Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang Formation

Abstract The micromechanical properties of organic matter (OM) and organic pore structures in the over-mature stage are crucial for determining shale reservoir quality and assessing shale gas resource potential. However, there is still debate about the influence of micromechanical properties of OM o...

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Main Authors: Hang Lei, Wenjibin Sun, Yujun Zuo, Zhonghu Wu, Qichi Dai, Wei Lv, Yueqin Li, Xionggang Xie
Format: Article
Language:English
Published: Nature Portfolio 2025-02-01
Series:Scientific Reports
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Online Access:https://doi.org/10.1038/s41598-025-89164-0
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author Hang Lei
Wenjibin Sun
Yujun Zuo
Zhonghu Wu
Qichi Dai
Wei Lv
Yueqin Li
Xionggang Xie
author_facet Hang Lei
Wenjibin Sun
Yujun Zuo
Zhonghu Wu
Qichi Dai
Wei Lv
Yueqin Li
Xionggang Xie
author_sort Hang Lei
collection DOAJ
description Abstract The micromechanical properties of organic matter (OM) and organic pore structures in the over-mature stage are crucial for determining shale reservoir quality and assessing shale gas resource potential. However, there is still debate about the influence of micromechanical properties of OM on the micro-mesopore structures in over-mature shale. In this study, shale cores from the Niutitang Formation have been specifically chosen for OM isolation, adsorption testing, atomic force microscopy examination, and focused ion beam scanning electron microscopy (FIB-SEM) analysis to assess the micromechanical properties of OM and pore structures. The findings indicate that organic micropores and mesopores predominantly exhibit elliptical, circular, or irregular shapes. Organic pores mainly provide pore volume (PV) and specific surface area (SSA) of shale. In the over-mature stage, residual kerogen and pyrobitumen transition towards a graphite structure, increasing Young’s modulus of OM. Additionally, as thermal maturity increases, the absence of a rigid mineral framework and pore fluid pressure results in the compaction of pores, leading to a decrease in PV and SSA. The organic micropores are more vulnerable to collapse and compaction because of the increased brittleness of OM. The organic micropores and mesopores gradually evolve from regular circular and elliptical shapes to irregular shapes during the over-mature stage. The research findings provide valuable insights into the micromechanical mechanism of pore evolution in over-mature marine shale within complex structural regions.
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spelling doaj-art-00110ae9378b463cb2c43c910b59ab5a2025-02-09T12:36:01ZengNature PortfolioScientific Reports2045-23222025-02-0115111910.1038/s41598-025-89164-0Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang FormationHang Lei0Wenjibin Sun1Yujun Zuo2Zhonghu Wu3Qichi Dai4Wei Lv5Yueqin Li6Xionggang Xie7Mining College, Guizhou UniversityMining College, Guizhou UniversityMining College, Guizhou UniversityCollege of Civil Engineering, Guizhou UniversityMining College, Guizhou UniversityMining College, Guizhou UniversityMining College, Guizhou UniversityMining College, Guizhou UniversityAbstract The micromechanical properties of organic matter (OM) and organic pore structures in the over-mature stage are crucial for determining shale reservoir quality and assessing shale gas resource potential. However, there is still debate about the influence of micromechanical properties of OM on the micro-mesopore structures in over-mature shale. In this study, shale cores from the Niutitang Formation have been specifically chosen for OM isolation, adsorption testing, atomic force microscopy examination, and focused ion beam scanning electron microscopy (FIB-SEM) analysis to assess the micromechanical properties of OM and pore structures. The findings indicate that organic micropores and mesopores predominantly exhibit elliptical, circular, or irregular shapes. Organic pores mainly provide pore volume (PV) and specific surface area (SSA) of shale. In the over-mature stage, residual kerogen and pyrobitumen transition towards a graphite structure, increasing Young’s modulus of OM. Additionally, as thermal maturity increases, the absence of a rigid mineral framework and pore fluid pressure results in the compaction of pores, leading to a decrease in PV and SSA. The organic micropores are more vulnerable to collapse and compaction because of the increased brittleness of OM. The organic micropores and mesopores gradually evolve from regular circular and elliptical shapes to irregular shapes during the over-mature stage. The research findings provide valuable insights into the micromechanical mechanism of pore evolution in over-mature marine shale within complex structural regions.https://doi.org/10.1038/s41598-025-89164-0Micromechanical propertiesOrganic matterOver-mature stagePore structures
spellingShingle Hang Lei
Wenjibin Sun
Yujun Zuo
Zhonghu Wu
Qichi Dai
Wei Lv
Yueqin Li
Xionggang Xie
Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang Formation
Scientific Reports
Micromechanical properties
Organic matter
Over-mature stage
Pore structures
title Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang Formation
title_full Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang Formation
title_fullStr Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang Formation
title_full_unstemmed Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang Formation
title_short Impact of micromechanical properties of organic matter on the micro-mesopore structures of the over-mature shale in the Niutitang Formation
title_sort impact of micromechanical properties of organic matter on the micro mesopore structures of the over mature shale in the niutitang formation
topic Micromechanical properties
Organic matter
Over-mature stage
Pore structures
url https://doi.org/10.1038/s41598-025-89164-0
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