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Figure 6
The dependence of merging success on phase accuracy, completeness and the angular spread of reflection data. A total of 25 920 simulated data sets were generated across three crystal systems, spanning a range of P1 completeness, phase errors and relative B factors. Pairs of data sets with similar starting characteristics and in random orientations were merged. (a) The fractional merge error was computed as the magnitude of the vector error between the true and estimated fractional shifts required to position data sets on a common phase origin. This metric is shown as a function of the mean phase error (left), P1 completeness (center) and how unevenly spread the reflections were across the tilt range (right) for the data sets being merged. The latter was estimated as the Jensen–Shannon (JS) distance to a uniform angular distribution spanning ±60° (see equation 8 ![]() |