基于AFM-Raman联用的岩屑跨尺度力学特性预测方法

    PREDICTION METHOD FOR CROSS-SCALE MECHANICAL PROPERTIES OF ROCK CUTTINGS BASED ON COMBINED AFM-RAMAN TECHNIQUE

    • 摘要: 针对深地资源钻井过程中岩石力学参数实时精准获取的技术需求,本研究提出了基于原子力显微镜(AFM)与激光拉曼光谱(Raman)联用的岩屑跨尺度力学特性预测方法。以共和盆地花岗闪长岩为研究对象,系统开展了从微观到宏观的跨尺度力学特性分析。采用激光拉曼光谱技术对岩石薄片进行面扫描测试,结合图像处理算法,实现了矿物组成的快速识别与空间分布的定量表征。通过原子力显微镜测试,获取了不同矿物颗粒内部及边界的弹性模量分布,揭示了矿物界面存在显著的力学弱化效应。基于微观测试结果和颗粒流离散元方法,构建了花岗闪长岩矿物尺度数值模型,并开展单轴压缩和直接拉伸加载,成功预测了岩石宏观力学性质,模拟值与试验值吻合良好。微观破坏分析表明,压缩条件下矿物内部拉伸裂纹是主导破坏机制;拉伸条件下主要形成垂直于加载方向的贯穿裂缝。矿物空间分布的随机性对岩石宏观力学性质的影响相对有限。该方法相较于传统测试,无需钻取岩心,具有测试周期短、时效性强等优势,为岩石力学参数的快速获取提供了新的技术途径,有望推动钻井工程评价方式从厘米尺度岩心向毫米尺度岩屑的转变。

       

      Abstract: To meet the technical requirements for real-time and accurate acquisition of rock mechanical parameters during deep resource drilling, this study proposes a cross-scale method for predicting mechanical properties using drilling cuttings, combining atomic force microscopy (AFM) and laser Raman spectroscopy. Using granodiorite from the Gonghe Basin as the research object, a systematic cross-scale mechanical analysis was conducted from the microscopic to macroscopic levels. Laser Raman spectroscopy was employed to perform surface scanning tests on rock thin sections, and together with image processing algorithms, enabled rapid mineral identification and quantitative characterization of spatial distribution. Atomic force microscopy testing provided the elastic modulus distribution within different mineral grains and at their boundaries, revealing significant mechanical weakening effects at mineral interfaces. Based on microscopic test results and the particle flow discrete element method, mineral-scale numerical models of granodiorite were constructed. Uniaxial compression and direct tensile loading simulations were performed, successfully predicting the macroscopic mechanical properties of the rock, with simulated results showing good agreement with experimental values. Microscopic failure analysis indicated that tensile cracks within minerals dominate under compressive conditions, while penetrating cracks perpendicular to the loading direction primarily form under tensile conditions. The randomness of mineral spatial distribution showed relatively limited influence on the macroscopic mechanical properties of the rock. Compared with traditional testing methods, this approach eliminates the need for coring, offers advantages of shorter testing cycles and enhanced timeliness, provides a new technical pathway for rapid acquisition of rock mechanical parameters, and is expected to facilitate the transition of drilling evaluation methods from centimeter-scale cores to millimeter-scale cuttings.

       

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