Experimental generation of patina on glass

Author:

Clifford Penelope1ORCID,Semeniuk Vic12

Affiliation:

1. School of Arts & Sciences University of Notre Dame Fremantle Western Australia Australia

2. V. & C. Semeniuk Research Group Warwick Western Australia Australia

Abstract

AbstractPatina formed on ancient glass holds potential to be a useful tool in determining the age of patina and to interpreting its formative environment climatically, pedogenically, hydrochemically and biologically. To date, its usefulness in this regard appears to have been underestimated. However, if patina is to be used as a reliable indicator of age and the environmental conditions underpinning its formation, there needs to be a systematic examination and understanding of its development under controlled laboratory conditions using various types of glass and with various climate types and soil types. As such, to calibrate and interpret the age of patina, processes of its development and products of its formation, we believe that it is useful to produce patina under varying experimental conditions in the laboratory. This paper focuses on the successful experimental development of patina on glass under controlled laboratory conditions and paves the way for further exploration of the rich resource of information that can result from such experimentation. We cannot produce in detail the full range of long‐term products of patination.

Publisher

Wiley

Reference20 articles.

1. Baxter J. L.(1977).Heavy mineral sand deposits of Western Australia. Mineral Resources Bulletin Geological Survey of Western Australia.

2. Bureau of Meteorology Climate Statistics for Mitchell Plateau Western Australia. (2019a).http://www.bom.gov.au/climate/averages/tables/cw_001012.shtml

3. Bureau of Meteorology Climate Statistics for Port Hedland Western Australia. (2019b).http://www.bom.gov.au/climate/averages/tables/cw_004032.shtml

4. Patinated glass from Cossack, Western Australia;Clifford P.;Journal of the Royal Society of Western Australia,2008

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