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首页> 外文期刊>Journal of porous media >A STUDY ON THE CHANGES IN PHYSICAL PROPERTIES OF DEMINERALIZED WATER PUT IN CONTACT WITH POROUS HYDROPHILIC MATERIALS: EXPERIMENTAL EVIDENCES ON METABRICK MATERIAL
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A STUDY ON THE CHANGES IN PHYSICAL PROPERTIES OF DEMINERALIZED WATER PUT IN CONTACT WITH POROUS HYDROPHILIC MATERIALS: EXPERIMENTAL EVIDENCES ON METABRICK MATERIAL

机译：多孔亲水材料与多孔水化液体物理性质变化的研究：Metabrick材料的实验证据

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摘要

Metabrick is a patented material made up of cooked clay as in common bricks but modified in order to increase its porosity up to 65% and broaden its range of pore diameters (less than 0.3 nm to 0.2 mm). Such a material shows unconventional experimental evidences when it is saturated by demineralized water through capillary rise. The latter causes a temperature reduction within both the volume of the metabrick and the capillary water. In addition, when a sponge is inserted into the metabrick the capillary water is taken by the sponge and poured out as free water. If the temperature of the poured water is measured, it is 3 degrees C-4 degrees C lower than the ambient temperature. Furthermore, when the electric conductibility of both the demineralized water passing through the metabrick and the water taken from a sponge inserted into the metabrick is measured, it becomes evident that these waters show values 3 orders of magnitude greater than a common value for demineralized water (the measure is about 1500 mu S). All the above-mentioned phenomena could be explained in light of the fourth phase of water applied to the capillary rise occurring in the metabrick. This statement is largely discussed throughout the paper.
机译：Metabrick是由熟粘土组成的专利材料，如普通砖，但改性，以使其孔隙率高达65％，并扩大其孔径范围（小于0.3nm至0.2mm）。这种材料表明，当通过毛细血管升起，它通过脱矿水饱和时非常规实验证据。后者导致元素的体积和毛细管水中的温度降低。另外，当海绵插入Metabrick中时，毛细管用海绵捕获并作为自由水倒入。如果测量倒水的温度，则比环境温度低3℃C-4℃。此外，当测量通过代谢的脱矿质水的可燃性和从插入核心克里克中的海绵中取出的水的可燃性时，这很明显，这些水显示值3大小的数量级大于脱矿质水的共同值（措施约为1500亩）。所有上述现象都可以根据适用于在Metabrick中发生的毛细血管升高的水的第四阶段来解释。本文主要讨论此声明。

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