Following up on Matt's following up on my answer:
Let's pretend that the Darwin curve is a simple rectangle, reflectivity=1 within the Darwin band and 0 outside. Now consider a given energy, with the source having a wide angular distribution. The first crystal will select a range of angles to reflect. Now, if the second crystal is exactly parallel to the first, it will reflect all of the rays. If it's off by the Darwin width, then it will reflect none. In between, the range of angles the two crystals have in common will be linearly related to the angular offset, so that the rocking curve of the one with respect to the other will be a triangle. Now, at other energies, the
same thing happens, so with a white incident beam, you still get a triangle.
A useful tool for visualizing this is the Dumand diagram, which is a plot of angle vs. wavelength or energy. The passband of a single crystal is a curve with a width to it (Darwin width). For the non-dispersive case (common in monochromators) the curves for the two crystals are parallel and offset in the angle direction by the angular offset. The transmission of the system is proportional to the overlap area of the two curves. Books on X-ray diffraction should have examples of these diagrams, which will make it clearer than I can do with words alone.
   mam
----- Original Message ----- From: "Matt Newville" <newvi...@cars.uchicago.edu>
To: "XAFS Analysis using Ifeffit" <ifeffit@millenia.cars.aps.anl.gov>
Sent: Friday, December 04, 2009 10:53 AM
Subject: Re: [Ifeffit] Double crystal monochromator


Just to follow up a little on Matthew's answer:

The Darwin width is the angular width over which a particular
reflection will diffract.   A rocking curve measurement usually leaves
one crystal at a fixed angle and rotates the second crystal.   For a
perfectly collimated beam, the resulting intensity would be a
convolution of the two Darwin widths.

In addition, real x-ray sources have a finite angular spread of the
incident beam, so that the rocking curve profile is further blurred.
For bending magnet beamlines on older sources, the angular spread of
the source can dominate the rocking curve.  Many such sources use a
collimating mirror before the monochromator in order to reduce the
angular spread of the beam on the monochromator.

In most cases, both contributions (natural Darwin width of the
reflection and angular spread of the source) need to be included to
get an accurate rocking curve.

--Matt
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