Fibula SMRA 20-19066-10
Christian. Degrigny (HE-Arc CR, Neuchâtel, Neuchâtel, Switzerland) & Naima. Gutknecht (HE-Arc CR, Neuchâtel, Neuchâtel, Switzerland) & Valentina. Valbi (Laboratoire Métallurgie et Culture LMC-IRAMAT-CNRS-UTBM, Belfort, Franche-Comté, France)
Fibula with an outwardly curved hinge, a profiled arch decorated with a succession of narrow, grooved and toric mouldings and a smooth triangular foot finished with two small mouldings. Typology Riha 5.6. Brown appearance with residues of a shiny metallic grey coating on the arch. The surface is flaking on the pin. Residue of soil sediment on the arch. L = 48mm. W = 4.7g.
Jewellery
Avenches, Switzerland, Avenches, Vaud, Switzerland
2020
Roman Times
Soil
Site et musée romains Avenches, Avenches, Vaud
Site et musée romains Avenches, Avenches, Vaud
SMRA 20/19066-10
Partially cleaned with ethanol and a soft brush.
The fibula was found at village Derrière les murs, near Avenches.
The schematic representation below gives an overview of the corrosion structure encountered on the pin of the fibula from a first visual macroscopic observation.
Strata | Type of strata | Principal characteristics |
S1 | Soil | crust, light brown, thin, discontinuous, matte, non compact, friable, very soft |
CP1 | Corrosion product | layer, olive green, thin, discontinuous, submetallic, compact, brittle, soft |
CP2 | Corrosion product | layer, brown, thin, discontinuous, matte, compact, brittle, very soft |
CP3 | Corrosion product | layer, olive green, thick, discontinuous, matte, compact, brittle, soft |
CP4 | Corrosion product | layer, dark brown, thin, discontinuous, matte, compact, brittle, soft |
CP5 | Corrosion product | layer, light green, thin, discontinuous, matte, non compact, powdery, very soft |
CP6 | Corrosion product | layer, dark green, thin, continuous, matte, non compact, friable, very soft |
CP7 | Corrosion product | layer, olive green, thin, continuous, matte, non compact, powdery, very soft |
M1 | Metal | layer, dark yellow, metallic, thick, continuous, compact, tough |
Table 1: Description of the principal characteristics of the strata as observed under binocular and described according to Bertholon's method.
The cross-section corresponds to a lateral cut (Fig. 2). The sample was cut from the central body of the pin after embedding one part of the object in the resin. A metal core is still present under the corrosion layers (Fig. 5).
Brass
Annealed after cold working
SMRA_fibule
Site et musée romains Avenches, Avenches, Vaud
Site et musée romains Avenches, Avenches, Vaud
January 2021
Sample taken from the object is embedded in resin and kept by the institution with the object if further analysis is needed.
Analysis performed :
Non-Invasive approach
- XRF with handheld portable X-ray fluorescence spectrometer (NITON XL3t 950 Air GOLDD+, Thermo Fischer®). General Metal mode, acquisition time 60s (filters: Li20/Lo20/M20).
Invasive approach (on the sample)
- Optical microscopy: the sample is polished, then it is observed using a digital microscope KEYENCE VHX-7000 in bright and dark field.
- Metallography: the polished sample is etched with alcoholic ferric chloride and observed by optical microscopy in bright field.
- SEM-EDS: the sample is coated with a carbon layer and analysis are performed on a SEM-FEG JEOL 7001-F equipped with a silicon-drift EDS Oxford detector (Aztec analysis software) with an accelerating voltage of 20 kV and probe current at about 9 nA. The relative error is considered of about 10% for content range <1wt%, and 2% for content range of >1wt%.
- µ-Raman spectroscopy: it is performed on a HORIBA Labram Xplora spectrometer equipped with a 532 nm laser with 1800 grating, the laser power employed is between 0.04 and 0.55 mW with acquisition time varying between 1 and 5 minutes.
XRF analyses were carried out on the surface of the object (Fig. 2). All strata (soil, corrosion products and metal) are analyzed at the same time. While the pin (point 1) is showing little sediments and a clear delimitation of the original surface with loss of the internal corrosion layers, the arch (point 2) has a thick layer of soil and external corrosion. The metal on the pin is presumably a copper-based alloy with high contents of Zn and Sn. The metal of the arch has a higher amount of Sn and shows the presence of lead. This could be due to the presence of decorative incrustation, surface tinning or a surface enrichment on the arch. Si, Fe, Al, S and P detected are probably coming from the burial environment.
Element (mass %) |
1 | σ |
2 | σ |
Cu | 80.9 | 0.54 | 33.6 | 0.12 |
Sn | 7.5 | 0.1 | 26.8 | 0.12 |
Zn | 7.7 | 0.09 | 2.1 | 0.03 |
Pb | 0.2 | 0.02 | 12.5 | 0.06 |
Si | 2.4 | 0.25 | 9.72 | 0.14 |
Fe | 0.3 | 0.02 | 8.9 | 0.08 |
Al | n.d. | n.d. | 3.4 | 0.19 |
S | 0.3 | 0.06 | n.d. | n.d. |
P | 0.4 | 0.08 | 2.2 | 0.05 |
Sb | 0.16 | 0.02 | 0.2 | 0.01 |
Table 2: Chemical composition of the surface of the fibula at two representative points shown in Fig. 2 (n.d.: below the detection limit), HE-Arc CR.
EDX analysis (Table 3) of the residual metal of the pin on cross-section shows that it is a Cu-Zn-Sn brass alloy with a medium amount of Zn (13 wt%) and 3 wt% of Sn. The results obtained are in agreement with the non-invasive XRF analysis (see table 2, point 1).
The observation of the metal in cross-section after etching (Fig. 6) shows a microstructure with polygonal grains and several twinned grains (Fig. 7), revealing that the object underwent cold working and annealing. The metal presents porosities and sulfide inclusions (Fig. 7) for a total of 1% of the metallic surface of the sample in cross-section.
Elements | wt % |
Cu | 83 |
Zn | 13 |
Sn | 3 |
Na | <0.5 |
Al | <0.5 |
S | <0.5 |
Fe | <0.5 |
Table 3: Chemical composition (wt %) of the alloy over a general area of analysis obtained by SEM-EDX, LMC-IRAMAT-CNRS-UTBM.
Polygonal and twinned grains
Cu
Zn, Sn
None.
The observation of the sample in cross-section in dark field (Fig. 8) allows to identify an external sediment soil (S1), a thin (5 µm) dark brown CP1, a thick (200 µm) foliated (alternative bands) green stratum (CP2), a dark green stratum 100 µm thick (CP3), a red 30 µm thin stratum (CP4) and M1.
The SEM-EDX analyses (Table 4, Fig. 9) and Raman spectroscopy (Fig. 10) allow to identifiy the CP4 as cuprite (Cu2O) while the other strata present too much fluorescence to be identified by Raman spectroscopy. The SEM-EDX shows that all the corrosion structure is depleted in Zn and enriched in Sn, especially the CP1 (Sn 41 wt%). CP1 and CP2 are also enriched in Fe, P and Ca from the soil. The S1 stratum presents an enrichment in Sn and O, as well as external elements such as Ca and Fe. It corresponds to the Transformed Medium (Neff et al. 2004), a transition zone between the Dense Product Layer (DPL) and the non altered soil, containing both corrosion products and markers from the soil. No significant Cl enrichment is observed.
wt% | S1 |
CP1 | CP2 | CP3 | CP4 |
O | 33 | 20 | 28 | 33 | 12 |
Cu | 12 | 17 | 33 | 30 | 79 |
Sn | 34 | 41 | 27 | 30 | 6 |
Zn | 2 | 1 | <0.5 | 1 | 1 |
Fe | 7 | 11 | 5 | 1 | n.d. |
Si | 1 | 3 | 3 | 2 | <0.5 |
P | 1 | 2 | 1 | <0.5 | <0.5 |
Ca | 6 | 3 | 2 | 1 | <0.5 |
Pb | 1 | 1 | 1 | <0.5 | <0.5 |
Al | <0.5 | 1 | <0.5 | n.d. | n.d. |
S | 1 | <0.5 | <0.5 | <0.5 | n.d. |
Cl | 1 | <0.5 | <0.5 | 1 | 1 |
Table 4: Chemical composition (wt%) of the corrosion products over a general area of analysis by SEM-EDX (n.d.: below the detection limit), LMC-IRAMAT-CNRS-UTBM.
Uniform
Unknown
None.
The observation under binocular microscope identified 7 CPs while the cross-section identified 4 CPs.
With binocular microscope, it is possible to differentiate strata according to texture and light color changes that do not always correspond to significative changes in chemical composition, thus leading to a regrouping of several strata into one in the cross-section observation and physicochemical characterization. The differences between the two observation modes could also be explained by different locations of observation.
Both observation modes identified one S1 stratum. The CP1 and CP2 under binocular microscope could be grouped and correspond to CP1 in CS. Similarly, the CP3 and CP4 under binocular probably correspond to CP2 in cross-section; the CP5 and CP6 under binocular could correspond to CP3 in cross-section. CP7 under binocular and CP4 in cross-section could not be linked as their characteristics are so different.
The fibula is a brass with a a medium amount of Zn (13 wt%) and low amount of Sn (3 wt%). The microstructure of the metal shows that it underwent cold working and annealing.
After observation of the corrosion structure in cross-section, it is possible to identify the original surface of the object that has been preserved and corresponds to the interface between CP1 and S1. As for the corrosion structure underneath, it presents the phenomenon of dezincification commonly observed in brasses, together with a decuprification phenomenon. In fact Zn is almost absent in the whole corrosion structure (1 mass%), Cu is strongly depleted (20-30 mass%) while a strong enrichment in Sn is observed (30-40 wt%). A strong fluorescence signal in Raman did not allow to clearly identify the compounds constituting CP2 and CP3, while CP4 was identified as copper oxide cuprite. However, EDX analysis indicates that CP2 shows a strong enrichment in soil elements (Fe, P), associated with a foliated and cracked morphology that could favor the penetration of these external elements.
This artefact is part of a corpus of objects, together with Earstick SMRA 20/19047-03 and Ring SMRA 16/17285-01 which all present a flaking phenomenon of the corrosion products.
References on object and sample
1. Earstick SMRA 20/19047-03
2. Ring SMRA 16/17285-01
References on analytical methods and interpretation
3. Lafuente, B., Downs, R. T., Yang, H., Stone, N. (2015) The power of databases: the RRUFF project. In: Highlights in Mineralogical Crystallography, T. Armbruster and R. M. Danisi, eds. Berlin, Germany, W. De Gruyter, 1-30.
4. Papadopoulou, O., Vassiliou, P., Grassini, S., Angelini, E. and Gouda, V. (2016) Soil-induced corrosion of ancient Roman brass – A case study. Materials and Corrosion, 67, 2.5. Scott, D. (2006) Metallography and microstructure of ancient and historic metals. J Paul Getty Museum Publications.
6. Robbiola L., Blengino M., Fiaud C., (1998) Morphology and mechanisms of formation of natural patinas on archaeological Cu–Sn alloys. Corrosion Science, 40 (12), 2083-2111.
7. Neff D., Reguer S., Bellot-Gurlet L., Dillmann P., Bertholon R. (2004) Structural characterization of corrosion products on archaeological iron: an integrated analytical approach to establish corrosion forms. J. Raman Spectrosc. 35: 739–745.