Abstract
W. J. C. ORR and D. W. Thomson1 have found the velocity of diffusion of HDO into H2O to be abnormally large, the diffusion constant D being 9 × 104 cm.2 sec.-1 at 15° C., whereas for all simple substances in water, diffusion constants are of the order of magnitude 105 cm.2 sec.-1. Since this result, if it were true, would be of considerable significance for the theory of the structure of water, experiments were made to verify it.
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 full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
NATURE, 134, 776; 1934.
Z. phys. Chem., A, 166, 254; 1933.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
TEMKIN, M. Diffusion of Heavy Water into Ordinary Water. Nature 136, 552 (1935). https://doi.org/10.1038/136552a0
Issue date:
DOI: https://doi.org/10.1038/136552a0
This article is cited by
-
Isotopes in research
Soviet Atomic Energy (1969)