Page 165 - Copper and Bronze in Art: Corrosion, Colorants, Getty Museum Conservation, By David Scott
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TABLE 5.1     CHARACTERISTICS OF SOME BASIC COPPER  SULFATE  MINERALS



            MINERAL        FORMULA                   CRYSTAL     COLOR        MOHS
            NAME                                     SYSTEM                   HARDNESS

            chalcanthite   CuS0 4 -5H 2 0            triclinic   deep blue    2 - 4
            brochantite    Cu 4 S0 4 (OH) 6          monoclinic   vitreous green   2.5-4
            antlerite      Cu 3 S0 4 (OH) 4          orthorhombic   vitreous green   3.5
            posnjakite     Cu 4 S0 4 (OH) 6 -H 3 0   monoclinic   vitreous green   2-3
            bonatite       CuS0 4 -3H 2 0            monoclinic   pale blue   2-3
            Strandberg's   Cu 2 . 5 (OH) 3 S0 4 -2H 2 0   monoclinic   pale green   ?
            compound
            langite        Cu 4 (S0 4 )(OH) 6 -2H 2 0   monoclinic   greenish blue   2.5-3
            Tutton's salt   Cu(NH 4 ,S0 4 ) 2 -6H 2 0
            schulenbergite   (Cu,Zn) 7 (SO 4 ,CO 3 ) 2 (OH) 10 .3H 2 O   rhombohedral   pearly light   2
                                                                 greenish blue
            synthetic      Pb 4 Cu(C0 3 )(S0 4 )
            compound
            caledonite     Cu 2 Pb 5 (S0 4 ) 3 C0 3 (OH) 6   orthorhombic   resinous green/   2.5-3
                                                                 bluish green
            beaverite     Pb (FeCuAl)  3 (S0 4 )  2  (OH)  6   rhombohedral   blue green   ?
            spangolite     Cu 6 Al(S0 4 )Cl(OH) 12 -3H 2 0   hexagonal   bluish green   2
            guildite       CuFe(S0 4 ) 2 (OH)-4H 2 0   monoclinic   yellow brown   2.5
            devilline      CaCu 4 (S0 4 ) 2 (OH) 6 .3H 2 0   monoclinic   pearly green   2.5
            ammonium copper   Cu(NH 4) S0 4 ) 2 -2H 2 0
            sulfate hydrate



            identification  of a basic copper (II)  sulfate  as  a patina  constituent  on bronzes from  Bourbon-
            l'Archambault in central France. This is the first reference in the literature to a basic sulfate com­
            pound in this context;  during the  late  nineteenth  and  early twentieth centuries,  difficulties in
            the identification of these various  compounds  often resulted in all of them being referred  to  as
            "brochantite."
                Brochantite  is a vitreous  green,  monoclinic mineral with  a Mohs hardness of 2.5-4,  first
            identified  from  the Bank mines of Sverdlovsk, Ekaterinburg, in the Ural Mountains of Russia.
            A melt-mount preparation  is shown in PLATE 34.
                Antlerite is a vitreous green, orthorhombic mineral with a Mohs hardness of 3.5; it is named
            after  the  Antler  mine  in Mohave  County, Arizona. Vernon  (1933)  appears  to  be  the  first  to





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