Page 287 - Copper and Bronze in Art: Corrosion, Colorants, Getty Museum Conservation, By David Scott
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crystal structure was determined by Tamura and coworkers (i98i). The structure consists of  infi­
           nite zigzag chains with HCOO and OH groups bridging neighboring copper ions. The structure
           is  of interest  since  many other  formate  salts adopt  a dimeric structure  rather  than  an  infinite
           chain structure.
               In  one of the  first  studies  of the basic formates,  Fowles  (1915) found that when solutions
           of  the  neutral copper(II) formate  were  boiled, 2Cu(HCOO) 2 -Cu(OH) 2 -2H 2 0,  an insoluble
           basic  salt,  was  formed.  Fowles  observed  that  copper (II)  hydroxide readily combined when
           shaken  with  a cold  solution of copper  formate  to form  the  salt Cu(HCOO) 2 -3Cu(OH) 2  that
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           tended  to revert to Cu(HCOO) 2 -2Cu(OH) 2 . f the  salt, Cu(HCOO) 2 -3Cu(OH) 2 ,  freshly pre­
           pared, is added to a dilute solution of the neutral formate, it will change into a heavy, green crys­
           talline powder  after  ten weeks. f an excess of a saturated  solution of the neutral salt is  used,
                                    I
           complete conversion requires seventeen days. The compound obtained, Cu(HCOO) 2 * Cu(OH) 2 ,
           is  a fine, emerald green color.
              If  copper  strips  are kept in an atmosphere  of 80%  RH with 200 ppm of formic  acid, dark
           green corrosion spots form on the copper surface. Powder X-ray diffraction  analysis shows  data
           very similar to that for the laboratory synthesis  of 2Cu(HCOO) 2 -Cu(OH) 2 -2H 2 0. This illus­
                                                  i
           trates the potential importance of the new data; f only the  ICDD  ( JCPDS) files were relied on
           for  reference  information,  the corrosion formed on the  copper  strips would remain unidenti­
           fied. Two  refractive indices could be determined from  the mounted crystals in Cargille liquids,
           one at μ =  i.620 and the other at about 1.652.
              Pey  (1998) makes an unusual mention of the formate anion in reference  to the  characteri­
           zation of some green pigments found in the Hafkenscheid  collection, a historical collection of
           Dutch pigments that dates from  the early decades of the nineteenth century. Pey describes one
           pigment, papegaaigroen  (parrot green),  as "possibly a formo-arsenite," which would make par­
           rot  green  an  analog of Schweinfurt green; 3  no further  analytical data  are provided, however.


       THE  COPPER  A C E T A T E S

           The  chemistry  of  verdigris  The preeminent organic salt of copper is verdigris, essentially a
                                    copper acetate, of which there are a bewildering number of pos­
           sible varieties or mixtures. The name,  however, is not always specific to copper  acetate.  Some
           compounds called verdigris may actually be a mixture of carboxylate salts, or they could be basic
           copper chlorides, carbonates, or other more exotic compounds.
              Verdigris, which ranges in color from  pale blue through turquoise to green, was made for
           use  as a synthetic pigment or as a medicinal preparation. It is also an undesirable  and disfigur­
           ing  corrosion product on copper or bronze alloys. Verdigris has been known from  at least Greek
           and Roman times and is mentioned by Theophrastus  and Dioscorides. The origin of the word
          aeruginous,  often used to describe  "copper rust" (verdigris)  goes back to Pliny.




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