Page 267 - Copper and Bronze in Art: Corrosion, Colorants, Getty Museum Conservation, By David Scott
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in  fact, faustite  (see APPENDIX  D, TABLE  7). The presence of both copper  and zinc in the beads
                was confirmed by X-ray fluorescence. Faustite  is a partially zinc-substituted turquoise mineral
                not  mentioned in any  Old World  contexts.  There  does not  seem to  be  any mention of chal-
                cosiderite  either,  which  raises  some  doubts  about  the  exactitude  of  the  identification  of
                turquoise in the original texts. Foord and Taggart (i998) state that the number  of  known  occur­
                rences of faustite is quite small compared with  occurrences  of other members  of the  turquoise
                group. This adds to the significance of this mineral's discovery from  Moche cultural contexts.
                Given  the variations that  may exist within  the  turquoise  group of minerals, there  is clearly a
                need  for the publication of more  detailed X-ray  diffraction  data and  for trace  elements  to  be
                examined  as a possible distinguishing tool in the study of these minerals.


            THE  C O P P E R  NITRATE  M I N E R A L S
                Copper nitrates are relatively rare  as minerals, pigments, or corrosion products, since the usual
                nitrate  salts  are  all water  soluble. The  basic nitrates  can  occasionally  be  found, however,  as
                pigments  or  as corrosion products. The most common copper  nitrate mineral is the basic salt
                gerhardtite, Cu 2 (N0 3 )(OH) 3 ,  which  has  been found  as  a secondary  mineral associated  with
                malachite and atacamite in massive cuprite deposits. Gerhardtite can occur as thick tabular crys­
                tals, dark green to emerald green in color (Palache, Berman, and Frondel 1951). The crystal struc­
                ture was determined by Imhoff  (1953), although the nitrate was characterized in 1885  and named
                after  Gerhardt, who first synthesized  the salt.
                   Other  nitrate  minerals  include  likasite,  Cu 3 (N0 3 )(OH) 5 -2H 2 0, and  buttgenbachite,
                Cu 1 8 (N0 3 ) 2 (OH) 3 2 Cl 3 -H 2 0, which has a complex and unusual stoichiometry. Neither mineral
                has  yet been found  as a corrosion product. Brief characteristics  of the  copper  nitrate minerals
                are given in TABLE 7.2.


                Copper nitrate           The most common occurrence  of  gerhardtite is as a component
                corrosion products       of  artificially  patinated  copper  alloys. Many recipes  for  green
                                         patinas  today contain ingredients such  as nitric acid, potassium
                nitrate, sodium nitrite,  or ammonium nitrate  (Hughes  and  Rowe 1982), which would  create a
                copper (II)  nitrate salt.
                   Copper nitrates should be rare  as a natural corrosion product since nitrate salts are usually
                                                                     i
                the  most water-soluble  group of copper  corrosion products  and, f formed, would invariably
                be expected  to be washed  away from  the  surface.  There  are, however, some noted  occurrences
                of  copper  nitrates  in corrosion. Otto  (1959)  identified  gerhardtite  as  a patina  component  on
                archaeological  bronzes,  and  Riederer  (19 8 8)  reported  an  occurrence  of this  basic  nitrate  on
                some  ancient  Mesopotamian  bronzes  in  the  collections of the  Institut für  Technologie  der
               Malerei in Stuttgart.




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