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Experimental Method to Determine Some Physical Properties in Physics Classes

机译:确定物理课中某些物理性质的实验方法

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ABSTRACT Particle density, gravimetric and volumetric water contents and porosity are important basic concepts to characterize porous systems such as soils. This paper presents a proposal of an experimental method to measure these physical properties, applicable in experimental physics classes, in porous media samples consisting of spheres with the same diameter (monodisperse medium) and with different diameters (polydisperse medium). Soil samples are not used given the difficulty of working with this porous medium in laboratories dedicated to teaching basic experimental physics. The paper describes the method to be followed and results of two case studies, one in monodisperse medium and the other in polydisperse medium. The particle density results were very close to theoretical values for lead spheres, whose relative deviation (RD) was -2.9 % and +0.1 % RD for the iron spheres. The RD of porosity was also low: -3.6 % for lead spheres and -1.2 % for iron spheres, in the comparison of procedures – using particle and porous medium densities and saturated volumetric water content – and monodisperse and polydisperse media.
机译:摘要颗粒密度,重量和体积水含量以及孔隙率是表征多孔系统(例如土壤)的重要基本概念。本文提出了一种测量这些物理性质的实验方法的建议,适用于实验物理类别,适用于由具有相同直径(单分散介质)和不同直径(多分散介质)的球体组成的多孔介质样品。由于在专门用于教授基础实验物理学的实验室中使用这种多孔介质存在困难,因此不使用土壤样品。本文介绍了要遵循的方法以及两个案例研究的结果,一个案例是在单分散介质中,另一个案例是在多分散介质中。铅球的颗粒密度结果非常接近理论值,铅球的相对偏差(RD)为-2.9%,铁球的相对偏差(RD)为+ 0.1%RD。孔隙度的RD也很低:在比较程序(使用颗粒和多孔介质密度以及饱和体积水含量)以及单分散和多分散介质的情况下,铅球为-3.6%,铁球为-1.2%。

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