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A simplified model for the combined wicking and evaporation of a NaCl solution in limestone

机译:石灰石中NaCl溶液的毛细作用和蒸发作用的简化模型

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摘要

Salt weathering is one of the major causes of the damage both in cultural heritage as well as in civil engineering constructions. A special case develops when there is a continuous wicking of a salt solution into a material in combination with evaporation of the moisture at its surface. In this study we are interested in the case where the absorption rate is much higher than the evaporation and as a result a salt concentration will build up at the drying surface resulting in crystallization. To this end we propose a simplified model to describe this mechanism. In order to check the model the NaCl concentration profiles were measured non-destructively by Nuclear Magnetic Resonance during a combined wicking and evaporation experiment with limestone. A good correlation was found between the model and the measured NaCl concentration profiles.
机译:盐风化是造成文化遗产和土木工程破坏的主要原因之一。当盐溶液连续芯吸到材料中并结合其表面的水分蒸发时,就会出现一种特殊情况。在这项研究中,我们对吸收速率远高于蒸发速率的情况感兴趣,因此盐浓度会在干燥表面积聚而导致结晶。为此,我们提出了一个简化的模型来描述这种机制。为了检查模型,在与石灰石的芯吸和蒸发实验相结合的过程中,通过核磁共振对NaCl的浓度进行了无损测量。在模型与测得的NaCl浓度曲线之间发现了良好的相关性。

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