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Characterising the Dependence of Coal Permeability to Methane Adsorption, Pore Pressure and Stress: Laboratory Testing of Walloon Coals from the Surat Basin

机译:表征煤渗透对甲烷吸附,孔隙压力和应力的依赖性:苏拉特盆地山煤的实验室试验

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This paper discusses a set of laboratory experiments on coal core samples, which seek to understand the changes in coal fracture permeability with varying confining stress, pore pressure and methane adsorption. Currently, no measurements exist to support QGC'sSurat Basin Coal Seam Gas (CSG) development, and therefore themagnitude of change in permeability relative to initial conditions is unknown. The set of experiments described here use a flow apparatus to measure the permeability of coal core samples as a single variable is changed. The ability to control the laboratory test to separate out the different variablesis an improvement on inferring coal permeability variations from well test data, which isaffected by multiple unknown variables at the same time. Four separate experiments have been carried out. The first investigated the impact of higher burial pressures on permeability, a four-fold reduction in permeability was measured with confining pressure increase from 150-750psi. The second replicated the reduction in pore pressure during dewatering the intention was to measure ‘stress-dependent permeability’, a halving of permeability was observed with pore pressure reduction from 220-30psi. The final two experiments used methane gas to investigate the effect of coal shrinkage with changing pore pressure. Under constant stress conditionspermeability halved and under constant volume conditions permeability saw a significant fifteen-fold reduction. Focus on the resulting magnitude of permeability change is more important at the current stage of this study than the absolute permeability change. The magnitude of permeability change can be used assensitivity in numerical simulation studies toassess the impact of pressure dependency of coal permeability and therefore better characterise coal reservoir behaviour and, consequently, improve the accuracy of any forecast derived from the reservoir model.
机译:本文讨论了一套关于煤核样品的实验室实验,该实验实验试图了解煤骨折渗透率的变化,随着不同的限制应激,孔隙压力和甲烷吸附。目前,不存在用于支持QGC'SURAT盆地煤层气(CSG)开发的测量,因此相对于初始条件的渗透性变化的对数是未知的。这里描述的一组实验使用流动装置来测量煤芯样品的渗透性,因为单个变量改变。控制实验室测试的能力将不同的变形性分离出来的改进了从井测试数据推断煤渗透性变化,这同时由多个未知变量感受。已经进行了四个单独的实验。第一次研究了较高的埋地压力对渗透性的影响,测量了渗透性的四倍降低,狭窄的压力增加到150-750psi。第二次复制在脱水期间孔隙压力的降​​低是测量“胁迫依赖性渗透性”,观察到孔隙压力减少的渗透率的一半,从220-30Psi中减少。最后的两种实验使用甲烷气体来研究煤收缩与变化孔隙压力的影响。在恒定胁迫下,耐折射率减半并且在恒定体积条件下,渗透率达到大约十五倍。重点关注所得到的渗透率变化在本研究的当前阶段比绝对渗透率变化更重要。可以使用渗透性变化的大小可以在数值模拟中进行可比性研究,研究煤渗透性的压力依赖性的影响,因此更好地表征煤储层行为,从而提高了储层模型的任何预测的准确性。

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