Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a2229193bcc19de8

Jump to content

Greninger chart

From Wikipedia, the free encyclopedia
GreningerChart

In crystallography, a Greninger chart[1] /ˈɡrɛnɪŋər/ is a chart that allows angular relations between zones and planes in a crystal to be directly read from an x-ray diffraction photograph.

The Greninger chart is a simple trigonometric tool to determine g and d for a fixed sample-to-film distance. (If one uses a 2-d detector the problem of determining g and d could be solved mathematically using the equations which generate the Greninger chart) A new chart must be generated for different sample to detector distances. (2s is 2q for the diffraction peak and tan m is x/y for the Cartesian coordinates of the diffraction peak.) The Greninger chart gives directly the two angles needed to plot poles on the Wulff net. It is critical to keep track of the relative arrangement of the sample to the film, if photographic film is used then this is achieved by cutting the corner of the film. For Polaroid film one must make a note of the arrangement of the face of the film in the camera.

See also

[edit]

References

[edit]
  1. It is named after Alden Buchanan Greninger (17 September 1907, Glendale, Oregon  20 April 1998).

Sources

[edit]
  • Greninger A. B. (1935). Zeitschrift für Kristallographie 91: 424.
[edit]