页岩基质压力相关当量渗透率演化评价:实验与建模

Yun Yang, Shimin Liu, An Liu
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摘要

建模和预测储层衰竭过程中基质渗透率变化的能力对于准确分析非常规气藏(包括页岩气和煤层气储层)的长期生产动态至关重要。然而,由于其复杂的孔隙结构和形态,纳米多孔基质中的流动定量仍然具有挑战性。为了了解压力依赖性基质渗透率演化,本研究使用粉碎样品进行了实验室渗透率测量。根据泥盆系页岩样品的压力衰减剖面估算了等效渗透率。建立了一种新的实验系统——差分体积单元,并应用于页岩样品的瞬态气体流动的精确捕获。页岩渗透率随压力降低总体呈下降趋势。由于滑流和Knudsen扩散的存在,低孔隙压力数据没有遵循页岩样品中高孔隙压力数据所拟合的下降趋势。本研究还利用甲烷作为入侵流体考察了吸附对基质渗透率的影响,由于吸附相在孔隙表面的凝结占据了可用的孔隙空间,因此在不进行吸附校正的情况下,其渗透率可比渗透率低40%。由于这些致密岩石基质由微孔和纳米孔组成,因此基质渗透率主要与孔隙结构(如孔径分布、孔隙度和弯曲度)有关。采用低压氮气吸附法对Marcellus页岩样品的复杂孔隙结构进行表征。提出了一种基于孔隙结构信息的多力学模型来预测压力依赖性基质渗透率,并研究了气体吸附对表观渗透率的影响。该模型成功地将页岩和煤的真实复杂孔隙结构与压力相关基质渗透率联系起来。所提出的模型可以与市售的模拟器相结合,以预测UGRs井的长期生产曲线。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluating the Pressure-Dependent Equivalent Permeability Evolutions for Shale Matrix: Experiments and Modeling
The ability to model and predict matrix permeability changes during reservoir depletion is critical for accurate analysis of long-term production performance in unconventional gas reservoirs (UGRs), including shale gas and coalbed methane reservoirs. Yet, flow quantification in the nanoporous matrix is still challenging due to the complex pore structure and morphology. To understand the pressure-dependent matrix permeability evolution, this study conducted laboratory permeability measurements using pulverized samples. Equivalent permeability was estimated from the pressure decay profile for the Devonian shale sample. A novel experimental system, a differential volumetric unit, has been established and applied to capture the accurate transient gas flows for the shale sample. The measured permeability of shale exhibited overall decreasing trends with pressure depletion. Due to the presence of slip flow and Knudsen diffusion, low-pore-pressure data did not follow the same decline trend fitted by high-pore-pressure data as observed in the shale sample. This study also utilized methane as the invasion fluid to examine the adsorption effect on matrix permeability, whose value could be up to 40% lower than permeability without correction for adsorption because of the condensation of adsorbed phase at pore surface occupying available pore space. Since these tight rock matrixes are composed of micro- and nanopores, matrix permeability is primarily related to pore structure (e.g., the pore size distribution, porosity and tortuosity). Low-pressure N2 adsorption was conducted to characterize the complex pore structure of the Marcellus shale sample. A multimechanic model was proposed to predict the pressure-dependent matrix permeability based on pore structure information and investigate the effect of gas adsorption on apparent permeability. This model has successfully linked the realistic, complex pore structure with the pressure-dependent matrix permeability of shale and coal. The proposed model could be coupled into the commercially available simulator to forecast long-term production profiles for UGRs wells.
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