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Mechanics of Fluids

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shared among the occupants <strong>of</strong> bb, and thus layer bb as a whole is speeded<br />

up. Similarly, molecules from the slower layer bb cross to aa and tend to<br />

retard the layer aa. Every such migration <strong>of</strong> molecules, then, causes forces<br />

<strong>of</strong> acceleration or deceleration in such directions as to tend to eliminate the<br />

differences <strong>of</strong> velocity between the layers.<br />

In gases this interchange <strong>of</strong> molecules forms the principal cause <strong>of</strong> viscosity,<br />

and the kinetic theory <strong>of</strong> gases (which deals with the random motions<br />

<strong>of</strong> the molecules) allows the predictions – borne out by experimental observations<br />

– that (a) the viscosity <strong>of</strong> a gas is independent <strong>of</strong> its pressure (except<br />

at very high or very low pressure) and (b) because the molecular motion<br />

increases with a rise <strong>of</strong> temperature, the viscosity also increases with a rise<br />

<strong>of</strong> temperature (unless the gas is so highly compressed that the kinetic theory<br />

is invalid).<br />

The process <strong>of</strong> momentum exchange also occurs in liquids. There is, however,<br />

a second mechanism at play. The molecules <strong>of</strong> a liquid are sufficiently<br />

close together for there to be appreciable forces between them. Relative<br />

movement <strong>of</strong> layers in a liquid modifies these inter-molecular forces, thereby<br />

causing a net shear force which resists the relative movement. Consequently,<br />

the viscosity <strong>of</strong> a liquid is the resultant <strong>of</strong> two mechanisms, each <strong>of</strong> which<br />

depends on temperature, and so the variation <strong>of</strong> viscosity with temperature<br />

is much more complex than for a gas. The viscosity <strong>of</strong> nearly all liquids<br />

decreases with rise <strong>of</strong> temperature, but the rate <strong>of</strong> decrease also falls. Except<br />

at very high pressures, however, the viscosity <strong>of</strong> a liquid is independent <strong>of</strong><br />

pressure.<br />

The variation with temperature <strong>of</strong> the viscosity <strong>of</strong> a few common fluids is<br />

given in Appendix 2.<br />

1.6.3 The dimensional formula and units <strong>of</strong> dynamic viscosity<br />

Dynamic viscosity is defined as the ratio <strong>of</strong> a shear stress to a velocity gradient.<br />

Since stress is defined as the ratio <strong>of</strong> a force to the area over which it<br />

acts, its dimensional formula is [FL −2 ]. Velocity gradient is defined as the<br />

ratio <strong>of</strong> increase <strong>of</strong> velocity to the distance across which the increase occurs,<br />

thus giving the dimensional formula [L/T]/[L] ≡ [T −1 ]. Consequently the<br />

dimensional formula <strong>of</strong> dynamic viscosity is [FL −2 ]/[T −1 ] ≡ [FTL −2 ]. Since<br />

[F] ≡ [MLT −2 ], the expression is equivalent to [ML −1 T −1 ].<br />

The SI unit <strong>of</strong> dynamic viscosity is Pa · s, or kg · m −1 · s −1 , but no special<br />

name for it has yet found international agreement. (The name poiseuille,<br />

abbreviated Pl, has been used in France but must be carefully distinguished<br />

Fig. 1.6<br />

Viscosity 25

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