Abstract
THE spectra which are obtained by the diffraction of X-rays by crystals are characteristic both of the substance which emits the X-rays and of the crystal which acts as the grating. If the lines of an accurately ruled plane grating are small in width compared with their distance apart, the intensities of the different orders of spectra are nearly the same. If, however, the lines have a width comparable with the grating constant, the intensities of the higher orders rapidly diminish. When a crystal diffracts a beam of X-rays, the different layers of atoms correspond to the lines of the ordinary transmission grating, so that the relative intensity of the higher orders of spectra will depend upon the ratio of the effective diameter of the atoms in scattering the X-rays to the distance between the successive layers of atoms.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to the full article PDF.
USD 39.95
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
COMPTON, A. The Distribution of the Electrons in Atoms . Nature 95, 343–344 (1915). https://doi.org/10.1038/095343b0
Issue date:
DOI: https://doi.org/10.1038/095343b0
This article is cited by
-
Charge density redistribution with pressure in a zeolite framework
Scientific Reports (2023)
-
Crystallographic Texture and Group Representations
Journal of Elasticity (2022)
-
A new crystallography is born
Nature (2014)


