2002
DOI: 10.1144/gsl.sp.2002.205.01.02
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Freeze-thaw cycles and their influence on marble deterioration: a long-term experiment

Abstract: The deterioration of three marbles (Palissandro, Sterzing and Carrara) differing in composition and rock fabric has been studied using measurements of the thermal dilatation in the temperature range from −40°C up to 60°C. A long-term freeze-thaw experiment was performed to characterize the frost weathering via Young’s modulus. The results show that the combined effect of heating and cooling under dry and water-saturated conditions significantly influences the material properties. The thermal dilatation and its… Show more

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Cited by 29 publications
(15 citation statements)
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“…Kessler (1919) found that repeated heating may lead to permanent dilatation due to microfracturing. Rosenholtz and Smith (1949), Sage (1988) or Ondrasina et al (2002) reported length changes of 1 mm/m due to heating and cooling. Thermally treated marbles which do not return to initial length changes after heating or cooling can show an inelastic residual strain even as a result of very small temperature changes (Battaglia et al 1993).…”
Section: Introductionmentioning
confidence: 99%
“…Kessler (1919) found that repeated heating may lead to permanent dilatation due to microfracturing. Rosenholtz and Smith (1949), Sage (1988) or Ondrasina et al (2002) reported length changes of 1 mm/m due to heating and cooling. Thermally treated marbles which do not return to initial length changes after heating or cooling can show an inelastic residual strain even as a result of very small temperature changes (Battaglia et al 1993).…”
Section: Introductionmentioning
confidence: 99%
“…When heated, calcite crystal expands (26 9 10 -6 /°C) parallel to the crystallographic c-axis and contracts (-6 9 10 -6 /°C) in a direction normal to it (Kleber 1990). Historically, some researchers have attributed the bowing exclusively to the effects of repeated heating-cooling cycles (Sir Rayleigh 1934;Rosenholtz and Schmidt 1949;Ondrasina et al 2002). Logan et al (1993) and Logan (2004) suggested that the bowing of the marble slabs in the Amoco building was due to the anomalous expansion-contraction behaviour of calcite combined with the release of locked residual stresses.…”
Section: Introductionmentioning
confidence: 99%
“…This implies that for the investigated samples freeze-thaw action only plays a secondary part. Other experiments have shown that if cracks are open to a certain extent, the capillary water uptake increases and weathering processes like chemical solution or freeze-thaw action plays a more important role for marble decay (Ondrasina et al 2002;Ruedrich 2003).…”
Section: Marble Weatheringmentioning
confidence: 99%