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An Experimental Investigation of Shale Osmotic Behavior on Geomechanical Property Alterations under Triaxial Stress State

机译:三轴应力状态下石岩渗透性对地质力学性能改变的实验研究

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Shale formations containing above a critical amount of clay present significant rock-fluid interactions that affect drilling, completion, stimulation, production and economic viability of the operations. Correlating the impacts of generated osmotic potential and physico-chemical effects to formation mechanical properties and strength will provide better efficiency in the shale field developments and production optimization. In this paper, we aim to minimize the uncertainties surrounding the structural changes observed with the osmotic pressure by conducting precisely controlled coupled measurements of membrane efficiency, permeability, dynamic and static Young’s moduli, and shear strength under triaxial stress state with elevated pore pressures up to 4000 psi. The results indicate that osmotic membrane efficiency increases from 16.5% to 30.3% due to shale structural changes associated with the increase in effective stress and changing salinity of the pore fluid.
机译:含有高于临界量的粘土的页岩形成具有影响钻井,完成,刺激,生产和经济可行性的显着岩石流体相互作用。 将产生的渗透潜力和物理化学效应的影响与地层机械性能和强度的影响相关性,在页岩现场发育和生产优化中会提供更好的效率。 在本文中,我们的目的是通过在三轴应力状态下进行精确控制的膜效率,渗透率,动态和静初的模育和剪切强度,使三轴应力状态下的膜效率,渗透率,动态和静态杨氏模数和剪切强度升高至孔压力 4000 psi。 结果表明,由于与孔隙流体的有效应力增加相关的页岩结构变化,渗透膜效率从16.5%增加到30.3%。

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