变压注水环境下煤体孔隙动态演化规律研究

Study on the dynamic evolution of coal pore under variable pressure water injection environment

  • 摘要: 为深入分析煤层注水过程中不同注水压力及围压对煤体初始孔隙结构的影响,提高煤层注水技术在降尘和防突方面的应用效果,以新桥煤矿二2煤层煤样为研究对象,基于低场核磁共振设备及配套的液体注入、高温高压循环实验系统,开展固定注水压力与固定围压、变化注水压力与固定围压及变化围压3种条件下煤体注水实验,从孔径分布、孔隙度和孔隙体积角度分析煤体孔隙的动态演化过程。结果表明,煤体初始孔隙T2谱图测试结果呈现三峰结构,在煤体初始孔隙中,微小孔的比例最大,其次是中孔,大孔最少;在注水压力与围压的影响下,煤体孔隙在注水过程中呈现动态变化的特性,压力水主要通过扩大煤体初始孔隙、增加孔隙数量和形成新的孔隙来影响煤孔隙,新形成的孔隙半径在0.19×105~1.62×105 nm内;水分的注入会增加各类型孔隙度和孔隙体积,其中大孔孔隙度平均增幅达到106.31%,平均孔隙体积增加262.08×10−3 cm3,增幅最大;其次为小孔和中孔,孔隙度分别增幅8.13%和9.83%,孔隙体积分别增加69.68×10−3 cm3和61.93×10−3 cm3;微孔孔隙度平均增幅为5.42%,平均孔隙体积增加57.30×10−3 cm3,增幅最小,同时增大注水压力可以有效缩短注水时间;变化注水压力与固定注水压力条件下孔隙演化规律类似,当注水压力达到11 MPa时出现大孔突增现象;围压主要通过压缩微孔和小孔来影响煤体孔隙,降幅分别为29.18%和28.66%。

     

    Abstract: The effects of different water injection pressures and confining pressures on the initial pore structure of coal during the water injection process in coal seams are investigated to improve the application effects of water injection technology in dust reduction and outburst prevention. Coal samples from the 2-2 coal seam of Xinqiao Coal Mine are studied based on the low-field nuclear magnetic resonance equipment and the supporting liquid injection and high temperature and pressure circulation experimental system. Water injection experiments on coal samples under three conditions: fixed water injection pressure and fixed confining pressure, variable water injection pressure and fixed confining pressure, and variable confining pressure, are carried out. The dynamic evolution process of coal pore size distribution, porosity and pore volume is analyzed. The results show that the initial pore T2 spectrum of coal samples presents a three-peak structure, with micropores having the largest proportion, followed by mesopores and macropores. Under the influence of water injection pressure and confining pressure, the coal pores show dynamic changes during the water injection process. Pressure water mainly affects the coal pore by expanding the initial pore of the coal body, increasing the number of pores and forming new pores. The radius of the newly formed pores ranges from 0.19×105−1.62×105 nm. The injection of water increases the porosity and pore volume of various types of pores, among which the average increase of macropore porosity reaches 106.31%, and the average pore volume increases by 262.08×10−3 cm3, which is the largest increase. The average increase of micropore porosity is 5.42%, and the average pore volume increases by 57.30×10−3 cm3, which is the smallest increase. The porosity and pore volume of mesopores and small pores also increase, with the porosity increasing by 8.13% and 9.83%, and the pore volume increasing by 69.68×10−3 cm3 and 61.93×10−3 cm3, respectively. At the same time, increasing the water injection pressure can effectively shorten the water injection time. The pore evolution law under variable water injection pressure and fixed water injection pressure conditions is similar, and a sudden increase of macropores occurs when the water injection pressure reaches 11 MPa. The confining pressure mainly affects the coal pores by compressing the micropores and small pores, with a decrease of 29.18% and 28.66%, respectively.

     

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