2014
DOI: 10.1520/acem20130095
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Measuring Freeze and Thaw Damage in Mortars Containing Deicing Salt Using a Low-Temperature Longitudinal Guarded Comparative Calorimeter and Acoustic Emission

Abstract: Deicing salts are often applied to the surface of pavements and bridge decks in the winter to melt ice, thereby improving safety for the traveling public. In this paper, the influence of NaCl deicing salt on freezing and thawing temperatures of pore solution and corresponding damage of mortar specimens were investigated. A low-temperature longitudinal guarded comparative calorimeter (LGCC) was developed to cool down a mortar sample at a rate of 2°C/h and to re-heat the mortar at a rate of 4°C/h. Heat flux duri… Show more

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Cited by 49 publications
(62 citation statements)
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“…The acoustic emission was used to relate this phase change with damage. For more description see (16).…”
Section: Using Acoustic Emission and Heat Flow Techniques To Quantifymentioning
confidence: 99%
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“…The acoustic emission was used to relate this phase change with damage. For more description see (16).…”
Section: Using Acoustic Emission and Heat Flow Techniques To Quantifymentioning
confidence: 99%
“…This can develop a zone with a high degree of saturation. This high level of saturation can result in freezing damage and/or in chemical reaction in some systems (e.g., the formation of Friedel salt that can infill air voids (5,(7)(8)(9)(10)(11), the production of oxychloride (15,16), or the replacement of calcium in calcium silicate hydrate (3)). While this mechanism would explain the 'soft zone' frequently observed at the base of the saw-cut, an alternative damage pattern is observed with the side of the saw-cut flaking off in layers that are fractions of an inch thick.…”
Section: Introduction and Overviewmentioning
confidence: 99%
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“…The air voids are usually larger than the capillary pores [10 nm to 10 mm (Mindess, Young, & Darwin, 2003)] of the cementitious systems, and ideally are isolated from each other but connected with the capillary pore systems of the cementitious matrix (Litvan, 1988;Sutter, Van Dam, & Thomas, 2007). Entrained air voids that remain unsaturated in service can release pressure for the expansive ice formation under the freezing temperature (Fagerlund, 1977;Farnam, Bentz, Sakulich, Flynn, & Weiss, 2014;Li, Pour-Ghaz, Castro, & Weiss, 2012;Pinto & Hover, 2001). …”
Section: Introductionmentioning
confidence: 99%