Conservation Journal
Spring 2005 Issue 49
Dating Alhambra stuccoes
Traditional materials were detected on four stucco fragments supposedly still covered by the original decoration. When mercury(II) sulfide (HgS, also called vermilion or cinnabar) was detected and identified by Raman microscopy, its particles examined by polarised light microscopy showed an irregular distribution of shape and size, as well as the presence of striations on some of the biggest particles. These features indicate that the red pigment is either of mineral origin, in which case it is more accurate to refer to it as cinnabar, or it is of synthetic origin, by means of the so-called dry process. Similarly, the particles of lazurite, seen under the optical microscope, showed the characteristics typical of a ground pigment, i.e. irregular size and shape, broken edges and non-uniform colour. This indicates that the pigment was obtained from lapis lazuli, and it is not the synthetic material called ultramarine blue, which was first synthesised in 1828. As expected for stuccoes, gypsum and occasionally calcite were detected in the mortar samples.
Figure 2: Raman spectra of a) lazurite from a blue area and b)vermillion from a red area on panel A.9-1913. Reference spectra of known sampls of lazurite and cinnabar are also shown for comparison purposes.
In contrast, modern pigments such as Prussian blue and lead chromate (also known as chrome yellow) were detected on stucco fragment A.10-1913 (see Figure 3). This indicates that either the whole fragment is a modern replica or the fragment is original, but was re-painted at some point in the 19th century. This 'terminus post quem' derives from the fact that Prussian blue was first synthesised in 1704, but it was not commercially available until the 1720s; on the other hand lead chromate, also known as chrome yellow, was first synthesised at the beginning of the 19th century. One of the fragments (A.10-1913) also shows traces of synthetic, wet-process vermilion, characterised by uniformly sized, small, rounded particles.
The analysis of pigments and materials found on these stucco panels from the Alhambra Palace in Granada, Spain, gave sufficient clues to hypothesise that one of the panels was not from the 14th century, as originally thought. Gypsum, and in one instance, calcite were detected in the stucco mortar, and traditional materials such as lazurite, cinnabar, and carbon black were detected on stucco fragments supposedly still covered by the original decoration. Pigments such as Prussian blue and lead chromate were found on one stucco fragment, which was therefore thought to be either an original fragment repainted at some point in the 19th century or a copy made in the 19th century. The latter hypothesis is supported by observations collected during the conservation treatment of the stucco fragments. 1
Acknowledgements
References
2. Burgio, Lucia, 'Microscopy analysis of Hispano-Moresque samples from the Alhambra', V&A Science Report 04.27.lb, June 2004.
3. Burgio, Lucia, Clark, Robin J.H., and Borges, Victor, Paper in preparation for submission to the Journal of Cultural Heritage.
Spring 2005 Issue 49
- Editorial
- Dating Alhambra stuccoes
- Conservation of Houghton Hall textiles and furniture
- Funding a collaborative conservation project: the Mazarin Chest
- The Safavid Cope
- The Ardabil Carpet - a new perspective
- Encounters with paper conservation: the treatment of a Chinese painted silk dress
- An insight into the craftsman's techniques
- William Blake's only surviving palette?
- Printer friendly version












