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Studies of the corrosion mechanisms related to the presence of chlorine onthe archaeological ferrous artefactsContribution of the local and structural characterisation

机译:考古亚铁文物上与氯的存在相关的腐蚀机理研究局部和结构特征的贡献

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During burial of iron archaeological artefacts, when water of the soil contains a certainrnamount of chlorine, Cl- ions migrate in the corrosion products conducting to highrnconcentrations in pores or fractures at the metal/oxide interface. After excavation, the suddenrnsupply of oxygen and the release of Cl- seems to lead to the development of specific phases.rnThe formation mechanisms of these phases are not understood up to now, but is often noticedrnthat the precipitation of such phases accelerates the deterioration of archaeological objects.rnThus, it is essential to apprehend the corrosion mechanism related to the presence of chlorine.rnFor this reason we are interested to the characterisation of the corrosion products of somernarchaeological artefacts coming from for different archaeological site. The compositionrnanalyses are performed by Energy Dispersive Spectroscopy (EDS) coupled to ScanningrnElectron Microscope (SEM) and Electron Probe Micro Analyses (EPMA). Respectively, EDSrnobservations show that chlorine seems to be mainly localised at the metal/oxide interface andrncomposition EPMA analyses allow evaluating the local absolute of these high-Cl zones andrnsuggest the presence of two different phases: the first one has a Cl amount about 3 to 8 mass %,rnand about 14 to 20 mass% for the second one. Moreover, for a precise local and structuralrnanalysis of the corrosion products, some fine techniques of materials characterisation arernimplemented: the micro diffraction under synchrotron radiation (μXRD at D15, LURE) andrnthe micro spectroscopy Raman (μRaman). The two phases identified are akaganeite ?β-rnFeOOH, and a ferrous hydroxychloride β-Fe2(OH)3Cl. These results are particularlyrninteresting because the only phase reported in literature is akaganeite. To our knowledge, thernβ-Fe2(OH)3Cl was never identified as archaeological artefacts corrosion products. Thesernresults will be discussed regarding the burial environment of the artefacts.
机译:在埋葬铁考古文物的过程中,当土壤中的水包含一定数量的氯时,Cl-离子会在腐蚀产物中迁移,从而在金属/氧化物界面的孔隙或裂缝中导致高浓度的腐蚀。开挖后,氧气的突然供应和Cl-的释放似乎导致特定相的发展。到目前为止,这些相的形成机理尚不清楚,但经常注意到,这些相的沉淀加速了考古学的恶化。因此,必须了解与氯的存在有关的腐蚀机理。因此,我们对表征来自不同考古现场的某些考古文物的腐蚀产物感兴趣。组成分析通过与扫描电子显微镜(SEM)和电子探针显微分析(EPMA)耦合的能量色散光谱(EDS)进行。 EDS的观测分别表明,氯似乎主要位于金属/氧化物界面,并且EPMA分析可以评估这些高Cl区的局部绝对值,并且建议存在两个不同的相:第一个相的Cl量约为3至8质量%,第二种为约14至20质量%。此外,为了对腐蚀产物进行精确的局部和结构分析,实施了一些精细的材料表征技术:同步辐射下的微衍射(D15处的X射线,LURE)和显微拉曼光谱(Raman)。鉴定出的两相是赤铁矿β-rnFeOOH和羟基氯化亚铁β-Fe2(OH)3Cl。这些结果特别有趣,因为文献中报道的唯一相是赤铁矿。据我们所知,β-Fe2(OH)3Cl从未被鉴定为考古文物腐蚀产物。这些结果将在文物的埋葬环境中进行讨论。

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