Abstract

Chemical analysis, optical absorption spectroscopy and mathematical modelling of high temperature viscosity have been carried out on five 1st–2nd century AD Roman blue-green bottle glass fragments from Coppergate, York. Modelled viscosities indicate remarkable consistency within the sample set studied and support the suggestion that temperatures of ∼1000–1150 °C were required to remelt these glasses and to provide suitable viscosities for forming articles. Iron redox ratios (Fe 2+/ΣFe), analysed SO 3 contents and the absence of characteristic Fe 3+–S 2− amber absorption bands suggest that melting conditions for all studied glasses were mildly, rather than strongly, reducing (estimated pO 2 ≈ 10 −1–10 −6 bar). These furnace conditions are consistent with the effects of combustion gases and carbonaceous matter contained in the raw materials.

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