1) Conception of Noise
The sound created in the
air is caused by the diaphragm moving back and forth
in the air which sets the air particles to vibrating,
producing a variation in normal atmospheric pressure.
As these pressure variations spread they may come into
contact with our ear drums causing them to vibrate.
The vibrations of our ear drums are then translated
by our complicated hearing mechanisms into the sensations
we call "SOUND". It should be noted here that
sound is defined in two ways; first as a physical disturbance
- in this case in the air, and secondly as a sensation
in the ear of the listener.
Normally when we hear the
sound of an orchestra, we refer to it as music, something
pleasing to the ear. But, if we were to hear an orchestra
during the middle of our normal sleeping period this
would then be noise to us. Noise is defined as unwanted
sound. Sound, in turn, can be described as repeated
pressure fluctuations characterized by its amplitude
or sound pressure, its frequency in time, and its spatial
variation or wave length. The velocity of sound in air
is approximately 1,130 ft per second at standard temperature
and pressure. Velocity, frequency, and wave length can
be expressed by the equation: frequency x wavelength
= velocity.
Sound propagates in air as
a longitudinal wave, that is a wave where the motion
of small regions of the medium is parallel to the direction
of propagation. These pressure variations will occur
at a given position with the frequency (f), equal to
the frequency of the source disturbance. The distance
between pressure peaks at any instant in time will be
the velocity divided by the frequency;
Wavelength = c / f = 1130
/ 1000 = 1.13 ft.
Octave
Band Center Frequencies (Hz)
|
Band
Edge Frequencies (Nominal Bandwidths)
|
31.5
|
22.3
- 44.6
|
63
|
44.6
- 88.5
|
125
|
88.5
- 177
|
250
|
177
- 354
|
500
|
354
- 707
|
1,000
|
707
- 1,414
|
2,000
|
1,414
- 2,830
|
4,000
|
2,830
- 5,650
|
8,000
|
5,650
- 11,300
|
16,000
|
11,300
- 22,600
|
Since our hearing mechanism
can only hear frequencies in the range of 20 Hz (CPS)
to 20 KHz this is all that most sound level meters attempt
to measure. Only those persons with very keen hearing
are able to hear 20 Hz to 20,000 Hz. For this reason
most codes are established to measure the sound energy
between 45 Hz and 11.3 Khz inclusive. But the initial
range mention has been divided into sub-divisions called
octave bands, as given in below table, with the width
of the band having a ratio for the lower frequency to
the higher frequency of 2:1. These standard octave bands
are named by their center frequencies. The purpose for
dividing the frequency range up in this manner is because
the ear seems to sense frequency on such a logarithmic
scale.
When more detailed analysis
of the distribution of sound energy as a function of
frequency is required the bands are normally divided
into one-third octave bands. This form of analysis gives
a better indication as to which frequencies are most
troublesome and is very useful when noise levels are
excessive and need to be lowered.
The term of decibel has been
borrowed from the electrical communications engineering
group, and is a dimensionless quantity. By definition,
it is 10 times the logarithm (to the base 10) of a quantity
(in dimensional units), to some reference quantity (in
the same dimensional units); with these units being
proportional to power. It is most convenient to use
this logarithmic scale because the range of acoustic
powers that are of interest in noise measurement are
approximately one quintillion to one (1018:
1). For example, the sound power of a soft whisper is
about 0.000000001 watts (10-9), whereas,
the sound power of a ram jet is about 100,000 watts.
This wound be extremely difficult to plot on a linear
scale but when plotted against decibels of sound power
(with reference to 10-12 watts) these equal
30 and 170 decibels.
As indicated in the previous
paragraph, sound power is normally expressed as a power
level with respect to a reference power. Power level
(PWL) is defined as; PWL = 10 Log (W / 10-12)
re 10-12 watts, where W is the acoustic
power in watts and re means referred to. It sound
be noted here that no instrument for directly measuring
the power level of a source is available. Sound power
is a measure of the intensity of a sound (watt/m2)
at its source and cannot be measured directly at some
distant point.
From the elementary physics
that the intensity I of a wave is defined as the time
average rate which energy is transported by the wave
per unit area across a surface perpendicular to the
direction of propagation. More briefly, the intensity
is the average power transported per unit area. Here
we would note that the power developed by a force equals
the product of force times velocity. Hence, the power
per unit area in a sound wave equals the product of
the excess pressure (force per unit area) times the
particle velocity. Averaging over one cycle, it can
be proved that I = rcv2
= P2/rc. Where
P (= rcv) is the pressure
amplitude, r is the average density of air, and c is
the velocity of the sound wave. It will be noted that
the intensity (power) is proportional to the square
of the pressure amplitude, a result which is true for
any sort of wave motion.
Obviously what we measure
with the sound-level meters are these pressure fluctuations
which we read as decibels of sound pressure levels.
The definition of sound pressure level (SPL) is 20 Log
(P in mirobars/0.0002 microbars) or 10 Log (I/10-12),
where P is the root mean-square sound pressure (RMS)
of sound in question. The unit used to measure pressure
here is the microbar which is approximately one-millionth
of the normal atmospheric pressure (standard atmospheric
pressure = 1,013,250 microbars). The reference sound
pressure was obtained from the relation of P0
= (rcI0)1/2
= (400 x 10 -12) 1/2 = 2 x 10
-5 (Pascal). (rc is
called Specific Acoustic Resistance and its value is
about 400(SI).)
If we can measure only sound
pressure at some distant point from a source, how do
we determine the sound power of the source in question?
Let us investigate the manner in which the sound intensity
radiates from a simple source. Assume for a moment that
we have a small spherical sound source, such as a balloon,
that radiates energy uniformly over its entire surface.
Also, let this sphere be located far enough away from
the ground and all other obstructions (free field) so
that it will radiate energy uniformly in all directions.
If the total energy is I0 at the sphere then
the total energy at some given radius from the source
will be spread over an area equal to the area of the
sphere at this radius. This area is equal to 4 pr2.
As we proceed radially outward from this sphere we notice
that energy per unit area varies as the ratio of the
square of the radii and, as we have already shown, this
energy also varies as the square of the pressure. From
this information we are able to write an expression
for sound power level (PWL) as
I = W / (Surface of Sphere
= 4 pr2) for free
field, or W = 4 pr2I,
where r is a distance from a source in meter.
SPL = 10 Log (I/10-12)
PWL = 10 Log (W/10-12)
= 10 Log (4 pr2I/10-12)
= 10 Log (I/10-12) + 10 Log (4 pr2)
= SPL + 10 Log r2 + 10 Log (4p)
= SPL + 10 Log r2 + 10.99 (or SPL + 10 Log
r2 + 0.67, r in foot)
I = W / (Surface of Half
Sphere = 2pr2)
for half free field (= smooth ground level)
PWL = 10 Log (2pr2I/10-12)
= SPL + 10 Log r2 + 7.98 (or SPL + 10 Log
r2 - 0.23)
From above equations, we
can see that SPL at half free field is higher than SPL
at free field by 3.01 dB(A). Most generally the sound
source is setting on the ground with obstacles around
it. These obstructions will either reflect or absorb
this sound.
Consider, for instance, a
source that is setting on a flat reflective surface
so that all the sound energy is being spread over a
hemisphere. Obviously there is twice as much energy
per unit area of any given hemisphere as there would
be for a similar sphere of the same radius; assuming
that we have the same uniform source. If we wished to
calculate the free field sound power level of the source
we would have to correct for this directivity factor.
Here we should define exactly what is meant by directivity
factor. It is the ratio of the mean-square pressure
(or intensity) on a specified axis of a transducer and
at a stated distance to the mean-square pressure (or
intensity) with reference to the mean-square pressure
that would be produced at the same position by a spherical
source if it were radiating the same total acoustical
power. A free field is assumed as the environment for
the measurement. The point of observation must be sufficiently
remote from the transducer for spherical divergence
to exist.
What does this mean? Here
we are saying that our previously defined equations
are good for a uniform sound source. Actually, there
are few, if any, uniform sound sources. Most will radiate
sound energy more directly in one direction than in
others. The directivity factor is the ratio of the mean-square
pressure at some point with reference to what a uniform
source would radiate in that direction in free space.
This says that a source may have a directivity factor
of more than 1.0 in some directions and less in others.
It also says that anytime sound is reflected, you change
the direcivity factor.
Let us take an example of
what this means in actual practice. Suppose a customer
buys some unit that is rated at 85 dB (SPL) in free
field tests at some specified distance. He installs
this unit in his place of business against a concrete
wall and takes a reading at the specified distance with
a calibrated sound-level meter. He determines the SPL
to be 90 dB, and assumes the manufacturers did not correctly
state the SPL at this distance. In actually, the manufacturers
stated free field test results were probably accurate,
but the customer did not properly consider such things
as the room characteristics (reverberation, absorption,
etc.) and the fact that the unit us not in free space.
It would suffice to say here that obtaining proper sound
power levels (PWL) and then applying these are complicated
to say the least.
A method of determining sound
power that is used by the compressed air, and the fan
and blower industry is essentially a comparison method
but it is very effective in giving reproducible test
results. This method requires the running of tests,
usually in octave bands, of two sources. One being the
source in question, the other being a calibrated reference
sound source. The reference sound source (RSS) is a
source with approximately the same sound spectrum as
the source in question, but whose PWL has been determined
from free field tests. The procedure goes like this:
- A test is run on the RSS
at some specified distance.
- The RSS is replaced with
the sound source in question and another test is run
with the microphone setting in the same place as the
first test.
- Since the PWL of the RSS
is known we can obtain the correction for distance,
directivity factor, absorption, etc. by subtracting
the SPL of the test on the RSS from the known PWL.
PWL - SPL (of the RSS) = correction
- This correction is then
added to the SPL of the source in question, which
gives you the PWL of the source in free field conditions.
So far, we have been discussing
sound from a purely physical view. What about our second
definition of sound. That of sound being the sensation
our ears translate as such. Three different filters,
called A, B, and C scales, are used to distinguish from
sound pressure levels. For example, a measurement of
80 dB on the A scale is reported as a sound level of
80 dB(A). It is well to note here that the A scale was
designed to correspond roughly to what our ears respond
to in the range of 0 dB to 65 dB over-all. The B scale
corresponds to the response in the range of 65 to 85
dB. The C scale, which is roughly linear, from 63 to
8000 Hz, corresponds fairly well to the ears response
above 85 dB.
To be continued. Please press the next button....
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