首页> 外文会议>Boundaries of Rock Mechanics: Recent Advances and Challenges for the 21st Century >Real-time CT testing of meso-damage evolution law of frozen cracked sandstone under uniaxial compression conditions
【24h】

Real-time CT testing of meso-damage evolution law of frozen cracked sandstone under uniaxial compression conditions

机译:单轴压缩条件下冻裂砂岩细观破坏演化规律的实时CT测试

获取原文
获取原文并翻译 | 示例

摘要

The CT real-time testing experiment have been done by applying the advanced CT techniques.The authors studied meso-damage mechanism of frozen sandstone test sample with two manmade prefabricated cracks under uniaxial compression conditions, and succeeded in getting CT images and CT values of frozen sandstone in various stages of damage from crack initiation and development to macroscopic crack formation and rock breaking. The results show that: so far as soft fractured sandstone with high water content is concerned,its strength will be improved considerably after it is frozen under negative temperature. Evolution of damage is of localized property and it is a non-linear real-times process. It is analogous to integral rock test sample that the course of frozen fractured sandstone from damage to destroy completely under the load of uniaxial compression can be divided into four stages: stage of linear development; stage of microscopic crack initiation and development; stage of rapid development of damage; and stage of accelerated development after reaching its peak. Damage evolution velocity of fractured rock at the four stages under the load of uniaxial compression is far quicker than intact rock. Split of new microcrack of frozen fractured rock and formation of final failure plane are closely related to the position and angle of existing prefabricated crack. The existence and geometric properties of prefabricated crack has important effects on dilatancy of fracture rock.
机译:运用先进的CT技术进行了CT实时测试实验,研究了单轴压缩条件下两个人造预制裂纹的冷冻砂岩试样的细观损伤机理,并成功获得了冷冻的CT图像和CT值砂岩处于从裂纹萌生和发展到宏观裂纹形成和碎石的各个阶段的破坏。结果表明:就高含水率的软压裂砂岩而言,在负温度下冻结后强度会大大提高。损害的演变具有局部性,它是一个非线性的实时过程。与整体岩样相似,单轴压缩载荷作用下,冻裂砂岩从破坏到完全破坏的过程可分为四个阶段:线性发展阶段;线性发展阶段。微观裂纹萌生和发展的阶段;损害迅速发展的阶段;达到顶峰之后的加速发展阶段。在单轴压缩的作用下,四个阶段的裂隙岩石的损伤演化速度要比完整岩石快得多。冻结裂缝性岩石新的微裂纹的分裂和最终破坏面的形成与现有预制裂缝的位置和角度密切相关。预制裂缝的存在和几何性质对裂隙岩的扩张性有重要影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号