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.\" RCSid "$Id$" |
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.TH PABOPTO2BSDF 1 2/24/2021 RADIANCE |
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.SH NAME |
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pabopto2bsdf - convert pab-opto BSDF measurements to scattering interpolant representation |
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pabopto2bsdf - convert BSDF measurements to a scattering interpolant representation |
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.SH SYNOPSIS |
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.B pabopto2bsdf |
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[ |
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.B "\-n nproc" |
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][ |
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.B "\-s symmetry" |
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][ |
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.B "\-g angle | 'A'" |
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] |
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.B "meas1 meas2 .." |
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.SH DESCRIPTION |
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front reflection, back reflection, front transmission, |
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and back transmission. |
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Theoretically, only one transmission direction is required, |
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but it is often safest to measure both if both directions |
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will be used in a simulation. |
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.PP |
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See |
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but it is often safest to measure both if they are to |
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be used in a simulation. |
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(See |
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.I bsdf2klems(1) |
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and |
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.I bsdf2ttree(1) |
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.I bsdf2rad(1) |
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and |
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.I bsdfview(1) |
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tools are also useful for visualizaing SIR and XML files. |
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tools are also useful for visualizaing SIR and XML files.) |
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.PP |
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The |
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.I pabopto2bsdf |
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.PP |
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Normally, |
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.I pabopto2bsdf |
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attempts to deduce BSDF symmetry from the incident phi angles |
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provided. |
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will assume a BSDF symmetry from the incident phi angles provided. |
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If every input data file uses the same incident phi angle, the |
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BSDF is assumed to be "isotropic", meaning rotationally symmetric. |
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BSDF is assumed to be "isotropic", or rotationally symmetric. |
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If input phi angles only cover one quarter of the incident hemisphere, |
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then the sample is assumed to have quadrilateral symmetry. |
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Similarly, half-hemisphere coverage implies "bilateral" symmetry, |
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meaning that the sample material looks identical when viewed in a mirror. |
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However, "up" symmetry means that the sample looks the same when |
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rotated by 180-degree (upside-down), but does not look the same in a mirror. |
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Although bilateral symmetry is a superset of "up" symmetry, |
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we assume the former when provided only half of the input hemisphere. |
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The "up" symmetry was a late addition, and involves rotating and copying the |
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input data, treating the result as anisotropic. |
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It is therefore less efficient, and should only be used when necessary. |
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Finally, if the incident hemisphere is fully covered, the BSDF is also anisotropic. |
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Finally, if the incident hemisphere is fully covered, the final BSDF |
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is anisotropic. |
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.PP |
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If a |
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.I \-s |
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Note that only the "up" and "bilateral" symmetry options have |
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identical input coverage, so this is the only time the |
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.I \-s |
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option must be specified if the default mirroring is inappropriate. |
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option must be specified if the default mirroring is not appropriate. |
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.PP |
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If a |
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.I \-g |
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option is present, it will cull scattered measurements that are nearer |
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to grazing than the given angle in degrees. |
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If the word "auto" (which can be abbreviated as 'a' or 'A') is given |
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instead of an angle, then the near-grazing angle will be determined |
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by the lowest incident angle measurement present in the input data. |
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This is sometimes necessary to eliminate noise and edge effects that |
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some measurements exhibit near grazing. |
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.PP |
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The |
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.I Mountain |
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software operates the pg2 goniophotometer to |
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capture BSDF scattering data in separate files for each incident |
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angle in a text file beginning with a header |
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capture BSDF scattering data in separate text files for each incident |
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angle, beginning with a header |
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whose lines each start with a pound sign ('#'). |
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Some header settings require colons and others do not, as indicated below. |
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The |
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are considered incident to the "front" side of the sample, and |
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theta values greater than 90 are incident to the "back" side in |
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the standard coordinate system. |
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Notions of sample "front" and "back" may be reversed using the |
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Notions of "front" and "back" may be reversed using the |
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.I -t |
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option if desired. |
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.TP |
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.BR #upphi |
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If present, this phi angle that corresponds to |
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the sample "up" orientation. |
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By default, it is assumed to be 0 degrees, meaning that "up" |
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By default, it is assumed to be 0, meaning that "up" |
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is phi=0. |
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To get the standard RADIANCE coordinates for BSDFs, "#upphi" should |
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be set to 90. |
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be set to 90 (degrees). |
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.TP |
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.BR #colorimetry: |
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Two colorimetry values are currently understood, "CIE-Y" and "CIE-XYZ". |
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The default colorimetry of "CIE-Y", which may be left unspecified, |
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Two colorimetry values are currently understood: "CIE-Y" and "CIE-XYZ". |
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The default "CIE-Y" colorimetry |
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takes each DSF or BSDF value as photometric. |
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If "CIE-XYZ" is specified, then the DSF or BSDF values must be triplets |
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corresponding to CIE XYZ values. |
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pabopto2bsdf -n 4 -s up f*_Rvis.txt > front_refl.sir |
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.br |
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bsdf2klems front_trans.sir front_refl.sir > Klems_bsdf.xml |
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.SH NOTES |
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If the BSDF is being mirrored and there is no measured theta=0 incident |
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angle data file, this part of the distribution is filled in |
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by a special procedure. |
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This is important because there is no way to extrapolate missing |
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data at normal incidence. |
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.PP |
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The BSDF is extrapolated past the last measured theta angles towards |
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grazing using a constant value plus a single Gaussian lobe if one can |
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be reasonably fit to the near-grazing data. |
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This lobe will always be in the mirror direction in the case of |
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reflection, or the "through" direction in the case |
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of transmission. |
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The magnitude and width of this lobe is stored in the output header, |
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along with the constant value. |
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Both the lobe and the constant are neutral values, even with CIE-XYZ |
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colorimetry. |
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.PP |
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While there is no explicit handling of infrared or solar radiometry, |
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any single-channel BSDF will be created the same, and the final XML |
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file generated by |
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.I bsdf2klems |
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or |
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.I bsdf2ttree |
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can be edited to specify a different radiometry. |
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The interpolation process in |
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.I pabopto2bsdf |
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is not affected by this. |
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.PP |
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The standard BSDF coordinates in RADIANCE have the theta=0 direction |
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corresponding to the front-side surface normal. |
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The phi=0 direction points to the right as seen from the front, and |
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phi=90 degrees corresponds to the "up" orientation for the sample. |
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The same theta and phi are used for incoming and scattered angles, |
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so theta=180 is the opposite side surface normal. |
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This differs from the WINDOW, which use separate |
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coordinate systems for the front and the back. |
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To confusing things further, notions of "front" and "back" are |
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opposite in WINDOW and RADIANCE. |
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In RADIANCE, the normal of a window surface usually faces the |
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interior of a space. |
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.PP |
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In the |
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.I genBSDF(1) |
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utility, the world coordinate system follows trigonometric |
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conventions with theta=0 aligning to the Z-axis, |
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the X-axis matches (theta,phi)=(90,0), and the Y-axis |
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corresponds to (theta,phi)=(90,90). |
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The latter is thought of as the "up" direction for the sample. |
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This usually needs to be rotated into position, since most |
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RADIANCE models use the Z-axis as the world "up" direction. |
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.SH AUTHOR |
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Greg Ward |
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.SH "SEE ALSO" |
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bsdf2klems(1), bsdf2rad(1), bsdf2ttree(1), bsdfview(1), pabopto2xyz(1) |
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bsdf2klems(1), bsdf2rad(1), bsdf2ttree(1), bsdfview(1), genBSDF(1), |
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pabopto2xyz(1) |