Studies of Von Karman's Similarity Theory and Its Extension to Compressible Flows. A Critical Examination of Similarity Theory For Incompressible Flows

Abstract

The classical theories for turbulent shear flow are the momentum transfer theory of Prandtl, the vorticity transfer theory of Taylor, and the similarity theory of Von Karman. The two transfer theories both involve a mixture length, which must be given by an additional assumption. On the other hand, the similarity theory is a more determinate scheme, because it makes a more definite hypothesis about the nature of the turbulent fluctuations. Goldstein, however, introduced an alternative form of the similarity theory. A great amount of work has been done to evaluate the relative merits of these three theories. Further investigation into the nature of turbulent motion is, however, done largely in connection with the simpler case of isotropic turbulence. In this field, much recent progress has been made, particularly following the concept of Kolmogoroff. The concept of similarity also plays a dominant role. Since Kolmogoroff's theory is also applicable to shear flow, it is natural that one should reexamine the similarity theory of Von Karman by using modern concepts. This is the main purpose of the present investigation. It is found that the original form of the theory is supported by modern concepts.

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Nov 01, 1951
Accession Number
ADA380505

Entities

People

  • C. C. Lin
  • S. F. Shen

Organizations

  • Massachusetts Institute of Technology

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Boundaries
  • Boundary Layer
  • Compressible Flow
  • Equations
  • Flow
  • Frequency
  • Incompressible Flow
  • Layers
  • Momentum
  • Momentum Transfer
  • Navier Stokes Equations
  • Reynolds Number
  • Shear Flow
  • Turbulent Boundary Layer
  • Turbulent Flow
  • Two Dimensional
  • Viscosity

Readers

  • Fluid Dynamics.
  • Theoretical Analysis.