Damage mechanisms of porous materials due to in-pore salt crystallization.
Pressure exerted by crystallization of salts within porous materials contributes to damage in historic and modern construction. By unequivocally identifying the precipitating phase(s) while simultaneously determining solution supersaturation and associated crystallization pressure in subsurface pores, we show that the formation of a thermodynamically metastable salt phase (heptahydrate; Na2SO4·7H2O) and the resulting transition to a less soluble stable phase (mirabilite; Na2SO4·10H2O) is largely responsible for the high supersaturation and crystallization pressure developed during evaporative crystallization of sodium sulfate, the most damaging salt known. These results help to explain why salts with various (stable and metastable) hydrated phases are the most damaging. We also show that damage associated with metastable-stable phase transitions can be suppressed by the use of crystallization promoters. These results open new ways for the prevention of salt damage to building materials.
Department of Mineralogy and Petrology, University of Granada, Fuentenueva s/n, 18002 Granada, Spain.
Mara
M
Schiro
Encarnacion
E
Ruiz-Agudo
Carlos
C
Rodriguez-Navarro
D002152:Calorimetry, Differential Scanning; D003252:Construction Materials; D003460:Crystallization; D016062:Porosity; D012492:Salts / Q000737:chemistry*; D013431:Sulfates / Q000737:chemistry*; D013816:Thermodynamics; D014867:Water / Q000737:chemistry
D012492:Salts; D013431:Sulfates; D014867:Water; C012036:sodium sulfate