Abstract
Albite (NaAlSi3O8), a framework silicate of the plagioclase feldspar family and a common constituent of felsic rocks, is often present in the siliceous mineral aggregates that compose concrete. When exposed to radiation (e.g., in the form of neutrons) in nuclear power plants, the crystal structure of albite can undergo significant alterations. These alterations may degrade its chemical durability. Indeed, careful examinations of Ar+-implanted albite carried out using Fourier transform infrared spectroscopy (FTIR) and molecular dynamics simulations show that albite's crystal structure, upon irradiation, undergoes progressive disordering, resulting in an expansion in its molar volume (i.e., a reduction of density) and a reduction in the connectivity of its atomic network. This loss of network connectivity (i.e., rigidity) results in an enhancement of the aqueous dissolution rate of albite - measured using vertical scanning interferometry (VSI) in alkaline environments - by a factor of 20. This enhancement in the dissolution rate (i.e., reduction in chemical durability) of albite following irradiation has significant impacts on the durability of felsic rocks and of concrete containing them upon their exposure to radiation in nuclear power plant (NPP) environments.
Original language | English |
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Pages (from-to) | 7835-7845 |
Number of pages | 11 |
Journal | Journal of Physical Chemistry A |
Volume | 121 |
Issue number | 41 |
DOIs | |
State | Published - Oct 19 2017 |
Funding
The authors acknowledge financial support for this research provisioned by the Department of Energy’s Nuclear Energy University Program (DOE-NEUP: DE-NE0008398), National Science Foundation (CAREER Award: 1253269), and University of California, Los Angeles (UCLA). The contents of this paper reflect the views and opinions of the authors who are responsible for the accuracy of data presented. This research was carried out in the Laboratory for the Chemistry of Construction Materials (LC2), Molecular Instrumentation Center, and Laboratory for the Physics of Amorphous and Inorganic Solids (PARISlab) at UCLA. As such, the authors gratefully acknowledge the support that has made these laboratories and their operations possible.