1965
DOI: 10.1007/978-3-663-06927-0
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Das mörteltechnische und chemische Verhalten verschiedener Trasse und Gesteinsmehle in Verbindung mit Kalk in wäßrigen Lösungen

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Cited by 4 publications
(7 citation statements)
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“…5b). This kind of crust does not change the morphology of the stone surface (Fitzner et al 1995) and seems to have very strong bonds with the stone surface (Török et al 2011;Siegesmund et al 2007). Scaling is often observed in context with laminar crusts.…”
Section: Crust Classificationmentioning
confidence: 99%
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“…5b). This kind of crust does not change the morphology of the stone surface (Fitzner et al 1995) and seems to have very strong bonds with the stone surface (Török et al 2011;Siegesmund et al 2007). Scaling is often observed in context with laminar crusts.…”
Section: Crust Classificationmentioning
confidence: 99%
“…Wolff (1972) addressed the formation of gypsum crusts on Obernkirchner sandstone-sandstone with very little calcium content-to leaching alkaline components of the joint mortars. Mortars with latently hydraulic binders, e.g., puzzolana and diatomaceous earth, or cement components are commonly known for their capability to release water-soluble forms of sodium, potassium, calcium, and magnesium components (Arnold 1981(Arnold , 1992Bläuer-Böhm 2005;Kraus 2002;Kraus and Droll 2009;Schwiete et al 1965). At Cologne cathedral, it can be observed that in many places the decay on the Drachenfels trachyte starts from the joints, which is indicated by gypsum crusts, flaking and scaling (Graue et al 2011).…”
Section: Sulfur and Calcium Sourcesmentioning
confidence: 99%
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“…These play an important part in the deterioration of natural building stones. Mortars may function as a source of alkaline components and contribute to the formation of damaging salts (Grün 1931;Wolff 1972;Arnold 1981Arnold , 1992Bläuer-Böhm 2005;Kraus 2002; Kraus and Droll 2009;Schwiete et al 1965). Furthermore, due to their different physical properties, e.g., strength, elasticity, density, water absorption, thermal and moisture dilatation, they might display divergent behavior from the stone materials and contribute to their decay, if not cause the deterioration of the natural building stones.…”
Section: Aims Of the Thesismentioning
confidence: 99%
“…Wolff (1972) addressed the formation of gypsum crusts on Obernkirchen sandstonesandstone with very little calcium contentto leaching alkaline components of the joint mortars. Mortars with latently hydraulic binders, e.g., puzzolana and diatomeous earth, or cement components are commonly known for their capability to release water-soluble forms of sodium, potassium, calcium and magnesium components (Arnold 1981(Arnold , 1992Bläuer-Böhm 2005;Kraus 2002;Kraus and Droll 2009;Schwiete et al 1965). At Cologne cathedral, it can be observed that in many places the decay on the Drachenfels trachyte starts from the joints, which is indicated by gypsum crusts, flaking and scaling (Graue et al 2011).…”
Section: Sulfur and Calcium Sourcesmentioning
confidence: 99%