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    煤层及其顶、底板岩石力学性质对水力压裂裂缝延伸的控制

    Control of mechanical properties of coal seam and its roof and floor rocks over the crack extension during hydraulic fracturing

    • 摘要: 为了揭示煤层及其顶、底板岩石力学性质对水力压裂裂缝延伸的影响,应用岩石三轴伺服机测试陕西韩城地区煤层及顶、底板岩石力学性质,总结不同类型岩石力学性质特征和差异; 剖析孔隙率和含水率与岩石力学性质之间的关系,探讨岩石力学性质差异对煤层水力压裂的影响。研究表明:岩石强度随孔隙度增大而降低; 岩石矿物成分及其胶结程度与孔隙度决定岩石的软化程度,水分对不同类型岩石强度的影响方式和程度差异较大; 当煤层埋藏较浅,煤层与顶、底板岩石的弹性模量存在较大差异时,水力压裂裂缝更易控制在煤层中,且延伸更长更远。

       

      Abstract: In order to reveal the influence of mechanical properties of coal seam and its roof and floor rocks on crack extension during hydraulic fracturing, rock three-axis stress was used to test rock mechanical properties of various coal seams and their roof, floor rocks in the Hancheng area, Shaanxi Province. Characteristics and differences of mechanical properties of various rocks are summarized in this study. Through analyzing the relationships between porosity and water content, we explored influences of the differences of mechanical properties on fracture extension. The testing results show that rock strength decreases with increasing porosity, rock softening property depends on mineral compositions and rock porosity, and water contents greatly affect the strength of various rocks in different ways. For a shallowly-buried coal seam, roof and floor rocks of which have significant differences in elastic modulus, hydraulic cracking can be easily restricted within coal seam but extends much further.

       

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