基于 FIB/SEM 的 Tamusu 泥岩孔隙特征描述

H. Yu, D. Yang, Y. Song, J. Huang, X. Qiu
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引用次数: 0

摘要

本研究采用聚焦离子束/扫描电子显微镜(FIB/SEM)技术,对中国首选的核废料处置承载介质--玉笥泥岩的孔隙空间进行了表征。研究在中观尺度上进行,样品体积为 7.96 × 9.16 × 10.00 μm3,体素尺寸为 5 × 5 × 10 nm3。研究结果表明,Tamusu 泥岩中的孔隙主要存在于纳米尺度,通常在其矿物基质内或与非多孔矿物的界面处。在 FIB/SEM 扫描的尺度上,Tamusu 泥岩的孔隙空间主要是无连接的,分析孔隙率约为 3.5%。试样内的孔隙特征在 6 ∼ 8 μm 的方框尺寸内表现出相对的一致性。此外,Tamusu 泥岩中的孔隙路径在基底面内表现出优先取向,表明孔隙空间存在各向异性,这可能是由于孔隙路径取向和迂回度的变化造成的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Pore space characterization of Tamusu mudstone based on FIB/SEM
This study focuses on characterizing the pore space in Tamusu mudstone, a preferred nuclear waste disposal host medium in China, using Focused Ion Beam/Scanning Electron Microscopy (FIB/SEM). The investigation is conducted at the mesoscale, with a sample volume of 7.96 × 9.16 × 10.00 μm3 and voxel sizes of 5 × 5 × 10 nm3. The findings reveal that the pores in Tamusu mudstone primarily exist at the nanoscale, typically within its mineral matrix or at interfaces with non-porous minerals. At the FIB/SEM-imaged scale, the pore space in the Tamusu mudstone is mainly unconnected, with an analyzed porosity of approximately 3.5%. Pore characteristics within the specimen exhibit relative consistency within a box size of 6∼8 μm. Furthermore, the pore paths in Tamusu mudstone exhibit a preferred orientation within the bedding plane, suggesting anisotropy in pore space, possibly attributed to changes in pore path orientation and tortuosity.
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