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Application of instantaneous profile measurement of moisture content and moisture potential in porous materials

机译:瞬时轮廓测量在多孔材料中水分含量和水分势的应用

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摘要

Due to limits in current moisture content and moisture potential measurement technology, moisture transport is normally investigated under equilibrium conditions. Most processes we observe in nature are, however, transient and hardly ever reach an equilibrium stage. This means that future experimental methods in moisture transport investigation will focus on transient processes. One such method is the instantaneous profile measurement (IPM) technique frequently used in soil science. It can be applied to investigate moisture transport under transient conditions. Two measurement principles are combined in one material to record data for moisture content and moisture potential at the same time and at various points. As output, moisture content and moisture potential profiles are plotted against space and time. The method was applied to different porous materials, and hygroscopic loading and deloading cycles were conducted in the relative humidity range between 30 and 97%. The data obtained is not in strict agreement with static or steady-state observations. This reveals information about moisture transport kinetics. These findings are discussed in the context of the literature and with regard to their significance for current moisture transport models, which are typically based on equilibrium data.
机译:由于当前水分含量和水分势测量技术的限制,通常在平衡条件下研究水分传输。但是,我们在自然界中观察到的大多数过程都是短暂的,几乎没有达到平衡阶段。这意味着未来水分输送研究中的实验方法将集中在瞬态过程上。一种这样的方法是土壤科学中经常使用的瞬时剖面测量(IPM)技术。它可用于研究瞬态条件下的水分传输。在一种材料中结合了两种测量原理,可以同时记录不同时间的水分含量和潜在水分数据。作为输出,将水分含量和水分势曲线与空间和时间作图。该方法适用于不同的多孔材料,并在30%至97%的相对湿度范围内进行吸湿性加载和卸载循环。所获得的数据与静态或稳态观测值并不完全一致。这揭示了有关水分传输动力学的信息。这些发现是在文献的背景下讨论的,并涉及它们对当前水分传输模型的意义,这些模型通常基于平衡数据。

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