2003
DOI: 10.1016/j.culher.2003.09.002
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Efflorescence on thin sections of calcareous stones

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Cited by 21 publications
(6 citation statements)
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“…The presence of gypsum may be explained as a possible environmental modification of residual material left over from the preparation of the parchment or perhaps the accidental or intentional addition of gypsum to the paint mixture itself. 39 Sulfation is a problem commonly encountered with structural marble 40 or wall paintings 41 but is rarely described in illuminated manuscripts. In this case, it does not appear to have affected the integrity or adhesion of the paint layers.…”
Section: Nativitymentioning
confidence: 99%
“…The presence of gypsum may be explained as a possible environmental modification of residual material left over from the preparation of the parchment or perhaps the accidental or intentional addition of gypsum to the paint mixture itself. 39 Sulfation is a problem commonly encountered with structural marble 40 or wall paintings 41 but is rarely described in illuminated manuscripts. In this case, it does not appear to have affected the integrity or adhesion of the paint layers.…”
Section: Nativitymentioning
confidence: 99%
“…The main factors responsible for physical degradation include water, salt crystallization, wind action, and thermal stress [65]. The result of these physical phenomena that affect the stone are the phenomena of alveolization [66,67], efflorescence [68], etc. Chemical degradation assumes a prominent role in stone materials due to its ability to induce chemical alterations in the original material, resulting in the formation of byproducts characterized by high solubility in many cases.…”
Section: Degradation Of Stone Materialsmentioning
confidence: 99%
“…In fact, various authors have suggested that the forms of decay, the habits of the gypsum crystals and the development of the gypsum crust depend on the intrinsic (crystal size, mineralogical composition, pore system, surface finish) and extrinsic (degree of relative humidity, atmospheric composition, temperature, etc.) properties of the rock (Elfving et al, 1994a;Malaga-Starzec et al, 2003;Charola et al, 2007;Thornbush and Viles, 2007;Urosevic et al, 2013). In particular, the clast/crystal size could be an important factor in the different alteration processes observed in the four types of rock studied (Gauri et al, 1982): in the rocks with a smaller grain size such as TA, AR and especially MR, more gypsum appeared, something that seemed to occur regardless of the type of rock, given that in MR much smaller amounts of calcite were available compared to any of the other three types.…”
Section: Roughnessmentioning
confidence: 99%