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Phys. Fluids 17, 013102 (2005); http://dx.doi.org/10.1063/1.1829625 (8 pages)

Exact solutions for two-dimensional steady flows of a power-law liquid on an incline

Carlos Alberto Perazzo1 and Julio Gratton2

1Universidad Favaloro, Solís 453, 1078 Buenos Aires, Argentina
2INFIP CONICET, Departamento de Física, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pab. I, Buenos Aires, Argentina

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(Received 7 June 2004; accepted 20 August 2004; published online 10 December 2004)

Under assumptions that are not too restrictive it is possible to reduce the equations that describe steady viscous gravity flows of a power-law liquid on an inclined plane to an equivalent problem consisting of an unsteady one-dimensional nonlinear diffusion process. In a paper dealing with the steady spreading flow of a Herschel–Buckley liquid, Wilson and Burgess [“The steady, spreading flow of a rivulet of mud,” J. Non-Newtonian Fluid Mech. 79, 77 (1998) ] noticed a formal analogy between the steady, two-dimensional viscous gravity flows of a power-law liquid on an incline and a one-dimensional time-dependent nonlinear diffusion phenomena; however, they did not pursue the matter further. Here we develop the analogy and show how it can be used to find a large number of exact solutions representing steady two-dimensional flows of power-law liquids, based on the available knowledge concerning nonlinear diffusion. We describe flows whose widths stay constant until a certain distance from the source, which are analogous to the well-known waiting-time solutions of nonlinear diffusion. We then introduce a phase-plane formalism that allows us to find self-similar solutions and we give as examples three different currents limited laterally by a wall that ends abruptly and currents on an inclined stripe. Finally we describe the two-dimensional currents that are analogous to the traveling wave solutions of the nonlinear diffusion equation. The approximations involved in the analogy are essentially equivalent to those of the lubrication theory, so that they do not impose restrictions more severe than those usually present in problems of this type. The present theory does not include surface tension effects, which implies that the appropriate Bond number must be large.

© 2005 American Institute of Physics

Article Outline

  1. THE ANALOGY
    1. Point source solution
  2. INITIALLY NONWIDENING SOLUTIONS
  3. SELF-SIMILAR SOLUTIONS
    1. Flows limited laterally by a wall that ends abruptly
    2. Flows on an inclined strip
  4. SOLUTIONS THAT DEPEND ON y–cx
  5. DISCUSSION

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1070-6631 (print)  
1089-7666 (online)

For access to fully linked references, you need to log in.
    L. Kondic and J. Diez, "Pattern formation in the flow of thin films down an incline: Constant flux configuration," Phys. Fluids 13, 3168 (2001)PHFLE6000013000011003168000001.

    C. A. Perazzo and J. Gratton, "Thin film of non-Newtonian fluid on an incline," Phys. Rev. E 67, 016307 (2003).

    J. A. Diez, R. Gratton, and J. Gratton, "Self-similar solution of the second kind for a convergent viscous gravity current," Phys. Fluids A 4, 1148 (1992)PFADEB000004000006001148000001.

    B. M. Marino, L. P. Thomas, R. Gratton, J. A. Diez, S. Betelú, and J. Gratton, "Waiting-time solutions of a nonlinear diffusion equation: Experimental study of a creeping flow near a waiting front," Phys. Rev. E 54, 2628 (1996).

    L. W. Schwartz and E. E. Michaelides, "Gravity flow of a viscous liquid down a slope with injection," Phys. Fluids 31, 2739 (1988)PFLDAS000031000010002739000001.

    J. Gratton, F. Minotti, and S. Mahajan, "Theory of creeping gravity currents of a non-Newtonian liquid," Phys. Rev. E 60, 6960 (1999).


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