论文标题

对流的密度分层的基础

Foundations of Convection with Density Stratification

论文作者

Mizerski, Krzysztof A.

论文摘要

热和组成(化学)对流的现象本质上非常普遍,因此从理解环境和宇宙的许多基本方面的角度来看,非常重要。已经写了许多关于该主题的书籍,例如Chandrasekhar(1961)在流体动力和水磁稳定性方面的开创性工作,其中很大一部分致力于其发作的对流不稳定性或Getling Of Getling(1998)的杰出书籍,在此,对对流的知识的系统化一直持续到对弱非线性阶段的详尽描述。但是,大多数作品被认为是弱分层的,即所谓的Boussinesq对流。 本书的目的是继续进行系统化过程。在两种情况下,将当前的知识放在薄弱和强烈分层的对流上,并提供对对流流的边际,弱非线性和完全发展的对流阶段的全面描述。为此,本书提供了有关Boussinesq对流的线性和弱非线性限制的简短知识汇编,作为读者的有用参考,而不是对完全发达,弱分层对流的理论进行回顾。整个第三章致力于详细的推导和对上述三个分层(无弹性)对流的研究。分层对流的描述需要极大的谨慎,因为必须同时考虑许多方面以达到完全的一致性。因此,提供了详细的和系统的解释。这本书是作为用于使用讲师和学生的流体动力学和对流流程课程的教科书,但是,整个科学界也可能使用它作为实际参考。

The phenomenon of thermal and compositional (chemical) convection is very common in nature and therefore of great importance from the point of view of understanding of many fundamental aspects of the environment and universe. A number of books have been written on the topic, such as e.g. the seminal work of Chandrasekhar (1961) on Hydrodynamic and Hydromagnetic Stability, a large portion of which is devoted to the convective instability near its onset or the outstanding book of Getling (1998) where systematization of the knowledge on convection has been continued with a thorough description of the weakly nonlinear stages. Most of the works, however, considered weakly stratified, that is the so-called Boussinesq convection. It is the aim of this book to continue the process of systematization. It seems important to put the current knowledge on weakly and strongly stratified convection in order and provide a comprehensive description of the marginal, weakly nonlinear and fully developed stages of convective flow in both cases. To that end the book provides a short compendium of knowledge on the linear and weakly nonlinear limits of the Boussinesq convection, as a useful reference for a reader and than proceeds with a review of the theory on fully developed, weakly stratified convection. The entire third chapter is devoted to a detailed derivation and a study of the three aforementioned stages of stratified (anelastic) convection. The description of stratified convection requires extreme care, since many aspects have to be considered simultaneously for full consistency. Detailed and systematic explanations are therefore provided. This book is meant as a textbook for courses on hydrodynamics and convective flows, for the use of lecturers and students, however, it may also be of use for the entire scientific community as a practical reference.

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