地下煤气化区前缘煤岩渗透率的温度-应力敏感性实验研究

    Experimental study on temperature-stress sensitivity of permeability of coal rock in front of underground coal gasification area

    • 摘要: 地下煤气化(UCG)是一种环保的煤炭资源利用方式,利用效率取决于气体在煤岩中的渗流特征,应力条件下煤岩的渗透特征是UCG高效实施的关键。燃烧区(温度高于500 ℃)煤岩的应力相关渗透率特性已得到广泛研究,针对气化炉前部边缘位置(温度低于500 ℃,煤岩主要发生热解反应)煤岩的渗透特性研究较少,但其显著影响注入井到生产井的气体流动效率。通过测试不同围压下煤岩渗透率随温度(25~500 ℃)的演化规律,基于煤岩渗透率模型研究温度对煤岩渗透率的影响机制。主要结果表明:①煤岩渗透率随温度升高先减小后增大。煤岩渗透率在300 ℃以下显著增大400%,高于300 ℃时增大幅度减弱。②煤岩渗透率的应力敏感性随温度升高而降低,300 ℃时降低幅度达60%。③煤岩样品渗透率具有显著各向异性,且各向异性随着温度升高而增大。水平90°取向煤岩的渗透率是垂向煤岩的4.56倍,且随温度升高增大至6.14倍。④渗透率模型与实验结果的平均误差小于4.3%,随着温度升高基质膨胀对煤岩渗透率的贡献增强而热损伤的贡献率降低。本文研究结果明确了气化前缘煤岩的渗透率演化特征,可为UCG可行性评价及工艺优化提供指导。

       

      Abstract: Underground coal gasification(UCG) is an environmentally friendly way to utilize coal resources, and its utilization efficiency depends on the characteristics of gas seepage in coal rock. Therefore, the permeability characteristics of coal rock under stress conditions are the key to the efficient implementation of UCG. The stress-related permeability characteristics of coal rocks in combustion zone(temperature above 500 ℃) have been extensively studied, while those in gasification zone(temperature below 500 ℃) have been less studied, but they significantly affect the gas flow efficiency from injection well to production well. In this study, the permeability evolution of coal rock with temperature(25-500 ℃) under different confining pressures is tested. The influence mechanism of temperature on the permeability of coal rock is studied based on the permeability model of coal rock. The main results show that: ① the permeability of coal rock decreases first and then increases with the increase of temperature. The permeability of coal rock increases significantly by 400% below 300 ℃, and decreases when it is above 300 ℃. ② The stress sensitivity of coal permeability decreases with increasing temperature. When the temperature is below 300 ℃, the reduction rate is 60%. ③ The permeability of coal rock samples has significant anisotropy, and the anisotropy increases with the increase of temperature. The permeability of horizontal 90° oriented coal rock is 4.56 times that of vertical coal rock, and increases to 6.14 times with the increase of temperature. ④ The average error between the permeability model and the experimental results is less than 4.3%. With the increase of temperature, the contribution of matrix expansion to the permeability of coal rock increases, while the contribution of thermal damage decreases. The research results of this paper clarify the permeability evolution characteristics of coal rock at the gasification front, which can provide guidance for the feasibility evaluation and process control of UCG.

       

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