Intensity and size , contradicting the prediction of
geometric optics. For an ideal
point source, the intensity of the Arago spot equals that of the undisturbed
wave front. Only the width of the Arago spot intensity peak depends on the distances between source, circular object and screen, as well as the source's wavelength and the diameter of the circular object. This means that one can compensate for a reduction in the source's
wavelength by increasing the distance between the circular object and screen or reducing the circular object's diameter. The lateral intensity distribution on the screen has in fact the shape of a squared
zeroth Bessel function of the first kind when close to the
optical axis and using a
plane wave source (point source at infinity): I_\text{rel}(w) = J_0^2\left(\frac{w R \pi}{g \lambda}\right) + J_1^2\left(\frac{w R \pi}{g \lambda}\right) where J_0and J_1are the Bessel functions of the first kind. R is the radius of the disc casting the shadow, \lambda the wavelength and g the distance between source and disc. For large sources the following asymptotic approximation applies: I_\text{rel}(w) \approx \frac{2 g \lambda }{\pi^2 w R}
Deviation from circularity If the cross-section of the circular object deviates slightly from its circular shape (but it still has a sharp edge on a smaller scale) the shape of the point-source Arago spot changes. In particular, if the object has an ellipsoidal cross-section the Arago spot has the shape of an
evolute. Note that this is only the case if the source is close to an ideal point source. From an extended source the Arago spot is only affected marginally, since one can interpret the Arago spot as a
point-spread function. Therefore, the image of the extended source only becomes washed out due to the convolution with the point-spread function, but it does not decrease in overall intensity.
Surface roughness of circular object The Arago spot is very sensitive to small-scale deviations from the ideal circular cross-section. This means that a small amount of surface roughness of the circular object can completely cancel out the bright spot. This is shown in the following three diagrams which are simulations of the Arago spot from a 4 mm diameter disc (): The simulation includes a regular sinusoidal corrugation of the circular shape of amplitude 10 μm, 50 μm and 100 μm, respectively. Note, that the 100 μm edge corrugation almost completely removes the central bright spot. This effect can be best understood using the
Fresnel zone concept. The field transmitted by a radial segment that stems from a point on the obstacle edge provides a contribution whose phase is tight to the position of the edge point relative to Fresnel zones. If the variance in the radius of the obstacle are much smaller than the width of Fresnel zone near the edge, the contributions form radial segments are approximately in phase and
interfere constructively. However, if random edge corrugation have amplitude comparable to or greater than the width of that adjacent Fresnel zone, the contributions from radial segments are no longer in phase and cancel each other reducing the Arago spot intensity. The adjacent Fresnel zone is approximately given by: \Delta r \approx \sqrt{r^2 + \lambda \frac{g b}{g + b}} - r. The edge corrugation should not be much more than 10% of this width to see a close to ideal Arago spot. In the above simulations with the 4 mm diameter disc the adjacent Fresnel zone has a width of about 77 μm. == Arago spot with matter waves ==