On the Pressure Response During Unsteady State Fluid Displacement Experiments

M. Mehana, M. Fahes
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Abstract

The pressure response observed during the unsteady state displacement is a critical factor in determining the steady value and contains valuable characteristics about the rock permeability and capillary pressure. Our objective is to elucidate the mechanism of the unsteady state displcment and its impact on the pressure reponse. We tried to match the experimentally-measured pressure profile using both numerical simulation and analytical solutions. Promising results are observed when the capillary pressure is considered. The results clarify that this response is not a function of gas compressibility or viscous fingering, but is directly linked to the ratio of liquid fractional flow to liquid relative permeability as a function of saturation. The relative permeability exponents have a direct role to play in this regard. This work highlights the inacpaibility observed in a reservoir simulator to capture the pressure signature. This brings into question the ability of such simulators to provide reliable data when it comes to model the displacement processes at the core-scale.
非定常流体驱替实验压力响应研究
在非稳态位移过程中观测到的压力响应是确定稳定值的关键因素,它包含了岩石渗透率和毛管压力的有价值特征。我们的目的是阐明非定常位移的机理及其对压力响应的影响。我们尝试使用数值模拟和解析解来匹配实验测量的压力分布。当考虑毛细压力时,得到了令人满意的结果。结果表明,这种响应不是气体可压缩性或粘性指压的函数,而是与液体分数流量与液体相对渗透率之比作为饱和度的函数直接相关。相对渗透率指数在这方面起着直接的作用。这项工作强调了在油藏模拟器中观察到的无法捕获压力特征的问题。当涉及到在核心尺度上模拟位移过程时,这种模拟器提供可靠数据的能力就受到了质疑。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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