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Vitreous silica formation within shear bands in a dynamically compacted granular crystalline α‐quartz

Journal Article · · International Journal of Applied Glass Science
DOI:https://doi.org/10.1111/ijag.16704· OSTI ID:2573466
A shear band is a heterogeneous, narrow seam within a solid material whose formation is caused by intense localized shearing when a sufficiently large amount of deformation occurs. If that deformation occurs at a sufficiently rapid rate, with operative friction, then co‐located ephemeral heating will occur in the shear band. In this study, shear bands were produced from dynamic shear‐induced compaction of a granular form of crystalline α‐quartz (SiO2). The produced shear bands were approximately 25‐µm thick and were examined with scanning electron microscopy/electron backscatter diffraction, transmission electron microscopy, Raman spectroscopy, and nanoindentation. Further, they were found to contain a mixture of vitreous silica and small‐sized crystallites. This finding is significant because the presence of the vitreous silica within the shear band is a postmortem indicator that the localized temperature had reached or exceeded the melting temperature (∼1723°C) of crystalline SiO2 during the rapid shear and compaction and then sufficiently rapid cooling quenched in that vitreous state.
Research Organization:
Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
AC05-00OR22725
OSTI ID:
2573466
Journal Information:
International Journal of Applied Glass Science, Journal Name: International Journal of Applied Glass Science Journal Issue: 3 Vol. 16; ISSN 2041-1294; ISSN 2041-1286
Publisher:
American Ceramic SocietyCopyright Statement
Country of Publication:
United States
Language:
English

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