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碳酸盐岩中铁基污染物的分析研究:铁锈的形成、扩散机制及形态。

Analytical Investigation of Iron-Based Stains on Carbonate Stones: Rust Formation, Diffusion Mechanisms, and Speciation.

机构信息

Chemistry Department, University of Rome 'La Sapienza' Piazzale Aldo Moro 5, 00185 Rome, Italy.

Earth Sciences Department, University of Rome 'La Sapienza' Piazzale Aldo Moro 5, 00185 Rome, Italy.

出版信息

Molecules. 2023 Feb 7;28(4):1582. doi: 10.3390/molecules28041582.

Abstract

In cultural heritage, unaesthetic stains on carbonate stones due to their close contacts with metals are of concern for the preservation of sculptures, monumental facades and archeological finds of various origin and antiquities. Rust stains made up of various oxidized iron compounds are the most frequent forms of alteration. The presence of ferric iron on rust-stained marble surfaces was confirmed in previous studies and oriented the choice of the best cleaning method (based on complexing agents specific for ferric ions). However, the composition of rust stains may vary along their extension. As the corrosion of the metallic iron proceeds, if the oxygen levels in the surroundings are low and there are no conditions to favor the oxidation, ferrous ions can also diffuse within the carbonate structure and form a variety of intermediate compounds. In this study, the iron stains on archeological marbles were compared with those artificially produced on Carrara marbles and Travertine samples. The use of integrated techniques (optical and scanning electron microscopy as well as Mössbauer and XPS spectroscopy) with complementary analytical depths, has provided the overall information. Rust formation and diffusion mechanisms in carbonates were revealed together with the evolution of iron speciation and identification of phases such as ferrihydrite, goethite, maghemite, nanomagnetite, and hematite.

摘要

在文化遗产中,由于碳酸盐岩石与金属密切接触而产生的不美观污渍,对雕塑、纪念性外墙和各种来源及古物的考古发现的保存构成了关注。由各种氧化铁化合物组成的铁锈污渍是最常见的变质形式。以前的研究证实了铁锈污渍表面存在三价铁,并为选择最佳清洁方法提供了指导(基于特定于三价铁离子的络合剂)。然而,铁锈污渍的组成可能会沿着其延伸方向发生变化。如果周围的氧气水平较低,并且没有有利于氧化的条件,金属铁的腐蚀过程中,二价铁离子也可以在碳酸盐结构内扩散,并形成各种中间化合物。在这项研究中,对考古大理石上的铁污渍进行了比较,这些污渍与人工制备的卡拉拉大理石和石灰华样品上的铁污渍进行了比较。综合运用各种技术(包括光学和扫描电子显微镜以及穆斯堡尔和 XPS 光谱学),并结合互补的分析深度,提供了全面的信息。揭示了碳酸盐中铁锈的形成和扩散机制,以及铁的形态演变和鉴定出了一些相,如水铁矿、针铁矿、磁赤铁矿、纳米磁铁矿和赤铁矿。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/08fb/9960802/64c8192030b7/molecules-28-01582-g001.jpg

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