Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeability

The apertures of cleats and micro-fractures in coal play an important role in the permeability of the coal bed. In this study, optical microscopy and scanning electron microscopy were used to investigate the morphology of cleats and micro-fractures and their apertures, distribution of minerals, and...

Full description

Bibliographic Details
Main Authors: Qiang Huang, Zhigang Du, Hewu Liu, Qinghe Niu, Huihuang Fang, Jinyang Yang, Minghang Lou
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-01-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.1048042/full
_version_ 1828063354945536000
author Qiang Huang
Zhigang Du
Zhigang Du
Hewu Liu
Qinghe Niu
Huihuang Fang
Jinyang Yang
Minghang Lou
author_facet Qiang Huang
Zhigang Du
Zhigang Du
Hewu Liu
Qinghe Niu
Huihuang Fang
Jinyang Yang
Minghang Lou
author_sort Qiang Huang
collection DOAJ
description The apertures of cleats and micro-fractures in coal play an important role in the permeability of the coal bed. In this study, optical microscopy and scanning electron microscopy were used to investigate the morphology of cleats and micro-fractures and their apertures, distribution of minerals, and matrix/fracture interactions. The neighboring mineralized and unmineralized cleats suggest the possibility of multi-stage evolutionary processes of cleat formation during the coalification process. The micro-fracture distribution of coals is closely related to their components, including organic macerals and inorganic minerals. Micro-fractures are prone to developing at the junction surface of organic macerals or the surface of organic and inorganic minerals. A mineral-genetic micro-fracture can be classified as an intra-crystal micro-fracture, an extra-crystal micro-scale fracture, or a grain-edge micro-scale fracture. Compared with the low- and middle-ranking coals, cleat and micro-scale fractures in high-ranking coal are usually filled with carbonate minerals and clay minerals. Statistical analysis reveals that the aperture distribution of cleat and micro-fracture in coal shows a log-normal distribution. The aperture of cleat and micro-fracture shows a decreasing trend with increase in coal rank. For low-ranking coal, cleats contribute more to the permeability than micro-fractures. However, for the middle- and high-ranking coals, the contribution of cleats and micro-fractures to the coal reservoir permeability will be close. As the rank of coal increases, the degree of cleat contribution to reservoir permeability decreases, while the degree of micro-fracture contributing to the reservoir permeability increases. Possible reasons for the extremely low reservoir permeability in China may be the following: 1) subsurface cleats and micro-fractures close their apertures significantly due to the in situ geo-stress or 2) cleats and micro-fractures have better permeability in the geological history, which makes the precipitation of minerals decrease the coal reservoir permeability. Therefore, the acid solvent (e.g., HAc, HCl, and HF) added to the drilling or hydraulic fracturing fluid or the geo-stress relief technologies may be an effective way of enlarging the cleat or micro-fracture aperture and enhance the reservoir permeability for coalbed methane production.
first_indexed 2024-04-10T22:41:55Z
format Article
id doaj.art-958f1a7c19124000b52a2b5e16451b7c
institution Directory Open Access Journal
issn 2296-6463
language English
last_indexed 2024-04-10T22:41:55Z
publishDate 2023-01-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Earth Science
spelling doaj.art-958f1a7c19124000b52a2b5e16451b7c2023-01-16T04:17:32ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632023-01-011010.3389/feart.2022.10480421048042Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeabilityQiang Huang0Zhigang Du1Zhigang Du2Hewu Liu3Qinghe Niu4Huihuang Fang5Jinyang Yang6Minghang Lou7School of Civil Engineering, Luoyang Institute of Science and Technology, Luoyang, ChinaSchool of Civil Engineering, Luoyang Institute of Science and Technology, Luoyang, ChinaYima Coal Corporation, Henan Energy Group Corporation, Sanmenxia, ChinaSchool of Earth and Environment, Anhui University of Science and Technology, Huainan, ChinaState Key Laboratory of Mechanical Behavior and System Safety of Traffic Engineering Structures, Shijiazhuang Tiedao University, Shijiazhuang, ChinaSchool of Earth and Environment, Anhui University of Science and Technology, Huainan, ChinaSchool of Civil Engineering, Luoyang Institute of Science and Technology, Luoyang, ChinaSchool of Civil Engineering, Luoyang Institute of Science and Technology, Luoyang, ChinaThe apertures of cleats and micro-fractures in coal play an important role in the permeability of the coal bed. In this study, optical microscopy and scanning electron microscopy were used to investigate the morphology of cleats and micro-fractures and their apertures, distribution of minerals, and matrix/fracture interactions. The neighboring mineralized and unmineralized cleats suggest the possibility of multi-stage evolutionary processes of cleat formation during the coalification process. The micro-fracture distribution of coals is closely related to their components, including organic macerals and inorganic minerals. Micro-fractures are prone to developing at the junction surface of organic macerals or the surface of organic and inorganic minerals. A mineral-genetic micro-fracture can be classified as an intra-crystal micro-fracture, an extra-crystal micro-scale fracture, or a grain-edge micro-scale fracture. Compared with the low- and middle-ranking coals, cleat and micro-scale fractures in high-ranking coal are usually filled with carbonate minerals and clay minerals. Statistical analysis reveals that the aperture distribution of cleat and micro-fracture in coal shows a log-normal distribution. The aperture of cleat and micro-fracture shows a decreasing trend with increase in coal rank. For low-ranking coal, cleats contribute more to the permeability than micro-fractures. However, for the middle- and high-ranking coals, the contribution of cleats and micro-fractures to the coal reservoir permeability will be close. As the rank of coal increases, the degree of cleat contribution to reservoir permeability decreases, while the degree of micro-fracture contributing to the reservoir permeability increases. Possible reasons for the extremely low reservoir permeability in China may be the following: 1) subsurface cleats and micro-fractures close their apertures significantly due to the in situ geo-stress or 2) cleats and micro-fractures have better permeability in the geological history, which makes the precipitation of minerals decrease the coal reservoir permeability. Therefore, the acid solvent (e.g., HAc, HCl, and HF) added to the drilling or hydraulic fracturing fluid or the geo-stress relief technologies may be an effective way of enlarging the cleat or micro-fracture aperture and enhance the reservoir permeability for coalbed methane production.https://www.frontiersin.org/articles/10.3389/feart.2022.1048042/fullcoalcleatmicro-fracturepermeabilitystatistical analysis
spellingShingle Qiang Huang
Zhigang Du
Zhigang Du
Hewu Liu
Qinghe Niu
Huihuang Fang
Jinyang Yang
Minghang Lou
Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeability
Frontiers in Earth Science
coal
cleat
micro-fracture
permeability
statistical analysis
title Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeability
title_full Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeability
title_fullStr Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeability
title_full_unstemmed Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeability
title_short Investigation of cleat and micro-fracture and its aperture distribution in the coals of different ranks in North China: Relative to reservoir permeability
title_sort investigation of cleat and micro fracture and its aperture distribution in the coals of different ranks in north china relative to reservoir permeability
topic coal
cleat
micro-fracture
permeability
statistical analysis
url https://www.frontiersin.org/articles/10.3389/feart.2022.1048042/full
work_keys_str_mv AT qianghuang investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability
AT zhigangdu investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability
AT zhigangdu investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability
AT hewuliu investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability
AT qingheniu investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability
AT huihuangfang investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability
AT jinyangyang investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability
AT minghanglou investigationofcleatandmicrofractureanditsaperturedistributioninthecoalsofdifferentranksinnorthchinarelativetoreservoirpermeability