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• W2003347521 abstract "SEM-EDAX textural-chemical alteration morphologies of man-made glass from Egypt and modern soda lime glass are compared to literature data for obsidian and sideromelane (rhyolitic and basaltic glass). A series of laboratory experiments using soda lime glass slides held at 90°C for 3–21 days in baths using different salt solutions (MgCl2, LiCl, NaCl, CaCl2and KCl) in various concentrations provides compelling evidence that for any particular glass composition the style of glass corrosion (hydration–dissolution) is dependent on solution geochemistry. Two fundamental styles of glass corrosion occur: pitting dissolution, and gel-lamination hydration. Glasses of different compositions may behave differently in similar anthrosols. Reaction style and kinetics, and hydration–dissolution rates are controlled by soil temperature, glass and soil water geochemistry, and ultimately alkali exchange between the glass artefact and the soil-zone pore water. Glass and gel thickness loss through dissolution reactions may compromise hydration dating and may be responsible for a variety of reported apparent chronological inconsistencies. Future studies with obsidian and sideromelane under bath conditions and in the natural environment are needed to assess their response to variable soil-zone solution geochemistry." @default.
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• W2003347521 date "1999-09-01" @default.
• W2003347521 modified "2023-10-17" @default.
• W2003347521 title "Considerations of Hydration-rind Dating of Glass Artefacts: Alteration Morphologies and Experimental Evidence of Hydrogeochemical Soil-zone Pore Water Control" @default.
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• W2003347521 doi "https://doi.org/10.1006/jasc.1998.0356" @default.
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