Page 360 - Copper and Bronze in Art: Corrosion, Colorants, Getty Museum Conservation, By David Scott
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These corrosion processes, Geilmann argues, occur in the absence of chloride ions, and his
           analytical results tend to support  this interpretation. The presence of humic acids in the  soil—
           along with  enhanced  levels of soil  minerals  such  as iron,  silicon, and aluminum—was  also
           shown to be an important factor in the corrosion of the bronze  objects  from  these sites.
               Several  papers have confirmed the essential fact of humic  acid's role in the corrosion of
           buried  copper-alloy  objects.  Taube,  King,  and  Chase  (1997), for example,  found  that  Chinese
           bronze  mirrors with a typical composition of 70Cu25Sn5Pb might have a 100 μπι thick patina






           TABLE  11.2   C O M P O S I T I O N A L  A N A L Y S I S  O F A  B U R I E D  S W O R D  B L A D E
                         D A T I N G  T O  T H E  M I D D L E  B R O N Z E  A G E


           M E T A L      C O M P O U N D S   O X I D E   O U T E R   C E N T E R   P O I N T
           (wt  %)                       PATINA  3   R E G I O N   R E G I O N   O F  B L A D E
                                                     O F  B L A D E  O F  B L A D E

           Cu     90.26   CuO             72.02       22.55        8.72         5.60
           Sn      8.70   Sn0 2           28.53       55.07        68.59        68.15
           Sb     0.20    s b 2 o 5        0.75        1.34        1.46         1.74
           As      0.05   As 2 0 5         0.42        1.09        0.93         0.91
           Pb     0.I8    PbO              0.01       0.05         0.05         0.05
           Fe     0.15    Fe 2 0 3         0.12       0.72         0.91         1.64
           Ni      0.24   NiO              0.07       0.15         —            —
           Co     0.10    CoO              0.06       0.09         —            —
           TOTAL  99.88   A1 2 0 3         0.01       0.15         0.25         0.52
                                           —           —           0.05         0.12
                          Mn0 2
                          CaO              —          0.05         0.10         0.09
                                           0.12        1.01        1.07         1.05
                          P 2 O 5
                                           —           —           0.12         0.05
                          s o 3
                                           0.02       0.06         0.08         0.05
                          Si0 2
                                           0.22       2.40         0.64         0.42
                          c o 2
                          Loss b          nil         15.41        17.28        19.83
                          TOTAL          102.35      100.14       100.20       100.19
                          Humus            —          0.16         0.15         0.49
                                           —          0.03         0.06         0.08
                          NH 4
           After Geilmann (1956).
            Composition of layer isolated from what appears to be a cuprite zone.
           1
           ' Loss of weight on ignition.



                                                S O M E  A S P E C T S  O F  B R O N Z E  PATINA S
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