Wilson Plot and E Statistics
https://xraytools.com/wilson?structure=rutile
The evidence systematic absences cannot give. A centre of inversion forces every phase to 0 or 180°, which leaves a mark on the distribution of the intensities rather than on which of them are missing — so it is measurable exactly where the determination runs out. The same shell averages give the Wilson plot, whose slope is the overall temperature factor.
- Before this
- The evidence here is the distribution of intensities rather than any one of them, so |F|² and what makes it large or small is assumed — see the structure factor.
- You supply
- One of the named structures. A full set of reflections is computed from its atoms, so nothing has to be measured — and an overall B can be added to see the plot tilt.
- Reading it
- Wilson's derivation assumes many atoms of comparable scattering power sitting at random. A structure whose atoms are all on special positions has no free coordinates at all, so the statistic means nothing there — and the page refuses a verdict rather than giving the wrong one.
Worked examples: albite, 52 atoms in the cell — centrosymmetric · quartz, no centre of inversion · cristobalite — the same, from different symmetry · albite with an overall B of 3 Ų · rutile — where the test does not apply · berlinite — where the test is confidently wrong · albite scaled by 1000 — the intercept gives it back · zirconia — where N(z) answers and the statistic cannot
Notation here: s · F, |F| · I · E · U, B · K — what each one means here
Terms here: centring · general position · zone
See also: Intensity Corrections · Space Group from Absences · Structure Factor Calculator
What each input changes
- Overall B
- An overall temperature factor added to the computed data. It tilts the plot: the slope IS this number, which is what makes the plot readable backwards.
Input
Systematic absences see the centring, the glide planes and the screw axes, and they cannot see a centre of inversion: two groups built from the same centring, glides and screws — C2/c and Cc, Pnma and Pn21a — extinguish exactly the same reflections whether or not one of them has that centre. That is why the determination hands back a family of groups, and this statistic is the independent evidence that separates them.
No verdict
This structure cannot be judged this way, and the number below is printed only so that you can see it is not to be believed.
Every atom in this structure sits on a special position, so no atom is free in the cell: the symmetry fixes its coordinates outright, or confines them to a line or a plane it chooses. Wilson's derivation puts atoms at random, and a symmetry-placed atom is the opposite of that — it has fewer copies than the group has operations, and their contributions to F move in step instead of independently. The number below is not evidence about a centre of inversion. Rutile is the case worth trying: it is centrosymmetric and the statistic points the other way.
〈||E|2 − 1|〉 = 0.828, where the space group P42/mnm does contain a centre of inversion.
|E|2 is an intensity divided by the mean of its own shell, so it says how strong a reflection is for its resolution and the fall-off is already gone. A centre of inversion forces every phase to 0 or 180°, which spreads the intensities wider than random phases do: 〈||E|2 − 1|〉 is 0.968 with a centre and 0.736 without one. One term of the full treatment is deliberately missing here: reflections lying in a zone that the symmetry maps onto itself have a mean intensity ε times the general one — ε is 2 or 3 in several zones of quartz, for instance — and a complete normalisation divides by ε before forming |E|. It is left out because it changes the verdict only for structures this page already declines to judge, and an uncheckable correction that buys nothing measurable is worse than a stated omission. Expect a small bias, not a different answer.
The Wilson plot
4 shells, from 1.55 Å down to 0.64 Å. Point at one to read it, or click to keep it.
B = 0.04 Ų from the slope, over 4 resolution shells.
Each point is one resolution shell: the mean intensity divided by the mean of Σf02, which is what the shell would scatter with stationary atoms. The ratio falls as exp(−2B s2), so the logarithm is a straight line and its slope is −2B, where s = sin θ/λ — the same s the structure factor and the powder pattern use, so a B means the same thing on all three pages. The intercept is the other half of the classical plot: on measured data it gives the scale factor that puts arbitrary detector counts onto the absolute scale of electrons, which is what lets a first model be built at all. This page starts from computed structure factors, so at K = 1 there is nothing for it to recover — put a scale factor in and it recovers that instead, which is the same arithmetic a first data set gets. The temperature factor is the only thing in the calculation that makes the line tilt; the scale is the only thing that lifts it. The recovered value carries a small offset of its own, because Wilson's derivation assumes atoms at random and a real structure is not random; what tracks the temperature factor exactly is the change in the slope, so put in two different values and compare.
N(z): the weak reflections
The other classical test, and it looks at the opposite end of the distribution from everything above: N(z) is the fraction of reflections weaker than z times the mean of their own resolution shell. A centre of inversion forces every phase to 0 or 180°, so an intensity is the square of one number and near-zero values are common; without a centre it is the square of a two-dimensional vector, and a near-zero value needs both components small at once. That is why the two ideals are furthest apart at the bottom of the table: at z = 0.1 they are 0.248 and 0.095, a factor of 2.6. The curve is drawn over 98 reflections, each divided by its own shell mean so the temperature factor is already gone.
| z | observed N(z) | centric | acentric |
|---|---|---|---|
| 0.1 | 0.235 | 0.248 | 0.095 |
| 0.2 | 0.306 | 0.345 | 0.181 |
| 0.3 | 0.388 | 0.416 | 0.259 |
| 0.4 | 0.429 | 0.473 | 0.330 |
| 0.5 | 0.449 | 0.520 | 0.393 |
| 0.6 | 0.480 | 0.561 | 0.451 |
| 0.8 | 0.520 | 0.629 | 0.551 |
| 1.0 | 0.551 | 0.683 | 0.632 |
This curve decides nothing, for the reason the statistic above decides nothing: every atom here sits on a special position, so the reflections are not the sum of random contributions Wilson’s derivation assumes. The numbers in the table are real and the comparison is not.
What was measured
| measured | ideal, centre | ideal, no centre | |
|---|---|---|---|
| Space group | P42/mnm, order 16 | ||
| Atoms in the cell | 6 | ||
| Effective scatterers | 3.09 | ||
| Scattering from general positions | 0% | ||
| Unique reflections | 98 to 0.60 Å | ||
| Resolution shells | 4 | ||
| 〈|E|2〉 | 1.000 | 1.000 | 1.000 |
| 〈|E|〉 | 0.846 | 0.798 | 0.886 |
| |E| > 1 | 44.9% | 31.7 % | 36.8 % |
| |E| > 2 | 0.0% | 4.6 % | 1.8 % |
| |E| > 3 | 0.0% | 0.3 % | 0.0 % |
The effective count is (Σf²)² / Σf4: it equals the atom count when every atom is the same element and falls below it as one atom starts to dominate, which is what Wilson’s “atoms of comparable scattering power” is asking for. It is that combination rather than any other because it is the one the fourth moment turns on — ⟨E4⟩ is 2 − 1/Neff for a structure with no centre and 3 − 2/Neff for one with a centre, and those two relations are what fix it.
The ideal values are in the two columns beside them — 31.7 / 4.6 / 0.3 % with a centre and 36.8 / 1.8 / 0.0 % without, for |E| above t = 1, 2 and 3, computed from erfc(t/) with a centre and exp(−t²) without rather than taken from a table — but a synthetic data set this size holds only a handful of reflections above |E| = 2 and none above 3 for most structures, so they describe the distribution here without deciding anything. The mean deviation above is what the verdict rests on.
Try it
albite, 52 atoms in the cell — centrosymmetric · quartz, no centre of inversion · cristobalite — the same, from different symmetry · albite with an overall B of 3 Ų · rutile — where the test does not apply · berlinite — where the test is confidently wrong · albite scaled by 1000 — the intercept gives it back · zirconia — where N(z) answers and the statistic cannot
Where this comes from
- The probability distribution of X-ray intensities
A. J. C. Wilson, Acta Cryst. 1949, 2, 318–321 · doi:10.1107/S0365110X49000813
The plot, the scaling, and the intensity statistics this page is entirely built on.