2. Natural internal convection
The concepts developed above are used in this section for situations, encountered in a large number of applications, where natural convection develops inside a duct or in a cavity. First we look at the "chimney" problem (natural convection in a vertical duct), then at convection in cavities. We'll then look at the case of threshold convection in a horizontal layer heated from below (Rayleigh-Bénard problem), followed by two cases of convection in cavities: thermal convection in a cavity whose vertical walls are differentially heated, and thermosolutal convection.
In this section, the conventions for axes are as follows: x (u ) represents the horizontal coordinate (velocity component), and z (w ) the vertical coordinate (velocity component).
Exclusive to subscribers. 97% yet to be discovered!
You do not have access to this resource.
Click here to request your free trial access!
Already subscribed? Log in!
The Ultimate Scientific and Technical Reference
This article is included in
Physics and chemistry
This offer includes:
Knowledge Base
Updated and enriched with articles validated by our scientific committees
Services
A set of exclusive tools to complement the resources
Practical Path
Operational and didactic, to guarantee the acquisition of transversal skills
Doc & Quiz
Interactive articles with quizzes, for constructive reading
Natural internal convection
Bibliography
A complete bibliography on natural convection goes far beyond the scope of the articles Natural convection. Theoretical aspects
Exclusive to subscribers. 97% yet to be discovered!
You do not have access to this resource.
Click here to request your free trial access!
Already subscribed? Log in!
The Ultimate Scientific and Technical Reference