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Damage Evolution of Rocks under Triaxial Compressions: An NMR Investigation

机译:三轴压缩作用下岩石的损伤演化:NMR研究

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摘要

To investigate the damage characteristics of rocks subjected to triaxial compression, marble specimens were prepared and subjected to varying levels of axial compressions with identical confining of 20 MPa. The loaded specimens were then tested using Nuclear Magnetic Resonance (NMR) technique to obtain their micro NMR parameters. The changes in transverse surface relaxation time (T-2) distribution, peak area, porosity and microcracks structure distribution of the specimens due to varying compression ratios were systematically analysed. It is found that with the increase of the axial compression, the size and the number of the microcracks, porosity and the peak area increase, indicating that severer damage is induced at high compression ratio. The proportion of the large microcracks area to the total T-2 area exceeds 96% in spite of the increase in compression ratio, indicating that the large microcracks dominate the degradation of the specimen. Based on the Magnetic Resonance (MR) images, the variation of the microcracks distribution can be visually presented under the different compression loadings. The NMR method presented in this study shows a good way of identifying meso-damage evolution characteristics of rock.
机译:为了研究受到三轴压缩的岩石的损伤特性,制备了大理石试样,并在相同的20 MPa限制下经受了不同水平的轴向压缩。然后,使用核磁共振(NMR)技术对加载的样品进行测试,以获得其微NMR参数。系统分析了由于压缩比的变化而引起的试样的横向弛豫时间(T-2)分布,峰面积,孔隙率和微裂纹结构分布的变化。发现随着轴向压缩的增加,微裂纹的尺寸和数量,孔隙率和峰面积增加,表明在高压缩比下引起更严重的破坏。尽管压缩比增加,但大的微裂纹面积占总T-2面积的比例仍超过96%,这表明大的微裂纹占样品降解的主导地位。基于磁共振(MR)图像,可以在不同的压缩载荷下直观地显示微裂纹分布的变化。这项研究中提出的NMR方法显示了一种识别岩石细观破坏演化特征的好方法。

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