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| What
is a decibel (dB)? |
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The decibel is a relative unit, not an absolute. Decibels are used
to compare values of like quantities, usually power and intensity,
on a numerical scale. For example:
- An intensity ratio
of 10 translates to 10 decibels
- An intensity ratio
of 100 translates to a level difference of 20 decibels
- An intensity ratio
of 1000 translates to a level difference of 30 decibels
To be meaningful,
a decibel needs a reference point. For example: |
- In water we use
a standard reference sound pressure of 1 microPascal
- In air we use a
higher standard of reference of 20 microPascals
- It is essential
that sound levels expressed in decibels include the reference
pressure
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Comparison of Various
Noise Sources in the Ocean:
| Noise
Sources |
Sound
Levels |
| Lightning
Strike on Water Surface |
260
dB (approximately) (1) |
| Seafloor
Volcanic Eruption |
255
dB (approximately) (2) |
| Sperm
Whale |
163-180
dB (3) |
| Fin
Whale |
160-186
dB (3) |
| Humpback
Whale |
144-174
dB (3) |
| Bowhead
Whale |
128-189
dB (3) |
| Blue
Whale |
155-188
dB (3)&(4) |
| Southern
Right Whale |
172-187
dB (3) |
| Gray
Whale |
142-185
dB (3) |
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Note: All decibels (dB) are re 1 µPa at 1 m. |
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References:
- Hill, R.D. 1985.
Investigation of lightning strikes to water surface. JASA 78(6):2096-2099.
- Dietz, R.S. and
M.J. Sheehy. 1954. Transpacific detection of myojin volcanic explosions
by underwater sound. Bull. of the Geolog. Soc. Vol. II: 942-956;
and Northrup, J. 1974. Detection of low-frequency underwater sounds
from a submarine volcano in the Western Pacific. JASA 56(3):837-841.
- Richardson, W.J.,
C.R. Greene, C.I. Malme, and D.H. Thomson. 1995. Marine mammals
and noise. Academic Press, Inc., San Diego, CA.
- Aroyan, J.L., M.A.
McDonald, S.C. Webb, J.A. Hildebrand, D. Clark, J.F. Laitman and
J.S. Reidenberg. 2000. Acoustic models of sound production and
propagation. In: Au, W.W.L., A.N. Popper and R.R. Fay (Eds.).
2000. Hearing by whales and dolphins. Springer-Verlag, New York,
NY.
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What is Source Level and Received Level? |
- In underwater acoustics,
source level usually represents the sound level at a distance
of one meter from the source, referenced to one microPascal
- The received level
is the sound level at the listener's actual position which is
usually considerably more distant that the reference source level
- Underwater, loudness
decreases rapidly with increasing source-receiver distance
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| Received
levels of sound underwater at 10, 100, and 1000 meters from a 200
dB source level referenced to one microPascal at one meter.
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| How
is Sound in Water Different from Sound in Air? |
- Comparing sound
levels in air against sound levels in water must be done very
carefully. First, by accepted convention, the reference pressure
values are different by 26 dB. Second, due to the difference in
impedance (the stiffness or density of the medium) between air
and water, roughly a 3,500 times greater power level (35.5 dB)
is required in air to produce an equivalent pressure level in
water. Combining these two values, a 61.5 dB difference, or correction
factor, between the two scales is required. Therefore, 61.5 dB
must be subtracted from a sound level in water to produce an equivalent
acoustic intensity in air. A 60 dB difference represents a million-fold
power difference. It is misleading to compare the underwater sound
made by a system like SURTASS LFA with sounds heard in the air.
- Given the potential
for confusion between sound levels in air and those in water,
the EIS generally avoids cross-media comparisons between air and
water. All sound values are water-standard values unless otherwise
specified. Also, all references are broadband-level values given
in dBs, standardized at 1 microPascal at 1 m (dB re 1 microPa
at 1 m) for source levels (SL) and dB re 1 microPa rms (root mean
squared) for received levels (RL).
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