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首页> 外文期刊>Pure and Applied Geophysics >Stress Transfer During Pressure Solution Compression of Rigidly Coupled Axisymmetric Asperities Pressed Against a Flat Semi-Infinite Solid
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Stress Transfer During Pressure Solution Compression of Rigidly Coupled Axisymmetric Asperities Pressed Against a Flat Semi-Infinite Solid

机译:刚性耦合轴对称粗糙物压在平坦半无限固体上的压力解决方案压缩过程中的应力传递

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摘要

In a previous work, we developed a numerical model of compression by pressure solution (PS) of a single axisymmetric asperity pressed against a flat semi-infinite solid. The dissolution rate at any point along the contact and at any time t was determined by (1) computing the normal stress distribution from the current shape of the asperity, and (2) solving the diffusion equation inside the fluid-saturated solid-solid interface, including local dissolution source terms corresponding to the stress field previously determined. The change in shape of the asperity during an infinitesimal time interval δt can then be calculated and the entire procedure repeated as many times as desired. Our results showed that, as the contact flattens and grows during PS, the initial elastic deformation is partially relaxed and the stress transferred from the contact center to the edge. Our goal in the present paper is to demonstrate that, among a population of asperities, stress can also be transferred from one contact to another and that the overall compaction rate can be significantly affected by this process. For this purpose we extended our previous numerical model to simulate PS of two rigidly coupled spherical asperities simultaneously pressed against a flat semi-infinite solid. We considered two end-member cases: 1) transfer of stress to a newly created, not initially present contact, 2) transfer of stress between asperities with different sizes. In both cases, stress was transferred from the most stressed asperity to the least, and, the overall PS displacement rate was reduced. Thus, formation of new contacts and heterogeneous distribution of asperity sizes, which are both expected to exist in rough fractures with self-affine aperture or in heterogeneous granular materials with variable grain-packing geometry, may significantly slow down PS creep compaction. Keywords Pressure solution - creep
机译:在先前的工作中,我们开发了一个压力解决方案(PS)的压缩模型,该解决方案是将单个轴对称粗糙物压在平坦的半无限大实体上。通过(1)根据当前的粗糙形状计算法向应力分布,以及(2)求解流体饱和固-固界面内部的扩散方程,可以确定沿接触的任何点以及在任何时间t的溶出速率。 ,包括与先前确定的应力场相对应的局部溶解源项。然后可以计算出无穷小时间间隔δt内粗糙形状的变化,并且整个过程可以根据需要重复多次。我们的结果表明,在PS期间,随着接触面的变平和增长,初始弹性变形被部分松弛,应力从接触中心转移到边缘。我们在本文中的目标是证明,在一系列粗糙区域中,应力也可以从一种接触转移到另一种接触,并且整个压实率会受到此过程的显着影响。为此,我们扩展了先前的数值模型,以模拟同时压在平坦的半无限实体上的两个刚性耦合的球形凹凸的PS。我们考虑了两种最终成员情况:1)将压力转移到新创建的,最初没有出现的接触中; 2)在大小不同的粗糙体之间转移压力。在这两种情况下,应力都从应力最大的粗糙处转移到应力最小的粗糙处,并且整体PS置换率降低了。因此,新的接触的形成和粗糙尺寸的异质分布,都预期存在于具有自仿射孔的粗糙裂缝中,或存在于具有不同晶粒堆积几何形状的异质粒状材料中,可能会大大减慢PS蠕变的压实。关键词压力解-蠕变

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