Interfacial Transport Phenomena
Interfacial Transport Phenomena
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DOI：
10.1007/978-1-4757-2090-7
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发表时间：
1990
期刊：
影响因子：
--
通讯作者：
J. C. Slattery
中科院分区：
文献类型：
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作者：
J. C. Slattery
这里用传递现象来描述动量、能量、质量和熵的传递[1,2]。它包括热力学，一个特殊的例子是吸热学。界面输运现象是指在一个相界面附近的动量、能量、质量和熵的传递，包括界面的热力学。在定性物理观察方面，这是一个非常古老的领域。老普林尼（Plinius Secundus，公元23-79年；Pliny b[3]）描述了潜水员从他们的嘴里释放少量的油，以潮湿海洋表面的毛细血管涟漪，从而为他们的工作提供更均匀的照明。本杰明·富兰克林（Benjamin Franklin）也讲过类似的故事，他自己也在英国做过实验。就分析而言，这是一个普遍年轻的领域。地面恒温器的发展相对较早，从吉布斯[5]开始，后来又有许多人做出了重要贡献（见第四章）。Derjaguin和landau b[6]， Verwey和Overbeek b[7]指出了伦敦-范德华力和静电双层力如何被纳入连续介质力学，现在通常被称为DLVO理论。但在1960年以前，有关动力系统分析的著名论文相对较少。有两个在我的脑海中很突出。Boussinesq[8]识别了表面应力张量，并提出了我们现在称之为Boussinesq表面流体模型的本构方程（第4节）。9. 5）.
Transport phenomena is used here to describe momentuin, energy, mass, and entropy transfer [1, 2]. It includes thermodynamics, a special case of which is thermosiaiics. Interfacial transport phenomena refers to momentum, energy, mass, and entropy transfer within the immediate neighborhood of a phase interface, including the thermodynamics of the interface. In terms of qualitative physical observations, this is a very old field. Pliny the Elder (Gains Plinius Secundus, 23-79 AD; Pliny [3]) described divers who released small quantities of oil from their mouths, in order to damp capillary ripples on the ocean surface and in this way provide more uniform lighting for their work. Similar stories were retold by Benjamin Franklin, who conducted experiments of his own in England [4]. In terms of analysis, this is a generally young field. Surface thermostat ics developed relatively early, starting with Gibbs [5] and continuing with important contributions by many others (see Chap. 4). Derjaguin and Lan dau [6] and Verwey and Overbeek [7] indicated how London-van der Waals and electrostatic double-layer forces were to be incorporated in continuum mechanics, now often referred to as DLVO theory. But prior to 1960, there were relatively few notable papers concerned with the analysis of dynamic systems. Two stand out in my mind. Boussinesq [8] recognized the surface stress tensor and proposed the constitutive equation that we now refer to as the Boussinesq surface fluid model (Sect. 4. 9. 5).