Kirchhoff's diffraction formula[1][2] (also calledFresnel–Kirchhoff diffraction formula) approximates light intensity and phase in opticaldiffraction: light fields in the boundary regions of shadows. The approximationcan be used to model lightpropagation in a wide range of configurations, eitheranalytically or usingnumerical modelling. It gives an expression for the wave disturbance when amonochromaticspherical wave is the incoming wave of a situation under consideration. This formula is derived by applying theKirchhoff integral theorem, which uses theGreen's second identity to derive the solution to the homogeneousscalar wave equation, to a spherical wave with some approximations.
Kirchhoff's integral theorem, sometimes referred to as the Fresnel–Kirchhoff integral theorem,[3] usesGreen's second identity to derive the solution of the homogeneousscalar wave equation at an arbitrary spatial positionP in terms of the solution of the wave equation and its first order derivative at all points on an arbitrary closed surface as the boundary of some volume includingP.
The solution provided by the integral theorem for amonochromatic source is[1]: 378 where is the spatial part of the solution of the homogeneousscalar wave equation (i.e., as the homogeneous scalar wave equation solution),k is thewavenumber, ands is the distance fromP to an (infinitesimally small) integral surface element, and denotes differentiation along the integral surface element normal unit vector (i.e., anormal derivative), i.e.,. Note that the surface normal or the direction of is toward the inside of the enclosed volume in this integral; if the more usualouter-pointing normal is used, the integral will have the opposite sign. And also note that, in the integral theorem shown here, andParevector quantities while other terms arescalar quantities.
For the below cases, the following basic assumptions are made.
The distance between apoint source of waves and an integral area, the distance between the integral area and an observation pointP, and the dimension of openingS are much greater than the wave wavelength.
and are discontinuous at the boundaries of the aperture, calledKirchhoff's boundary conditions. This may be related with another assumption that waves on an aperture (or an open area) is same to the waves that would be present if there was no obstacle for the waves.
A geometrical arrangement used in deriving the Kirchhoff's diffraction formula. The area designated by A1 is the aperture (opening), the areas marked by A2 are opaque areas, and A3 is the hemisphere as a part of the closed integral surface (consisted of the areas A1, A2, and A3) for theKirchhoff's integral theorem.
Consider a monochromatic point source atP0, which illuminates an aperture in a screen. Theintensity of the wave emitted by a point source falls off as the inverse square of the distance traveled, so the amplitude falls off as the inverse of the distance. The complex amplitude of the disturbance at a distance is given by
where represents themagnitude of the disturbance at the point source.
The disturbance at a spatial positionP can be found by applying theKirchhoff's integral theorem to the closed surface formed by the intersection of a sphere of radiusR with the screen. The integration is performed over the areasA1,A2 andA3, giving
To solve the equation, it is assumed that the values of and in the aperture areaA1 are the same as when the screen is not present, so at the positionQ,where is the length of the straight lineP0Q, and is the angle between a straightly extended version ofP0Q and the (inward) normal to the aperture. Note that so is a positive real number onA1.
AtQ, we also havewhere is the length of the straight linePQ, and is the angle between a straightly extended version ofPQ and the (inward) normal to the aperture. Note that so is a negative real number onA1.
Two more following assumptions are made.
In the above normal derivatives, the terms and in the both square brackets are assumed to be negligible compared with thewavenumber, means and are much greater than thewavelength.
Kirchhoff assumes that the values of and on the opaque areas marked byA2 are zero. This implies that and are discontinuous at the edge of the apertureA1. This is not the case, and this isone of the approximations used in deriving the Kirchhoff's diffraction formula.[4][5] These assumptions are sometimes referred to asKirchhoff's boundary conditions.
The contribution from the hemisphereA3 to the integral is expected to be zero, and it can be justified by one of the following reasons.
Make the assumption that the source starts to radiate at a particular time, and then makeR large enough, so that when the disturbance atP is being considered, no contributions fromA3 will have arrived there.[1] Such a wave is no longermonochromatic, since a monochromatic wave must exist at all times, but that assumption is not necessary, and a more formal argument avoiding its use has been derived.[6]
A wave emanated from the apertureA1 is expected to evolve toward a spherical wave as it propagates (Water wave examples of this can be found in many pictures showing a water wave passing through a relatively narrow opening.). So, ifR is large enough, then the integral onA3 becomes where and are the distance from the center of the apertureA1 to an integral surface element andthe differential solid angle in the spherical coordinate system respectively.
As a result, finally, the integral above, which represents the complex amplitude atP, becomes
This is theKirchhoff orFresnel–Kirchhoff diffraction formula.
Geometric arrangement used to express Kirchhoff's formula in a form similar to Huygens–Fresnel
TheHuygens–Fresnel principle can be derived by integrating over a different closed surface (the boundary of some volume having an observation pointP). The areaA1 above is replaced by a part of a wavefront (emitted from aP0) atr0, which is the closest to the aperture, and a portion of a cone with a vertex atP0, which is labeledA4 in the right diagram. If the wavefront is positioned such that the wavefront is very close to the edges of the aperture, then the contribution fromA4 can be neglected (assumed here). On this newA1, the inward (toward the volume enclosed by the closed integral surface, so toward the right side in the diagram) normal toA1 is along the radial direction fromP0, i.e., the direction perpendicular to the wavefront. As a result, the angle and the angle is related with the angle (the angle as defined inHuygens–Fresnel principle) as
The complex amplitude of the wavefront atr0 is given by
So, the diffraction formula becomeswhere the integral is done over the part of the wavefront atr0 which is the closest to the aperture in the diagram. This integral leads to theHuygens–Fresnel principle (with the obliquity factor).
In the derivation of this integral, instead of the geometry depicted in the right diagram, double spheres centered atP0 with the inner sphere radiusr0 and an infinite outer sphere radius can be used.[7] In this geometry, the observation pointP is located in the volume enclosed by the two spheres so the Fresnel-Kirchhoff diffraction formula is applied on the two spheres. (The surface normal on these integral surfaces are, say again, toward the enclosed volume in the diffraction formula above.) In the formula application, the integral on the outer sphere is zero by a similar reason of the integral on the hemisphere as zero above.
Assume that the aperture is illuminated by an extended source wave.[8] The complex amplitude at the aperture is given byU0(r).
It is assumed, as before, that the values of and in the areaA1 are the same as when the screen is not present, that the values of and inA2 are zero (Kirchhoff's boundary conditions) and that the contribution fromA3 to the integral are also zero. It is also assumed that 1/s is negligible compared withk. We then have
This is the most general form of the Kirchhoff diffraction formula. To solve this equation for an extended source, an additional integration would be required to sum the contributions made by the individual points in the source. If, however, we assume that the light from the source at each point in the aperture has a well-defined direction, which is the case if the distance between the source and the aperture is significantly greater than the wavelength, then we can writewherea(r) is the magnitude of the disturbance at the pointr in the aperture. We then haveand thus
In spite of the various approximations that were made in arriving at the formula, it is adequate to describe the majority of problems in instrumental optics. This is mainly because the wavelength of light is much smaller than the dimensions of any obstacles encountered. Analytical solutions are not possible for most configurations, but theFresnel diffraction equation andFraunhofer diffraction equation, which are approximations of Kirchhoff's formula for thenear field andfar field, can be applied to a very wide range of optical systems.
One of the important assumptions made in arriving at the Kirchhoff diffraction formula is thatr ands are significantly greater than λ. Another approximation can be made, which significantly simplifies the equation further: this is that the distancesP0Q andQP are much greater than the dimensions of the aperture. This allows one to make two further approximations:
cos(n, r) − cos(n, s) is replaced with 2cos β, where β is the angle betweenP0P and the normal to the aperture. The factor 1/rs is replaced with 1/r's', wherer' ands' are the distances fromP0 andP to the origin, which is located in the aperture. The complex amplitude then becomes:
Assume that the aperture lies in thexy plane, and the coordinates ofP0,P andQ (a general point in the aperture) are (x0,y0,z0), (x,y,z) and (x',y', 0) respectively. We then have:
The complex amplitude atP can now be expressed aswheref(x',y') includes all the terms in the expressions above fors andr apart from the first term in each expression and can be written in the formwhere theci are constants.
If all the terms inf(x',y') can be neglected except for the terms inx' andy', we have theFraunhofer diffraction equation. If the direction cosines ofP0Q andPQ are
TheFraunhofer diffraction equation is thenwhereC is a constant. This can also be written in the formwherek0 andk are thewave vectors of the waves traveling fromP0 to the aperture and from the aperture toP respectively, andr' is a point in the aperture.
If the point source is replaced by an extended source whose complex amplitude at the aperture is given byU0(r'), then theFraunhofer diffraction equation is:wherea0(r') is, as before, the magnitude of the disturbance at the aperture.
In addition to the approximations made in deriving the Kirchhoff equation, it is assumed that
r ands are significantly greater than the size of the aperture,
second- and higher-order terms in the expressionf(x',y') can be neglected.
When the quadratic terms cannot be neglected but all higher order terms can, the equation becomes theFresnel diffraction equation. The approximations for the Kirchhoff equation are used, and additional assumptions are:
r ands are significantly greater than the size of the aperture,
third- and higher-order terms in the expressionf(x',y') can be neglected.
^J. Saatsi & P. Vickers, "Miraculous success? Inconsistency and untruth in Kirchhoff’s diffraction theory",British J. for the Philosophy of Science, vol. 62, no. 1 (March 2011), pp. 29–46;jstor.org/stable/41241806. (Pre-publication version, with different pagination:dro.dur.ac.uk/10523/1/10523.pdf.)
^M. Born,Optik: ein Lehrbuch der elektromagnetischen Lichttheorie. Berlin, Springer, 1933, reprinted 1965, p. 149.