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泥页岩井壁稳定流固化耦合模型

     

摘要

A fluid-solid-chemistry coupling model is built considering fluid flow and ion transmission induced by shale-drilling fluid system electrochemical potential osmosis, nonlinearity of flow and solute diffusion in shale-drilling fluid system, and solid deformation resulted from fluid flow and ion transmission. The model is used to compute the time-varying pore pressure, stress and damage index in formations around the wellbore of a well. The result shows that the pore pressure and stress are lower without consideration of the diffusion potential induced by ion selective character of shale membrane. The linear model overestimates the pore pressure and stress fields around the sidewall. The damage index reveals that collapse first occurs in formations near the wellbore, the caving pressure increases and changes obviously with time, the fracture pressure reduces but doesn't change significantly with time, and the drilling fluid density window narrows down with time.%考虑泥页岩-钻井液体系电化势渗透产生的流体流动和离子运移、泥页岩-钻井液体系中流体流动和溶质扩散过程的非线性、流体流动和离子运移对固体变形的影响,建立泥页岩井壁稳定流-固-化耦合模型.应用建立的模型计算实例井井眼周围地层随时间变化的孔隙压力、应力以及破坏指数.结果表明,若不考虑泥页岩膜离子选择性形成的扩散电势,计算的孔隙压力和应力偏小,而线性模型过高地预测了井壁周围的孔隙压力场和应力场.根据破坏指数可以看出,坍塌破坏首先发生在井壁附近地层,坍塌压力随时间延长增大且变化较明显,破裂压力随时间延长减小但变化不显著,钻井液密度窗口随时间变窄.

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