The Sampled as a Function of Spherical Angles direction apodization type scales all source rays to an arbitrary intensity pattern defined in spherical coordinates. Apodization factors are entered as a function of azimuth and polar angles and values are linearly interpolated between these data points. If data is entered for only one Azimuth angle, then the apodization profile is considered rotationally symmetric. The following images show the source and intensity distribution for an isotropic plane of random rays emitting into a 90o cone half angle with the Sampled as a Function of Spherical Angles apodization applied.
The Sampled as a function of spherical angles directional apodization is available on the Power tab of a Detailed Source dialog. From the Power tab, select "Sampled as a function of spherical angles" from the drop down menu of directional apodization types.
The following table describes the available controls on the Power tab of a Detailed Source dialog. Of interest to this help topic are the Direction Apodization parameter settings.
Rows and columns can be added/inserted/deleted by right mouse clicking in the spreadsheet area and selecting either "Append Polar Angle", "Append Azimuthal Angle", "Insert Polar Angle", "Insert Azimuthal Angle", "Delete Polar Angle", or "Delete Azimuthal Angle". The azimuth angles must lie in the range of –180o to 180o and the polar angles must be in the range of 0o to 180o. If polar angle data for only one azimuth angle (column) is entered, then the apodization is assumed to be rotationally symmetric. If polar data is entered for more than one azimuth angle, then apodization factors for angles in between the entered data is linearly interpolated.
Apodization data can be read from a properly formatted text file using the "Replace With Data From a File" option, accessible by right mouse clicking in the spreadsheet area. The text file contains two header lines, two vectors (polar and azimuthal direction vectors) and then the data. The first header line must read "type direction_apodization", the second header line must read "format xyz_xyz_a", the third line contains the X, Y and Z components of the polar vector, the fourth line contains the X, Y and Z components of the azimuthal vector, the fifth line is a "0" followed by each of the sampled azimuthal angles (the zero is ignored), and the remaining lines are the polar angles and apodization factors in the form "angle val val val .....". The apodization values must be <= 1. An example file format is shown below with four azimuthal angles (-90o, 0o, 90o, 180o) and eighteen polar angles (0-85deg in 5o steps).
Apodization data can also be digitized from a bitmap or other graphic file types.
Direction Apodization - Uniform Unit Apodization Direction Apodization - Inverse Lambertian in a given direction Direction Apodization - Gaussian Direction Apodization - cos^n or sin^n in a given direction Direction Apodization - Lambertian in a given direction
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