Heavy-atom refinement/SIR phasing


The information present in the isomorphous diffraction differences between a native and different derivative datasets can be used to derive phases. In order to do this there must be a sufficient number of heavy atom sites in the derivative. A common reason for the failure of isomorphous replacement is a large degree of non-isomorphism between native and derivative. This may be apparent from large unit cell changes (more than 1%) or isomorphous differences which are too large (more than 25%). In general there is often some non-isomorphism, which is usually more significant at higher resolution, this will limit the effective resolution of the phasing.

The heavy-atom sites are usually found using an automated method (see previous tutorial). It is important to remember that there is a hand ambiguity in the location of the sites. The search procedures are based purely on amplitude information. However, a given heavy-atom configuration and its inverse image give rise to identical diffraction amplitudes. The hand ambiguity cannot be resolved unless anomalous diffraction information is available. In general therefore the hand ambiguity can only be resolved by visual analysis of the resulting electron density map. The handedness of secondary structure elements such as alpha-helices or the chirality of amino acids (given sufficient resolution of the data) will indicate if the heavy atom sites need to be inverted.

In this example SIR phasing is performed with the CNS task file ir_phase_kuof.inp. We will perform SIR phasing using the native amplitudes and a uranyl derivative dataset. Three heavy atom sites have already been located using automated methods (see previous tutorial).

      cns_solve < ir_phase_kuof.inp > ir_phase_kuof.out  [3 minutes]
There are several output files:
        ir_phase_kuof.summary 
        ir_phase_kuof.sdb     
        ir_phase_kuof.hkl     
        ir_phase_grad_kuof.hkl
The *.summary file contains information about the progress of the SIR phasing procedure. The refined heavy-atom parameters are stored in the *.sdb site database file. The refined phases are written to the *.hkl files as Hendrickson-Lattman coefficients, and also as centroid phases and corresponding figures of merit. The Fourier coefficients for the gradient maps are stored in the *_grad.hkl file. The use of the hkl file for the detection of additional heavy-atom sites is shown in the following tutorials.

Script to run this tutorial


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