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论文摘要

层状大理岩间接拉伸试验及断口形貌和断裂机理分析

Indirect Tensile Test of Layered Marble and Analysis of Fracture Morphology and Mechanism

作者:裴建良(中国长江三峡集团公司博士后工作站;中国长江三峡集团公司工程建设管理局;四川大学 水利水电学院);苏立(中国长江三峡集团公司工程建设管理局);刘建锋(四川大学 水利水电学院);左建平(中国矿业大学 煤炭资源与安全开采国家重点实验室)

Author:Pei Jianliang(Post-DoctoralScientificResearchStation,ChinaThreeGorgesCo.;ProjectConstructionManagementDept.,ChinaThreeGorgesCo.;CollegeofWaterResourceandHydropower,SichuanUniv.);Su Li(ProjectConstructionManagementDept.,ChinaThreeGorgesCo.);Liu Jianfeng(CollegeofWaterResourceandHydropower,SichuanUniv.);Zuo Jianping(StateKeyLab.ofCoalResourcesandSafeMining,ChinaUniv.ofMiningandTechnol.)

收稿日期:2013-11-05          年卷(期)页码:2014,46(4):39-45

期刊名称:工程科学与技术

Journal Name:Advanced Engineering Sciences

关键字:岩石力学;间接拉伸试验;断口形貌;分形维数;断裂模式

Key words:rockmechanics;indirecttensiletest;fracturemorphology;fractaldimension;fracturemode

基金项目:国家“973”重点基础研究发展计划资助项目(2010CB226802;2010CB732002);国家自然科学基金资助项目(51209180);国家“211工程”项目资助(cers-1-114)

中文摘要

通过MTS815试验系统、激光扫描仪和SEM电镜对锦屏Ⅱ级水电站交通辅助洞的盐塘组互层状大理岩进行间接拉伸试验研究、断口形貌测试和细观断裂机理分析。结果表明:拉应力的作用方向与层理面的夹角显著影响岩石的抗拉强度及破坏机理,当拉应力平行层理面时,岩样的平均抗拉强度约为6.32 MPa,断口形貌较为粗糙,表面分维约为D=2.14~2.17;而当拉应力垂直层理面时,岩样的平均抗拉强度仅约2.57 MPa,断口形貌较为平缓,表面分维约为D=2.07~2.10。对于同一种岩石,断口形貌特征与其抗拉力学性能具有明显的对应关系,即断裂表面越粗糙,其分形维数越大,对应的抗拉强度也越高,反之亦然。通过SEM揭示了产生这种现象的细观断裂机理,当拉应力垂直层理面时,岩石主要发生沿晶断裂,穿晶断裂相对要少些;而当拉应力平行层理面时,岩样的断裂模式主要为沿晶和穿晶耦合断裂。研究表明,不同的微细观断裂模式是层状大理岩断口形貌迥异和力学性质差异的根本原因。

英文摘要

With the aid of MTS815,large scale laser profilometer and SEM testing system,indirect tensile tests,fractography and meso fracture mechanism analysis were carried out on layered marbles taken from transportation tunnel of JinpinⅡ hydropower station.Experimental results indicated that the included angle between tensile stress direction and bedding plane significantly influenced tensile strength and fracture mechanism of marble.The average tensile strength is approximately 6.32 MPa when the direction of tensile stress is parallel to the bedding plane.And the fractography is rough and surface fractal dimension is about 2.14~2.17 in this case.However,the average tensile strength is about 6.32 MPa when the direction of tensile stress is perpendicular to the bedding plane.And the fractography is more smooth and surface fractal dimension is only 2.07~2.10 in this case, which indicates clearly that there is a good corresponding relationship between tensile mechanical properties and fractography in layered marble. For the same kind of rock,the rougher the fracture surface presents,the greater its fractal dimension will be.And it will correspond to a higher tensile strength,vise versa.The meso-fracture mechanism was also studied through SEM. When the tensile stress is parallel to the bedding plane,the intergranular fracture occurs,but the transgranular fracture is relatively less. When the tensile stress is perpendicular to bedding plane,the facture mode changes to mixed fracture mode,namely,coupled intergranular fracture and transgranular fracture. Different micro/meso-fracture modes are the fundamental reasons which induce different fracture morphology and tensile properties in layered marble.

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