2008
DOI: 10.1016/j.culher.2007.09.002
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Swelling damage in clay-rich sandstones used in the church of San Mateo in Tarifa (Spain)

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Cited by 84 publications
(51 citation statements)
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“…This creates an area of tension that results in development of fractures between the wet zone of the rock and the dry zone behind it. Swelling stresses lead to the development of scaling and flaking as well as contour-scaling [16]. Once the external wet layer has dried as a result of evaporation due to the action of the sun, temperature increase during the day, and evaporation accelerated by the effects of the wind, the clays contract causing the appearance of drying or retraction fractures perpendicular to the surface as observed all over the Al-Hijr rocks.…”
Section: Discussionmentioning
confidence: 99%
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“…This creates an area of tension that results in development of fractures between the wet zone of the rock and the dry zone behind it. Swelling stresses lead to the development of scaling and flaking as well as contour-scaling [16]. Once the external wet layer has dried as a result of evaporation due to the action of the sun, temperature increase during the day, and evaporation accelerated by the effects of the wind, the clays contract causing the appearance of drying or retraction fractures perpendicular to the surface as observed all over the Al-Hijr rocks.…”
Section: Discussionmentioning
confidence: 99%
“…Clay minerals have a flat shape like small flakes. These flaked shapes are typical of Kaolinite [16]. Different spots of sandstone samples were investigated by EDS to identify their elemental composition, tab.…”
Section: Sem Investigation Resultsmentioning
confidence: 99%
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“…Jiménez-González et al 2008;Wangler and Scherer 2008). It is the case of smectites or interstratified chlorite/smectite clays in the Scrabo sandstone of St. Matthew's Church in Belfast (Smith et al 2002); the lower Keuper sandstones of SainteCroix's Church in Bouzonville, East France (Mertz and Guiavarc'h 2005); and the Tarifa sandstone of San Mateo's Church in Cádiz, Spain (Sebastián et al 2008). Swelling clays have been shown experimentally to enhance hydric/ hygric expansion, e.g.…”
Section: Comparison With Other Building Sandstonesmentioning
confidence: 95%
“…Another damage mechanism arises with sandstones that have swelling clay inclusions in the binding phase, where stresses on the order of the strength of the stone can arise due to differential wetting and drying. The problem of swelling clays in conservation has been recognized by a number of authors previously (Rodríguez-Navarro et al 1997;Delgado Rodrigues 2001), and continues to generate interest in recent years (Franzini et al 2007;Sébastian et al 2008). It has been demonstrated that the expansion of Portland brownstone results from intracrystalline swelling of mixed-layer chlorite/smectite clays in the cementing phase by incorporation of as many as four layers of water molecules (Wangler and Scherer 2008).…”
Section: Introductionmentioning
confidence: 97%