Zhuo Gong, Shangbin Chen, Hubert Ishimwe, Shaojie Zhang, Jamil Khan, Yang Wang, Xiong Sun
{"title":"基于原子力显微镜的页岩中矿物和有机物微观力学性能研究","authors":"Zhuo Gong, Shangbin Chen, Hubert Ishimwe, Shaojie Zhang, Jamil Khan, Yang Wang, Xiong Sun","doi":"10.1306/11152322060","DOIUrl":null,"url":null,"abstract":"The micromechanical properties of shale are crucial for the modeling and prediction of its macromechanical properties. However, the elastic properties have not been comprehensively understood at nano- and microscales. In the present study, the mechanics-component mapping and logarithm filtering methods are proposed to overcome the defect of atomic force microscopy in identifying shale components to investigate the micromechanical properties of shale. Microscopically, the elasticity of shale is heterogeneous. Heterogeneous elastic characteristics of dolomite and quartz are caused by crystal structure anisotropy, isomorphism, and lattice defects. The anisotropy of crystal structure dominates the variation of Young’s modulus of dolomite and quartz. The Young’s modulus of framboidal pyrite depends greatly on its crystal evolution. The heterogeneous elasticity of organic matter is caused by the disordered molecular structure, the maturity variation, and the mixing of different organic macerals. Because of the difference in Young’s modulus among minerals, the metasomatism of feldspar by calcite, quartz, and clay minerals alters the micromechanical properties of shale. Our study reveals that mineral crystal structure characteristics, diagenesis, and organic petrological factors control the mechanical properties of shale microscopically.","PeriodicalId":7124,"journal":{"name":"AAPG Bulletin","volume":"170 1","pages":""},"PeriodicalIF":2.7000,"publicationDate":"2024-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Study on microscale mechanical properties of minerals and organic matter in shale based on atomic force microscopy\",\"authors\":\"Zhuo Gong, Shangbin Chen, Hubert Ishimwe, Shaojie Zhang, Jamil Khan, Yang Wang, Xiong Sun\",\"doi\":\"10.1306/11152322060\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The micromechanical properties of shale are crucial for the modeling and prediction of its macromechanical properties. However, the elastic properties have not been comprehensively understood at nano- and microscales. In the present study, the mechanics-component mapping and logarithm filtering methods are proposed to overcome the defect of atomic force microscopy in identifying shale components to investigate the micromechanical properties of shale. Microscopically, the elasticity of shale is heterogeneous. Heterogeneous elastic characteristics of dolomite and quartz are caused by crystal structure anisotropy, isomorphism, and lattice defects. The anisotropy of crystal structure dominates the variation of Young’s modulus of dolomite and quartz. The Young’s modulus of framboidal pyrite depends greatly on its crystal evolution. The heterogeneous elasticity of organic matter is caused by the disordered molecular structure, the maturity variation, and the mixing of different organic macerals. Because of the difference in Young’s modulus among minerals, the metasomatism of feldspar by calcite, quartz, and clay minerals alters the micromechanical properties of shale. Our study reveals that mineral crystal structure characteristics, diagenesis, and organic petrological factors control the mechanical properties of shale microscopically.\",\"PeriodicalId\":7124,\"journal\":{\"name\":\"AAPG Bulletin\",\"volume\":\"170 1\",\"pages\":\"\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2024-03-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"AAPG Bulletin\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1306/11152322060\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"AAPG Bulletin","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1306/11152322060","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Study on microscale mechanical properties of minerals and organic matter in shale based on atomic force microscopy
The micromechanical properties of shale are crucial for the modeling and prediction of its macromechanical properties. However, the elastic properties have not been comprehensively understood at nano- and microscales. In the present study, the mechanics-component mapping and logarithm filtering methods are proposed to overcome the defect of atomic force microscopy in identifying shale components to investigate the micromechanical properties of shale. Microscopically, the elasticity of shale is heterogeneous. Heterogeneous elastic characteristics of dolomite and quartz are caused by crystal structure anisotropy, isomorphism, and lattice defects. The anisotropy of crystal structure dominates the variation of Young’s modulus of dolomite and quartz. The Young’s modulus of framboidal pyrite depends greatly on its crystal evolution. The heterogeneous elasticity of organic matter is caused by the disordered molecular structure, the maturity variation, and the mixing of different organic macerals. Because of the difference in Young’s modulus among minerals, the metasomatism of feldspar by calcite, quartz, and clay minerals alters the micromechanical properties of shale. Our study reveals that mineral crystal structure characteristics, diagenesis, and organic petrological factors control the mechanical properties of shale microscopically.
期刊介绍:
While the 21st-century AAPG Bulletin has undergone some changes since 1917, enlarging to 8 ½ x 11” size to incorporate more material and being published digitally as well as in print, it continues to adhere to the primary purpose of the organization, which is to advance the science of geology especially as it relates to petroleum, natural gas, other subsurface fluids, and mineral resources.
Delivered digitally or in print monthly to each AAPG Member as a part of membership dues, the AAPG Bulletin is one of the most respected, peer-reviewed technical journals in existence, with recent issues containing papers focused on such topics as the Middle East, channel detection, China, permeability, subseismic fault prediction, the U.S., and Africa.