|
2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | |
12 | 14 | 15 | 16 | 18 | 20 | 21 | 24 | 28 | |
30 | 35 | 36 | 40 | 42 | 45 | 48 | 56 | 60 | |
63 | 70 | 72 | 80 | 84 | 90 | 105 | 112 | 120 | |
126 | 140 | 144 | 168 | 180 | 210 | 240 | 252 | 280 | |
315 | 336 | 360 | 420 | 504 | 560 | 630 | 720 | 840 | |
1008 | 1260 | 1680 | 2520 | 5040 | |||||
The last restriction is that the summation order of
the map must be consistent with the sort order of the
reflections on the bdf. The algorithm in RFOURR depends
upon the sort order of the reflections and the summation
order of the input density map. Table 2 gives the
relationship between the two parameters in terms of the
instructions used for
SORTRF
and
FOURR
.
Table 2: Reflection Order Related to Map Directions
Reflection order | Map directions | ||
slow/med/fast | a | b | c |
|
across | down | layer |
|
across | layer | down |
|
down | across | layer |
|
layer | across | down |
|
down | layer | across |
|
layer | down | across |
If the sort order is not established by the
SORTRF
program it may be specified on the
RFOURR line. In addition
to the sort order another related parameter is required.
They are a set of signals which indicate whether the miller
indices on the bdf are negative. This information is stored
on the bdf by SORTRF or may be explicitly stated on the
RFOURR line. The
option must be used in SORTRF.
Note that the slow changing index must have no
negative indices. That is for triclinic the
hemisphere of data is always +++, -++, +-+, --+ when a
sort 3
or
lhk
sort has been specified. For monoclinic only
+++ and -++ would be present. For orthorhombic only +++
would be present on the file.lkh
The most efficient order for a Fourier transform is over the short axis first (across), medium length axis next (down) and finally the long axis (layer). This produces the fewest groups of reflections and results in the most efficient Fourier transformations.
RFOURR depends upon the input map being of the entire unit cell (no more, no less) with all symmetry equivalent points having identical electron density. The XTAL system stores only the unique asymmetric set of reflections in the bdf. The following algorithm in employed. As each line of the input map is loaded it is transformed, . The second sum coefficients G are stored until one layer, all for a given , has been treated. The layer is tranformed for all values to produce P( , , ) coefficients of the third sum direction. This is the massive array required by the FFT algorithm. The third direction summation is driven by the input bdf, resulting in only the phases of the unique asymmetric set of reflections within the resolution of the input map being calculated. In this summation the F( , , ) is produced and stored on the output bdf as A( , , ), B( , , ) and ( , , ).
The RFOURR calculation produces four structure factor
coefficients: the calculated magnitude (CAL); the phase
(PHI) and the complex components (A & B). These
coefficients are inserted into the
lrrefl:
packets of the output bdf. In the simplest case
these coefficients CAL, A, B and PHI will the standard
structure factor items represented by the ID numbers n800,
n801, n802 and n700, respectively. In other cases, the ID
numbers will be determined by the type of density map, and
the nature of the filtering that it has undergone. For the
non-standard case the user may define the ID numbers of the
output items with the
idnums line.
The ID number of the input coefficient (OBS) may also
defined on this line. The default is Frel with dispersion
removed (n701), or if this is not present, Frel (n304).
Note that the input coefficient is only important if the
results are to be printed (see the
option on the
RFOURR line) and the
calculated R -factor (see below) is to be
meaningful.pr
Map Resolution And Precision
An R factor
is calculated during the
transformation. This R factor is useful if the input
density has been filtered. For an input map prepared by
FOURR
the result is of academic interest since it should
be zero (OBS->density->OBS results in no differences
in OBS). If, however, there is a reduction in resolution by
restricting the fineness of the grid during FOURR then the
resulting OBS produced by the back transform will be
distorted and a higher R value will result.
When RFOURR is applied the resolution of the input density map will determine the extent of the reflections for which phases are determined. In order that every reflection be phased it is necessary that the input map have a resolution of at least 2 , 2 and 2 grid points respectively in the x,y and z directions. Anything less will result in the high order reflections being left unphased. Output idems for these reflections are set to voidflg:.
To avoid the indeterminacy associated with phasing
structure factors where
both A and B are very small, the user
may define a threshold via the
option on the
RFOURR line. The default
value is 0.005. Items for reflections below the threshold,
are set to
voidflg:.Similarly, if a reflection is
outside the limits defined by the
maxhkl line, or the
values from
th
lrdset:
of the input bdf, the output items will be set
to
voidflg:.
Reads reflection data from the input archive bdf
Writes output items to the output archive bdf
Reads density map from the bdf
map
RFOURR lhk
This is a standard run. The inclusion of
is only required if
lhk
SORTRF
has not been used to sort the reflection data on the
bdf. If SORTRF has not been applied the
indicates the sort order l slow; k fast is
how the data is supplied (the program will fail if the
reflection data is not sorted -- you are strongly advised
to use
lhk
SORTRF
). The output coefficients are Fcal, Acal, Bcal and
. No reflection
data is printed.
RFOURR ds 2 th .5 print 100 idnums 900 950 951 952 953
This is a special run using reflections from dataset
2. The input comparison coefficient has the idnum 2900; the
output coefficients CAL, A, B and PHI are stored as 2950,
2951, 2952 and 2953. The first 100 reflections are printed
and only reflections with A and B > 0.5 will be phased.
The sort order of the reflection data is extracted from
lrdset:
and checked against the map orientation.