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Sound pressure
Sound pressure
from Wikipedia
Sound measurements
Characteristic
Symbols
 Sound pressure p, SPL, LPA
 Particle velocity v, SVL
 Particle displacement δ
 Sound intensity I, SIL
 Sound power P, SWL, LWA
 Sound energy W
 Sound energy density w
 Sound exposure E, SEL
 Acoustic impedance Z
 Audio frequency AF
 Transmission loss TL

Sound pressure or acoustic pressure is the local pressure deviation from the ambient (average or equilibrium) atmospheric pressure, caused by a sound wave. In air, sound pressure can be measured using a microphone, and in water with a hydrophone. The SI unit of sound pressure is the pascal (Pa).[1]

Mathematical definition

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Sound pressure diagram:
  1. Silence
  2. Audible sound
  3. Atmospheric pressure
  4. Sound pressure

A sound wave in a transmission medium causes a deviation (sound pressure, a dynamic pressure) in the local ambient pressure, a static pressure.

Sound pressure, denoted p, is defined by where

  • ptotal is the total pressure,
  • pstat is the static pressure.

Sound measurements

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Sound intensity

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In a sound wave, the complementary variable to sound pressure is the particle velocity. Together, they determine the sound intensity of the wave.

Sound intensity, denoted I and measured in W·m−2 in SI units, is defined by where

  • p is the sound pressure,
  • v is the particle velocity.

Acoustic impedance

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Acoustic impedance, denoted Z and measured in Pa·m−3·s in SI units, is defined by[2] where

  • is the Laplace transform of sound pressure,[citation needed]
  • is the Laplace transform of sound volume flow rate.

Specific acoustic impedance, denoted z and measured in Pa·m−1·s in SI units, is defined by[2] where

  • is the Laplace transform of sound pressure,
  • is the Laplace transform of particle velocity.

Particle displacement

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The particle displacement of a progressive sine wave is given by where

It follows that the particle velocity and the sound pressure along the direction of propagation of the sound wave x are given by where

  • vm is the amplitude of the particle velocity,
  • is the phase shift of the particle velocity,
  • pm is the amplitude of the acoustic pressure,
  • is the phase shift of the acoustic pressure.

Taking the Laplace transforms of v and p with respect to time yields

Since , the amplitude of the specific acoustic impedance is given by

Consequently, the amplitude of the particle displacement is related to that of the acoustic velocity and the sound pressure by

Inverse-proportional law

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When measuring the sound pressure created by a sound source, it is important to measure the distance from the object as well, since the sound pressure of a spherical sound wave decreases as 1/r from the centre of the sphere (and not as 1/r2, like the sound intensity):[3]

This relationship is an inverse-proportional law.

If the sound pressure p1 is measured at a distance r1 from the centre of the sphere, the sound pressure p2 at another position r2 can be calculated:

The inverse-proportional law for sound pressure comes from the inverse-square law for sound intensity: Indeed, where

hence the inverse-proportional law:

Sound pressure level

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Sound pressure level (SPL) or acoustic pressure level (APL) is a logarithmic measure of the effective pressure of a sound relative to a reference value.

Sound pressure level, denoted Lp and measured in dB,[4] is defined by:[5] where

  • p is the root mean square sound pressure,[6]
  • p0 is a reference sound pressure,
  • 1 Np is the neper,
  • 1 B = (1/2 ln 10) Np is the bel,
  • 1 dB = (1/20 ln 10) Np is the decibel.

The commonly used reference sound pressure in air is[7]

p0 = 20 μPa,

which is often considered as the threshold of human hearing (roughly the sound of a mosquito flying 3 m away). The proper notations for sound pressure level using this reference are Lp/(20 μPa) or Lp (re 20 μPa), but the suffix notations dB SPL, dB(SPL), dBSPL, and dBSPL are very common, even if they are not accepted by the SI.[8]

Most sound-level measurements will be made relative to this reference, meaning 1 Pa will equal an SPL of . In other media, such as underwater, a reference level of 1 μPa is used.[9] These references are defined in ANSI S1.1-2013.[10]

The main instrument for measuring sound levels in the environment is the sound level meter. Most sound level meters provide readings in A, C, and Z-weighted decibels and must meet international standards such as IEC 61672-2013.

Examples

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The lower limit of audibility is defined as SPL of 0 dB, but the upper limit is not as clearly defined. While 1 atm (194 dB peak or 191 dB SPL)[11][12] is the largest pressure variation an undistorted sound wave can have in Earth's atmosphere (i. e., if the thermodynamic properties of the air are disregarded; in reality, the sound waves become progressively non-linear starting over 150 dB), larger sound waves can be present in other atmospheres or other media, such as underwater or through the Earth.[13]

Equal-loudness contour, showing sound-pressure-vs-frequency at different perceived loudness levels

Ears detect changes in sound pressure. Human hearing does not have a flat spectral sensitivity (frequency response) relative to frequency versus amplitude. Humans do not perceive low- and high-frequency sounds as well as they perceive sounds between 3,000 and 4,000 Hz, as shown in the equal-loudness contour. Because the frequency response of human hearing changes with amplitude, three weightings have been established for measuring sound pressure: A, B and C.

In order to distinguish the different sound measures, a suffix is used: A-weighted sound pressure level is written either as dBA or LA, B-weighted sound pressure level is written either as dBB or LB, and C-weighted sound pressure level is written either as dBC or LC. Unweighted sound pressure level is called "linear sound pressure level" and is often written as dBL or just L. Some sound measuring instruments use the letter "Z" as an indication of linear SPL.[13]

Distance

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The distance of the measuring microphone from a sound source is often omitted when SPL measurements are quoted, making the data useless, due to the inherent effect of the inverse proportional law. In the case of ambient environmental measurements of "background" noise, distance need not be quoted, as no single source is present, but when measuring the noise level of a specific piece of equipment, the distance should always be stated. A distance of one metre (1 m) from the source is a frequently used standard distance. Because of the effects of reflected noise within a closed room, the use of an anechoic chamber allows sound to be comparable to measurements made in a free field environment.[13]

According to the inverse proportional law, when sound level Lp1 is measured at a distance r1, the sound level Lp2 at the distance r2 is

Multiple sources

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The formula for the sum of the sound pressure levels of n incoherent radiating sources is

Inserting the formulas in the formula for the sum of the sound pressure levels yields

Examples of sound pressure

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Examples of sound pressure in air at standard atmospheric pressure
Source of sound Distance Sound pressure level[a]
(Pa) (dBSPL)
Shock wave (distorted sound waves > 1 atm; waveform valleys are clipped at zero pressure)[11][12] >1.01×105 >191
Simple open-ended thermoacoustic device[14] [clarification needed] 1.26×104 176
1883 eruption of Krakatoa[15][16] 165 km 172
.30-06 rifle being fired m to
shooter's side
7.09×103 171
Firecracker[17] 0.5 m 7.09×103 171
Stun grenade[18] Ambient 1.60×103
...8.00×103
158–172
9-inch (23 cm) party balloon inflated to rupture[19] At ear 4.92×103 168
9-inch (23 cm) diameter balloon crushed to rupture[19] At ear 1.79×103 159
9-inch (23 cm) party balloon inflated to rupture[19] 0.5 m 1.42×103 157
9-inch (23 cm) diameter balloon popped with a pin[19] At ear 1.13×103 155
LRAD 1000Xi Long Range Acoustic Device[20] 1 m 8.93×102 153
9-inch (23 cm) party balloon inflated to rupture[19] 1 m 731 151
Jet engine[13] 1 m 632 150
9-inch (23 cm) diameter balloon crushed to rupture[19] 0.95 m 448 147
9-inch (23 cm) diameter balloon popped with a pin[19] 1 m 282.5 143
Loudest human voice[21] 1 inch 110 135
Trumpet[22] 0.5 m 63.2 130
Vuvuzela horn[23] 1 m 20.0 120
Threshold of pain[24][25][21] At ear 20–100 120–134
Risk of instantaneous noise-induced hearing loss At ear 20.0 120
Jet engine 100–30 m 6.32–200 110–140
Two-stroke chainsaw[26] 1 m 6.32 110
Jackhammer 1 m 2.00 100
Hearing damage (over long-term exposure, need not be continuous)[27] At ear 0.36 85
EPA-identified maximum to protect against hearing loss and other disruptive effects from noise, such as sleep disturbance, stress, learning detriment, etc.[28] Ambient 0.06 70
Passenger car at 30 kph (electric and combustion engines)[29] 10 m 0.045–0.063 67-70
TV (set at home level) 1 m 0.02 60
Normal conversation 1 m 2×10−3–0.02 40–60
Passenger car at 10 kph (combustion)[29] 10 m 12.6×10−3 56
Passenger car at 10 kph (electric)[29] 10 m 6.32×10−3 50
Very calm room Ambient 2.00×10−4
...6.32×10−4
20–30
Light leaf rustling, calm breathing[13] Ambient 6.32×10−5 10
Auditory threshold at 1 kHz[27] At ear 2.00×10−5 0
Anechoic chamber, Orfield Labs, A-weighted[30][31] Ambient 6.80×10−6 −9.4
Anechoic chamber, University of Salford, A-weighted[32] Ambient 4.80×10−6 −12.4
Anechoic chamber, Microsoft, A-weighted[33][34] Ambient 1.90×10−6 −20.35
  1. ^ All values listed are the effective sound pressure unless otherwise stated.

See also

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  • Acoustics – Branch of physics involving mechanical waves
  • Phon – Logarithmic unit of loudness level
  • Loudness – Subjective perception of sound pressure
  • Sone – Unit of perceived loudness
  • Sound level meter – Device for acoustic measurements
  • Stevens's power law – Empirical relationship between actual and perceived changed intensity of stimulus
  • Weber–Fechner law – Related laws in the field of psychophysics

References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Sound pressure, also known as acoustic pressure, is the local deviation from the of a medium caused by the of a wave through it. It represents the instantaneous variation in at a specific point in space and is a scalar quantity, distinct from vector quantities like . The SI unit of sound pressure is the pascal (Pa), equivalent to newtons per square meter (N/m²), reflecting the force per unit area exerted by the sound wave. Because sound pressure spans an extremely wide range—from about 20 μPa (the approximate threshold of human hearing) to over 100 Pa for painful levels— it is commonly expressed on a as the sound pressure level (SPL) in decibels (dB). The SPL is calculated using the Lp=20log10(pp0)L_p = 20 \log_{10} \left( \frac{p}{p_0} \right) dB, where pp is the root-mean-square sound and p0=20μPap_0 = 20 \, \mu \mathrm{Pa} is the standard reference in air at 1 kHz, chosen because it aligns closely with the faintest detectable sound for normal human hearing. This reference value ensures that 0 dB SPL corresponds to the threshold of audibility, while typical reaches around 60 dB SPL and jet aircraft can exceed 120 dB SPL. Sound pressure is fundamental to acoustics, enabling the measurement and assessment of noise in environments ranging from everyday settings to industrial and underwater applications. It is typically measured using microphones that convert pressure variations into electrical signals, often with frequency weighting (e.g., A-weighting to mimic human ear sensitivity) to compute metrics like dB(A). Key applications include noise pollution control, audio engineering, hearing conservation, and architectural design for sound insulation, where understanding SPL helps mitigate health risks from excessive exposure, such as hearing loss above 85 dB SPL for prolonged periods. Unlike sound power, which quantifies a source's total acoustic output independently of environment, sound pressure depends on distance, reflections, and medium properties, making it essential for evaluating how sound propagates and affects listeners.

Fundamentals

Definition

Sound pressure is defined as the difference between the instantaneous total pressure and the at a given point in a sound field. This local deviation arises from the passage of a wave, distinguishing it from , which represents the uniform ambient in the absence of , and total pressure, which is the sum of the static pressure and the sound pressure deviation. In the International System of Units (SI), sound pressure is measured in pascals (Pa), where 1 Pa equals 1 newton per square meter (N/m²). Historically, acoustics literature has employed the microbar (μbar) as a unit, with 1 μbar equivalent to 0.1 Pa, particularly in older meteorological and geophysical contexts. Sound pressure plays a central role in describing longitudinal pressure waves, which are the primary mechanism for sound propagation in fluids such as air and water, where particle motion occurs parallel to the direction of wave travel, resulting in alternating compressions and rarefactions. These waves transmit acoustic energy through variations in pressure without net displacement of the medium. Sound pressure level, a related logarithmic measure, quantifies these variations relative to a standard reference pressure of 20 μPa.

Physical Nature

Sound waves manifest as longitudinal mechanical disturbances that propagate through an elastic medium, characterized by alternating regions of compression and . In compressions, molecules are pushed closer together, resulting in elevated local , while rarefactions involve molecules spreading apart, creating zones of reduced relative to the surrounding equilibrium. These pressure fluctuations arise from the vibration of a sound source, which disturbs nearby particles and initiates the wave. Propagation occurs in elastic media—such as gases, liquids, and solids—through successive interactions among the medium's molecules or atoms. When a particle vibrates, it collides with adjacent particles, transferring and causing them to oscillate in turn; this sustains the wave without net displacement of the medium itself. The medium's elasticity, which enables it to resist and recover from deformation, is essential for this transmission, as cannot propagate in a lacking such interactions. These pressure variations represent deviations from the ambient pressure: positive deviations during compressions and negative ones during rarefactions. The magnitude of the peak pressure deviation corresponds to the amplitude of the wave, which governs the wave's overall intensity and the perceptual loudness of the sound. Sound pressure is intrinsically linked to the acoustic energy density within the medium, encompassing both potential energy from the compression and expansion of the material, and kinetic energy from the oscillatory motion of its particles. In a traveling plane wave, the time-averaged potential and kinetic energy densities are equal, reflecting the balanced conversion between these forms as the wave progresses. This energy relation underscores how greater pressure amplitudes correspond to higher total acoustic energy carried by the wave.

Mathematical Description

Instantaneous Pressure

The instantaneous sound pressure represents the time-dependent local deviation from the equilibrium atmospheric pressure caused by a propagating sound wave. In the sinusoidal model, which approximates many harmonic sound sources, the pressure at a fixed point in space is expressed as p(t)=p0sin(ωt+ϕ),p(t) = p_0 \sin(\omega t + \phi), where p0p_0 is the pressure amplitude (peak deviation), ω=2πf\omega = 2\pi f is the angular frequency with ff the frequency in hertz, tt is time, and ϕ\phi is the phase angle. This form arises from the one-dimensional assumption, where the sound propagates linearly through a medium without boundaries or . Starting from the linearized derived from Newton's second law, continuity, and of state for small perturbations, 2pz2=1c22pt2,\frac{\partial^2 p}{\partial z^2} = \frac{1}{c^2} \frac{\partial^2 p}{\partial t^2}, with cc as the , a general solution for a monochromatic wave traveling in the positive zz-direction is p(z,t)=p0sin(ωtkz+ϕ)p(z,t) = p_0 \sin(\omega t - kz + \phi), where k=ω/ck = \omega / c is the . This satisfies the wave equation by direct substitution, confirming the sinusoidal variation in both time and space under the plane wave approximation. For analytical convenience, especially in handling phase shifts and superpositions, complex exponential notation is commonly employed: p(z,t)=Re{p^ej(ωtkz)},p(z,t) = \mathrm{Re} \left\{ \hat{p} \, e^{j(\omega t - kz)} \right\}, where p^=p0ejϕ\hat{p} = p_0 e^{j\phi} is the complex amplitude incorporating magnitude and phase. Only the real part is physically meaningful, and this representation aligns with the phasor method in linear acoustics. Sound pressure, being a scalar, does not have directional properties like velocity but exhibits spatial variation in the plane wave: at a fixed time, p(z)p(z) forms a standing sinusoidal profile along the propagation axis, with compressions where p>0p > 0 and rarefactions where p<0p < 0. This positional dependence underscores the wave's progressive nature in one dimension.

Root-Mean-Square Pressure

The root-mean-square (RMS) sound pressure represents the effective value of the time-varying sound pressure, obtained as the of the mean of the squared instantaneous pressures. This measure quantifies the magnitude of sound waves in a way that corresponds to their energy content, making it essential for acoustic analyses. For a sinusoidal sound wave, where the instantaneous pressure is p(t)=p0cos(ωt)p(t) = p_0 \cos(\omega t) and p0p_0 is the peak pressure amplitude, the RMS pressure simplifies to prms=p02p_{\text{rms}} = \frac{p_0}{\sqrt{2}}
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