2020
DOI: 10.3390/min10030255
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Clay Minerals in European Painting of the Mediaeval and Baroque Periods

Abstract: Clay-based pigments are among the most traditional. Unlike other mineral pigments, they have never been fully replaced by synthetic analogues and are still used in painting today. Since their analysis requires a specific approach, detailed distinction of clay pigments has never been a part of routine chemical-technological research in fine arts—regardless of a great potential of clay minerals for determining regional provenance of the material. This review article maps and summarizes research on clay pigments … Show more

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Cited by 17 publications
(15 citation statements)
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“…IC analysis shows no evidence of sodium ions, and considering the low contribution of magnesium ions, gypsum crystallization might occur. This could happen if the ambient relative humidity becomes lower than the equilibrium relative humidity (RH eq ) of the saturated solution of the salt in the system [ 15 ]. Gypsum is characterized by the highest deliquescence RH, which is around 99.6% at 20 °C [ 15 , 16 ].…”
Section: Resultsmentioning
confidence: 99%
“…IC analysis shows no evidence of sodium ions, and considering the low contribution of magnesium ions, gypsum crystallization might occur. This could happen if the ambient relative humidity becomes lower than the equilibrium relative humidity (RH eq ) of the saturated solution of the salt in the system [ 15 ]. Gypsum is characterized by the highest deliquescence RH, which is around 99.6% at 20 °C [ 15 , 16 ].…”
Section: Resultsmentioning
confidence: 99%
“…This was followed by a layer of oil-based lead white that serves to reflect diffuse light striking it through the added translucent layers of tempera and oil. A wide variety of pigments were used to achieve the desired colors in the paintings (Hradil et al 2020). Lastly, relief decorations were applied to the frame and background (cf.…”
Section: The Enduring Legacy Of the Saint Agnes Conventmentioning
confidence: 99%
“…Still, the most abundant minerals in green earths are either celadonite or glauconite [7], [8]. These two species are both phyllosilicates from the mica group and both contain structural Fe II , which explains their green colour, the hues of which depend on the exact Fe II /Fe III ratio.…”
Section: Introductionmentioning
confidence: 99%