Factors Influencing Full-Scale Pore–Fracture Heterogeneity in Low-to-Middle Rank Coal Reservoirs: Evidence from the Tarim Basin, Northwest China
- 1State Key Laboratory of Disaster Prevention and Ecology Protection in Open-Pit Coal Mines, Shandong University of Science and Technology, Qingdao 266590, China
- 2Jiangsu Key Laboratory of Carbon Capture, Utilization and Storage, China University of Mining & Technology, Xuzhou 221008, China
Abstract
To investigate the factors of pore–fracture structure heterogeneity in middle rank coal reservoirs, middle rank coal samples collected from the deep coal seams in the northern part of the Kuqa area in the Tarim Basin are analyzed. Firstly, according to the maximum vitrinite reflectance (Ro,max), all the samples are divided into two types, Type A and B (A: Ro,max is larger than 1.2%; B: Ro,max is smaller than 1.2%). Secondly, the full-scale pore–fracture system was characterized using a combination of three experiments: high-pressure mercury intrusion testing, low-temperature CO2 adsorption testing, and low-temperature nitrogen adsorption testing. Subsequently, multifractal theory was applied to evaluate pore structure heterogeneity and investigate its governing factors. The results are as follows: (1) Type A samples exhibit superior micropore development, whereas Type B samples show a higher degree of mesopore and macropore development. Both types of samples display a “bimodal” distribution across the full-scale pore. Type A pore structure is affected by Ro,max and macerals, with mineral components having a minor impact, while Type B is regulated by all three factors. (2) The coal samples exhibit distinct multifractal characteristics. Type A pore structure heterogeneity is higher than that of Type B. This heterogeneity in Type A is dominated by the differences in the development and distribution of small-scale pores (micro- and mesopores), whereas in Type B, it is governed by the full-scale pore system distribution.
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BibTeX
@article{chang2026factors,
title = {{Factors Influencing Full-Scale Pore–Fracture Heterogeneity in Low-to-Middle Rank Coal Reservoirs: Evidence from the Tarim Basin, Northwest China}},
author = {Xiangchun Chang and Hui Zhang and Meng Wang and Mengna Zhou and Junjian Zhang},
journal = {Fractal and Fractional},
year = {2026},
month = oct,
doi = {10.3390/fractalfract10100709},
url = {https://www.mdpi.com/2504-3110/10/10/709},
note = {CC BY 4.0},
}
RIS
TY - JOUR
TI - Factors Influencing Full-Scale Pore–Fracture Heterogeneity in Low-to-Middle Rank Coal Reservoirs: Evidence from the Tarim Basin, Northwest China
AU - Xiangchun Chang
AU - Hui Zhang
AU - Meng Wang
AU - Mengna Zhou
AU - Junjian Zhang
PY - 2026
DA - 2026/10/09
JO - Fractal and Fractional
DO - 10.3390/fractalfract10100709
UR - https://www.mdpi.com/2504-3110/10/10/709
AB - To investigate the factors of pore–fracture structure heterogeneity in middle rank coal reservoirs, middle rank coal samples collected from the deep coal seams in the northern part of the Kuqa area in the Tarim Basin are analyzed. Firstly, according to the maximum vitrinite reflectance (Ro,max), all the samples are divided into two types, Type A and B (A: Ro,max is larger than 1.2%; B: Ro,max is smaller than 1.2%). Secondly, the full-scale pore–fracture system was characterized using a combination of three experiments: high-pressure mercury intrusion testing, low-temperature CO2 adsorption testing, and low-temperature nitrogen adsorption testing. Subsequently, multifractal theory was applied to evaluate pore structure heterogeneity and investigate its governing factors. The results are as follows: (1) Type A samples exhibit superior micropore development, whereas Type B samples show a higher degree of mesopore and macropore development. Both types of samples display a “bimodal” distribution across the full-scale pore. Type A pore structure is affected by Ro,max and macerals, with mineral components having a minor impact, while Type B is regulated by all three factors. (2) The coal samples exhibit distinct multifractal characteristics. Type A pore structure heterogeneity is higher than that of Type B. This heterogeneity in Type A is dominated by the differences in the development and distribution of small-scale pores (micro- and mesopores), whereas in Type B, it is governed by the full-scale pore system distribution.
SN - 2504-3110
ER -