Subject: Calcium oxalate on easel paintings
Flavia de Souza <fluksy2000 [at] hotmail__com> writes >I am a conservation student currently writing my thesis on calcium >oxalate film encountered on easel paintings. ... >... >... In my review I intend to >summarize the analysis methods performed for identification of >calcium oxalate ... With reference to Calcium oxalate, in the case of films on stone it has been discussed extensively as both a natural and artificial protective layer, (the latter characteristically described as scialbatura), and is widely found on monuments, within crusts or between the crusts and rainwashed areas, and as a yellowish discolouration/patina. On stone it's derived either from the incomplete combustion of fossil fuels, the transformation of previous restoration treatments using oils and waxes, and/or due to the bio-infestations which produce oxalic acid that reacts with the underlying carbonate matrix. For example, one mechanism is where saxicolous lichens are reported to produce up to 50% of their total weight in oxalic acid which reacts with marble to produce calcium oxalate. Scialbatura consists mainly of calcium oxalate in two forms: monohydrated whewellite and dehydrated weddelite. Both are chemically pure, although impurities are bound up in the crust during their formation. Calcium oxalate is itself colourless but when organic fragments, mainly lichen, and inorganic fragments of quartz, feldspar and other minerals are present they give the patina a yellowish brown colour. Calcite crystals become isolated creating a mixed oxalate/calcite band with no clear definition between the carbonates and oxalates, making it difficult to detect in cross-section, and this layer can be less than 100 um thick, or as a heavy encrustation. Calcium carbonate is significantly more soluble than calcium oxalate at pH 7. As the solubility of the carbonate increases until pH 5, beyond which irreversible decomposition occurs the oxalate is far more acid resistant and not as susceptible to the degradation caused by acid gases. Non invasive portable Raman spectroscopy can be used to identify monohydrated whewellite and dehydrated weddelite One of the things I'd like to investigate but have never had the time is developing some kind of portable test kit (and I too would like to know of anything that can be adapted for testing stone surfaces/samples non-invasively). Three things I have been aware of are: The possibility of identifying calcium oxalate crystals using techniques developed around alizarin red S staining as a spot test. The re-examinination of the Raspail spot test, a test developed in 1827 by Francois-Vincent Raspail in which he originally demonstrated the presence of calcium oxalate in the starch of monocotyledon plants. Nowadays the test is standardised only as a method for detecting rosin in paper <URL:http://www.modernmicroscopy.com/ main.asp?article=69&page=2> There might be something to investigate in using a standard silver nitrate stain test on samples <URL:http://www.histosearch.com/ histonet/Jul07A/Re.HistonetYasuesSilverNiA.html> **** Moderator's comments: The above URLs have been wrapped for email. There should be no newlines. Jonathan Kemp Senior Sculpture Conservator Sculpture Conservation V&A Museum Cromwell Road South Kensington London SW7 2RL +44 2079422121 *** Conservation DistList Instance 22:56 Distributed: Tuesday, March 31, 2009 Message Id: cdl-22-56-004 ***Received on Friday, 27 March, 2009