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Effect of Young’s Modulus and Surface Roughness on the Inter-Particle Friction of Granular Materials

机译:杨氏模量和表面粗糙度对颗粒材料颗粒间摩擦的影响

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摘要

In the study we experimentally examine the influence of elastic properties and surface morphology on the inter-particle friction of natural soil grains. The experiments are conducted with a custom-built micromechanical apparatus and the database is enhanced by testing engineered-reference grains. Naturally-occurring geological materials are characterized by a wide spectrum of mechanical properties (e.g., Young’s modulus) and surface morphology (e.g., roughness), whereas engineered grains have much more consistent characteristics. Comparing to engineered materials, geological materials are found to display more pronounced initial plastic behavior during compression. Under the low normal load range applied in the study, between 1 and 5 N, we found that the frictional force is linearly correlated with the applied normal load, but we acknowledge that the data are found more scattered for natural soil grains, especially for rough and weathered materials which have inconsistent characteristics. The inter-particle coefficient of friction is found to be inversely correlated with the Young’s modulus and the surface roughness. These findings are important in geophysical and petroleum engineering contents, since a number of applications, such as landslides and granular flows, hydraulic fracturing using proppants, and weathering process of cliffs, among others, can be simulated using discrete numerical methods. These methods employ contact mechanics properties at the grain scale and the inter-particle friction is one of these critical components. It is stressed in our study that friction is well correlated with the elastic and morphological characteristics of the grains.
机译:在研究中,我们通过实验研究了弹性特性和表面形态对天然土壤颗粒间摩擦的影响。实验是使用定制的微机械设备进行的,并且通过测试工程参考颗粒来增强数据库。天然地质材料的特点是具有广泛的机械性能(例如,杨氏模量)和表面形态(例如,粗糙度),而工程颗粒具有更为一致的特性。与工程材料相比,发现地质材料在压缩过程中表现出更明显的初始塑性行为。在研究中使用的低法向载荷范围内(介于1和5 N之间),我们发现摩擦力与法向载荷线性相关,但我们承认,发现的数据对于天然土壤颗粒(尤其是粗糙的土壤颗粒)更加分散以及特性不一致的风化材料。发现颗粒间的摩擦系数与杨氏模量和表面粗糙度成反比。这些发现对于地球物理和石油工程领域非常重要,因为可以使用离散数值方法来模拟许多应用,例如滑坡和颗粒流,使用支撑剂的水力压裂以及悬崖的风化过程等。这些方法利用了晶粒尺度的接触力学特性,而颗粒间的摩擦是这些关键因素之一。我们的研究强调,摩擦力与晶粒的弹性和形态特征密切相关。

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