Raman analysis of red-brown and gray shards from 16th and 17th century Portuguese shipwrecks

M.A. Legodi, D. de Waal
{"title":"Raman analysis of red-brown and gray shards from 16th and 17th century Portuguese shipwrecks","authors":"M.A. Legodi,&nbsp;D. de Waal","doi":"10.1016/j.cryseng.2004.04.005","DOIUrl":null,"url":null,"abstract":"<div><p><span>The artifacts under investigation (three red clay shards, two gray clay shards and a red clay teapot) are from the J A Van Tilburg museum at the University of Pretoria (UP). The large red clay shard was recovered from the 1552 Portuguese shipwreck, São João, found in the region of Port Edward, South Africa. The other shards were recovered from the 1622 Portuguese shipwreck, the São João Baptista, which sank around Kenton-on-sea off the South African coast. The results from these are compared to those obtained from the analysis of a red-brown teapot. The oldest of this type of teapot was made in China during the second half of the 18th century. Raman spectroscopy<span> has proven to be a useful tool for qualitative determination of the composition of these clay artifacts. The red clays were characterized by the presence of hematite, kaolin, quartz, amorphous carbon<span><span> and aluminosilicates<span>. The results of the clay teapot differed from those of red clay shards in that no quartz Raman bands were observed for the clay teapot. The gray clay shards were characterized mainly by the presence of quartz, kaolin, amorphous carbon and aluminosilicates. The presence of </span></span>mullite in all samples could not be ascertained unambiguously using Raman spectroscopy. The pigments found in the investigated samples are hematite (α-Fe</span></span></span><sub>2</sub>O<sub>3</sub>) (for red samples) and amorphous carbon (for both red and gray samples).</p></div>","PeriodicalId":10766,"journal":{"name":"Crystal Engineering","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2003-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.cryseng.2004.04.005","citationCount":"13","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Crystal Engineering","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1463018404000140","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 13

Abstract

The artifacts under investigation (three red clay shards, two gray clay shards and a red clay teapot) are from the J A Van Tilburg museum at the University of Pretoria (UP). The large red clay shard was recovered from the 1552 Portuguese shipwreck, São João, found in the region of Port Edward, South Africa. The other shards were recovered from the 1622 Portuguese shipwreck, the São João Baptista, which sank around Kenton-on-sea off the South African coast. The results from these are compared to those obtained from the analysis of a red-brown teapot. The oldest of this type of teapot was made in China during the second half of the 18th century. Raman spectroscopy has proven to be a useful tool for qualitative determination of the composition of these clay artifacts. The red clays were characterized by the presence of hematite, kaolin, quartz, amorphous carbon and aluminosilicates. The results of the clay teapot differed from those of red clay shards in that no quartz Raman bands were observed for the clay teapot. The gray clay shards were characterized mainly by the presence of quartz, kaolin, amorphous carbon and aluminosilicates. The presence of mullite in all samples could not be ascertained unambiguously using Raman spectroscopy. The pigments found in the investigated samples are hematite (α-Fe2O3) (for red samples) and amorphous carbon (for both red and gray samples).

对16和17世纪葡萄牙沉船上的红棕色和灰色碎片进行拉曼分析
正在调查的文物(三个红色粘土碎片,两个灰色粘土碎片和一个红色粘土茶壶)来自比勒陀利亚大学(UP)的J a Van Tilburg博物馆。这块巨大的红色粘土碎片是从1552年在南非爱德华港地区发现的葡萄牙沉船 o jo号上找到的。其他的碎片是从1622年的葡萄牙沉船—— o jo o巴普蒂斯塔号上找到的,这艘船在南非肯顿附近沉没。将这些结果与红棕色茶壶的分析结果进行了比较。这种类型的最古老的茶壶是在18世纪下半叶在中国制造的。拉曼光谱已被证明是一个有用的工具,定性确定这些粘土文物的组成。红粘土的主要成分为赤铁矿、高岭土、石英、无定形碳和硅铝酸盐。粘土茶壶的结果与红粘土碎片的结果不同,粘土茶壶没有观察到石英拉曼带。灰色粘土碎屑的主要特征是石英、高岭土、无定形碳和铝硅酸盐。所有样品中莫来石的存在都不能用拉曼光谱明确地确定。在所研究的样品中发现的颜料是赤铁矿(α-Fe2O3)(用于红色样品)和无定形碳(用于红色和灰色样品)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信