2007
DOI: 10.1007/s00254-006-0590-9
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Investigation of NaCl deliquescence in porous substrates using RH-XRD

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Cited by 27 publications
(11 citation statements)
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“…Specifically, the impedance behavior of an IDE sensor loaded with inorganic salt microparticles down to the size range of coarse mode tropospheric aerosols is characterized and deliquescence (solid to liquid) and efflorescence (liquid to solid) phase transitions determined with respect to relative humidity (RH). The hygroscopic behavior of soluble salts bears importance in many fields including pharmaceuticals, , porous building materials, , corrosion, and atmospheric sciences. Regarding the latter, tropospheric aerosols and their constituent chemistries have received extensive attention due to their governance of the chemistry and dynamics of the atmosphere and climate. ,, …”
Section: Introductionmentioning
confidence: 99%
“…Specifically, the impedance behavior of an IDE sensor loaded with inorganic salt microparticles down to the size range of coarse mode tropospheric aerosols is characterized and deliquescence (solid to liquid) and efflorescence (liquid to solid) phase transitions determined with respect to relative humidity (RH). The hygroscopic behavior of soluble salts bears importance in many fields including pharmaceuticals, , porous building materials, , corrosion, and atmospheric sciences. Regarding the latter, tropospheric aerosols and their constituent chemistries have received extensive attention due to their governance of the chemistry and dynamics of the atmosphere and climate. ,, …”
Section: Introductionmentioning
confidence: 99%
“…The crystal growth is usually induced by changes in ambient temperature or relative humidity. Unfavorable environmental conditions may cause repeated cycles of deliquescence-crystallization or hydration-dehydration, which lead to the rapid decay of building materials (Linnow et al 2007). Salt weathering is thus controlled by fluctuations in temperature and moisture, where repeated oscillations in these parameters can cause recrystallization, hydration/dehydration of salts, bringing about stone surface loss in the form of, for example, granular disaggregation, scaling, and multiple flaking (McCabe et al 2013).…”
Section: Phase Changes For Soluble Salts In Poresmentioning
confidence: 99%
“…Tab. In addition, from the comparison of the mineral composition analysis results of the soil samples (as Tab.2 is shown), it shows that the crispy soil sample on the surface of the Shenna ruins contains gypsum, which further shows that the soluble salt on the surface of the soil at the Shenna ruins is mainly CaSO 4 [18][19][20] . It and NaCl are the main salts that cause soil salinization and will destroy the structure of the soil.…”
Section: Microstructure Of the Ruins And Soluble Salt Analysismentioning
confidence: 99%
“…More importantly, the Shenna ruins are in a special environment, and shallow surface water is still active in the ruins. Therefore, the soluble salt in the soil continuously migrates and accumulates to the surface soil layer of the ruins along with the movement of shallow water [19] . In fact, the harm of soluble salt to the ruins is obvious, especially in winter, the annual average temperature of the area is 2.6~5.3℃, the temperature difference between day and night is large, and the annual minimum temperature is around minus 20 degrees, the freezing and thawing expansion is severe in winter, when the water content of the soil is high, the freezing and thawing expansion will inevitably occur, which will also cause the expansion of the soil and make the surface powdery [22] .…”
Section: Correlation Between Occurrence Environment and The Cause Of Deteriorationmentioning
confidence: 99%