Micro-FTIR and FTIR spectroscopy is useful for the study of degradation forms of cultural heritage. In particular it permits to identify the degradation phases and to establish the structural relationship between them and the substratum. In this paper, we report the results obtained on marble from a Roman sarcophagus, located in the medieval cloister of St. Cosimato Convent (Rome), and on oolitic limestone from the facade of St. Giuseppe Church in Syracuse (Sicily). The main components found in the samples of both monuments are: gypsum, calcium oxalate, and organic matter due to probably conservation treatments. In particular, the qualitative distribution maps of degradation products, obtained by means of micro-FTIR operating in ATR mode, revealed that the degradation process is present deep inside the stones also if it is not visible macroscopically. This process represents the main cause of crumbling of the substrate. The results of this research highlight the benefits of the -FTIR analysis providing useful insights on the polishing and consolidation processes of stone materials.

1. Introduction

The diagnostic analysis of the degradation process of the monument stone has acquired ever more importance regarding its restoration and maintenance. Such studies require analysis of the materials used and an accurate characterization of the degradation products with the aim of evaluating the effects of the degradation.

Fourier transform-infrared spectroscopy (FTIR) represents a powerful technique in diagnostic analysis of cultural heritage [13], in particular the micro-FTIR ( -FTIR) is more recent technique that improved the potential of vibrational spectroscopy in the field of diagnostic and conservation of art works [48].

The reliability of the measurements even with an extremely small amount of sampled material is very high, the high analytical sensitivity and high spatial resolution of -FTIR technique allow the identification of micrometric mixtures of compounds that constitute samples and the determination of minor and trace compounds, such as reaction and weathering compounds.

The present paper is a research aimed at characterizing degradation products and determination of the previous restoration works on a roman sarcophagus and on the facade of the Church of San Giuseppe. In particular the roman sarcophagus is located in the cloister of San Cosimato convent in Rome, actually the Regina Margherita Hospital (Rome), while the Church of San Giuseppe is located in the Island of Ortigia, historical centre of the city of Syracusa (Sicily).

2. The Samples

The analyzed samples are fragments coming from a Roman sarcophagus, located in the medieval cloister of St. Cosimato Convent (Rome), and from the facade of St. Giuseppe Church in Syracuse (Sicily). Before sampling, the stone surface was brushed in order to remove the incoherent deposits. After that, few milligrams of sample were scratched from the surface in different points. Then the samples were crushed, and homogeneous fine powders were obtained. Furthermore some microfragments containing both degraded phases and substrate were taken in order to make stratigraphic thin sections.

2.1. Roman Sarcophagus

The small-sized Roman sarcophagus was made from a single marble piece with a trapezoidal vertical section and has the following measurements: length 124 cm, width 37 cm, and depth 55 cm. The external side of the sarcophagus is adorned with strigile flutes and by a central clipeo, which before restoration, seemed to have no decorations. The sarcophagus has a hole in the centre which suggests a past use as a wash-basin. Inside the sarcophagus, a low pillow is visible on the right side. The marble appears fine grained and covered by a pink-coloured thick layer (Figure 1(a)); in this layer is evident the small portions of detachment material.

The sampling on the sarcophagus is made up of six samples, taken from the degraded areas (Table 1).

2.2. The Church of San Giuseppe

The Church of San Giuseppe was built in the second half of the eighteenth century and is constituted exclusively by oolitic limestone. The building, surmounted by a belfry, has an octagonal plan and a single nave with a semicircular apse. The facades show typical baroque architectonical elements [9].

After a careful macroscopic examination, several types of different stone decay were found. In particular alveolitation and granular disintegration are mainly located on the columns of the main portal, while black crusts and brown-orange-coloured chromatic alterations are present on almost all of the facade (Figure 1(b)).

The sampling on the facade is made up of six samples, taken from the degraded areas (Table 2).

3. Experimental

Fourier transform-infrared spectroscopy (FTIR) was performed for a mineralogical characterization of the powdered samples by means of comparison to a data base [10]. The equipment used was a Nicolet 380 with a Smart Orbit accessory used in the following arrangement: a K-Br beam-splitter, an HP-DTGS-KBr detector, and an Ever-Glow lamp used as source. In this configuration, the resolution was 4 cm-1. The great advantage of this spectroscopic technique is the high sensibility which allows the detection of many components, even at very low amounts.

The qualitative distribution maps of mineralogical phases, performed on thin sections, have been obtained by using a micro-Fourier transform-infrared spectrometer ( -FTIR) Spotlight 200 (Perkin Elmer) microscope, equipped with an MCT detector cooled by liquid nitrogen, a germanium ATR crystal, and a computer-controlled mapping stage programmable in the and directions. The spectra were recorded at 4 cm-1 resolution, mode with a spot of m2.

Point-by-point spectral mapping of the thin section was carried out in a grid pattern with the computer-controlled microscope stage with a spot of . Each spectrum was collected between 4000 and 700 cm-1 at a spectral resolution of 4 cm-1. The map spectra were collected with 4 scans for each spectrum. Maps have a resolution of 625 dots and a spatial resolution of 100  m. They are based on the compare correlation value (calculated by Spotlight 200 software) of the recorded spectra with references ones. A compare correlation map indicates the areas of a map, where the spectra are most similar to a reference spectrum.

4. Results and Discussion

4.1. FTIR Analysis

The spectroscopic study was aimed at essentially characterizing the main degradation products present on both typologies of materials sampled.

In all the analysed samples, the stretching vibrations of calcium carbonate ( ) peaked at 1409, 705, and 611 cm-1 and identified since the substrate (marble and oolitic limestone).

The IR spectra of all samples (taken from sarcophagus and facade of S. Giuseppe Church) showed the presence of typical vibration bands of calcium sulphate hydrate, commonly called gypsum ( ), centred at 1109, 669, and 596 cm-1 as well as the stretching and deformation vibrations of the O–H bond of water at 3525, 3492, 3401 cm-1 and at 1692 and 1627 cm-1, respectively. In all the analyzed samples, representative band of silicates was present at 1032 and 1006 cm−1. Gypsum originates from the transformation of calcite in the presence of sulphur oxides, while silicate was subsequently embedded in the crust due to the deposition of wind-born particles [11] (Figure 2).

Most notably, the prominent bands of calcium oxalate ( ) at 1324 and 780 cm−1 were present [12]. The band presence at 1324 cm−1 is typical of whewellite represent stretching [13]. As gypsum is also present, the calcium oxalate band around 1640–1620 cm−1 cannot be clearly established (Figure 2) [14].

The presence of organic matter was highlighted exclusively on the sarcophagus samples by the weak bands at 2950 cm-1, 2919 cm-1, and 2855 cm-1 attributed to the stretching of and groups (Figure 2). The weak absorbance peak at 729 cm-1 may be assigned to the rocking of group ( with ). Furthermore, there is no evidence of the presence of carbonyl groups (in the range of 1700–1750 cm-1), so it can be presumed that an aliphatic hydrocarbon compound, such as paraffin [15], was used as a protective treatment.

From these results, it can be presumed that an organic compound should not be used for protection treatment. In fact, the areas where the organic compounds were found showed a chromatic alteration that could be related to the degradation process of the organic matter used in the previous restorations.

4.2. -FTIR Analysis

Ultrathin sections of samples containing patinas were studied by using a -FTIR microscope. The analysis was aimed at investigating the superficial layer coating of the stone substrate.

The qualitative distribution maps of calcite, gypsum, and whewellite have been obtained by using the correlation of the recorded spectra with the reference ones of calcite, gypsum, and whewellite. The bright areas indicate regions of high correlation (therefore high concentration), while dark areas indicate a low concentration (Figure 3).

In Figure 3(c) it is evident that gypsum is present in different areas of the bulk. In all samples investigated we have found a penetration of the gypsum into the substrate. Unfortunately, from the samples taken from the artwork, it is very hard to give a value to the penetration depth because we found gypsum dishomogeneously distributed throughout the bulk, so deeper samples are needed to assess the penetration degree.

This process represents the main cause of crumbling of the substrate. As described in literature [16], whewellite is more localized within the sample (Figure 3(d)) and often combined with black crust.

The maps of sample of S. Giuseppe Church are also based on the correlation of the recorded spectra with the reference ones of gypsum and whewellite.

The bright areas indicate regions of high correlation (therefore high concentration), while dark areas indicate a low concentration (Figure 4).

They confirm the presence of gypsum and whewellite, as shown in the FTIR analysis, and also confirmed that degradation products are exclusively sited on the external surface of the sample. Figure 5 is obtained by overlap gypsum and oxalate maps, it is evident that the distribution of the two mineralogical phases, in particular oxalate, is mainly located below the gypsum.

This analytical technique has provided useful information for the manufact cleaning process. In fact, during restoration, the thin oxalate layer lying below the gypsum crust was preserved.

This patina is considered very useful for the protection [17] of stones, even if it involves only the surface of the sample, because the surface is not alternated. The characteristics of absorbance and wetting do not change; the porosity decreases but does not interfere with the passing of liquid water; therefore, resistance towards acid substances is increased.

5. Conclusions

This paper represents an example of diagnostic analysis for conservation of historical cultural heritage. Results, obtained by using spectroscopic analytical techniques, allow the awareness on degradation products as well as the conservational state of marble and calcarenite to be advanced. In particular, the combined used of FTIR and -FTIR analysis highlighted the presence and the distribution of gypsum and calcium oxalate on the stone surface.

Furthermore, this research confirms the importance of infrared spectroscopy for a semiquantitative determination of both inorganic and organic phases and demonstrates how the micro-FTIR provides information about restoration process.

In particular, by means of degradation products mapping, it is possible to discriminate with cleaning, and consolidation methods are more appropriate for preserving the oxalate layers that represent a natural protective coating.