Dear Francis,

the spots will be excluded individually based on the inhomogeneous background, 
so you don't need to apply a resolution cutoff.
However, once you have determined and refined your structure it may be worth 
predicting the intensity of these spots and put them back for map calculation,
this might avoid gaps in your map corresponding to inter-atom distances for 
which data are missing in the resolution range of the ice rings; as long as 
this is done only for a relatively small set of reflections there is not much 
risk of introducing a bias here.

HTH,

Bruno




-----Message d'origine-----
De : CCP4 bulletin board [mailto:CCP4BB@JISCMAIL.AC.UK] De la part de Francis E 
Reyes
Envoyé : Tuesday, October 11, 2011 5:17 PM
À : CCP4BB@JISCMAIL.AC.UK
Objet : [ccp4bb] Ice rings...

All,


So I have two intense ice rings where there appear to be lattice spots in 
between them. 

I understand that any reflections that lie directly on the ice ring are 
useless, however, how do software programs (HKL2000, d*Trek, mosflm, XDS) deal 
with these intermediate spots? 

It would seem to me that employing a 'resolution cut off' just before the ice 
ring (on the low resolution side) would be improper, as there are spots on the 
high resolution side of the ice. (see enclosed .tiff)


In fact, how do these programs deal with spots lying on ice rings? Are they 
rejected by some algorithm by those programs during integration, or is it up to 
the scaling/merging (by SCALA for example) step to deal with them? 

Thanks!

F

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