In a body submerged in a fluid, unsteady forces due to acceleration of that body with respect to the fluid, can be divided into two parts: the virtual mass effect and the Basset force.
The Basset force term describes the force due to the lagging boundary layer development with changing relative velocity (acceleration) of bodies moving through a fluid.[1] The Basset term accounts for viscous effects and addresses the temporal delay in boundary layer development as the relative velocity changes with time. It is also known as the "history" term. The Basset force is difficult to implement and is commonly neglected for practical reasons; however, it can be substantially large when the body is accelerated at a high rate.[2]
Consider an infinitely large plate started impulsively with a step change in velocity—from 0 to u0—in a direction parallel to the plate–fluid interface plane.
where u(y,t) is the velocity of the fluid, at some time t, parallel to the plate, at a distance y from the plate, and vc is the kinematic viscosity of the fluid (c~continuous phase). The solution to this equation is,[5]
Assuming that an acceleration of the plate can be broken up into a series of such step changes in the velocity, it can be shown[citation needed] that the cumulative effect on the shear stress on the plate is
where up(t) is the velocity of the plate, ρc is the mass density of the fluid, and μc is the viscosity of the fluid.
Acceleration of a spherical particle
Boussinesq (1885) and Basset (1888) found that the force F on an accelerating spherical particle in a viscous fluid is[3][4][6][7]
where D is the particle diameter, and u and v are the fluid and particle velocity vectors, respectively.
↑ C. Crowe et al., Multiphase flows with droplets and particles, CRC Press, 1998, ISBN0-8493-9469-4, p. 81
↑ R.W. Johnson, The handbook of fluid dynamics, CRC Press, 1998, ISBN0-8493-2509-9, pp.18–3
1 2 F. Candelier; J. R. Angilella; M. Souhar (2004), "On the effect of the Boussinesq–Basset force on the radial migration of a Stokes particle in a vortex", Physics of Fluids, 16 (5): 1765–1776, Bibcode:2004PhFl...16.1765C, doi:10.1063/1.1689970
1 2 E. E. Michaelides (2003), "Hydrodynamic force and heat/mass transfer from particles, bubbles, and drops—The Freeman Scholar Lecture", Journal of Fluids Engineering, 125 (2): 209–238, doi:10.1115/1.1537258
↑ F. M. White (2006) [2006], Viscous fluid flow, New York: McGraw Hill, Chapter 3
↑ J. V. Boussinesq (1885), "Sur la résistance qu'oppose un fluide indéfini au repos, sans pesanteur, au mouvement varié d'une sphère solide qu'il mouille sur toute sa surface, quand les vitesses restent bien continues et assez faibles pour que leurs carrés et produits soient négligeables", Comptes Rendus de l'Académie des Sciences, 100: 935–937
↑ A. B. Basset (1961) [1888], Treatise on hydrodynamics, vol.2, Cambridge: Deighton, Bell and Co., Chapter 22
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