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Experimental study of historical processing of cobalt arsenide ore for colouring glazes (15-16th century Europe)

Bibliographic Data

ID13095134
AuthorsJudit Molera (0000-0003-3116-0456, Universitat de Vic - Universitat Central de Catalunya, corresponding author), A Climent‐Font (0000-0002-4095-2837, Universidad Autónoma de Madrid), Y Zamora Garcia (0000-0002-1866-4871, ALBA Synchrotron (Spain)), Trinitat Pradell (0000-0002-8720-5492, Universitat Politècnica de Catalunya), Oriol Vallcorba (0000-0001-6499-7688, ALBA Synchrotron (Spain)), A Zucchiatti (University of the Witwatersrand)
Year2021
Volume36
Pages102797-102797
Publication date2021-01-25
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueJournal of Archaeological Science Reports (JOURNAL)
Journal identifiersISSN: 2352-409X • E-ISSN: 2352-4103
PublisherElsevier BV (PUBLISHER)
DOI10.1016/j.jasrep.2021.102797
OpenAlexW3126100376
LanguageEN
Citations received7
References cited34

Cobalt was used since the early antiquity to tinge glass and glazes in blue. The presence of arsenic in blue decorated glazes since ~1500 onwards and absence beforehand, observed in Europe, might be related to the processing of the ore: roasting of the cobalt mineral (saffre) and obtaining a glass adding sand and potash (smalt) or as by-product of other metallurgical processes, e.g. silver smelting slag. We have replicated the roasting of cobalt arsenide ore (CoAs3) and the processing of silver smelting as described in historical treatises following the transformations by in situ variable temperature SR-XRD, PIXE and SEM. Our laboratory tests have proved that roasting cobalt arsenide ore either alone or mixed with fluxes (PbO, CaF2), CaCO3, SiO2 and kaolinite was unable to remove the arsenic completely. Roasting cobalt arsenide ore (saffre) alone explains the presence of arsenic in the cobalt blue glasses and glazes after 1520. The product obtained as described by Agricola contains less arsenic forming calcium arsenates, lead arsenates (Pb5(AsO4)3F, Pb8As2O13) and calcium lead arsenates (Ca,Pb)5(AsO4)3(F,Cl,OH) with an hedyphane structure, while cobalt is incorporated into a glassy matrix. As the physical separation of the arsenic free cobalt vitreous phase does not seem possible, these processes can explain the variable content of arsenic shown by the historical blue glazes but not the arsenic free glazes. In this case, the use of an arsenic free cobalt ore such as linnaeite is the most likely source

Arsenic · Arsenide · Cobalt · Gallium arsenide · Metallurgy · Mineralogy · Roasting · Smelting · Building materials and conservation · Cultural Heritage Materials Analysis · Materials Science · Mineralogy and Gemology Studies · Geology

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Unique citing works7
Citations per year1,4
Citation span2021 - 2026 (6)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 6

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