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The '''speed of sound''' c varies depending on the medium through which the ] waves pass. It is usually quoted in describing properties of substances (e.g. see the article on ]).

More commonly the term refers to the speed of sound in ]. The ] affects very little the speed of sound nor does it the sound pressure, but more important is the temperature. An approximate speed (in metres/second) can be calculated from:

:<math>c_{\mathrm{air}} = (331{.}5 + 0{.}6 \ \cdot \vartheta) \ \mathrm{m/s}</math>

where <math>\vartheta</math> (theta) is the temperature in degrees ] or centigrade.

A more accurate expression is

:<math>c = \sqrt{\gamma RT}</math>

where ''R'' is the ] (287 J/kgK for air), &gamma; is the ] (1.4 for air), and ''T'' is the absolute temperature in ]. In the standard atmosphere, ''T''<sub>0</sub> is 298.15 K, giving a value of 346 m/s (25°C = 77°F).

In fluids, using the theory of ], the speed of sound can be calculated using

:<math>c = \sqrt{{\gamma p}\over\rho}</math>

This is correct for adiabatic flow; Newton famously used isothermal calculations and omitted the &gamma; from the numerator.

The speed of sound is typically measured given a "standard atmosphere". Under these conditions the speed of sound is approximately 346 ] at 25°C, or 750 miles/hour.

In solids the speed of sound is given by:

:<math>c = \sqrt{\frac{E}{\rho}}</math>

where ''E'' is ] and &rho; is ]. Thus in ] the speed of sound is approximately 5100 m/s.<br>
For air, see ].

The speed of sound in water is of interest to those mapping the ] floor. In saltwater, sound travels at about 1500 m/s and in freshwater 1435 m/s. These speeds vary due to pressure, depth, temperature, salinity and other factors.

See also ].

Revision as of 19:39, 8 March 2004