On 03/31/11 18:08, Patrick Loll wrote:
We've just collected a number of inverse beam data sets. It turns out the
crystals showed little radiation damage, so we have a lot of data: 2 x 360 deg
for each crystal, broken up into 30 deg wedges. The collection order went like
this: 0-30 deg, 180-210, 30-60, 210-240, etc.
Now, assuming no slippage, I could simply integrate the first set of data
(non-inverse?) in one run: 0-360 deg. However, since the 12 individual wedges
making up this 360 deg sweep were not collected immediately one after the
other, I don't expect the scale factors for individual images to vary smoothly
(there should be discontinuities at the boundaries between wedges).
So? Isn't that the purpose of scale factors?
--
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All Things Serve the Beam
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David J. Schuller
modern man in a post-modern world
MacCHESS, Cornell University
[email protected]
