{"title":"基于 FIB/SEM 的 Tamusu 泥岩孔隙特征描述","authors":"H. Yu, D. Yang, Y. Song, J. Huang, X. Qiu","doi":"10.1680/jgele.23.00101","DOIUrl":null,"url":null,"abstract":"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.","PeriodicalId":501470,"journal":{"name":"Géotechnique Letters","volume":"8 11","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Pore space characterization of Tamusu mudstone based on FIB/SEM\",\"authors\":\"H. Yu, D. Yang, Y. Song, J. Huang, X. Qiu\",\"doi\":\"10.1680/jgele.23.00101\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"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.\",\"PeriodicalId\":501470,\"journal\":{\"name\":\"Géotechnique Letters\",\"volume\":\"8 11\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Géotechnique Letters\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1680/jgele.23.00101\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Géotechnique Letters","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1680/jgele.23.00101","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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.