Page 134 - Copper and Bronze in Art: Corrosion, Colorants, Getty Museum Conservation, By David Scott
P. 134

Pourbaix diagrams for the three mixed basic carbonates are not yet available, and an under­
            standing of the likelihood of formation of these products  will  need to wait until  such stability
            diagrams  are  established.

            Synthetic pigments  with  Because of their availability  and low cost,  zinc  salts were  fre­
                                                           i
            copper and zinc salts    quently  used  as  additives n  nineteenth-century  commercial
                                     pigment preparations  based on copper.  Riffault,  Vergnand, and
            Toussaint  (i874),  for  example,  describe  the  synthesis of a  "mineral  green  lake," which,  the
            authors point out, is a misnomer because it is not precipitated onto an inert base like a dye. The
            pigment was prepared from  a mixture of copper and zinc oxides obtained from a saturated  solu­
            tion  of copper in ι part nitric acid and 3 parts hydrochloric acid combined with a solution of zinc
            in  concentrated  nitric acid. Potassium  carbonate was used to precipitate a light green product  of
            mixed carbonates. This precipitate was washed,  dried, powdered, and then heated in a crucible
            until the "carbonic acid" (an early name for  C0 2 ) was expelled, and the product acquired a fine
            greenish hue. Ground very fine, the durable pigment was used for watercolors and for oil colors.
               Depending on the proportions of copper and zinc salts dissolved in the acidic solutions, the
            precipitated carbonate might represent any of the mixed copper-zinc  salts discussed here.


        C H A L C O N A T R O N I T E :  A  S O D I U M - C O P P E R  C A R B O N A T E
            Chalconatronite,  Na 2 Cu(C0 3 ) 2 -3H 2 0,  is  the  best known sodium-copper-carbonate  mineral.
            It was  first  identified by Frondel and Gettens  (1955)  as a bluish green, chalky crust found in the
            hollow interior of an Egyptian bronze  figurine  of the  deity Sekmet  from  the  Saite-Ptolemaic
            period 663-630  B.CE.)  in the  Fogg Museum of Art,  Boston. The mineral was  also identified
                  (
            on  an Egyptian bronze  group of a cat and kittens in the Gulbenkian Collection in Lisbon and
            on  a Coptic censer, dating from  about  the  seventh  century, in the Freer Gallery of Art,  Wash­
            ington, D.C.
               Chalconatronite  was  subsequendy identified on a copper pin from  St. Mark's Basilica in
            Venice (Staffeldt and Paleni 1978). Shordy thereafter,  Horie and Vint  (1982) found  chalconatro­
            nite  crystals  on  Roman  copper  and  iron  armor  from  a  site  at  Chester, England. The  armor
            had been conserved  many years earlier,  and  the  authors  suggest that  the  chalconatronite  is a
            by-product of that treatment. In addition, the author  (Scott  1999)  identified chalconatronite  as
            an  alteration product  on  a New Kingdom Egyptian gilt-bronze  figurine of Osiris in the  col­
            lections  of the  Department  of Near  Eastern  Studies,  University of Southern  California. The
            alteration had penetrated  to a considerable  depth, with whole regions of the preserved  surface
            being transformed  to  chalconatronite.








                                                      BASI C  C O P P E R  CARBONATE S
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