注水煤不同尺度结构的分形特征及其对动态水迁移的控制机制

Fractals Pub Date : 2023-11-15 DOI:10.1142/s0218348x2350130x
Zhenguo Liu, Zehan Yu, He Yang, Muyao Zhu, Shuyang Sun, Meiru Yao, Shuai Dong, Zheng Li
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引用次数: 0

摘要

阐明注水煤层结构对动态输水的控制机理是提高预湿降尘效果的基础。利用核磁共振实验系统,我们模拟了真实的注水煤层条件。获得了注水煤层的真实力学环境和不同尺度孔隙结构的[公式:见正文]谱曲线,实现了液体渗透率的精细测量,提出了结合曲折分形维度算法的比表面积分形维度计算方法,划分了微孔和中大孔,明确了结构孔隙率、比表面积、曲折度和渗透率之间的定量关系,研究了结构特征对动态输水过程的控制机理。结果表明,在不同的力学环境下,微小孔隙比表面积的分形维数接近 2,而中大孔隙比表面积的分形维数接近 3,前者的分形维数增加更为明显,表明中大孔隙比微小孔隙更容易被压缩。在这种情况下,孔径分布的复杂性增加。此外,中大孔隙比微小孔隙的迂回度分形维数增加更多,这表明水力重构过程在大尺度上更为明显。根据结构孔隙度、比表面积、迂回度和渗透率之间的定量关系,中大孔隙控制了大柳塔煤矿煤体大部分的动态水迁移,而整个孔隙尺寸范围对庐陵煤矿煤体的动态水迁移具有重要影响。我们的研究结果为开发难渗透煤层的水力渗透技术提供了坚实的科学依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
FRACTAL CHARACTERISTICS OF DIFFERENT-SCALE STRUCTURES IN WATER INJECTION COAL AND THEIR CONTROL MECHANISM ON DYNAMIC WATER MIGRATION
Clarifying the control mechanism of structures in water injection coal on dynamic water transport is fundamental for improving the effect of pre-wetting and dust reduction. Using nuclear magnetic resonance experimental system, we simulated realistic water injection coal seam conditions. We obtained the real mechanical environment of water injection coal seam, the [Formula: see text] spectrum curves of the pore structure at different scales, realized a fine measurement of liquid permeability, proposed a method for calculating the fractal dimension of the specific surface area which combined a tortuosity fractal dimension algorithm, delineated micro-holes and medium–large holes, clarified the quantitative relationships between the structural porosity, the specific surface area, tortuosity, and permeability, and investigated the control mechanism of structural characteristics on the dynamic water transport process. The results showed that, under different mechanical environments, the fractal dimension of the specific surface area of micro–small pores was close to 2, while that of medium–large pores was close to 3. The former fractal dimension increased more obviously, indicating that medium–large pores are more easily compressed than micro–small ones. Under such conditions, the complexity of pore size distribution increased. Additionally, the fractal dimension increase of tortuosity was higher for medium–large pores than for micro–small pores, indicating that the hydraulic reconstruction process was more obvious at a large scale. According to the quantitative relationship between structural porosity, the specific surface area, tortuosity, and permeability, medium–large pores control most of the dynamic water migration in the coal bodies of Daliuta Coal Mine, while the whole pore size range has an important influence on dynamic water migration in the coal bodies of Luling Coal Mine. Our findings provide a solid scientific basis for the development of hydraulic permeability technologies for difficult-to-penetrate coal seams.
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