Abstract
THE low-temperature chemical alteration of natural glass occurs in two stages: an initial stage in which it remains glassy but absorbs as much as 6 per cent water1, and a final stage in which devitrification to clay minerals, with release of silica, occurs2,3. During the first stage the composition of the glass may change, with gain of K2O and water and loss of Na2O (Smith, R. L., personal communication). This change is due to ion exchange.
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 Springer Link
- 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
Ross, C. S., and Smith, R. L., Amer. Min., 40, 1071 (1955).
Friedman, I., and Harris, J., U.S. Geol. Surv. Prof. Paper 424-C, C-304 (1961).
Marshall, R. R., Geol. Soc. Amer. Bull., 72, 1493 (1961).
Nikolsky, B. P., Acta Physicochim. U.R.S.S., 7, 597 (1937).
Eisenman, G., Rudin, D. O., and Casby, J. U., Science, 126, 831 (1957).
Garrels, R. M., Sato, M., Thompson, M. E., and Truesdell, A. H., Science (in the press).
Marshall, C. E., J. Phys. Chem., 43, 1155 (1939).
Anders, R. B., Texas Board of Wafer Engineers Bull., 6007 (1960).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
TRUESDELL, A. Study of Natural Glasses through their Behaviour as Membrane Electrodes. Nature 194, 77–79 (1962). https://doi.org/10.1038/194077b0
Issue Date:
DOI: https://doi.org/10.1038/194077b0
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.