Fluctuating XRD Sapphire Intensity

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Discussion Overview

The discussion revolves around the fluctuations in intensity of sapphire peaks observed during X-ray diffraction (XRD) phase analysis. Participants explore the potential influence of the sapphire substrate's orientation with respect to the phi axis and the implications for accurate measurements in XRD experiments.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • One participant notes that the intensity fluctuations may be related to the orientation of the sapphire substrate with respect to the phi axis during XRD scans.
  • Another participant suggests that the sharpness of sapphire peaks means that even slight misalignments can significantly affect intensity, indicating the need for precise alignment.
  • It is proposed that the observed behavior resembles an azimuth scan, which requires exact alignment of the reciprocal lattice vector along the phi axis for accurate results.
  • A recommendation is made to perform rocking curve scans at various phi angles to assess the integrated intensity and identify any misalignment issues.
  • Participants discuss the UB matrix, which consists of two components: a transformation matrix (B) and a rotation matrix (U), which are crucial for understanding crystal orientation in relation to the diffractometer.
  • Clarification is sought regarding the UB matrix and its role in XRD, with references to literature for further reading.

Areas of Agreement / Disagreement

Participants express varying views on the causes of intensity fluctuations, with some agreeing on the importance of alignment while others provide different perspectives on the implications of the azimuth scan and the UB matrix. The discussion remains unresolved regarding the exact nature of the fluctuations and the best approach to mitigate them.

Contextual Notes

There are limitations related to the assumptions about the alignment of the crystal and the specific conditions under which the XRD scans are performed. The discussion does not resolve the mathematical details of the UB matrix or the precise alignment techniques necessary for optimal results.

maxxlr8
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A few months back my colleagues and I are facing a problem where the intensity of our sapphire peak fluctuates every time an XRD phase analysis was done, even when the scan was done on the same sample.

By accident, I found that the orientation of the sapphire substrate with respect to phi axis somehow plays a part in the situation.

So, I decided to do a scan following the procedure below:
  1. Moved the 2-theta to the diffraction angle of (30-30) plane of my sapphire substrate, which is ~68.3 degrees
  2. As this is a symmetric scan, omega has been rotated to ~34.2 degrees
  3. Shutter was opened, and the phi axis has been rotated 360 degrees

Below is the result:
asdf.JPG


It can be seen that although 2-theta has been placed at the diffraction angle of the sapphire substrate, diffraction only occurs at two main regions in phi, which are approximately:
  1. -63 to -12 degrees
  2. 85 to 140 degrees

For now, only samples with sapphire substrates have this kind of problem. It is not known if other samples involving silicon or GaAs substrates have the same issue.

Can anyone help explain the theory behind this observation?

Thank you
 
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Sapphire peaks are very sharp, so even a slight misalignment will kill your intensity. It looks as if you tried to perform an azimuth scan, i.e. rotate the crystal about the Bragg planes while keeping the Bragg peak aligned. This will work only if the reciprocal lattice vector is aligned *exactly* along the phi axis of rotation. In practice that is a bit difficult to achieve. If there is some misalignment, then phi couples to the Bragg angle and you combine a rocking curve scan and an azimuth scan. If you carefully examine your UB matrix you can probably determine the angle of misalignment.

You might try to step phi in, say, steps of 5 degrees and perform a rocking curve scan at each value of phi. The integrated intensity of the rocking curve scans should not very - at least not strongly.
 
M Quack said:
Sapphire peaks are very sharp, so even a slight misalignment will kill your intensity. It looks as if you tried to perform an azimuth scan, i.e. rotate the crystal about the Bragg planes while keeping the Bragg peak aligned. This will work only if the reciprocal lattice vector is aligned *exactly* along the phi axis of rotation. In practice that is a bit difficult to achieve. If there is some misalignment, then phi couples to the Bragg angle and you combine a rocking curve scan and an azimuth scan. If you carefully examine your UB matrix you can probably determine the angle of misalignment.

You might try to step phi in, say, steps of 5 degrees and perform a rocking curve scan at each value of phi. The integrated intensity of the rocking curve scans should not very - at least not strongly.

Million thanks for the reply and explanation.
  1. I did not realize that this is an azimuth scan.
  2. Since this result, we have always align the phi axis to the angle with the best intensity before performing phase analysis scans.
  3. I am sorry, M Quack, but can you explain the term UB matrix? Thank you.
 
The UB matrix is actually the product of two matrices, U and B.

B performs the transformation from HKL coordinates to an orthonormal coordinate system of reciprocal space with the c-axis along z. For cubic crystals B is just (2pi/a, 0,0; 0, 2pi/a, 0; 0,0,2pi/a). For hexagonal it is not diagonal because the angle between the a* and b* axes is not 90 deg, and so on. It depends only on the lattice parameters a,b,c and lattice angles alpha, beta, gamma.

U is a rotation matrix that describes how the crystal is oriented relative to the innermost rotation axis of your diffractometer. If your sample is mounted on a goniometer head on the phi axis, then tweaking the goniometer head tilts will modify the matrix U.

This is described in most books about x-ray diffraction, but I highly recommend reading the original article by Busing and Levy:

Acta Cryst. (1967). 22, 457-464 [ doi:10.1107/S0365110X67000970 ]
Angle calculations for 3- and 4-circle X-ray and neutron diffractometers
W. R. Busing and H. A. Levy

http://scripts.iucr.org/cgi-bin/paper?a05492
 
M Quack said:
The UB matrix is actually the product of two matrices, U and B.

B performs the transformation from HKL coordinates to an orthonormal coordinate system of reciprocal space with the c-axis along z. For cubic crystals B is just (2pi/a, 0,0; 0, 2pi/a, 0; 0,0,2pi/a). For hexagonal it is not diagonal because the angle between the a* and b* axes is not 90 deg, and so on. It depends only on the lattice parameters a,b,c and lattice angles alpha, beta, gamma.

U is a rotation matrix that describes how the crystal is oriented relative to the innermost rotation axis of your diffractometer. If your sample is mounted on a goniometer head on the phi axis, then tweaking the goniometer head tilts will modify the matrix U.

This is described in most books about x-ray diffraction, but I highly recommend reading the original article by Busing and Levy:

Acta Cryst. (1967). 22, 457-464 [ doi:10.1107/S0365110X67000970 ]
Angle calculations for 3- and 4-circle X-ray and neutron diffractometers
W. R. Busing and H. A. Levy

http://scripts.iucr.org/cgi-bin/paper?a05492

Thank you for introducing the UB matrix. Somehow I am not aware of this.

The literature is very interesting, although I may have to digest the contents slowly.
 

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