岩石破裂前红外热像的时空演化特征  

Temporal-Spatial Evolution Features of Infrared Thermal Images Before Rock Failure

作　　者：刘善军[1] 吴立新[1,3] 张艳博[2] 

机构地区：[1]东北大学资源与土木工程学院,辽宁沈阳110004 [2]河北理工大学资源与环境学院,河北唐山063000: [3]北京师范大学减灾与应急管理研究院,北京100875

出　　处：《东北大学学报（自然科学版）》2009年第7期1034-1038,共5页Journal of Northeastern University(Natural Science)

基　　金：国家自然科学基金资助项目(50774017);国家杰出青年基金资助项目(50525414);河北省自然科学基金资助项目(E2008000410)

摘　　要：以花岗闪长岩和大理岩试件单轴加载红外观测实验为例,对岩石破裂前红外热像的时空演化特征进行了分析.结果表明:岩石在塑性变形阶段随着微破裂的产生出现热像空间分异现象,表现为在未来剪性破裂位置出现高温异常条带,且高温异常条带之间的区域出现低温辐射异常,这种热像异常特征是岩石宏观破裂的早期红外前兆.而临失稳前热像整体表现出的短暂降温是岩石宏观破裂的晚期红外前兆.两种红外前兆的出现及其空间特征与岩石破裂形式及应力场分布格局有密切关系.Exemplifying the granodiorite and marble specimens which were loaded uniaxially for observation via infrared thermal images, the characteristics of temporal-spatial evolution of infrared thermal images before rock failure were analyzed. The results showed that a differentiation was found in the space of thermal image with the initiation of microcracks during the plastic deformation of specimens, where the formation of high-temperature abnormal stripes indicates the possible shear failure position in future and the low-temperature abnormal radiation is found between those stripes. Both the abnormalities mean the early infrared precursor of macrofailure of rock, while the short-time rock temperature drop as shown in all thermal images is facing an out-of-stability state and means the late infrared precursor of macrofailure of rock. The occurrence of the two precursors and their spatial characteristics relate closely to the form of rock failure and distribution of stress field.

关 键 词：遥感-岩石力学 岩石破裂 红外前兆 热像 灾变遥感 

分 类 号：TU452[建筑科学—岩土工程]