首页> 外文期刊>Minerals >Multi-Analytical Investigation of Stains on Dimension Stones in Master Valentim’s Fountain, Brazil
【24h】

Multi-Analytical Investigation of Stains on Dimension Stones in Master Valentim’s Fountain, Brazil

机译:对巴西瓦伦丁大师喷泉中尺寸石上污渍的多分析研究

获取原文
           

摘要

Master Valentim’s fountain has become an important historical patrimony for Brazil, being portrayed by famous artists, among them Jean-Baptiste Debret. In 1938, it was registered as cultural heritage by the Brazilian National Historical and Artistic Heritage Institute (IPHAN), and in 1990 it was subjected to excavation and restoration works. The fountain was built in Gneiss and Lioz limestone, with metallic plates and mortar connecting the Gneiss blocks. Currently, deteriorations in the fountain stones can be observed, such as light stains and some aesthetic modifications caused by inadequate restorations. Petrography, X-ray fluorescence (XRF), XRD, physical properties, colorimetry, electrical conductivity, inductively coupled plasma optical emission spectrometry (ICP-OES), scanning electron microscopy-energy dispersive X-ray (SEM-EDX), and TGA were performed in order to characterize the Gneiss blocks, the metallic plates, and the stones used in previous restorations, as well as light stains observed on the Gneiss blocks. The petrography and XRD analyses inferred that the light stains may have been caused by the formation of an insoluble salt as a result of the association of the lead from the plates with other elements. The XRD analysis on the light staining area indicated the presence of cerussite (PbCO 3 ) and anglesite (PbSO 4 ), which are the probable cause of the light stains. The SEM-EDX results suggested that sulfur is the main element associated to lead.
机译:瓦伦丁大师的喷泉已成为巴西的重要历史遗产,由著名艺术家(其中包括让·巴蒂斯特·德布雷特)进行了描绘。 1938年,它被巴西国家历史与艺术遗产研究所(IPHAN)注册为文化遗产,并在1990年进行了挖掘和修复工作。喷泉建于片麻岩和Lioz石灰岩中,用金属板和砂浆连接片麻岩块。目前,可以观察到喷泉石的变质,例如由于不适当的修复而引起的光渍和一些美学修饰。岩石学,X射线荧光(XRF),XRD,物理性质,比色法,电导率,电感耦合等离子体发射光谱(ICP-OES),扫描电子显微镜-能量色散X射线(SEM-EDX)和TGA分别为为了表征片麻岩块,金属板和先前修复中使用的石头,以及在片麻岩块上观察到的浅色斑点,进行了测试。岩相学和X射线衍射分析推断出,由于来自板的铅与其他元素的缔合,形成不溶性盐可能导致了浅色斑点。浅色区域的X射线衍射分析表明,存在着铜铁矿(PbCO 3)和角铁矿(PbSO 4),这可能是造成浅色污点的原因。 SEM-EDX结果表明,硫是与铅相关的主要元素。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号