大岗山水电站坝区辉绿岩流变特性的三轴试验研究  

Triaxial Test Research into Rheological Properties of Diabase in Dagangshan Hydropower Station Dam Site

作　　者：杨文东[1,2] 张强勇[2] 陈芳[2] 李术才[2] 李文纲[3] 王建洪[3] 贺如平[3] 曾纪全[3] 张功实[2] 

机构地区：[1]中国石油大学(华东)储运与建筑工程学院,山东青岛266555 [2]山东大学岩土与结构工程研究中心,山东济南250061 [3]中国水电顾问集团成都勘测设计研究院,四川成都610072

出　　处：《四川大学学报（工程科学版）》2011年第5期64-70,101,共8页Journal of Sichuan University (Engineering Science Edition)

基　　金：国家重点基础研究发展计划资助项目(2009CB724607);国家自然科学基金资助项目(40772173);教育部新世纪优秀人才支持计划资助项目(NCET-08-0336)

摘　　要：为解决大岗山水电站坝基的辉绿岩的流变力学问题,利用RLW-1000三轴流变仪进行了不同应力路径下的三轴流变试验,得到了各工况下的应力-应变-时间曲线。结果表明:辉绿岩是典型的硬脆性岩石,存在明显的流变门槛值,破坏时表现为突发性的脆性破裂。在破裂应力水平下表现出减速蠕变、等速蠕变和加速蠕变,减速蠕变和加速蠕变历时都十分短暂。临近破裂时的横向蠕变速率均不同程度的大于轴向,这是导致岩石扩容的主要原因。由于流变过程中损伤不断发展,导致岩石整体强度下降,因此流变破坏强度普遍低于常规三轴压缩试验瞬时破坏强度。辉绿岩存在一定的蚀变现象,蚀变矿物呈细鳞片状集合体。由于蚀变带的存在,使得岩块的强度受到影响,岩石破裂极易发生在结晶程度较差的矿物颗粒部位或胶结程度较差的两种矿物接触部位。In order to study the long-term mechanical properties of the diabase in Dagangshan hydropower station dam site,triaxial rheological tests under different stress paths were carried out on RLW-1000 rheology testing machine,and the stress-strain-time curves under different conditions were obtained.The results showed that the diabase was typical hard-brittle rock which had obvious rheological threshold,and sudden brittle fracture was shown at failure of specimen.Shortly prior to failure,each specimen experienced transient creep,steady-state creep and tertiary creep stage in the fracture stress level,but the transient creep and tertiary creep stage maintained short time.When the applied stress level was closed to the fracture stress,the circumferential creep rates were higher than those of axial,which were the main reason of the volume dilatancy phenomenon of specimen.The continuous development of damage in rheological process caused the decrease of whole strength of rock mass,so the rheological failure strength was lower than the instantaneous failure strength by the triaxial compression test.There was some degree of alteration in the diabase of Dagangshan hydropower station dam site,and the altered minerals showed fine scale-like aggregation.The strength of rock was impaired by the existence of alerted strip,the rupture of rock can occur easily in the interface of poorly crystallized mineral grains and the poorly cemented ones.

关 键 词：流变试验 辉绿岩 三轴流变 流变破裂机制 硬脆岩体 

分 类 号：TU45[建筑科学—岩土工程]