水分
风化作用
盐(化学)
多孔性
砖石建筑
材料科学
多孔介质
吸水率
含水量
化学工程
矿物学
化学
地质学
复合材料
岩土工程
地球化学
有机化学
工程类
土木工程
标识
DOI:10.1179/019713600806113176
摘要
The present overview on salt-induced deterioration of inorganic porous materials focuses on those topics considered the most relevant for understanding this phenomenon. These are movement of both water/moisture and salts within the pore system; influence of the presence of salts in moisture absorption; effect of the simultaneous presence of more than one salt; salt distribution in masonry; deterioration mechanisms; and weathering patterns. Of the latter, the most ubiquitous are powdering and scaling, and they have been found to occur on most stone types. However, the mechanism that induces the same outward appearance on different stones can vary significantly depending on the synergism that develops among porous material, salt, and moisture.
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