Equilibrium Contact Angle and Adsorption Layer Properties with Surfactants

被引:31
|
作者
Thiele, Uwe [1 ,2 ,3 ]
Snoeijer, Jacco H. [4 ,5 ]
Trinschek, Sarah [1 ,6 ]
John, Karin [6 ]
机构
[1] Westfalische Wilhelms Univ Munster, Inst Theoret Phys, D-48149 Munster, Germany
[2] Westfalische Wilhelms Univ Munster, Ctr Nonlinear Sci CeNoS, D-48149 Munster, Germany
[3] Westfalische Wilhelms Univ Munster, CMTC, D-48149 Munster, Germany
[4] Univ Twente, Phys Fluids Grp, POB 217, NL-7500 AE Enschede, Netherlands
[5] Univ Twente, JM Burgers Ctr Fluid Dynam, POB 217, NL-7500 AE Enschede, Netherlands
[6] Univ Grenoble Alpes, CNRS, Lab Interdisciplinaire Phys, F-38000 Grenoble, France
关键词
GENERIC GRID INTERFACE; THIN LIQUID-FILMS; LINE TENSION; FINGERING INSTABILITY; HYDROPHILIC SURFACES; DYNAMICS; DROPS; SIMULATION; STABILITY; EVOLUTION;
D O I
10.1021/acs.langmuir.8b00513
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The three-phase contact line of a droplet on a smooth surface can be characterized by the Young equation. It relates the interfacial energies to the macroscopic contact angle theta(e). On the mesoscale, wettability is modeled by a film-heightdependent wetting energy f(h). Macro- and mesoscale descriptions are consistent if gamma cos theta(e) = gamma + f(h(a)), where gamma and h(a) are the liquid-gas interface energy and the thickness of the equilibrium liquid adsorption layer, respectively. Here, we derive a similar consistency condition for the case of a liquid covered by an insoluble surfactant. At equilibrium, the surfactant is spatially inhomogeneously distributed, implying a nontrivial dependence of theta(e) on surfactant concentration. We derive macroscopic and mesoscopic descriptions of a contact line at equilibrium and show that they are consistent only if a particular dependence of the wetting energy on the surfactant concentration is imposed. This is illustrated by a simple example of dilute surfactants, for which we show excellent agreement between theory and time-dependent numerical simulations.
引用
收藏
页码:7210 / 7221
页数:12
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