盐(化学)
蒸发
多孔介质
沉积(地质)
多孔性
材料科学
风化作用
化学工程
化学物理
地质学
化学
复合材料
热力学
物理
沉积物
地貌学
工程类
物理化学
作者
Nour Sghaier,Sandrine Geoffroy,M. Prat,H. Eloukabi,Sassi Ben Nasrallah
出处
期刊:Physical Review E
[American Physical Society]
日期:2014-10-14
卷期号:90 (4): 042402-042402
被引量:38
标识
DOI:10.1103/physreve.90.042402
摘要
Subflorescence refers to crystallized salt structures that form inside a porous medium. We report a drying experiment revealing major development of subflorescence in the dry region of the porous medium away from the liquid zone. Using a combination of image analyses and numerical computations, we show that the growth is directly correlated to the evaporation flux distribution along the boundary of the growing salt structure. This indicates that the salt is transported into the domain occupied by the salt structure in the porous medium up to the structure periphery, where salt deposition takes place. This is confirmed when a growing salt structure encounters dry subflorescence formed earlier during the drying process. The dry subflorescence is reimbibed and resumes its growth. The analysis also suggests that the solution within the growing subflorescence is in equilibrium with the crystallized salt wall. These results shed light on the growth mechanisms of subflorescence, a phenomenon that can play a fundamental role in several important issues such as carbon dioxide sequestration or salt weathering.
科研通智能强力驱动
Strongly Powered by AbleSci AI