Acoustic impedance
Basic Principles
Acoustic impedance
Z (or sound impedance) is the ratio
of sound pressure p to particle velocity v. Also it is the product of the density
of air ρ (rho) and the speed
of sound c. The acoustic impedance Z is expressed in rayl (from Rayleigh,
in N·s·m-3=Pa·s/m):
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with p = sound pressure, in N/m2
= Pa = pascal,
v = particle velocity in m/s,
J = sound intensity in W/m2,
ρ (rho) = density of the medium (air)
air in kg/m3,
c = speed of sound (the acoustic wave velocity) in m/s.
v is
the acoustic analogue of electric current, and p the analogue of voltage. Table
3 gives the densities (ρ), sound velocities (c) and acoustic impedance (Z)
is of some bio-materials.
Table 1

In dry air at
Under normal conditions air is nearly a
perfect gas,
and so its speed does hardly depend on air pressure and on humidity.
Sound travels
slower with an increased altitude, primarily as a result of temperature and
humidity changes. The approximate speed (in m/s) is:
(7)
where tC
is the temperature in o C. A more accurate expression is
(8)
where γ is the adiabatic
index or cp/cV ratio, the ratio of heat capacity of
the gas (cp) with constant p and the specific heat capacity of the
gas (cV) with constant V, T the absolute temperature (K), and R (287.05 J/(kg·K) for air) the
universal gas constant (see Gas laws) In this case, the gas constant R, which normally has units of
J/(mol·K), is divided by the molar mass of air. The derivation can be found in various textbooks. For air γ
= 1.402.
Ultrasound Sound speed is a basic parameter in ultrasound
applications, especially for moving objects (like the valves of the heart)
which movement is determined by the Doppler effect (see Doppler principle).
More info
Hearing For an equal sound pressure in two
materials, v is reciprocally with Z. For instance Zwater ≈
4000 Zair, and so the particle velocity in water is 4000 smaller
than that in air. Therefore, also the particle velocity of a sound impinging
from a source in the air onto the head is 4000 times smaller than in the air.
The resulting vibration of the head gives rise to bone conduction, but with
respect to the sound sensation evoked by the pressure impinging onto the
eardrum it is irrelevant.
Speed of sound Under normal
conditions air is nearly a perfect gas, and so its speed does hardly
depend on air pressure and on humidity.
Sound travels
slower with an increased altitude, primarily as a result of temperature and
humidity changes. The approximate speed (in m/s) is:
(7)
where tC
is the temperature in o C. A more accurate expression is
(8)
where γ is the adiabatic
index or cp/cV ratio, the ratio of heat capacity of
the gas (cp) with constant p and the specific heat capacity of the
gas (cV) with constant V, T the absolute temperature (K), and R (287.05 J/(kg·K) for air) the
universal gas constant (see Gas laws) In this case, the gas constant R, which normally has units of
J/(mol·K), is divided by the molar mass of air. The derivation can be found in various textbooks. For air γ
= 1.402.
See further Sound and acoustics, Ultrasound and the Doppler principle.