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Acoustics

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Acoustics Week 1: *Fundamentals of Sound *Sound Levels and the Decibel Fundamentals of Sound Sound can be defined as a wave motion in air or other elastic media ... – PowerPoint PPT presentation

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Title: Acoustics


1
Acoustics
  • Week 1
  • Fundamentals of Sound
  • Sound Levels and the Decibel

2
Fundamentals of Sound
  • Sound can be defined as a wave motion in air or
    other elastic media (stimulus) or as that
    excitation of the hearing mechanism that results
    in the perception of sound (sensation).
  • Frequency is a characteristic of periodic waves
    measured in hertz (cycles per second), readable
    on an oscilloscope or frequency counter. The ear
    perceives a different pitch for a quiet tone than
    a loud one. The pitch of a low-frequency tone
    goes down, while the pitch of a high-frequency
    tone goes up as intensity increases. We cannot
    equate frequency and pitch, but they are
    analogous.
  • The same situation exists between intensity and
    loudness. The relationship between the two is not
    linear.
  • Similarly, the relationship between waveform (or
    spectrum) and perceived quality (or timbre) is
    complicated by the functioning of the hearing
    mechanism.

3
Sine Waves
  • The sine wave is a basic waveform closely related
    to simple harmonic motion. Vibration or
    oscillation is possible because of the elasticity
    of the spring and the inertia of the weight.
    Elasticity and inertia are two things all media
    must possess to be capable of conducting sound.

4
Sine Wave Language
  • The easiest value to read is the peak-to-peak
    value (of voltage, current, sound pressure,
    etc.). If the wave is symmetrical, the
    peak-to-peak value is twice the peak value.
    Another common way to measure the sine wave is
    using RMS (Root Mean Square) values. The other
    two scales of measurement used are peak and
    average. The picture to the right shows four
    different ways that a sine waves amplitude can
    be measured and the equations used for
    conversions.

5
Propagation of Sound
  • If an air particle is displaced from its original
    position, elastic forces of the air tend to
    restore it to its original position. Because of
    the inertia of the particle, it overshoots the
    resting position.
  • Sound is readily conducted in gases, liquids, and
    solids such as air, water, steel, etc., which are
    all elastic media.
  • Without a medium, sound cannot be propagated.
    Outer space is an almost perfect vacuum no sound
    can be conducted due to the absence of air.
  • Particles of air propagating a sound wave do not
    move far from their undisplaced positions.

6
Forms of Particle Motion
  • There is more than a million molecules in a cubic
    inch of air.
  • The molecules crowded together represent areas of
    compression and the sparse areas represent
    rarefactions.

7
Sound in Free Space
  • The intensity of sound decreases as the distance
    to the source is increased.
  • Doubling the distance reduces the intensity to
    1/4 the initial value, tripling the distance
    yields 1/9, increasing the distance four times
    yields 1/16 the initial intensity.
  • The inverse square law states that the intensity
    of sound in a free field is inversely
    proportional to the square of the distance from
    the source.

8
Wavelength, Period, Frequency
  • The wavelength is the distance a wave travels in
    the time it takes to complete one cycle. The
    period is the time it takes a wave to complete
    one cycle. The frequency is the number of cycles
    per second (Hertz).

9
Wavelength and Frequency
Formulas for calculating wavelength and
frequency. The speed of sound in air is about
1,130 feet per second at normal temperature and
pressure.
Two graphical approaches for an easy solution to
the above equations.
10
Complex Waves
  • The sine wave with the lowest frequency (f1) is
    called the fundamental, the one with twice the
    frequency (f2) is called the second harmonic, and
    the one three times the frequency (f3) is the
    third harmonic. Harmonics are whole number
    multiples of the fundamental frequency.

11
Phase
  • Phase is the time relationship between waveforms.
    Each waveform is lagging the previous by 90
    degrees.

12
Combinations of Waveforms
  • Combinations of waveforms that are not in phase.
    The difference in waveshapes is due entirely to
    the shifting of the phase of the harmonics with
    respect to the fundamental.

13
Harmonics and Octaves
14
Spectrum
  • The audio or frequency spectrum of the human ear
    is about 20 Hz to 20 kHz. The spectrum tells how
    the energy of the signal is distributed in
    frequency. For the ideal sine wave, all the
    energy is concentrated at one frequency. All
    other types of waveforms have more than one
    frequency present.
  • The diagram shows various types of waveforms and
    their harmonic content. The sine, triangle, and
    square waves are known as period waves due to
    their cyclic pattern.

15
Sound Levels and the Decibel
  • Levels in decibels make it easy to handle the
    extremely wide range of sensitivity in human
    hearing.
  • The threshold of hearing matches the ultimate
    lower limit of perceptible sound in air.
  • A level in decibels is a convenient way of
    handling the billion fold range of sound
    pressures to which the ear is sensitive without
    getting bogged down in a long string of zeros.

16
Ratios vs. Difference
  • Ratios of pressure seem to describe loudness
    changes better than difference in pressure.
  • Ernst Weber (1834), Gustaf Fechner (1860),
    Hermann von Helmholtz (1873), and other
    researchers pointed out the importance of ratios.
  • Ratios of stimuli come closer to matching up with
    human perception than do differences of stimuli.
  • Ratios of powers, intensities, sound pressure,
    voltage, or anything else are unitless. This is
    important because logarithms can be taken only of
    unitless numbers.

17
Handling Numbers
  • Here are three different ways that numbers can be
    expressed

18
Handling Numbers, contd.
19
Back to Basics Math
  • The study of acoustics requires a knowledge of
    some basic algebra.

20
More Math...
21
More Math...
22
More Math...
23
More Math...
24
More Math...
25
More Math...
26
More Math...
27
More Math...
28
More Math...
29
More Math...
30
More Math...
31
More Math...
32
Exponents A Review
33
Exponents, contd.
34
Exponents, contd.
35
Exponents, contd.
36
Exponents, contd.
37
Exponents, contd.
38
Exponents, contd.
39
Exponents, contd.
40
Practice Problems
41
Logarithms
42
Logarithms
43
Logarithms
44
Practice Problems
45
Practice Problems
Theorem 1
46
Decibels
  • A level is a logarithm of a ratio of two
    like-power quantities.
  • A level in decibels is ten times the logarithm to
    the base 10 of the ratio of two power quantities.

47
Decibels
  • Sound pressure is proportional to (sound power)2.
  • The squaring of the sound power results in the
    equation SPL 20 log (p1/p2) instead of 10 log.

48
Sound Pressure Level (SPL)
  • Sound pressure is usually the most accessible
    parameter to measure in acoustics, as voltage is
    for electronic circuits. For this reason, the
    Equation (2-3) form is more often encountered in
    day-to-day technical work.

49
Reference Levels
  • A sound level meter is used to read sound
    pressure levels. A sound level meter reading is a
    certain sound pressure level, 20 log (p1/p2). For
    sound in air, the standard reference pressure is
    20 µPa (micropascal). The µPa is a very minute
    sound pressure and corresponds closely to the
    threshold of human hearing.
  • The equations to the right show how to convert
    SPL (in dB) to µPa.

50
Log-to-Exponent Conversion
  • Heres another quick look at the math used to
    convert logs to exponents

51
Acoustic Reference Levels
52
Acoustic Reference Levels
  • Greek prefixes used for the powers of 10

53
Pascals vs. Decibels
  • Doubling of acoustic power is an increase of 3 dB
    (10 log 2 3.01).
  • Doubling of acoustic pressure is an increase of 6
    dB (20 log 2 6.02)

54
Pascals vs. Decibels
55
Decibel Level Examples
  • Here are some examples of decibel level
    conversions

56
Decibel Level Examples
57
Examples, contd.
58
Examples, contd.
59
Reflected Sound
  • The equations below show how to calculate
    Reflection Delay and Reflection Level.

60
Examples, contd.
61
Examples, contd.
62
Examples, contd.
63
Ratios and Octaves
  • An octave is defined as a 21 ratio of two
    frequencies. The ratio 32 is a fifth and 43 is
    a fourth.

64
Examples
65
Examples, contd.
66
Measuring Sound Pressure Level
  • Sound level meters usually offer a selection of
    weighting networks designated A, B, and C.
    Network selection is based on the general level
    of sounds to be measured. For SPLs of 20 55 dB,
    use network A. For 55 85 dB use network B, and
    for 85 140 dB, use network C.

67
Equal Loudness Contours
68
The Precedence (Haas) Effect
69
SPL Changes With Distance
  • The Inverse Square Law says that the intensity of
    sound is inversely proportional to the square of
    the distance from the point source.

70
Inverse Distance Law
  • The Inverse Square Law of intensity becomes the
    Inverse Distance Law for sound pressure. Sound
    pressure level is reduced 6 dB for each doubling
    of distance.

71
Critical Distance
  • The Critical Distance is that distance at which
    the direct sound pressure is equal to the
    reverberant sound pressure.
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