2017
DOI: 10.1016/j.corsci.2017.03.025
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New insight into atmospheric alteration of alkali-lime silicate glasses

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Cited by 36 publications
(79 citation statements)
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“…, and HPO 4 2-) did not drive glass alteration because the formed secondary phases required less Si than the glass. For Fe 2+ , an additional source was derived from the COx claystone, especially from pyrite dissolution.…”
Section: -mentioning
confidence: 98%
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“…, and HPO 4 2-) did not drive glass alteration because the formed secondary phases required less Si than the glass. For Fe 2+ , an additional source was derived from the COx claystone, especially from pyrite dissolution.…”
Section: -mentioning
confidence: 98%
“…5a). The secondary phases consumed elements from the glass: pimelite controlled Ni + while zincsilite, powellite, hydroxyapatite, and nontronite governed Zn 2+ , MoO 4 2-, HPO 4 2-, and Fe 2+ , respectively (Supplementary Fig. 5).…”
Section: Modelling Of Glass Corrosion: Pri Altered Layer and Interamentioning
confidence: 99%
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“…Besides its brittleness and sensitivity to cracks and flaws, glass is affected by stress corrosion, a degradation phenomenon that is due to the subcritical growth of surface flaws and microcracks, with a consequent decrease of the tensile strength of the material over time [9]. The stress corrosion mechanism depends on intrinsic factors as size and shape of surface flaws and external variables, namely environmental conditions and applied loads [10,11]. Currently, different studies agree that the presence of water favors the growth of micrometric surface defects and cracks.…”
Section: Introductionmentioning
confidence: 99%