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Diffraction
Diffraction
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A diffraction pattern of a red laser beam projected onto a plate after passing through a small circular aperture in another plate

Diffraction is the deviation of waves from straight-line propagation without any change in their energy due to an obstacle or through an aperture. The diffracting object or aperture effectively becomes a secondary source of the propagating wave. Diffraction is the same physical effect as interference, but interference is typically applied to superposition of a few waves and the term diffraction is used when many waves are superposed.[1]: 433 

Italian scientist Francesco Maria Grimaldi coined the word diffraction and was the first to record accurate observations of the phenomenon in 1660.

Infinitely many points (three shown) along length project phase contributions from the wavefront, producing a continuously varying intensity on the registering plate

In classical physics, the diffraction phenomenon is described by the Huygens–Fresnel principle that treats each point in a propagating wavefront as a collection of individual spherical wavelets.[2] The characteristic pattern is most pronounced when a wave from a coherent source (such as a laser) encounters a slit/aperture that is comparable in size to its wavelength, as shown in the inserted image. This is due to the addition, or interference, of different points on the wavefront (or, equivalently, each wavelet) that travel by paths of different lengths to the registering surface. If there are multiple closely spaced openings, a complex pattern of varying intensity can result.

These effects also occur when a light wave travels through a medium with a varying refractive index, or when a sound wave travels through a medium with varying acoustic impedance – all waves diffract,[3] including gravitational waves,[4] water waves, and other electromagnetic waves such as X-rays and radio waves. Furthermore, quantum mechanics also demonstrates that matter possesses wave-like properties and, therefore, undergoes diffraction (which is measurable at subatomic to molecular levels).[5]

History

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Thomas Young's sketch of two-slit diffraction for water ripple tank from his 1807 Lectures[6]: 139 

The effects of diffraction of light were first carefully observed and characterized by Francesco Maria Grimaldi, who also coined the term diffraction, from the Latin diffringere, 'to break into pieces', referring to light breaking up into different directions.[7] The results of Grimaldi's observations were published posthumously in 1665.[8][9] Isaac Newton studied these effects and attributed them to inflexion of light rays. James Gregory (16381675) observed the diffraction patterns caused by a bird feather, which was effectively the first diffraction grating to be discovered.[10]

Thomas Young developed the first wave treatment of diffraction in 1800. In his model Young proposed that the fringes observed behind an illuminated sharp edge arose from interference between the direct transmitted plane wave and a cylindrical wave that appears to emitted from the edge.[11]: 57 

Augustin-Jean Fresnel revisited the problem and devised an alternative wave theory based on Huygens' principle. In this model, point sources of light are distributed up to the diffraction edge but not in the barrier. These point sources are driven by the incoming plane wave and they interfere beyond the barrier. Fresnel developed a mathematical treatment from his approach and Young's model was initially considered incorrect. Later work showed that Young's more physical approach is equivalent to Fresnel mathematical one.[11]: 58 

In 1818, supporters of the corpuscular theory of light proposed that the Paris Academy prize question address diffraction, expecting to see the wave theory defeated. When Fresnel's presentation on his new theory based on wave propagation looked like it might take the prize, Siméon Denis Poisson challenged the Fresnel theory by showing that it predicted light in the shadow behind a circular obstruction. Dominique-François-Jean Arago proceeded to demonstrate experimentally that such light is visible, confirming Fresnel's diffraction model.[12]: xxiii [13]

In 1859 Hermann von Helmholtz and later in 1882 Gustav Kirchhoff developed integral equations for diffraction based on the concepts proposed by Frenel as well as approximations needed to apply them. In general all these approaches require formulating the problem in terms of virtual sources. Cases like absorbing barrier require methods developed in the 1940s based on transverse amplitude diffusion.[11]: 58 

Mechanism

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Single-slit diffraction in a circular ripple tank

In classical physics diffraction arises because of how waves propagate; this is described by the Huygens–Fresnel principle and the principle of superposition of waves. The propagation of a wave can be visualized by considering every particle of the transmitted medium on a wavefront as a point source for a secondary spherical wave. The wave displacement at any subsequent point is the sum of these secondary waves. When waves are added together, their sum is determined by the relative phases as well as the amplitudes of the individual waves so that the summed amplitude of the waves can have any value between zero and the sum of the individual amplitudes. Hence, diffraction patterns usually have a series of maxima and minima.

In the modern quantum mechanical understanding of light propagation through a slit (or slits) every photon is described by its wavefunction that determines the probability distribution for the photon: the light and dark bands are the areas where the photons are more or less likely to be detected. The wavefunction is determined by the physical surroundings such as slit geometry, screen distance, and initial conditions when the photon is created. The wave nature of individual photons (as opposed to wave properties only arising from the interactions between multitudes of photons) was implied by a low-intensity double-slit experiment first performed by G. I. Taylor in 1909. The quantum approach has some striking similarities to the Huygens-Fresnel principle; based on that principle, as light travels through slits and boundaries, secondary point light sources are created near or along these obstacles, and the resulting diffraction pattern is going to be the intensity profile based on the collective interference of all these light sources that have different optical paths. In the quantum formalism, that is similar to considering the limited regions around the slits and boundaries from which photons are more likely to originate, and calculating the probability distribution (that is proportional to the resulting intensity of classical formalism).

There are various analytical models for photons which allow the diffracted field to be calculated, including the Kirchhoff diffraction equation (derived from the wave equation),[14] the Fraunhofer diffraction approximation of the Kirchhoff equation (applicable to the far field), the Fresnel diffraction approximation (applicable to the near field) and the Feynman path integral formulation. Most configurations cannot be solved analytically, but can yield numerical solutions through finite element and boundary element methods. In many cases it is assumed that there is only one scattering event, what is called kinematical diffraction, with an Ewald's sphere construction used to represent that there is no change in energy during the diffraction process. For matter waves a similar but slightly different approach is used based upon a relativistically corrected form of the Schrödinger equation,[15] as first detailed by Hans Bethe.[16] The Fraunhofer and Fresnel limits exist for these as well, although they correspond more to approximations for the matter wave Green's function (propagator)[17] for the Schrödinger equation.[18][19] More common is full multiple scattering models particular in electron diffraction;[20] in some cases similar dynamical diffraction models are also used for X-rays.[21]

It is possible to obtain a qualitative understanding of many diffraction phenomena by considering how the relative phases of the individual secondary wave sources vary, and, in particular, the conditions in which the phase difference equals half a cycle in which case waves will cancel one another out.

The simplest descriptions of diffraction are those in which the situation can be reduced to a two-dimensional problem. For water waves, this is already the case; water waves propagate only on the surface of the water. For light, we can often neglect one direction if the diffracting object extends in that direction over a distance far greater than the wavelength. In the case of light shining through small circular holes, we will have to take into account the full three-dimensional nature of the problem.

Examples

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The effects of diffraction are often seen in everyday life. The most striking examples of diffraction are those that involve light; for example, the closely spaced tracks on a CD or DVD act as a diffraction grating to form the familiar rainbow pattern seen when looking at a disc.

Pixels on smart phone screen acting as diffraction grating
Data is written on CDs as pits and lands; the pits on the surface act as diffracting elements.

This principle can be extended to engineer a grating with a structure such that it will produce any diffraction pattern desired; the hologram on a credit card is an example.

Diffraction in the atmosphere by small particles can cause a corona - a bright disc and rings around a bright light source like the sun or the moon. At the opposite point one may also observe glory - bright rings around the shadow of the observer. In contrast to the corona, glory requires the particles to be transparent spheres (like fog droplets), since the backscattering of the light that forms the glory involves refraction and internal reflection within the droplet.

Lunar corona.
A solar glory, as seen from a plane on the underlying clouds.

A shadow of a solid object, using light from a compact source, shows small fringes near its edges.

The bright spot (Arago spot) seen in the center of the shadow of a circular obstacle is due to diffraction

Diffraction spikes are diffraction patterns caused due to non-circular aperture in camera or support struts in telescope; In normal vision, diffraction through eyelashes may produce such spikes.

View from the end of Millennium Bridge; Moon rising above the Southwark Bridge. Street lights are reflecting in the Thames.
Simulated diffraction spikes in hexagonal telescope mirrors

The speckle pattern which is observed when laser light falls on an optically rough surface is also a diffraction phenomenon. When deli meat appears to be iridescent, that is diffraction off the meat fibers.[23] All these effects are a consequence of the fact that light propagates as a wave.

Diffraction can occur with any kind of wave. Ocean waves diffract around jetties and other obstacles.

Circular waves generated by diffraction from the narrow entrance of a flooded coastal quarry

Sound waves can diffract around objects, which is why one can still hear someone calling even when hiding behind a tree.[24]

Diffraction can also be a concern in some technical applications; it sets a fundamental limit to the resolution of a camera, telescope, or microscope.

Other examples of diffraction are considered below.

Single-slit diffraction

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2D Single-slit diffraction with width changing animation
Numerical approximation of diffraction pattern from a slit of width four wavelengths with an incident plane wave. The main central beam, nulls, and phase reversals are apparent.
Graph and image of single-slit diffraction

A long slit of infinitesimal width which is illuminated by light diffracts the light into a series of circular waves and the wavefront which emerges from the slit is a cylindrical wave of uniform intensity, in accordance with the Huygens–Fresnel principle.

An illuminated slit that is wider than a wavelength produces interference effects in the space downstream of the slit. Assuming that the slit behaves as though it has a large number of point sources spaced evenly across the width of the slit interference effects can be calculated. The analysis of this system is simplified if we consider light of a single wavelength. If the incident light is coherent, these sources all have the same phase. Light incident at a given point in the space downstream of the slit is made up of contributions from each of these point sources and if the relative phases of these contributions vary by or more, we may expect to find minima and maxima in the diffracted light. Such phase differences are caused by differences in the path lengths over which contributing rays reach the point from the slit.

We can find the angle at which a first minimum is obtained in the diffracted light by the following reasoning. The light from a source located at the top edge of the slit interferes destructively with a source located at the middle of the slit, when the path difference between them is equal to . Similarly, the source just below the top of the slit will interfere destructively with the source located just below the middle of the slit at the same angle. We can continue this reasoning along the entire height of the slit to conclude that the condition for destructive interference for the entire slit is the same as the condition for destructive interference between two narrow slits a distance apart that is half the width of the slit. The path difference is approximately so that the minimum intensity occurs at an angle given by where is the width of the slit, is the angle of incidence at which the minimum intensity occurs, and is the wavelength of the light.

A similar argument can be used to show that if we imagine the slit to be divided into four, six, eight parts, etc., minima are obtained at angles given by where is an integer other than zero.

There is no such simple argument to enable us to find the maxima of the diffraction pattern. The intensity profile can be calculated using the Fraunhofer diffraction equation as where is the intensity at a given angle, is the intensity at the central maximum (), which is also a normalization factor of the intensity profile that can be determined by an integration from to and conservation of energy, and , which is the unnormalized sinc function.

This analysis applies only to the far field (Fraunhofer diffraction), that is, at a distance much larger than the width of the slit.

From the intensity profile above, if , the intensity will have little dependency on , hence the wavefront emerging from the slit would resemble a cylindrical wave with azimuthal symmetry; If , only would have appreciable intensity, hence the wavefront emerging from the slit would resemble that of geometrical optics.

When the incident angle of the light onto the slit is non-zero (which causes a change in the path length), the intensity profile in the Fraunhofer regime (i.e. far field) becomes:

The choice of plus/minus sign depends on the definition of the incident angle .

2-slit (top) and 5-slit diffraction of red laser light
Diffraction of a red laser using a diffraction grating
A diffraction pattern of a 633 nm laser through a grid of 150 slits

Diffraction grating

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Diffraction grating

A diffraction grating is an optical component with a regular pattern. The form of the light diffracted by a grating depends on the structure of the elements and the number of elements present, but all gratings have intensity maxima at angles θm which are given by the grating equation where is the angle at which the light is incident, is the separation of grating elements, and is an integer which can be positive or negative.

The light diffracted by a grating is found by summing the light diffracted from each of the elements, and is essentially a convolution of diffraction and interference patterns.

The figure shows the light diffracted by 2-element and 5-element gratings where the grating spacings are the same; it can be seen that the maxima are in the same position, but the detailed structures of the intensities are different.

Circular aperture

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A computer-generated image of an Airy disk
Diffraction pattern from a circular aperture at various distances

The far-field diffraction of a plane wave incident on a circular aperture is often referred to as the Airy disk. The variation in intensity with angle is given by where is the radius of the circular aperture, is equal to and is a Bessel function. The smaller the aperture, the larger the spot size at a given distance, and the greater the divergence of the diffracted beams.

General aperture

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The wave that emerges from a point source has amplitude at location that is given by the solution of the frequency domain wave equation for a point source (the Helmholtz equation), where is the 3-dimensional delta function. The delta function has only radial dependence, so the Laplace operator (a.k.a. scalar Laplacian) in the spherical coordinate system simplifies to

(See del in cylindrical and spherical coordinates.) By direct substitution, the solution to this equation can be readily shown to be the scalar Green's function, which in the spherical coordinate system (and using the physics time convention ) is

This solution assumes that the delta function source is located at the origin. If the source is located at an arbitrary source point, denoted by the vector and the field point is located at the point , then we may represent the scalar Green's function (for arbitrary source location) as

Therefore, if an electric field is incident on the aperture, the field produced by this aperture distribution is given by the surface integral

On the calculation of Fraunhofer region fields

where the source point in the aperture is given by the vector

In the far field, wherein the parallel rays approximation can be employed, the Green's function, simplifies to as can be seen in the adjacent figure.

The expression for the far-zone (Fraunhofer region) field becomes

Now, since and the expression for the Fraunhofer region field from a planar aperture now becomes

Letting and the Fraunhofer region field of the planar aperture assumes the form of a Fourier transform

In the far-field / Fraunhofer region, this becomes the spatial Fourier transform of the aperture distribution. Huygens' principle when applied to an aperture simply says that the far-field diffraction pattern is the spatial Fourier transform of the aperture shape, and this is a direct by-product of using the parallel-rays approximation, which is identical to doing a plane wave decomposition of the aperture plane fields (see Fourier optics).

Propagation of a laser beam

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The way in which the beam profile of a laser beam changes as it propagates is determined by diffraction. When the entire emitted beam has a planar, spatially coherent wave front, it approximates Gaussian beam profile and has the lowest divergence for a given diameter. The smaller the output beam, the quicker it diverges. It is possible to reduce the divergence of a laser beam by first expanding it with one convex lens, and then collimating it with a second convex lens whose focal point is coincident with that of the first lens. The resulting beam has a larger diameter, and hence a lower divergence. Divergence of a laser beam may be reduced below the diffraction of a Gaussian beam or even reversed to convergence if the refractive index of the propagation media increases with the light intensity.[25] This may result in a self-focusing effect.

When the wave front of the emitted beam has perturbations, only the transverse coherence length (where the wave front perturbation is less than 1/4 of the wavelength) should be considered as a Gaussian beam diameter when determining the divergence of the laser beam. If the transverse coherence length in the vertical direction is higher than in horizontal, the laser beam divergence will be lower in the vertical direction than in the horizontal.

Diffraction-limited imaging

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The Airy disk around each of the stars from the 2.56 m telescope aperture can be seen in this lucky image of the binary star zeta Boötis.

The ability of an imaging system to resolve detail is ultimately limited by diffraction. This is because a plane wave incident on a circular lens or mirror is diffracted as described above. The light is not focused to a point but forms an Airy disk having a central spot in the focal plane whose radius (as measured to the first null) is where is the wavelength of the light and is the f-number (focal length divided by aperture diameter ) of the imaging optics; this is strictly accurate for (paraxial case). In object space, the corresponding angular resolution is where is the diameter of the entrance pupil of the imaging lens (e.g., of a telescope's main mirror).

Two point sources will each produce an Airy pattern – see the photo of a binary star. As the point sources move closer together, the patterns will start to overlap, and ultimately they will merge to form a single pattern, in which case the two point sources cannot be resolved in the image. The Rayleigh criterion specifies that two point sources are considered "resolved" if the separation of the two images is at least the radius of the Airy disk, i.e. if the first minimum of one coincides with the maximum of the other.

Thus, the larger the aperture of the lens compared to the wavelength, the finer the resolution of an imaging system. This is one reason astronomical telescopes require large objectives, and why microscope objectives require a large numerical aperture (large aperture diameter compared to working distance) in order to obtain the highest possible resolution.

Speckle patterns

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The speckle pattern seen when using a laser pointer is another diffraction phenomenon. It is a result of the superposition of many waves with different phases, which are produced when a laser beam illuminates a rough surface. They add together to give a resultant wave whose amplitude, and therefore intensity, varies randomly.

Babinet's principle

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Babinet's principle is a useful theorem stating that the diffraction pattern from an opaque body is identical to that from a hole of the same size and shape, but with differing intensities. This means that the interference conditions of a single obstruction would be the same as that of a single slit.

"Knife edge"

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The knife-edge effect or knife-edge diffraction is a truncation of a portion of the incident radiation that strikes a sharp well-defined obstacle, such as a mountain range or the wall of a building. The knife-edge effect is explained by the Huygens–Fresnel principle, which states that a well-defined obstruction to an electromagnetic wave acts as a secondary source, and creates a new wavefront. This new wavefront propagates into the geometric shadow area of the obstacle.

Knife-edge diffraction is an outgrowth of the "half-plane problem", originally solved by Arnold Sommerfeld using a plane wave spectrum formulation. A generalization of the half-plane problem is the "wedge problem", solvable as a boundary value problem in cylindrical coordinates. The solution in cylindrical coordinates was then extended to the optical regime by Joseph B. Keller, who introduced the notion of diffraction coefficients through his geometrical theory of diffraction (GTD). In 1974, Prabhakar Pathak and Robert Kouyoumjian extended the (singular) Keller coefficients via the uniform theory of diffraction (UTD).[26][27]

Patterns

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The upper half of this image shows a diffraction pattern of He-Ne laser beam on an elliptic aperture. The lower half is its 2D Fourier transform approximately reconstructing the shape of the aperture.

Several qualitative observations can be made of diffraction in general:

  • The angular spacing of the features in the diffraction pattern is inversely proportional to the dimensions of the object causing the diffraction. In other words: The smaller the diffracting object, the 'wider' the resulting diffraction pattern, and vice versa. (More precisely, this is true of the sines of the angles.)
  • The diffraction angles are invariant under scaling; that is, they depend only on the ratio of the wavelength to the size of the diffracting object.
  • When the diffracting object has a periodic structure, for example in a diffraction grating, the features generally become sharper. The third figure, for example, shows a comparison of a double-slit pattern with a pattern formed by five slits, both sets of slits having the same spacing, between the center of one slit and the next.

Matter wave diffraction

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According to quantum theory every particle exhibits wave properties and can therefore diffract. Diffraction of electrons and neutrons is one of the powerful arguments in favor of quantum mechanics. The wavelength associated with a non-relativistic particle is the de Broglie wavelength where is the Planck constant and is the momentum of the particle (mass × velocity for slow-moving particles). For example, a sodium atom traveling at about 300 m/s would have a de Broglie wavelength of about 50 picometres.

Diffraction of matter waves has been observed for small particles, like electrons, neutrons, atoms, and even large molecules. The short wavelength of these matter waves makes them ideally suited to study the atomic structure of solids, molecules and proteins.

Bragg diffraction

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Following Bragg's law, each dot (or reflection) in this diffraction pattern forms from the constructive interference of X-rays passing through a crystal. The data can be used to determine the crystal's atomic structure.

Diffraction from a large three-dimensional periodic structure such as many thousands of atoms in a crystal is called Bragg diffraction. It is similar to what occurs when waves are scattered from a diffraction grating. Bragg diffraction is a consequence of interference between waves reflecting from many different crystal planes. The condition of constructive interference is given by Bragg's law: where is the wavelength, is the distance between crystal planes, is the angle of the diffracted wave, and is an integer known as the order of the diffracted beam.

Bragg diffraction may be carried out using either electromagnetic radiation of very short wavelength like X-rays or matter waves like neutrons (and electrons) whose wavelength is on the order of (or much smaller than) the atomic spacing.[28] The pattern produced gives information of the separations of crystallographic planes , allowing one to deduce the crystal structure.

For completeness, Bragg diffraction is a limit for a large number of atoms with X-rays or neutrons, and is rarely valid for electron diffraction or with solid particles in the size range of less than 50 nanometers.[28]

Coherence

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The description of diffraction relies on the interference of waves emanating from the same source taking different paths to the same point on a screen. In this description, the difference in phase between waves that took different paths is only dependent on the effective path length. This does not take into account the fact that waves that arrive at the screen at the same time were emitted by the source at different times. The initial phase with which the source emits waves can change over time in an unpredictable way. This means that waves emitted by the source at times that are too far apart can no longer form a constant interference pattern since the relation between their phases is no longer time independent.[29]: 919 

The length over which the phase in a beam of light is correlated is called the coherence length. In order for interference to occur, the path length difference must be smaller than the coherence length. This is sometimes referred to as spectral coherence, as it is related to the presence of different frequency components in the wave. In the case of light emitted by an atomic transition, the coherence length is related to the lifetime of the excited state from which the atom made its transition.[30]: 71–74 [1]: 314–316 

If waves are emitted from an extended source, this can lead to incoherence in the transversal direction. When looking at a cross section of a beam of light, the length over which the phase is correlated is called the transverse coherence length. In the case of Young's double-slit experiment, this would mean that if the transverse coherence length is smaller than the spacing between the two slits, the resulting pattern on a screen would look like two single-slit diffraction patterns.[30]: 74–79 

In the case of particles like electrons, neutrons, and atoms, the coherence length is related to the spatial extent of the wave function that describes the particle.[31]: 107 

Applications

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Diffraction before destruction

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A new way to image single biological particles has emerged since the 2010s, utilising the bright X-rays generated by X-ray free-electron lasers. These femtosecond-duration pulses will allow for the (potential) imaging of single biological macromolecules. Due to these short pulses, radiation damage can be outrun, and diffraction patterns of single biological macromolecules will be able to be obtained.[32][33]

See also

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Diffraction is the bending of waves around the edges of an opening or an obstacle and the spreading out of waves beyond small openings, a fundamental characteristic of wave propagation observed in phenomena such as passing through slits, navigating corners, and water waves encountering barriers. This effect becomes prominent when the size of the obstacle or is comparable to the of the wave, leading to interference patterns that reveal the wave nature of the propagating . Diffraction occurs for all types of waves, including mechanical waves like and water waves, as well as electromagnetic waves such as and X-rays, and it underpins key experimental evidence for the wave-particle duality in . The historical development of diffraction theory traces back to early observations in the 17th century, with Italian physicist Francesco Grimaldi first documenting the bending of light around obstacles in 1665, though without a wave-based explanation at the time. In 1678, Dutch scientist Christiaan Huygens proposed his principle, stating that every point on a wavefront acts as a source of secondary spherical wavelets that propagate forward, providing a foundational framework for understanding wave propagation, reflection, and refraction, which later extended to diffraction. The modern wave theory of diffraction was advanced in 1818 by Augustin-Jean Fresnel, who applied Huygens's ideas to predict diffraction patterns mathematically, including the counterintuitive Poisson spot—a bright point at the center of a circular shadow—verified experimentally by Dominique Arago, thus supporting the wave model of light against prevailing particle theories. Further refinements came in the 19th century through the work of Gustav Kirchhoff in 1882, who derived diffraction from the wave equation using Green's theorem. At its core, diffraction is governed by the Huygens-Fresnel principle, which treats each point on an incoming wavefront as a secondary source of waves whose superposition determines the resulting intensity pattern, often expressed as I=I0sin2(Nϕ/2)sin2(ϕ/2)I = I_0 \frac{\sin^2(N \phi / 2)}{\sin^2(\phi / 2)} for NN slits separated by distance dd, where ϕ=2πdsinθ/λ\phi = 2\pi d \sin \theta / \lambda accounts for phase differences due to path length variations. Common manifestations include single-slit diffraction, producing a central bright band flanked by minima at angles θ=mλ/a\theta = m \lambda / a (where aa is slit width and mm is an integer), and multi-slit or grating diffraction, which enhances resolution through narrower principal maxima. These patterns arise from constructive and destructive interference, with the degree of spreading inversely proportional to the aperture size relative to the wavelength, limiting the precision of optical instruments like microscopes and telescopes via the diffraction limit Δθ1.22λ/D\Delta \theta \approx 1.22 \lambda / D for circular apertures of diameter DD. Diffraction plays a pivotal role in numerous scientific and technological applications, particularly in spectroscopy where diffraction gratings disperse light into its constituent wavelengths for atomic analysis, enabling the measurement of spectral lines with resolving power λ/Δλ=mN\lambda / \Delta \lambda = m N ( mm being the order and NN the number of slits). In X-ray crystallography, diffraction patterns from crystal lattices, first demonstrated by Max von Laue in 1912, allow determination of atomic structures essential for chemistry, biology, and materials science, as seen in the elucidation of DNA's double helix. Other uses include acoustic design, where diffraction influences sound propagation around barriers, and modern optics, such as in spectrometers that separate visible light spectra for astronomical observations.

History

Early Observations

The phenomenon of diffraction was first systematically observed and documented by the Italian Jesuit and in the mid-17th century. In experiments conducted around 1660 and published posthumously in 1665 in his work Physico-mathesis de lumine, Grimaldi noted that passing through narrow slits or around the edges of opaque obstacles would spread out and produce colored bands beyond the geometric shadow, rather than strictly adhering to straight-line propagation. He coined the term "diffraction" (from the Latin diffractio, meaning "breaking apart") to describe this bending and dispersion, likening it to the way a stream of splits when encountering a thin obstacle. Building on such initial findings, early experiments in the late 17th and early 18th centuries further explored these and fringes. Scottish mathematician and astronomer James Gregory, in a 1673 letter to (secretary of the Royal Society), described observing spectral patterns produced by sunlight passing through the fine barbs of a bird feather, which acted as an early form of and revealed iridescent colors due to light's deviation around the structures. These observations highlighted the irregular bending of light near edges, though Gregory did not fully theorize the cause. Isaac Newton addressed these phenomena in his 1704 publication Opticks, where he referred to diffraction as "inflexions" of light rays. While Newton staunchly advocated a corpuscular (particle) theory of light and rejected wave explanations, he acknowledged the existence of colored fringes and patterns near obstacles or slits, describing experiments where light produced unexpected spectral displays beyond sharp shadows. In Book III and the appended Queries, Newton detailed how these inflexions generated rings and bands, attributing them to subtle deviations in ray paths without resolving their underlying mechanism, thus paving empirical groundwork for later wave-based interpretations. Diffraction-like effects were also recognized in natural atmospheric phenomena long before laboratory settings, with descriptions dating back to antiquity. Ancient observers, including in his (circa 350 BCE), documented luminous rings or halos encircling the , attributing them to interactions with atmospheric vapors, though modern understanding links these primarily to by suspended crystals in high-altitude cirrus clouds. These lunar halos, often appearing as 22-degree rings with subtle colored edges due to dispersion, arise when moonlight refracts through hexagonal ice prisms; related diffraction effects produce smaller around the through clouds containing tiny water droplets. Such events were routinely recorded in Chinese astronomical annals from the (481–221 BCE) onward, serving as omens or weather indicators.

Theoretical Development

In 1678, Dutch scientist proposed his principle, stating that every point on a wavefront acts as a source of secondary spherical wavelets that propagate forward, providing a foundational framework for understanding wave propagation, which later extended to diffraction. The theoretical development of diffraction began in the early with Thomas Young's double-slit experiment in 1801, which provided key evidence for the wave theory of light by demonstrating interference patterns, thereby linking wave propagation to diffraction effects. Young's work challenged the prevailing corpuscular model and laid the groundwork for understanding diffraction as a consequence of wave superposition. Building on this and Huygens' principle, advanced diffraction theory in his 1818 memoir submitted to the , where he modeled diffraction as the interference of secondary wavelets from wavefronts, earning a prize for his contributions. Fresnel's analysis predicted a bright spot at the center of a circular shadow due to constructive interference, known as Poisson's spot, which initially seemed counterintuitive to proponents of the particle theory. In 1818, Dominique Arago experimentally confirmed this spot, providing empirical validation that solidified the wave model of diffraction. Concurrently in the 1810s, developed high-precision diffraction gratings using fine wires and ruled lines on glass, enabling the observation of lines in and establishing the far-field approximation now termed . His gratings, first constructed around 1821, allowed quantitative measurements of wavelengths and absorption features, transforming diffraction into a tool for . Further refinements came in the 19th century through the work of in 1882, who derived diffraction from the wave equation using . In the 20th century, diffraction theory extended to quantum realms with Louis de Broglie's 1924 hypothesis that particles exhibit wave-like properties, proposing matter waves with λ = h/p, which implied diffraction for electrons and other particles. This wave-particle duality was experimentally supported by diffraction patterns in electron beams. Further quantum formulation came through Richard Feynman's path integral approach in the 1940s, which reinterpreted diffraction as the summation of probability amplitudes over all possible paths, unifying wave and particle descriptions in . A pivotal quantum application occurred in 1912 when demonstrated diffraction by crystals, revealing atomic lattice structures and confirming the wave nature of X-rays.

Fundamental Principles

Huygens-Fresnel Principle

The Huygens-Fresnel principle provides the foundational mechanism for understanding wave propagation and diffraction in . In 1678, proposed that every point on an advancing acts as a source of secondary spherical wavelets, which spread outward with the ; the new wavefront at any later time is the common tangent envelope to these wavelets. This construction reconciles the wave nature of light with observed phenomena like reflection and , while contrasting sharply with geometric , where light travels in straight rays without bending. For instance, when a encounters an opaque obstacle, the secondary wavelets emanating from points along the unobstructed portions of the initial curve around the edges, allowing light to penetrate into shadowed regions through the superposition of these expanding spheres—thus explaining the bending of light that geometric cannot account for. In 1818, refined Huygens's idea by incorporating the principle of interference among the secondary wavelets, recognizing that their must combine constructively or destructively depending on path length differences to produce the observed intensity patterns. also introduced an obliquity factor, approximately (1+cosθ)/2(1 + \cos \theta)/2, where θ\theta is the angle between the secondary wavelet's propagation direction and the normal to the initial , to model the observed decay in for wavelets propagating obliquely rather than perpendicularly. This factor ensures that contributions from secondary sources diminish appropriately with angle, enhancing the principle's predictive power for diffraction effects. Mathematically, the principle states that the disturbance ( and phase) at an observation point PP is determined by integrating the contributions from all secondary sources across the initial Σ\Sigma: the total field is proportional to Σ1+cosθreikrdS\int_\Sigma \frac{1 + \cos \theta}{r} e^{i k r} \, dS, where rr is the distance from a source point on Σ\Sigma to PP, k=2π/λk = 2\pi / \lambda is the , and dSdS is the surface element—without deriving the full form here. This superposition propagates the wavefront forward, capturing how initial conditions evolve over distance. The principle assumes monochromatic waves of a single wavelength λ\lambda, as polychromatic light would require separate treatments for each frequency component to avoid phase complications. It also relies on far-field approximations for simplified calculations, though extensions handle near-field effects; these limitations ensure its applicability primarily to coherent, scalar wave scenarios in classical optics.

Interference and Superposition

The principle of superposition states that when multiple waves overlap in space, the total wavefield at any point is the vector sum of the individual wave amplitudes from each source. This linear addition applies to all wave phenomena, including , , and water waves, and is fundamental to understanding how complex wave patterns emerge from simpler components. In the context of interference, superposition leads to constructive interference when waves arrive in phase, meaning their crests and troughs align, resulting in maxima of intensity where amplitudes add up. Conversely, destructive interference occurs when waves are out of phase, such as when a crest meets a trough, leading to minima where amplitudes cancel out. These effects produce the alternating bright and dark fringes observed in interference patterns. Phase shifts arise from path length differences between waves, quantified by the phase difference δ = (2π/λ) Δx, where λ is the and Δx is the extra path length traveled by one wave relative to another. When Δx is an multiple of λ, the waves are in phase (δ = 2π n, n ), favoring constructive interference; fractional multiples lead to partial or full cancellation. In diffraction, superposition of secondary wavelets—emanating from points across an or —interferes to form characteristic fringe patterns that extend beyond the geometric shadows expected from simple reflection or . This interference redistributes wave into regions of reinforcement and cancellation, creating the bending and spreading of waves around edges. Diffraction inherently requires the wave nature of the phenomenon, as particle models predict straight-line trajectories without such spreading or interference effects, whereas waves propagate continuously and overlap to produce these observable deviations.

Mathematical Framework

Fraunhofer Diffraction

Fraunhofer diffraction describes the diffraction pattern observed in the far-field limit, where both the source and the observation point are effectively at infinite distance from the diffracting , resulting in plane wave propagation. This approximation simplifies the analysis by assuming that incoming and outgoing wavefronts are planar, which is valid when the observation distance zz satisfies za2/λz \gg a^2 / \lambda, with aa being the characteristic size of the and λ\lambda the of the . The formulation begins with the Huygens-Fresnel principle, which posits that the field at an observation point PP is the superposition of secondary wavelets emanating from each point in the . The general diffraction from this principle is approximated in the far field by neglecting higher-order terms in the phase expansion. Specifically, the distance rr from an aperture point (ξ,η)(\xi, \eta) to P(x,y,z)P(x, y, z) is expanded as rz+(xξ+yη)/zr \approx z + (x\xi + y\eta)/z, under the linear phase approximation, where the quadratic term (ξ2+η2)/(2z)( \xi^2 + \eta^2 ) / (2z) is omitted. Angular coordinates are scaled such that θxx/z\theta_x \approx x/z and θyy/z\theta_y \approx y/z, leading to a that depends linearly on these angles. This yields the Fraunhofer diffraction for the field U(x,y)U(x, y) at the observation plane: U(x,y)=iλzeikzA(ξ,η)exp[i2πλz(xξ+yη)]dξdη,U(x, y) = \frac{i}{\lambda z} e^{ikz} \iint A(\xi, \eta) \exp\left[ -i \frac{2\pi}{\lambda z} (x \xi + y \eta) \right] d\xi \, d\eta, where A(ξ,η)A(\xi, \eta) is the aperture function (complex amplitude transmittance), assuming monochromatic illumination and paraxial propagation. A key insight is that this integral represents the Fourier transform of the aperture function A(ξ,η)A(\xi, \eta), with spatial frequencies fx=x/(λz)f_x = x / (\lambda z) and fy=y/(λz)f_y = y / (\lambda z). Thus, the far-field diffraction pattern is the of the aperture transmittance, scaled by the observation geometry; the intensity pattern I(x,y)=U(x,y)2I(x, y) = |U(x, y)|^2 then follows from the squared modulus. This interpretation, central to , assumes monochromatic light and neglects obliquity factors for simplicity in the paraxial regime. This framework is foundational for analyzing patterns from simple apertures, such as the sinc distribution in single-slit diffraction or periodic intensity in gratings.

Fresnel Diffraction

Fresnel diffraction describes the bending of waves around obstacles or through when the observation point is in the near-field or , where the distance zz from the aperture to is comparable to the square of the aperture dimension aa divided by the λ\lambda, specifically za2/λz \lesssim a^2 / \lambda. This regime accounts for the of the wavefronts, unlike the far-field where spherical waves can be treated as plane waves. In this near-field setup, the diffraction pattern exhibits complex intensity variations due to the finite distance, including effects like the Poisson spot in circular . The amplitude of the diffracted field U(P)U(P) at an observation point P(x,y,z)P(x, y, z) is calculated using the full Huygens-Fresnel diffraction , which integrates contributions from secondary wavelets across the : U(P)=1iλA(ξ,η)rexp(ikr)cosχdξdη,U(P) = \frac{1}{i\lambda} \iint \frac{A(\xi, \eta)}{r} \exp(ikr) \cos \chi \, d\xi \, d\eta, where A(ξ,η)A(\xi, \eta) is the field, r=z2+(xξ)2+(yη)2r = \sqrt{z^2 + (x - \xi)^2 + (y - \eta)^2}
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