Page 163 - Copper and Bronze in Art: Corrosion, Colorants, Getty Museum Conservation, By David Scott
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nitrogen  oxides, whose  effect  may not become  apparent  for many years.  Recent  studies  have
            identified a large number of corrosion products on exposed statuary, and it is apparent  that gen­
            eralized statements about their formation may represent an oversimplification  of a very com­
            plex problem. For example, each exposed  bronze  may be influenced by a special microclimate
            within  the overall climatic parameters of the atmosphere.  Consequently,  additional studies  are
            needed to piece  together  all available information  and produce  a more  comprehensive  under­
            standing of the deterioration of exposed  bronzes.


         H I S T O R I C A L  R E F E R E N C E S  TO  C O P P E R  S U L F A T E S

            Sasyaka (blue vitriol)  has the play of colour in the throat of the peacock. Mayaratuttham is
            an emetic,  an antidote to poisons and a destroyer of the whiteness of the skin.— VAGBHATA 2
            Blue vitriol,  or what  the  ninth-century Indian physician and writer  Vagbhata  calls "sasyaka"
            (Ray 1956), is copper (II) sulfate pentahydrate. It was well known in antiquity as a mineral whose
            uses may have included pigment and medicinal preparations,  and would have been found in an
            impure form  as a secondary  mineral from  the leaching of various primary ore deposits. In rich
            copper  mines, particularly in Cyprus,  the  leaching of copper  sulfide ore  deposits  resulted in
            a variety of copper (II)  sulfate  minerals. Blue vitriol was called "chalcanthum" or "chalitis" by
            other  writers from  ancient  times. From these names come  the  modern  one  for this mineral:
            chalcanthite, CuS0 4 -5H 2 0.
                Dioscorides describes chalcanthum  (chalcanthite)  as "appearing  as a concretion of liquids
            that filters drop by drop through the roof of mines. It is for this reason called 'stalacton' by those
            who work in the mines of Cyprus."  This copper  sulfate  exudate  is similar to a compound that
                                         3
            Pliny the Elder describes as occurring

                in  Spain  in  wells  or  pools,  the  water  of which  holds  it in  solution. This  solution  is
                mixed with an equal volume of fresh water, concentrated  by heat and poured into wooden
                tanks.  From beams  fixed  permanently  over  these  tanks  hang  ropes kept  taut  by stones,
                and on these the slime deposits in glassy berries, not unlike grapes. This material is taken
                out  and  dried for thirty  days. It is blue, with  a very notable  brilliance,  and  may  be mis­
                taken for glass. 4

                This lustrous botryoidal appearance is an apt description for basic copper-sulfate  salts that
            could be either chalcanthite or partially iron-substituted copper sulfates  such  as pisanite, which
            is essentially a copper-rich melanterite, (Fe,Cu)S0 4 -7H 2 0. Pliny also refers  to copper  sulfates
            when  he writes, "The  Greeks  by their name for shoemakers black have made out an  affinity
            between it and copper:  they call it chalcanthon,  'flower of copper/"  5  The allusion to  shoemak­
            ers' black is not accidental, since using copper  sulfate solutions to treat many organic materials,
            such  as felt or matting,  will result in a black color.



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