Author:
Bates J. K.,Ebert W. L.,Mazer J. J.,Bradley J. P.,Bradley C. R.,Dietz N. L.
Abstract
ABSTRACTThe examination of reacted layers that form as glass reacts can provide insight into reaction mechanisms that control long-term glass reaction, and into processes by which radionuclides are released to solution. Examples are given for the natural glasses obsidian and tektite, and the nuclear waste glasses 131 and 165, where the layers form bothin-situand precipitated from solution, where they are both amorphous and crystal 1ine, where selective incorporation of actinide elements Into stable phases may offer a barrier to release, and where sloughing of the layers from the glass acts as an alternative radionuclide release process to solubility-limited control.Several reaction processes occur simultaneously as glass reacts, and the projection of glass performance to long time periods requires the identification of those processes that dominate the long-term reaction.
Publisher
Springer Science and Business Media LLC
Reference25 articles.
1. Volcanic glasses, their origins and alteration processes
2. Experimental Hydration Studies of Natural and Synthetic Glasses
3. Hydration of obsidian
4. 23. Bates J. K. , Ebert W. L. , Bradley J. P. , and Bourcier W. L. , High-Level Radioactive Waste Mgmt. 3, American Nuclear Society (in press).
Cited by
9 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献