Laboratory observations of transient frictional slip in rock-analog materials at co-seismic slip rates and rapid changes in normal stress
文献类型：期刊论文
| 作者 | Yuan FP(袁福平) ; Prakash V
|
| 刊名 | TECTONOPHYSICS
 |
| 出版日期 | 2012-08-10 |
| 卷号 | 558页码:58-69 |
| 通讯作者邮箱 | fpyuan@lnm.imech.ac.cn;vikas.prakash@case.edu |
| 关键词 | Rock-analog materials Co-seismic slip rates Rate weakening and strengthening Flash heating Rapid change in normal stress Plate-impact pressure-shear friction experiments Velocity-Dependent Friction Variable Normal Stress Molten-Metal Films Dynamic Rupture Constitutive-Equations Earthquake Prediction Sliding Conditions Melt Lubrication Fault Gouge Behavior |
| ISSN号 | 0040-1951 |
| 产权排序 | [Prakash, Vikas] Case Western Reserve Univ, Case Sch Engn, Dept Mech & Aerosp Engn, Cleveland, OH 44106 USA;[Yuan, Fuping] Chinese Acad Sci, Inst Mech, State Key Lab Nonlinear Mech, Beijing 100190, Peoples R China |
| 通讯作者 | Prakash, V ; Case Western Reserve Univ, Case Sch Engn, Dept Mech & Aerosp Engn, Cleveland, OH 44106 USA. |
| 合作状况 | 国际 |
| 中文摘要 | Knowledge of frictional (shear) resistance and its dependency on slip distance, slip velocity, normal stress, and surface roughness is fundamental information for understanding earthquake physics and the energy released during such events. In view of this, in the present study, plate-impact pressure-shear friction experiments are conducted to investigate the frictional resistance in a rock analog material, i.e. soda-lime glass, under interfacial conditions of relevance to fault rupture. The results of the experiments indicate that a wide range of frictional slip conditions exist at the slip interface ranging from initial no-slip and followed by slip weakening, slip strengthening (healing), and seizure all during a single slip event. The slip-weakening phase is understood to be most likely due to thermal-induced flash heating and incipient melting at asperity junctions, while the slip strengthening (slip-healing) phase is understood to be a result of coalescence and solidification of local melt patches on the slip interface. In addition, plate impact pressure-shear normal-stress change (drop) experiments are employed to probe the response of the slip interface due to sudden alterations in normal stress. In particular, the location (timing) of the stress drop is varied so as to investigate the behavior of the slip interface in its slip-weakening, slip-strengthening (healing) phase, or the seized phase, in response to sudden drop in normal stress. These experimental results provide a rich set of data to better understand the range of possible friction slip states that can be achieved and/or critically examine existing dynamic friction models for fault slip behavior. |
| 学科主题 | 损伤、破坏机理和微结构演化 |
| 分类号 | 二类/Q2 |
| 收录类别 | SCI ; EI |
| 资助信息 | The authors would like to acknowledge the financial support of National Science Foundation Earth Division through grants EAR: 0710975 and EAR: 0810083 for conducting this research. The authors would also like to acknowledge the Major Research Instrumentation Award CMS-0079458 by the National Science Foundation for the acquisition of the Multi-beam VALYN VISAR used in the present experiments. |
| 原文出处 | http://dx.doi.org/10.1016/j.tecto.2012.06.026 |
| 语种 | 英语 |
| WOS记录号 | WOS:000307802900004 |
| 公开日期 | 2013-01-18 |
| 源URL | [http://dspace.imech.ac.cn/handle/311007/46710]  |
| 专题 | 力学研究所_非线性力学国家重点实验室 |
| 推荐引用方式 GB/T 7714 | Yuan FP,Prakash V. Laboratory observations of transient frictional slip in rock-analog materials at co-seismic slip rates and rapid changes in normal stress[J]. TECTONOPHYSICS,2012,558:58-69. |
| APA | 袁福平,&Prakash V.(2012).Laboratory observations of transient frictional slip in rock-analog materials at co-seismic slip rates and rapid changes in normal stress.TECTONOPHYSICS,558,58-69. |
| MLA | 袁福平,et al."Laboratory observations of transient frictional slip in rock-analog materials at co-seismic slip rates and rapid changes in normal stress".TECTONOPHYSICS 558(2012):58-69. |
入库方式： OAI收割
来源：力学研究所
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