Bhattacharjee Arun J, Lisabeth Harrison P, Parkinson Dilworth, MacDowell Alastair
Energy Geosciences Division, Lawrence Berkeley National Laboratory, 1 Cyclotron Rd, Berkeley, CA 94720, USA.
Advanced Light Source, Lawrence Berkeley National Laboratory, 1 Cyclotron Rd, Berkeley, CA 94720, USA.
J Synchrotron Radiat. 2024 Nov 1;31(Pt 6):1561-1570. doi: 10.1107/S1600577524009305. Epub 2024 Oct 29.
Geological samples are inherently multi-scale. Understanding their bulk physical and chemical properties requires characterization down to the nano-scale. A powerful technique to study the three-dimensional microstructure is X-ray tomography, but it lacks information about the chemistry of samples. To develop a methodology for measuring the multi-scale 3D microstructure of geological samples, correlative X-ray micro- and nanotomography were performed on two rocks followed by scanning electron microscopy with energy-dispersive spectroscopy (SEM-EDS) analysis. The study was performed in five steps: (i) micro X-ray tomography was performed on rock sample cores, (ii) samples for nanotomography were prepared using laser milling, (iii) nanotomography was performed on the milled sub-samples, (iv) samples were mounted and polished for SEM analysis and (v) SEM imaging and compositional mapping was performed on micro and nanotomography samples for complimentary information. Correlative study performed on samples of serpentine and basalt revealed multiscale 3D structures involving both solid mineral phases and pore networks. Significant differences in the volume fraction of pores and mineral phases were also observed dependent on the imaging spatial resolution employed. This highlights the necessity for the application of such a multiscale approach for the characterization of complex aggregates such as rocks. Information acquired from the chemical mapping of different phases was also helpful in segmentation of phases that did not exhibit significant contrast in X-ray imaging. Adoption of the protocol used in this study can be broadly applied to 3D imaging studies being performed at the Advanced Light Source and other user facilities.
地质样品本质上具有多尺度性。了解它们的整体物理和化学性质需要对纳米尺度进行表征。研究三维微观结构的一种强大技术是X射线断层扫描,但它缺乏关于样品化学性质的信息。为了开发一种测量地质样品多尺度三维微观结构的方法,对两块岩石进行了相关的X射线微断层扫描和纳米断层扫描,随后进行了带有能量色散光谱的扫描电子显微镜(SEM-EDS)分析。该研究分五个步骤进行:(i)对岩石样品岩芯进行微X射线断层扫描,(ii)使用激光铣削制备用于纳米断层扫描的样品,(iii)对铣削后的子样品进行纳米断层扫描,(iv)将样品安装并抛光以进行SEM分析,(v)对微断层扫描和纳米断层扫描样品进行SEM成像和成分映射以获取补充信息。对蛇纹石和玄武岩样品进行的相关研究揭示了涉及固体矿物相和孔隙网络的多尺度三维结构。根据所采用的成像空间分辨率,还观察到孔隙和矿物相体积分数的显著差异。这突出了应用这种多尺度方法来表征诸如岩石等复杂聚集体的必要性。从不同相的化学映射中获得的信息也有助于在X射线成像中没有明显对比度的相的分割。采用本研究中使用的方案可广泛应用于在先进光源和其他用户设施进行的三维成像研究。