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Mechanics of Fluids

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496 Compressible flow <strong>of</strong> gases<br />

Sonic velocity<br />

Mach number<br />

If the fluid is a gas obeying Boyle’s Law, then from eqn 11.4<br />

� �<br />

∂p<br />

∂ρ<br />

= dv<br />

� �<br />

∂p<br />

dρ ∂v<br />

= pγ<br />

ρ<br />

1<br />

since ρ =<br />

v<br />

s<br />

s<br />

The speed <strong>of</strong> propagation <strong>of</strong> a very small pressure wave (relative to the fluid)<br />

is therefore<br />

B, I<br />

a = � (pγ/ρ) B, I (11.19)<br />

Alternatively, from the equation <strong>of</strong> state for a thermally perfect gas,<br />

a = � (γ RT) TPG, I (11.20)<br />

Sound is propagated by means <strong>of</strong> a succession <strong>of</strong> very small pressure waves<br />

in which δp is alternately positive and negative. (The faintest sound that<br />

the human ear can detect unaided corresponds to a pressure fluctuation <strong>of</strong><br />

about 3 × 10−5 Pa; the loudest that can be tolerated without physical pain<br />

corresponds to a fluctuation <strong>of</strong> about 100 Pa.) The velocity represented by<br />

eqns 11.13–11.20 is therefore known as the speed <strong>of</strong> sound or velocity <strong>of</strong><br />

sound or sonic velocity or acoustic velocity in the gas. As it is a function <strong>of</strong><br />

temperature it varies in general from point to point in the fluid. The validity<br />

<strong>of</strong> the assumptions made in deriving the expressions is indicated by the<br />

excellent agreement found with experimental determinations <strong>of</strong> the velocity<br />

<strong>of</strong> sound. For air <strong>of</strong> moderate humidity γ = 1.4 and R = 287 J · kg −1 · K −1 ;<br />

so at 15 ◦C �<br />

�<br />

a = 1.4 × 287 J · kg −1 · K −1 �<br />

(273 + 15) K = 340 m · s −1<br />

The velocity <strong>of</strong> sound is appreciably less at high altitudes because <strong>of</strong> the<br />

lower temperature there.<br />

It is important to note that the preceding expressions refer only to waves<br />

in which the change <strong>of</strong> pressure is very small compared with the pressure<br />

itself. Waves in which a comparatively large pressure change occurs will<br />

be considered in Section 11.5. The assumption <strong>of</strong> constant entropy is not<br />

justified for these larger waves, and they move at velocities greater than that<br />

<strong>of</strong> sound.<br />

When the velocity <strong>of</strong> the fluid at a particular point is less than the velocity<br />

<strong>of</strong> sound there, small pressure waves can be propagated both upstream and<br />

downstream. When, however, the velocity <strong>of</strong> the fluid exceeds the local sonic<br />

velocity a, a small pressure wave cannot be propagated upstream. A velocity<br />

equal to a thus sharply divides two essentially different types <strong>of</strong> flow.<br />

We have seen already in Sections 1.5 and 5.3.4 that it is useful to express<br />

the velocity <strong>of</strong> a gaseous flow in relation to that <strong>of</strong> the sonic velocity. The<br />

Mach number, M, is defined by the relation<br />

M = u/a<br />

where u is the local velocity and a is the speed <strong>of</strong> sound. Fluid velocities less<br />

than the sonic velocity are known as subsonic (M < 1), those greater than

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