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A Validated Digital Rock Workflow to Accurately Predict Apparent Permeability in Tight Rocks

机译:经过验证的数字摇滚工作流程,以准确预测紧密岩石的明显渗透性

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Core analysis of tight rocks is a challenging task. In terms of fluid flow analysis, conventional techniques to determine absolute permeability commonly do not match field observations and provide a wide range of results. The low permeability of tight rocks makes the time to perform flow-through experiments impractical. Additionally, fluid flow in tight pores occurs at different flow regimes as determined by the Knudsen number. To calculate the apparent rock permeability, we use a lattice Boltzmann solver that accounts for high Knudsen number effects and validate the results against experimental data. Simulations for a range of Knudsen numbers up to 30 are performed on 3D microtubes for comparison to experiments. Overall, we observe that the apparent permeability can be up to two orders of magnitude higher than Darcy permeability in these cases. With the numerical solver validated for simple geometries, simulations on the complex pore space as obtained from FIB-SEM image stacks of clay rich sands and a shale sample are performed. Simulations on the shale sample with a calcite mineral matrix, kerogen, pores within the kerogen, and intergranular pores, show absolute permeability values of up to an order of magnitude higher than Darcy values. For the tight sands containing significant amounts of illite and chlorite clay between quartz grains, variations in absolute permeability by a factor of 5 were predicted at relevant conditions. While the accuracy of the numerical solver has been demonstrated, some uncertainty is still tied to the accuracy of the pore space representation from FIB-SEM images and subsequent pore structure extraction. Accurate assessment of permeability in unconventional reservoirs is needed for reservoir modeling and simulation and is critically dependent on the Knudsen number, especially for gas flow. Accurate modelling of fluid flow in unconventional reservoirs is essential for proper prediction of drainage patterns, which can impact decision such as well spacing, optimal lateral length, and completions style. The digital rock approach provides a significant amount of data in a very short time but must include high Knudsen number effects to provide reliability in low permeability rocks typical of unconventional reservoirs.
机译:紧身岩石的核心分析是一个具有挑战性的任务。在流体流动分析方面,常规技术以确定绝对渗透性通常不匹配场观察并提供各种结果。紧密岩石的低渗透性使得时间执行流动的实验不切实际。另外,在由knudsen数确定的不同流动状态下发生紧密孔的流体流动。为了计算表观岩石渗透率,我们使用格子Boltzmann求解器来计算高knudsen号效应并验证结果针对实验数据的结果。在3D Microtubes上执行高达30的knudsen编号范围的模拟,以便与实验相比。总体而言,我们观察到在这些情况下,表观渗透率高于达西渗透率的两个数量级。使用验证的数值求解器,用于简单的几何形状,从粘土富砂和页岩样品中获得的复杂孔隙空间模拟。用方解石矿物基质,角膜炎,后孔和晶状体孔的仿真对页岩样品的模拟,显示绝对渗透率,高达达到达锡值的数量级。对于含有大量illite和石英粒之间的亚氯酸盐粘土的紧密砂,在相关条件下预测了绝对渗透率的变化。虽然已经证明了数值求解器的准确性,但是一些不确定性仍然与来自FIB-SEM图像和随后的孔结构提取的孔隙空间表示的准确性相关。储层建模和模拟需要准确地评估非传统储层中的渗透性,并且统治性地依赖于Chaudsen数,特别是对于气流。在非传统水库中的流体流动的精确建模对于正确预测排水模式是必不可少的,这可能会影响诸如间距,最佳横向长度和完井样式的决策。数字岩石方法在很短的时间内提供大量数据,但必须包括高knudsen数效应,以提供典型的非传统水库的低渗透岩石的可靠性。

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