2012
DOI: 10.1002/jrs.4068
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Raman investigation of artificial patinas on recent bronze – Part I: climatic chamber exposure

Abstract: In humid air, copper and its high copper alloys (bronze) tend to form an oxide layer (patina). Natural patinas protect copper and its alloys from further corrosion processes. On the other hand, artists have frequently deliberately patinated bronze for visual effects. Thus, it is of great importance to study the patina changing mechanism to follow its chemical changes and to predict in advance the likely corrosion processes. Green chloride and green nitrate patinas, applied over the brown artist's patina, were … Show more

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Cited by 47 publications
(60 citation statements)
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References 31 publications
(62 reference statements)
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“…However, in the absence of Ni, Zn or Co cations, the mineral phase more likely to form is clinoatacamite rather than paratacamite. In fact, the Raman spectral features recorded in the samples from the Hall of the Kings with three characteristic bands at 3440, 3348 and 3309 cm −1 together with those at 142, 362, 511, 897, 933 and 967 cm −1 are strongly coincident with those reported for clinoatacamite . Clinoatacamite was probably formed as a result of the degradation of the original azurite pigment in the presence of chloride.…”
Section: Resultssupporting
confidence: 77%
“…However, in the absence of Ni, Zn or Co cations, the mineral phase more likely to form is clinoatacamite rather than paratacamite. In fact, the Raman spectral features recorded in the samples from the Hall of the Kings with three characteristic bands at 3440, 3348 and 3309 cm −1 together with those at 142, 362, 511, 897, 933 and 967 cm −1 are strongly coincident with those reported for clinoatacamite . Clinoatacamite was probably formed as a result of the degradation of the original azurite pigment in the presence of chloride.…”
Section: Resultssupporting
confidence: 77%
“…(c)], respectively, can also be found. The bands of atacamite appear at 3438, 3350, 980, 970, 910, 816, 678, 514, 441, 417, and 355 cm −1 , whereas modes of gerhardite (Cu 2 (OH) 3 NO 3 ) can be found at 3550, 3472, 1324, 1049, 815, 713, 507, 475, 456, 416, and 259 cm −1 .…”
Section: Resultsmentioning
confidence: 99%
“…(d)], only the bands arising from the patina could be noticed. The broader band, with several maxima in the region between 350 and 700 cm −1 , suggests the presence of Cu and Sn oxides, whereas the well‐defined bands at 218 and 146 cm −1 suggest the presence of cuprite . The weak band at 289 cm −1 could also indicate the presence of Cu 2 S …”
Section: Resultsmentioning
confidence: 99%
“…Niektoré tími použili aj doplnkovú techniku na odlíšenie minerálov vytvorených na bronze v rôznych prostrediach [86]. Len málo štúdií uvádza Ramanovú spektroskópiu ako jedinú techniku pre charakterizáciu rôznych koróznych produktov na bronze [21,24,[86][87][88][89][90]. De la Roja et al študoval rozdielne zelené patiny, ktoré boli vytvorené na medi a jej zliatinách pomocou zelených pigmentov, tak zvanej medenky [87].…”
unclassified
“…De la Roja et al študoval rozdielne zelené patiny, ktoré boli vytvorené na medi a jej zliatinách pomocou zelených pigmentov, tak zvanej medenky [87]. Existujú rôzne dáta z Ramanovej spektroskopie chloridov a minerálov medi [88,89] a Ramanove spektrá niektorých bežných fáz skorodovanej medi [90]. Ale je pomerne málo štúdií o Ramanových spektrách týkajúcich sa rôznych patín na medi a jej zliatinách [21,24].…”
unclassified