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Longitudinal wave
Longitudinal wave
from Wikipedia
Graph depicting a planar wave moving left-to-right
A type of longitudinal wave: A plane pressure pulse wave.
Nonfree image: detailed animation of a longitudinal wave
image icon Detailed animation of longitudinal wave motion (CC-BY-NC-ND 4.0)

Longitudinal waves are waves which oscillate in the direction which is parallel to the direction in which the wave travels and displacement of the medium is in the same (or opposite) direction of the wave propagation. Mechanical longitudinal waves are also called compressional or compression waves, because they produce compression and rarefaction when travelling through a medium, and pressure waves, because they produce increases and decreases in pressure. A wave along the length of a stretched Slinky toy, where the distance between coils increases and decreases, is a good visualization. Real-world examples include sound waves (vibrations in pressure, a particle of displacement, and particle velocity propagated in an elastic medium) and seismic P waves (created by earthquakes and explosions).

The other main type of wave is the transverse wave, in which the displacements of the medium are at right angles to the direction of propagation. Transverse waves, for instance, describe some bulk sound waves in solid materials (but not in fluids); these are also called "shear waves" to differentiate them from the (longitudinal) pressure waves that these materials also support.

Nomenclature

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"Longitudinal waves" and "transverse waves" have been abbreviated by some authors as "L-waves" and "T-waves", respectively, for their own convenience.[1] While these 2 abbreviations have specific meanings in seismology (L-wave for Love wave[2] or long wave[3]) and electrocardiography (see T wave), some authors chose to use "ℓ-waves" (lowercase 'L') and "t-waves" instead, although they are not commonly found in physics writings except for some popular science books.[4]

Sound waves

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For longitudinal harmonic sound waves, the frequency and wavelength can be described by the formula

where:

is the displacement of the point on the traveling sound wave;
Graph depicting a symmetrical wave spreading outwards from the center in all directions
Representation of the propagation of an omnidirectional pulse wave on a 2‑D grid (empirical shape)
is the distance from the point to the wave's source;
is the time elapsed;
is the amplitude of the oscillations,
is the speed of the wave; and
is the angular frequency of the wave.

The quantity is the time that the wave takes to travel the distance

The ordinary frequency () of the wave is given by

The wavelength can be calculated as the relation between a wave's speed and ordinary frequency.

For sound waves, the amplitude of the wave is the difference between the pressure of the undisturbed air and the maximum pressure caused by the wave.

Sound's propagation speed depends on the type, temperature, and composition of the medium through which it propagates.

Speed of longitudinal waves

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Isotropic medium

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For isotropic solids and liquids, the speed of a longitudinal wave can be described by

where

is the elastic modulus, such that
where is the shear modulus and is the bulk modulus;
is the mass density of the medium.

Attenuation of longitudinal waves

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The attenuation of a wave in a medium describes the loss of energy a wave carries as it propagates throughout the medium.[5] This is caused by the scattering of the wave at interfaces, the loss of energy due to the friction between molecules, or geometric divergence.[5] The study of attenuation of elastic waves in materials has increased in recent years, particularly within the study of polycrystalline materials where researchers aim to "nondestructively evaluate the degree of damage of engineering components" and to "develop improved procedures for characterizing microstructures" according to a research team led by R. Bruce Thompson in a Wave Motion publication.[6]

Attenuation in viscoelastic materials

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In viscoelastic materials, the attenuation coefficients per length for longitudinal waves and for transverse waves must satisfy the following ratio:

where and are the transverse and longitudinal wave speeds respectively.[7]

Attenuation in polycrystalline materials

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Polycrystalline materials are made up of various crystal grains which form the bulk material. Due to the difference in crystal structure and properties of these grains, when a wave propagating through a poly-crystal crosses a grain boundary, a scattering event occurs causing scattering based attenuation of the wave.[8] Additionally it has been shown that the ratio rule for viscoelastic materials,

applies equally successfully to polycrystalline materials.[8]

A current prediction for modeling attenuation of waves in polycrystalline materials with elongated grains is the second-order approximation (SOA) model which accounts the second order of inhomogeneity allowing for the consideration multiple scattering in the crystal system.[9][10] This model predicts that the shape of the grains in a poly-crystal has little effect on attenuation.[9]

Pressure waves

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The equations for sound in a fluid given above also apply to acoustic waves in an elastic solid. Although solids also support transverse waves (known as S-waves in seismology), longitudinal sound waves in the solid exist with a velocity and wave impedance dependent on the material's density and its rigidity, the latter of which is described (as with sound in a gas) by the material's bulk modulus.[11]

In May 2022, NASA reported the sonification (converting astronomical data associated with pressure waves into sound) of the black hole at the center of the Perseus galaxy cluster.[12][13]

Electromagnetics

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Maxwell's equations lead to the prediction of electromagnetic waves in a vacuum, which are strictly transverse waves; due to the fact that they would need particles to vibrate upon, the electric and magnetic fields of which the wave consists are perpendicular to the direction of the wave's propagation.[14] However plasma waves are longitudinal since these are not electromagnetic waves but density waves of charged particles, but which can couple to the electromagnetic field.[14][15][16]

After Heaviside's attempts to generalize Maxwell's equations, Heaviside concluded that electromagnetic waves were not to be found as longitudinal waves in "free space" or homogeneous media.[17] Maxwell's equations, as we now understand them, retain that conclusion: in free-space or other uniform isotropic dielectrics, electro-magnetic waves are strictly transverse. However electromagnetic waves can display a longitudinal component in the electric and/or magnetic fields when traversing birefringent materials, or inhomogeneous materials especially at interfaces (surface waves for instance) such as Zenneck waves.[18]

In the development of modern physics, Alexandru Proca (1897–1955) was known for developing relativistic quantum field equations bearing his name (Proca's equations) which apply to the massive vector spin-1 mesons. In recent decades some other theorists, such as Jean-Pierre Vigier and Bo Lehnert of the Swedish Royal Society, have used the Proca equation in an attempt to demonstrate photon mass[19] as a longitudinal electromagnetic component of Maxwell's equations, suggesting that longitudinal electromagnetic waves could exist in a Dirac polarized vacuum. However photon rest mass is strongly doubted by almost all physicists and is incompatible with the Standard Model of physics.[citation needed]

See also

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
A longitudinal wave is a type of in which the particles of the medium oscillate parallel to the direction of wave propagation, resulting in alternating regions of compression (high particle ) and (low particle ). This particle motion distinguishes longitudinal waves from transverse waves, where oscillations occur perpendicular to the propagation direction. Unlike transverse waves, which require a medium capable of (such as solids), longitudinal waves can propagate through solids, liquids, and gases due to the medium's compressibility. Key characteristics of longitudinal waves include their dependence on the medium's elastic properties and density for propagation speed, typically expressed as v=fλv = f \lambda, where vv is the wave speed, ff is the frequency, and λ\lambda is the wavelength. The amplitude represents the maximum displacement from equilibrium, while the wavelength corresponds to the distance between consecutive compressions or rarefactions. Prominent examples include sound waves, which transmit pressure disturbances through air or other fluids as longitudinal pressure variations, and primary (P) waves generated during earthquakes, which travel fastest through Earth's interior by compressing and expanding rock and other materials. Other applications encompass ultrasound waves used in medical imaging and longitudinal vibrations in solids, such as those in coiled springs like a slinky.

Fundamentals

Definition

A is a in which the of particles in the medium occurs parallel to the direction of energy propagation. This contrasts with transverse waves, where is perpendicular to the propagation direction. In longitudinal waves, the disturbance creates a series of compressions and rarefactions along the path of travel, with compressions representing regions of increased particle density and rarefactions indicating decreased density. The deformation of the medium in a longitudinal wave can be visualized as alternating bunches and stretches in a coiled spring or as high- and low-pressure zones in a , where particles momentarily cluster tightly before spreading out. These patterns allow the wave to transmit through the medium without net displacement of the particles from their original positions over time. The term "longitudinal wave" originated in the early 19th century, with its first known use recorded in 1813 amid developing theories of wave motion in physics. Physicists such as John William Strutt, 3rd Baron Rayleigh, furthered the conceptual framework in the late 19th century through studies of sound propagation, as detailed in his influential two-volume work The Theory of Sound (1877–1878), which analyzed longitudinal vibrations in various media. Understanding longitudinal waves requires familiarity with fundamental wave properties, including (the distance between consecutive compressions or rarefactions), (the number of wave cycles per unit time), (the maximum displacement of particles from equilibrium), and phase (the position of a point within the wave cycle).

Nomenclature

The term "longitudinal" originates from the Latin longitudo, meaning "length," reflecting the parallel alignment of particle oscillations with the direction of wave propagation. In the context of wave mechanics, key terminology includes compression, denoting regions where medium particles are densely packed, increasing local or , and , referring to regions of expanded spacing with reduced or . Longitudinal strain describes the fractional change in length along the propagation direction, quantifying the deformation in the medium. Standard symbols in physics for longitudinal waves include ξ(x,t)\xi(x, t) to represent the longitudinal displacement of particles from their equilibrium positions, where xx is the position coordinate and tt is time. The associated longitudinal strain is conventionally expressed as ξ/x\partial \xi / \partial x, capturing the spatial of displacement. In fluid media, the pressure variation induced by the wave is denoted by pp, often related to the and strain. Conventions for wave parameters in longitudinal contexts follow general wave physics, with kk as the wave number (k=2π/λk = 2\pi / \lambda, where λ\lambda is ) describing spatial periodicity, and ω\omega as the (ω=2πf\omega = 2\pi f, where ff is ) characterizing temporal . Longitudinal waves differ from vector-based transverse waves by being irrotational and representable via a in formulations, where the displacement field derives from the of a scalar function.

Mathematical Formulation

Displacement and Particle Motion

In a longitudinal wave, the displacement of particles from their equilibrium positions is parallel to the direction of wave . The particle displacement ξ(x,t)\xi(x, t) for a traveling in the positive xx-direction can be expressed as ξ(x,t)=Acos(kxωt)\xi(x, t) = A \cos(kx - \omega t), where AA is the , k=2π/λk = 2\pi / \lambda is the wave number, and ω=2πf\omega = 2\pi f is the . This oscillatory motion results in particles moving back and forth along the axis, creating regions of compression and without any transverse component. The variation in density arises directly from the spatial gradient of the displacement. The local density ρ\rho is related to the equilibrium density ρ0\rho_0 by ρ=ρ0(1ξx)\rho = \rho_0 \left(1 - \frac{\partial \xi}{\partial x}\right), where the term ξx\frac{\partial \xi}{\partial x} represents . Regions of compression occur when ξx<0\frac{\partial \xi}{\partial x} < 0, leading to increased density, while rarefaction happens when ξx>0\frac{\partial \xi}{\partial x} > 0, resulting in decreased density. For the displacement function above, ξx=kAsin(kxωt)\frac{\partial \xi}{\partial x} = -k A \sin(kx - \omega t), which oscillates between positive and negative values, driving these density fluctuations. The velocity of the particles is the time derivative of the displacement, given by u(x,t)=ξt=ωAsin(kxωt)u(x, t) = \frac{\partial \xi}{\partial t} = -\omega A \sin(kx - \omega t). The acceleration follows as a(x,t)=2ξt2=ω2Acos(kxωt)a(x, t) = \frac{\partial^2 \xi}{\partial t^2} = -\omega^2 A \cos(kx - \omega t). This acceleration links to the initiation and propagation of the wave through Newton's second law, where the net force on a particle element, typically from pressure gradients, equals mass times acceleration, enabling the wave to sustain oscillatory motion. In fluids, longitudinal waves involve purely irrotational motion, meaning the velocity field satisfies ×u=0\nabla \times \mathbf{u} = 0, with no vorticity generated due to the absence of shear stresses. In solids, however, longitudinal waves correspond to shear-free compression, where the displacement is dilatational without shear deformation, propagating via the material's bulk modulus and density, distinct from transverse shear waves that solids also support.

Wave Equation

The wave equation for longitudinal waves describes the propagation of particle displacements or pressure variations in a medium. In one dimension, it is derived by considering the dynamics of a small element of the medium, combining Newton's second law with the constitutive relations from elasticity theory. For solids, such as a thin elastic rod, the longitudinal displacement ξ(x,t)\xi(x, t) along the propagation direction xx produces a strain ξ/x\partial \xi / \partial x. By , the resulting stress is σ=Eξ/x\sigma = E \partial \xi / \partial x, where EE is the . The net on an infinitesimal element of length Δx\Delta x and cross-sectional area AA is then A(σ/x)Δx=AE(2ξ/x2)ΔxA (\partial \sigma / \partial x) \Delta x = A E (\partial^2 \xi / \partial x^2) \Delta x. Applying Newton's second law to this element of mass ρAΔx\rho A \Delta x (with ρ\rho the ) yields ρAΔx(2ξ/t2)=AE(2ξ/x2)Δx\rho A \Delta x (\partial^2 \xi / \partial t^2) = A E (\partial^2 \xi / \partial x^2) \Delta x, simplifying in the limit Δx0\Delta x \to 0 to the one-dimensional : 2ξt2=c22ξx2,\frac{\partial^2 \xi}{\partial t^2} = c^2 \frac{\partial^2 \xi}{\partial x^2}, where the longitudinal wave speed is c=E/ρc = \sqrt{E / \rho}
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