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Use of sodium fluorescein dye to visualize the vaporization plane within porous media

机译:使用荧光素染料在多孔介质内可视化蒸发平面

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摘要

The vaporization plane in porous media separates the region of capillary flow from the dry surface layer, where the water transports only in its gas phase. Knowledge of the depth and geometry of the vaporization plane is critical for estimating water flux in the soil-atmosphere interphase, for understanding evaporating processes in general, and for prediction of locations of damaging salt crystallization, etc. However, detection of the vaporization plane is a challenging task. This paper explores the use of sodium fluorescein dye (uranine), a popular hydrological tracer, to visualize the vaporization plane in porous media. Uranine was used in the forms of solution or powder on sand, sandstone, and autoclaved aerated concrete, in both laboratory and field experiments. The property of uranine solution to change its color according to its concentration can be used to: i) visualize the vaporization plane by forming a distinctive dark-orange zone where the pore water evaporates, and ii) to distinguish the zone of vapor flow from the zone where capillary flow is present. Similarly, uranine powder, when applied onto a porous material, clearly visualizes the dry surface layer and the capillary zone, divided by the vaporization plane. This technique can also visualize a complex-shaped vaporization plane in hydrophobic materials. In comparison with other techniques, such as sensible heat balance or heat pulse methods, the use of uranine is accurate, cost-effective, and straightforward.
机译:多孔介质中的汽化平面与干燥表面层分离毛细血管流动区域,其中水仅在其气相中运输。汽化平面的深度和几何形状的知识对于估计土壤气氛中的水通量是至关重要的,用于了解蒸发过程,并且用于预测损伤盐结晶的位置等,但是,蒸发平面的检测是一个具有挑战性的任务。本文探讨了荧光素染料(铀),一种流行的水文示踪剂的使用,以使多孔介质中的汽化平面观察。在实验室和现场实验中,铀以砂,砂岩和高压灭菌混凝土的溶液或粉末的形式使用。根据其浓度改变其颜色的铀溶液的性质可用于:i)通过形成孔水蒸发的独特暗橙色区域,并将蒸汽流区分开来可视化蒸发平面。存在毛细管流动的区域。类似地,铀粉,当施加到多孔材料上时,清楚地可视化干表面层和毛细管区,除以蒸发平面。该技术还可以在疏水材料中可视化复杂形状的汽化平面。与其他技术相比,例如明智的热平衡或热脉冲方法,铀的使用是准确的,性价比和简单的。

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