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通过有意埋藏再现青铜考古铜绿:与土壤短期和长期相互作用的比较。

Reproducing bronze archaeological patinas through intentional burial: A comparison between short- and long-term interactions with soil.

作者信息

Boccaccini Francesca, Riccucci Cristina, Messina Elena, Pascucci Marianna, Bosi Ferdinando, Chelazzi David, Guaragnone Teresa, Baglioni Piero, Ingo Gabriel Maria, Di Carlo Gabriella

机构信息

Institute for the Study of Nanostructured Materials (ISMN), National Research Council (CNR), Via Salaria km 29300, 00015 Monterotondo, Italy.

Department of Earth Sciences, Sapienza University of Rome, Piazzale Aldo Moro, 5, I-00185 Rome, Italy.

出版信息

Heliyon. 2023 Aug 29;9(9):e19626. doi: 10.1016/j.heliyon.2023.e19626. eCollection 2023 Sep.

DOI:10.1016/j.heliyon.2023.e19626
PMID:37810079
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10558880/
Abstract

The reproduction of archaeological corrosion patinas is a key issue for the reliable validation of conservation materials before their use on cultural objects. In this study, bronze disks were intentionally buried for 15 years in the soil of the archaeological site of Tharros, both in laboratory and , with the aim of reproducing corrosion patinas typical of archaeological artifacts to be used as representative surfaces for testing novel cleaning gels. The microstructural, microchemical and mineralogical features of the patinas were analyzed by a multianalytical approach, based on optical microscopy (OM), field emission scanning electron microscopy coupled with energy dispersive spectrometry (FE-SEM-EDS) and X-ray diffraction (XRD). The patinas developed in 15 years were compared with an archaeological bronze recovered from the same site after about two thousand years of burial (referred as short-term and long-term interaction, respectively). Results revealed a similar corrosion behavior, especially in terms of chemical composition and corrosion mechanisms. XRD detected the ubiquitous presence of cuprite, copper hydroxychlorides and terrigenous minerals, while OM and FE-SEM-EDS analyses of cross-sections evidenced similar patinas' stratigraphy, identifying decuprification as driving corrosion mechanism. However, some differences related to the type of local environment and to the time spent in soil were evidenced. In particular, patinas developed are more heterogeneous and rougher, while the archaeological one is thicker and presents a major amount of cuprite, terrigenous deposits and uncommon corrosion compounds. Based on our findings, the disks buried were selected and used as disposable substrates to study the cleaning effect of a novel polyvinyl alcohol (PVA)-based gel loaded with a chelating agent (NaEDTA · 2HO). Results show that the gel is effective in removing disfiguring degradation compounds and preserving the stable and protective patina. Based on the conservation needs, the time of application can be properly tuned. It is worth noticing that after a few minutes the green corrosion products can be selectively removed. The EDS analysis performed on the gels after cleaning reveals that they are highly selective for the removal of copper(II) compounds rather than Cu(I) oxide or Cu(0) from bronze substrates.

摘要

在将保护材料用于文物之前,可靠验证这些材料时,考古腐蚀锈层的再现是一个关键问题。在本研究中,青铜圆盘被有意埋在撒罗斯考古遗址的土壤中15年,一次是在实验室环境下,另一次是实地埋藏,目的是再现考古文物典型的腐蚀锈层,用作测试新型清洁凝胶的代表性表面。通过基于光学显微镜(OM)、场发射扫描电子显微镜与能谱仪联用(FE-SEM-EDS)以及X射线衍射(XRD)的多分析方法,对锈层的微观结构、微化学和矿物学特征进行了分析。将15年形成的锈层与在同一地点埋藏约两千年后出土的一件考古青铜器上的锈层进行了比较(分别称为短期和长期相互作用)。结果显示出相似的腐蚀行为,特别是在化学成分和腐蚀机制方面。XRD检测到普遍存在赤铜矿、氯氧化铜和陆源矿物,而对横截面的OM和FE-SEM-EDS分析证明了锈层具有相似的地层结构,确定脱铜是主要腐蚀机制。然而,也发现了一些与局部环境类型和在土壤中停留时间有关的差异。特别是,实验室埋藏形成的锈层更不均匀且更粗糙,而考古出土的锈层更厚,含有大量赤铜矿、陆源沉积物和不常见的腐蚀化合物。基于我们的研究结果,选择了实验室埋藏的圆盘并用作一次性基材,以研究一种新型的负载螯合剂(NaEDTA·2H₂O)的聚乙烯醇(PVA)基凝胶的清洁效果。结果表明,该凝胶能有效去除有损外观的降解化合物,并保留稳定且具保护作用的锈层。根据保护需求,可以适当调整应用时间。值得注意的是,几分钟后就能选择性地去除绿色腐蚀产物。清洁后对凝胶进行的EDS分析表明,它们对从青铜基材上去除铜(II)化合物具有高度选择性,而不是对氧化亚铜或铜(0)。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/a2c3eaf83040/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/7cd149a03afd/ga1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/0ff647c9f1c0/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/7bb36d314751/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/7e2ebdbda8f2/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/234ba352fc29/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/afd4d246e7a2/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/e5dacbed0bce/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/a2c3eaf83040/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/7cd149a03afd/ga1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/0ff647c9f1c0/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/7bb36d314751/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/7e2ebdbda8f2/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/234ba352fc29/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/afd4d246e7a2/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/e5dacbed0bce/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8341/10558880/a2c3eaf83040/gr7.jpg

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