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Characterization of Mineral Building Materials by Mercury-Intrusion Porosimetry

机译:压汞法表征矿物建材

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摘要

Mineral building materials are generally heterogeneous and porous solids.Their engineering properties are closely associated with their porosity and pore-size distribution,which can be studied by mercury intrusion.The entire pore-size distribution curves are used to determine changes in the pore structure of a material class in a qualitative way.Certain parameters derived from pore-size distributions can be correlated to engineering properties.These key values are applied as criteria to evaluate the quality and durability of a building mate-rial.However,because of the heterogeneity of natural and artificial building materials and the influence of moisture content on their pore structure the results are strongly affected by preparation conditions such as sampling and drying.A correct analysis requires a knowledge of these effects.The paper describes the use of mercury porosimetry to study mineral building materials such as cementitious materials,bricks,and renderings.Furthermore,the influence of preparation effects on the precision of measurements is discussed.
机译:矿物建筑材料通常为非均质和多孔固体,其工程性质与其孔隙率和孔径分布密切相关,可以通过压汞法对其进行研究。整个孔径分布曲线用于确定矿物的孔隙结构变化。从孔径分布中得出的某些参数可以与工程特性相关联。这些关键值用作评估建筑材料质量和耐久性的标准。天然和人造建筑材料以及水分对其孔隙结构的影响,结果会受到诸如采样和干燥之类的制备条件的强烈影响。正确的分析需要了解这些影响。建筑材料,例如水泥材料,砖和效果图。此外,INF讨论了准备工作对测量精度的影响。

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