DATA ON 61 CHEMICAL ELEMENTS FOR THE CHARACTERIZATION OF THREE MAJOR GLASS COMPOSITIONS IN LATE ANTIQUITY AND THE MIDDLE {AGES

Year:

2011

Type of Publication:

Article

Authors:

Wedepohl, Karl Hans; Simon, Klaus; Kronz, Andreas

Journal:

Archaeometry

Volume:

53

Number:

1

Pages:

81-102

ISSN:

1475-4754

BibTex:

@article{ARCM:ARCM536, author = "Karl Hans Wedepohl and Klaus Simon and Andreas Kronz", abstract = "Sets of 20 soda ash, 16 soda lime and 23 wood ash glasses mainly from excavations in Europe were analysed by microprobe and LA–ICP-MS for 61 elements and are presented as average concentrations with standard deviations. Concentrations of sodium, potassium and magnesium allow the major glass type to be identified. Specific compositions of the raw materials of glass production indicate certain sources, technical processes and ages. Heavy minerals etc. of quartz sands contain rare earth elements (REE) from crustal fractionations that are different for the three major glass types. Accumulations of P, B, Ba, Mn and K in wood from soils by organic processes can characterize glass from certain regions.", doi = "10.1111/j.1475-4754.2010.00536.x", issn = "1475-4754", journal = "Archaeometry", number = "1", pages = "81--102", publisher = "Blackwell Publishing Ltd", title = "{DATA} {ON} 61 {CHEMICAL} {ELEMENTS} {FOR} {THE} {CHARACTERIZATION} {OF} {THREE} {MAJOR} {GLASS} {COMPOSITIONS} {IN} {LATE} {ANTIQUITY} {AND} {THE} {MIDDLE} {{AGES}", url = "http://dx.doi.org/10.1111/j.1475-4754.2010.00536.x", volume = "53", year = "2011", }

Abstract:

Sets of 20 soda ash, 16 soda lime and 23 wood ash glasses mainly from excavations in Europe were analysed by microprobe and LA–ICP-MS for 61 elements and are presented as average concentrations with standard deviations. Concentrations of sodium, potassium and magnesium allow the major glass type to be identified. Specific compositions of the raw materials of glass production indicate certain sources, technical processes and ages. Heavy minerals etc. of quartz sands contain rare earth elements (REE) from crustal fractionations that are different for the three major glass types. Accumulations of P, B, Ba, Mn and K in wood from soils by organic processes can characterize glass from certain regions.