatile compounds into air. Since the evaporation rate is much smaller than the rate of capillary-pressure-driven liquid imbibition, the wick is considered fully-saturated while the evaporation from the wick top is modeled as a boundary effect. A volume-averaged model based on the work of Quintard and Whitaker is adapted to set the nonlinear species-transport equations inside the fully-saturated porous wick. Three numerical models with progressively increasing levels of complexity are employed to solve the governing equations in a one-dimensional domain representing the unidirectional, axial flow in a cylindrical wick. The Darcy velocity inside the wick is determined from evaporation rate at the wick-top, which in turn is a function of mole-fractions of all components at the liquid-air interface. Using the proposed numerical models, the evaporated liquid-mass and the composition of liquid mixture within the wick are predicted as functions of time. Results of the simulations are compared with experiments for a non-dilute mixture of decane, dodecane and hexadecane. Good agreement is observed for the three models, especially for the component concentration distributions along the wick, without the use of any fitting parameters. The evaporation rate is found to be a strong function of two model parameters: the porous-medium tortuosity and the air-film thickness at wick top. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:5216 / 5230
页数:15
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