Christopher M. Stevenson , Mary Gurnick , Oleksandr Misiats , David Hurst Thomas , Anna M. Semon
{"title":"Ceramic rehydroxylation dating by infrared diffuse reflectance spectroscopy","authors":"Christopher M. Stevenson , Mary Gurnick , Oleksandr Misiats , David Hurst Thomas , Anna M. Semon","doi":"10.1016/j.jas.2025.106181","DOIUrl":null,"url":null,"abstract":"<div><div>We provide a new approach to the method of ceramic dating by tracking the dehydroxylation and rehydroxylation of water species using infrared diffuse reflectance spectroscopy. Water bands at 3655 cm<sup>−1</sup> (OH/H<sub>2</sub>O), 4550 cm<sup>−1</sup> (OH), and 5160 cm<sup>−1</sup>(H<sub>2</sub>O) were used to determine the various forms of water absorbed or released from the ceramic surface and the interior, which permitted the calculation of prehistoric hydroxyl gain since the time of manufacture. Ramped temperature rehydroxylation experiments (30–500 °C) were used to establish the activation energy (<em>E</em>) of OH diffusion. This was followed by an isothermal diffusion experiment, which provided a high temperature (240 °C) diffusion coefficient that was extrapolated to archaeological temperature. This new variant of the dating method is an alternative to the conventional mass gain experiments that have been applied in the past. Our ceramic dates are in agreement with associated radiocarbon dates within shell midden deposits created by the 17th century Native Americans on St. Catherines Island, Georgia, USA.</div></div>","PeriodicalId":50254,"journal":{"name":"Journal of Archaeological Science","volume":"177 ","pages":"Article 106181"},"PeriodicalIF":2.6000,"publicationDate":"2025-02-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Archaeological Science","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0305440325000305","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ANTHROPOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
We provide a new approach to the method of ceramic dating by tracking the dehydroxylation and rehydroxylation of water species using infrared diffuse reflectance spectroscopy. Water bands at 3655 cm−1 (OH/H2O), 4550 cm−1 (OH), and 5160 cm−1(H2O) were used to determine the various forms of water absorbed or released from the ceramic surface and the interior, which permitted the calculation of prehistoric hydroxyl gain since the time of manufacture. Ramped temperature rehydroxylation experiments (30–500 °C) were used to establish the activation energy (E) of OH diffusion. This was followed by an isothermal diffusion experiment, which provided a high temperature (240 °C) diffusion coefficient that was extrapolated to archaeological temperature. This new variant of the dating method is an alternative to the conventional mass gain experiments that have been applied in the past. Our ceramic dates are in agreement with associated radiocarbon dates within shell midden deposits created by the 17th century Native Americans on St. Catherines Island, Georgia, USA.
期刊介绍:
The Journal of Archaeological Science is aimed at archaeologists and scientists with particular interests in advancing the development and application of scientific techniques and methodologies to all areas of archaeology. This established monthly journal publishes focus articles, original research papers and major review articles, of wide archaeological significance. The journal provides an international forum for archaeologists and scientists from widely different scientific backgrounds who share a common interest in developing and applying scientific methods to inform major debates through improving the quality and reliability of scientific information derived from archaeological research.