Page 359 - Copper and Bronze in Art: Corrosion, Colorants, Getty Museum Conservation, By David Scott
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[I]f  this  proceeds,  the  copper  is  dissolved  by  carbon  dioxide containing waters,  so  that
               finally  pure  tin oxide remains  which combines  with various  compounds  from  the  soil
               [T]he  degree of this  decomposition  depends on  the  ratio of oxygen  and  aggressive car­
               bon  dioxide in  the  groundwaters.  If oxygen  is  missing  the  decomposition  will  be  slow,
               even in the presence of high amounts of carbon dioxide.... [I] f there is a lot of oxygen, but
               little carbon dioxide, then the metal is often oxidized and covered with a carbonate patina.
               (Geilmann 1956:210)





           TABLE  l l . l  COMPOSITIONAL ANALYSIS OF A BURIED  BRONZE URN
                         DATING TO THE EARLY IRON ACE


           METAL         COMPOUNDS      PATINA        TIN  OXIDE    TIN  OXIDE
           (wt  %)                                    ANALYSIS      ANALYSIS
                                                      NO.  1        NO.  2
           Cu      83.70   CuO          54.84           9.30          0.78
           Sn      11.85   Sn0 2        28.31          56.07         63.20
           Sb       0.53   s b 2 o 5     1.91           2.35          2.80
           As       0.14   As 2 0 5     0.40            0.78          0.90
           Pb       2.98   PbO          0.27            0.20          0.01
           Fe       0.96   Fe 2 0 3      1.90           2.42          2.67
                         NiO             —              —             —
           TOTAL   100.16   CoO          -              —             —
                                        0.05            2.24          2.75
                         A1 2 0 3
                                         —              0.09          0.15
                         Mn0 2
                         CaO            0.05            0.10          0.03
                                        0.76            2.39          2.69
                         P 2 O 5
                                        0.10            0.05          0.02
                         S0 3
                                        0.37            3.17          3.20
                         s i o 2
                         c o            6.45            1.58          0.05
                           2
                         Loss 3         6.32           19.31         21.30
                         TOTAL          99.83         100.05        100.25
                         Humus          trace         trace           0.08
                                         -              -             —
                         NH 4
                         CI             0.05            0.08          0.03

           After Geilmann  (1956).
           Loss of weight on ignition.
          l
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