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Title: Nonlinear dynamics and instability of aqueous dissolution of silicate glasses and minerals

Abstract

Aqueous dissolution of silicate glasses and minerals plays a critical role in global biogeochemical cycles and climate evolution. The reactivity of these materials is also important to numerous engineering applications including nuclear waste disposal. The dissolution process has long been considered to be controlled by a leached surface layer in which cations in the silicate framework are gradually leached out and replaced by protons from the solution. This view has recently been challenged by observations of extremely sharp corrosion fronts and oscillatory zonings in altered rims of the materials, suggesting that corrosion of these materials may proceed directly through congruent dissolution followed by secondary mineral precipitation. Here we show that complex silicate material dissolution behaviors can emerge from a simple positive feedback between dissolution-induced cation release and cation-enhanced dissolution kinetics. This self-accelerating mechanism enables a systematic prediction of the occurrence of sharp dissolution fronts (vs. leached surface layers), oscillatory dissolution behaviors and multiple stages of glass dissolution (in particular the alteration resumption at a late stage of a corrosion process). In conclusion, our work provides a new perspective for predicting long-term silicate weathering rates in actual geochemical systems and developing durable silicate materials for various engineering applications.

Authors:
 [1];  [1];  [1]
  1. Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Publication Date:
Research Org.:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Sponsoring Org.:
USDOE Office of Nuclear Energy (NE), Fuel Cycle Technologies (NE-5)
OSTI Identifier:
1313074
Report Number(s):
SAND-2016-4035J
Journal ID: ISSN 2045-2322; srep30256
Grant/Contract Number:
AC04-94AL85000
Resource Type:
Journal Article: Accepted Manuscript
Journal Name:
Scientific Reports
Additional Journal Information:
Journal Volume: 6; Journal ID: ISSN 2045-2322
Publisher:
Nature Publishing Group
Country of Publication:
United States
Language:
English
Subject:
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY

Citation Formats

Wang, Yifeng, Jove-Colon, Carlos F., and Kuhlman, Kristopher L. Nonlinear dynamics and instability of aqueous dissolution of silicate glasses and minerals. United States: N. p., 2016. Web. doi:10.1038/srep30256.
Wang, Yifeng, Jove-Colon, Carlos F., & Kuhlman, Kristopher L. Nonlinear dynamics and instability of aqueous dissolution of silicate glasses and minerals. United States. doi:10.1038/srep30256.
Wang, Yifeng, Jove-Colon, Carlos F., and Kuhlman, Kristopher L. 2016. "Nonlinear dynamics and instability of aqueous dissolution of silicate glasses and minerals". United States. doi:10.1038/srep30256. https://www.osti.gov/servlets/purl/1313074.
@article{osti_1313074,
title = {Nonlinear dynamics and instability of aqueous dissolution of silicate glasses and minerals},
author = {Wang, Yifeng and Jove-Colon, Carlos F. and Kuhlman, Kristopher L.},
abstractNote = {Aqueous dissolution of silicate glasses and minerals plays a critical role in global biogeochemical cycles and climate evolution. The reactivity of these materials is also important to numerous engineering applications including nuclear waste disposal. The dissolution process has long been considered to be controlled by a leached surface layer in which cations in the silicate framework are gradually leached out and replaced by protons from the solution. This view has recently been challenged by observations of extremely sharp corrosion fronts and oscillatory zonings in altered rims of the materials, suggesting that corrosion of these materials may proceed directly through congruent dissolution followed by secondary mineral precipitation. Here we show that complex silicate material dissolution behaviors can emerge from a simple positive feedback between dissolution-induced cation release and cation-enhanced dissolution kinetics. This self-accelerating mechanism enables a systematic prediction of the occurrence of sharp dissolution fronts (vs. leached surface layers), oscillatory dissolution behaviors and multiple stages of glass dissolution (in particular the alteration resumption at a late stage of a corrosion process). In conclusion, our work provides a new perspective for predicting long-term silicate weathering rates in actual geochemical systems and developing durable silicate materials for various engineering applications.},
doi = {10.1038/srep30256},
journal = {Scientific Reports},
number = ,
volume = 6,
place = {United States},
year = 2016,
month = 7
}

Journal Article:
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