Definitive equations for the fluid resistance of spheres

Published under licence by IOP Publishing Ltd
, , Citation C N Davies 1945 Proc. Phys. Soc. 57 259 DOI 10.1088/0959-5309/57/4/301

0959-5309/57/4/259

Abstract

For calculation of terminal velocities it is convenient to express the Reynolds' number, Re, of a moving sphere as a function of the dimensionless group ψRe2, where ψ is the drag coefficient. The following equations have been fitted by the method of least squares to critically selected data from a number of experimenters:

  1. Re = ψRe2/24 -0.00023363(ψRe2)2 + 0.0000020154(ψRe2)3 - 0.0000000069105(ψRe2)4 for Re<4 or ψRe2<140. This tends to Stokes' law for low values ofRe. It is specially suited to calculation of the sedimentation of air-borne particles. The upper limit corresponds to a sphere weighing 1.5 μg. falling in the normal atmosphere, that is, one having a diameter of 142 μ for unit density.

  2. logRe=-1.29536+0.986 (logψRe2)-0.046677 (logψRe2)2+0.0011235 (logψRe2)3 for 3<Re<10,000 or 100<ψRe2<4.5.107.

Correction for slip in gases should be applied to Stokes' law by the following expression, based on the best results available:

1 + l/a[1.257 + 0.400exp(-1.10a/l)],

where the mean free path l is given by η/0.499σc.

This conveniently transforms to the following for the sedimentation of particles in air at pressure p cm. mercury

1 + l/pa[6.32.10-4 + 2.01.10-4exp(-2190ap)]

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