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基于压缩多孔二氧化硅材料中的雪崩现象。

Avalanches in compressed porous SiO(2)-based materials.

作者信息

Nataf Guillaume F, Castillo-Villa Pedro O, Baró Jordi, Illa Xavier, Vives Eduard, Planes Antoni, Salje Ekhard K H

机构信息

Departament d'Estructura i Constituents de la Matèria, Facultat de Física, Universitat de Barcelona, Diagonal 647, E-08028 Barcelona, Catalonia, and INP Grenoble, 38031 Grenoble Cedex 1, France.

Departament d'Estructura i Constituents de la Matèria, Facultat de Física, Universitat de Barcelona, Diagonal 647, E-08028 Barcelona, Catalonia.

出版信息

Phys Rev E Stat Nonlin Soft Matter Phys. 2014 Aug;90(2):022405. doi: 10.1103/PhysRevE.90.022405. Epub 2014 Aug 15.

DOI:10.1103/PhysRevE.90.022405
PMID:25215740
Abstract

The failure dynamics in SiO(2)-based porous materials under compression, namely the synthetic glass Gelsil and three natural sandstones, has been studied for slowly increasing compressive uniaxial stress with rates between 0.2 and 2.8 kPa/s. The measured collapsed dynamics is similar to Vycor, which is another synthetic porous SiO(2) glass similar to Gelsil but with a different porous mesostructure. Compression occurs by jerks of strain release and a major collapse at the failure point. The acoustic emission and shrinking of the samples during jerks are measured and analyzed. The energy of acoustic emission events, its duration, and waiting times between events show that the failure process follows avalanche criticality with power law statistics over ca. 4 decades with a power law exponent ɛ≃ 1.4 for the energy distribution. This exponent is consistent with the mean-field value for the collapse of granular media. Besides the absence of length, energy, and time scales, we demonstrate the existence of aftershock correlations during the failure process.

摘要

研究了基于SiO₂的多孔材料(即合成玻璃Gelsil和三种天然砂岩)在压缩过程中的破坏动力学,该过程是在0.2至2.8 kPa/s的速率下缓慢增加单轴压缩应力。测得的坍塌动力学与Vycor相似,Vycor是另一种类似于Gelsil的合成多孔SiO₂玻璃,但具有不同的多孔介观结构。压缩通过应变释放的突变和破坏点处的主要坍塌发生。测量并分析了突变过程中样品的声发射和收缩情况。声发射事件的能量、持续时间以及事件之间的等待时间表明,破坏过程遵循雪崩临界性,在约4个数量级上具有幂律统计,能量分布的幂律指数ɛ≃1.4。该指数与颗粒介质坍塌的平均场值一致。除了不存在长度、能量和时间尺度外,我们还证明了破坏过程中余震相关性的存在。

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