Effects of natural micro-fracture morphology, temperature and pressure on fluid flow in coals through fractal theory combined with lattice Boltzmann method

FUEL

卷:286

Article

Li, Qian^1,2  Liu, Dameng^1,2  Cai, Yidong^1,2  Zhao, Bo³  Lu, Yuejian^1,2  Zhou, Yingfang⁴ 

[1] China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China

[2] China Univ Geosci, Coal Reservoir Lab Natl Engn Res Ctr CBM Dev & Ut, Beijing 100083, Peoples R China

[3] China Univ Geosci, Sch Water Resources & Environm, Beijing 100083, Peoples R China

[4] Univ Aberdeen, Sch Engn, Kings Coll, Fraser Noble Bldg, Aberdeen AB24 3UE, Scotland

关键词: Coal;    Micro-fractures morphology;    Permeability;    Fractal theory;    Lattice Boltzmann method;   

DOI  :  10.1016/j.fuel.2020.119468

来源: Elsevier

【 摘 要 】

The fluid flow behaviors during the production of coalbed methane (CBM) are generally restricted by the preexisting natural fractures in coal seams. To better understand the effect of natural micro-fracture morphology on the flow capability, nine coals collected from Ordos Basin were subjected to optical microscope observations to obtain micro-fractures morphology. And then, the box-counting method (BCM) was used to quantify the complexity of the micro-fracture network planar distribution. Besides, the lattice Boltzmann method (LBM) was adopted to simulate the flow in the complex micro-fracture network under different pressures and temperatures. Finally, factors affecting the flow capability in micro-fracture were elaborated. The results show that the micro fractures generally present dendritic, reticular, filamentous and orthogonal structures. The natural micro-fracture morphology has a remarkable impact on flow behavior, in which the presence of dominant channels with a length of similar to 498.26 mu m and a width of similar to 10.96 mu m has a significant contribution to permeability, while the orthogonal micro-fracture network normally is not conducive to fluid flow. The fractal dimension extracted from the nine coals varies from 1.321 to 1.584, and the permeability calculated from LBM method varies from 0.147 to 0.345 D; in contrast to other studies, a non-monotonic change, an inverted U-shaped, of permeability on fractal dimension was observed. Moreover, permeability decreases as pressure increases and increases with increasing temperature due to the physical properties of methane and coal matrix. Therefore, this work may contribute to understanding the process of hydrofracturing and hydrothermal methods for improving CBM reservoirs during enhancing CBM recovery.

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