Journal of the Society of Materials Science, Japan
Online ISSN : 1880-7488
Print ISSN : 0514-5163
ISSN-L : 0514-5163
Voidage Function of Sedimentation Related with Reynolds Number
Kouji SAKASHITAHaruo WATANABE
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1975 Volume 24 Issue 262 Pages 682-685

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Abstract
The sedimentation rate of multiparticle suspension in a stationary fluid, um, decreases with increasing particle concentrations. The voidage function F(ε) is defined as F(ε)=v/um, where v is the terminal velocity of single particle in the infinite stationary fluid.
In order to generalize the voidage function to cover the entire ranges of flow, namely, laminar (St), intermediate (Al), and turbulent (N) flow regions, the following equation is given.
FSt(ε)=[FAl(ε)]m=[FN(ε)]2
where m varies from 1 to 1.63 continuously with Reynolds number in the intermediate flow region, when calculated from the drag coefficient correlation of a single sphere motion according to Schiller. Previously, Richardson-Zaki has pointed out that m varies from 1 to 2 in the same intermediate flow region and some other investigators reported m to be 1.4 or constant.
The voidage function in each flow region, obtained from the correlations of Kozeny-Carman or Ergun, has been found in good agreement with the voidage function of Richardson-Zaki in a certain range of voidage.
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© by The Society of Materials Science, Japan
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