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  • Other Sources  (3)
  • FLUID MECHANICS AND HEAT TRANSFER  (3)
  • 2005-2009
  • 1985-1989  (3)
  • 1989  (3)
  • 1
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    Modulated stagnation-point flow and steady streaming (1989)
    In:  Other Sources
    Details
    Publication Date: 2011-08-19
    Description: Plane stagnation-point flow is modulated in the free stream so that the velocity components are proportional to K(H) + K cos omega t. Similarity solutions of the Navier-Stokes equations are examined using high-frequency asymptotics for K and K(H) of unit order. Special attention is focused on the steady streaming generated in this flow with strongly non-parallel streamlines.
    Keywords: FLUID MECHANICS AND HEAT TRANSFER
    Type: Journal of Fluid Mechanics (ISSN 0022-1120); 198; 543-555
    Format: text
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    NASA TECHNICAL REPORTS
  • 2
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    The lubrication force between two viscous drops (1989)
    In:  Other Sources
    Details
    Publication Date: 2019-07-12
    Description: The present determination of the hydrodynamic force resisting the relative motion of two unequal drops moving in Stokes flow conditions along their line of centers assumes that the drops are in near-contact, and possess sufficiently high interfacial tension to remain spherical. Depending on the ratio of drop viscosity to that of the continuous phase, as well as on the ratio of the distance between drops to their reduced radius, three possible flow situations arise: these correspond to nearly-rigid drops, drops with partially mobile interfaces, and drops with fully mobile interfaces.
    Keywords: FLUID MECHANICS AND HEAT TRANSFER
    Type: Physics of Fluids A (ISSN 0899-8213); 1; 77-81
    Format: text
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    NASA TECHNICAL REPORTS
  • 3
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    An asymptotic description of transient settling and ultrafiltration of colloidal dispersions (1989)
    In:  Other Sources
    Details
    Publication Date: 2019-07-12
    Description: The present model for the sedimentation of colloidal systems includes a diffusion term in the governing equation which, in the regions above the sediment, acts as small perturbation to the Kynch (1952) theory. Within the sediment, diffusion is comparable to convection due to the the high solid volume fraction. An application of the method of matched asymptotic expansions to the conservation equation allows a complete description of the settling process to be formulated, with specific attention to volume-fraction evolution in the sediment.
    Keywords: FLUID MECHANICS AND HEAT TRANSFER
    Type: Physics of Fluids A (ISSN 0899-8213); 1; 82-100
    Format: text
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    NASA TECHNICAL REPORTS
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