Hostname: page-component-78c5997874-m6dg7 Total loading time: 0 Render date: 2024-11-10T09:03:44.444Z Has data issue: false hasContentIssue false

On Grassmann's method of axial representation, and its application to the solution of certain crystallographic problems

Published online by Cambridge University Press:  14 March 2018

W. J. Lewis*
Affiliation:
Professor of Mineralogy in the University of Cambridge

Extract

Grassmann, in his Memoir, Zur physlschen Krystallographie und geometrischen Combinationslehre, published in 1829, referred a crystal to three face-normals--rays--as axes of reference; the parameters being the edges along the axes of a parallelepiped having for diagonal a definite length of a known normal which is not co-planar with any pair of the axial rays. Any other normal is then represented as the diagonal of a similarly formed parallelepiped having for its edges along the axes lengths which are rational multiples of the parameters. Grassmann gave no formulæ for finding in general the indices of face-normals from measurements of the angles on the crystal; nor for determining the angles from the crystal-elements and indices.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1900

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)