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首页> 外文期刊>Acta Geotechnica >Nanochemomechanical assessment of shale: a coupled WDS-indentation analysis
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Nanochemomechanical assessment of shale: a coupled WDS-indentation analysis

机译:页岩的纳米化学力学评估:耦合的WDS压痕分析

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Establishing the links between the composition, microstructure and mechanics of shale continues to be a formidable challenge for the geomechanics community. In this study, a robust methodology is implemented to access the in situ chemomechanics of this sedimentary rock at micrometer length scales. Massive grids of coupled wave dispersive spectroscopy (WDS) and instrumented indentation experiments were performed over representative material surfaces to accommodate the highly heterogeneous composition and microstructure of shale. The extensive datasets of compositional and mechanical properties were analyzed using multi-variate clustering statistics to determine the attributes of active phases present in shale at microscales. Our chemomechanical analysis confirmed that the porous clay (PC) mechanical phase inferred by statistical indentation corresponds to the clay mineral phase defined strictly on chemical grounds. The characteristic stiffness and hardness behaviors of the PC are realized spatially in regions removed from silt inclusions of quartz and feldspar. At the microscale shared by indentation and WDS experiments, a consistent chemomechanical signature for shale emerges in which the heterogeneities of the PC are captured by the standard deviations of indentation properties and concentrations of chemical elements. However, these local behaviors are of second order compared to the global trend observed for mean mechanical properties and the clay packing density, which synthesizes the relative volumes of clay and nanoporosity in the material. The coupled statistical indentation and WDS technique represents a viable approach to characterize the chemomechanics of shale and other natural porous composites at a consistent scale below the macroscopic level.
机译:在页岩的组成,微观结构和力学之间建立联系仍然是地质力学界的巨大挑战。在这项研究中,采用了一种强大的方法来以微米长度尺度访问该沉积岩的原位化学力学。在代表性的材料表面上进行了耦合波色散光谱(WDS)的大型网格和仪器压痕实验,以适应页岩的高度异质组成和微观结构。使用多变量聚类统计分析了广泛的成分和力学性能数据集,以确定微尺度上存在于页岩中的活性相的属性。我们的化学力学分析证实,通过统计压痕推断出的多孔粘土(PC)机械相对应于严格根据化学基础定义的粘土矿物相。 PC的特征刚度和硬度行为在空间上从石英和长石的粉砂夹杂物中去除。在压痕和WDS实验共享的微观尺度上,出现了页岩的一致化学力学特征,其中压痕性质和化学元素浓度的标准偏差捕获了PC的异质性。但是,与观察到的平均力学性能和粘土堆积密度的总体趋势相比,这些局部行为是二阶的,这综合了材料中粘土的相对体积和纳米孔隙度。统计压痕和WDS技术相结合代表了一种可行的方法,可以在宏观水平以下的恒定范围内表征页岩和其他天然多孔复合材料的化学力学。

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