str (101)

str (101)



GE X ERA.


FLOW


J E<?cr.4rj0L

iq>6. tiret ąuoted the eąuation in | {


paper, the calculation having been Dryden ; but the authorehip of the enJSS J generally ascribed to Farrow, Lowe aJJ&0*1 is


equation m ąuestion is

(w ~r 3)^

8®


I


PRy |

LJ


%


where n is the Ostwald exponent, and p repre mobility, but, having dimensions which depe^^is best written with a | bar.” .    111‘, I

This eąuation, of course, reduces to the p0ise eąuation when n — i. It is useful in practi because, when, for different capillaries, log| is plotted against log(PR/2L), the slope gives n, and I is given by

I =: log-1 [log(« + 3) ~ Wt]

where i is the intercept of the log-log curve on the stTess axis. In generał, regarding the capillary tubę as a special case, we can wnte

IB log-1 (log | — I log S),

where i is the ratę of shear, and S the shearing stress.

The dimensional difficulty can be overcome, though admittedly only by a mathematical trick, by taking fjl — — log 1 as the criterion. This is in eftect the log of the viscosity, when the stress is exceedingly smali (i dyne/cm.2), and is, of course, a pure number. The objection to this method is that, in practice, the most useful viscosity is not that found at a very Iow stress, but that which obtains at the kind of stress at włńch the materiał will be used. This objection can be met by ąuoting a true viscosity at some arbitrarily chosen stress. Since viscosities of true fluids all have to be ąuoted at an

GENERAL FLOW EQUAT10N 79

rbitrary temperaturę there is good precedent for

^The^p^ysical significance of this relationship betweenvelocity gradient and shearing stress is not eaSy to appreciate. Some idea of the processes involved will emerge when the work of Eisenschitz is considered in a later chapter.

The Poiseuille, the Buckingham-Reiner, and the Farrow eąuations are clearly special cases of the generał eąuation relating ratę of shear to stress in a capillary, when the functional relationship between velocity gradient and stress is kept generał. This generał eąuation appears in a footnote in a paper by Rabinowitsch; but it was Mooney who first dis-cussed its importance.1 Schofield points out that this generał eąuation is no morę than an algebraic simplification of the Schofield-Scott Blair eąuation, which has already been ąuoted (p. 38).

V 2 rw rw

= w4oSI/(S^'dS>

where W is the stress at the wali, and S the stress at any point (T). This may be written

differentiating

mammm

Schofield gives very interesting grapłucal treat-ments to demonstrate the conditions imder which a

1

The eqnation has been used by others as weli, e.g., Porter and Rao.


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