岩石材料基于天然散斑场的变形观测方法研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
许多类岩石材料由于其成分的原因在表面形成良好的散斑结构,用DSCM方法对这些岩石材料进行变形观测时可直接拍摄表面得到散斑图。基于这种天然散斑场的变形观测方法,进行了岩石材料变形的观测实验,验证了方法的可行性和优越性。
Many kinds of rock materials bear random speckle pattern on their surface due to the componential reason. This speckle structure can be captured and saved as speckle images for DSCM method when doing deformation measurement. DSCM method based on the natural speckle pattern is studied. Some rock material experiments are completed and the results of experiments prove the feasibility and advantage of the method.
引文
1LaermannKarl-Hans.New achievements and perspectives of optical methods in experimental solid mechanics[J].Optics andLasers inEngineering,1995,22(4/5):249~270
    2金观昌.计算机辅助光学测量.清华大学出版社,1997,143~174
    3潘一山.冲击地压发生和破坏过程研究[博士学位论文][D].北京:清华大学,1999,54~63
    4AsundiA,NorthH.White-light speckle methodcurrent trends[J].Optics andLasers inEngineering,1998,29(2/3):159~169
    5芮嘉白,金观昌,徐秉业.一种新的数字散斑相关方法及其应用[J].力学学报,1994,26(5):599~607
    6BerthaudY,TorrentiJ M,FondC.Analysis of localization in brittle materials through optical techniques[J].ExperimentalMechanics,1997,37(2):216~220
    7袁旭东,范厚彬,潘一山.地震包体形成的塑性应变梯度理论[J].辽宁工程技术大学学报,1999,6;566~569
    8白义如.相似材料模拟位移场的光学测量技术研究及应用(博士学位论文摘要)[J].岩石力学与工程学报,2001,20(1):5~5

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心