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Porosity and permeability prediction through forward stratigraphic simulations using GPM? and Petrel?: application in shallow marine depositional settings

机译:孔隙度和渗透率预测通过GPM前向地层模拟预测? 和Petrel?:在浅海沉积设置中的应用

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The forward stratigraphic simulation approach is applied to predict porosity and permeability distribution. Synthetic well logs from the forward stratigraphic model served as secondary data to control porosity and permeability representation in the reservoir model. Building a reservoir model that fits data at different locations comes with high levels of uncertainty. Therefore, it is critical to generate an appropriate stratigraphic framework to guide lithofacies and associated porosity–permeability simulation. The workflow adopted for this task consists of three parts: first, there is simulation of 20 scenarios of sediment transportation and deposition using the geological process modelling (GPM?) software developed by Schlumberger. Secondly, there is an estimation of the extent and proportion of lithofacies units in the stratigraphic model using the property calculator tool in Petrel?. Finally, porosity and permeability values are assigned to corresponding lithofacies units in the forward stratigraphic model to produce a forward stratigraphic-based porosity and permeability model. Results show a forward stratigraphic-based lithofacies model, which depends on sediment diffusion rate, sea-level variation, sediment movement, wave processes, and tectonic events. This observation is consistent with the natural occurrence, where variations in sea level, sediment supply, and accommodation control stratigraphic sequences and therefore facies distribution in a geological basin. Validation wells VP1 and VP2 showed a notable match after a comparing the original and forward stratigraphic-based porosity models. However, a significant discrepancy is recorded in the permeability estimates. These results suggest that the forward stratigraphic modelling approach can be a practical addition to geostatistical-based workflows for realistic prediction of porosity and permeability.
机译:前向地层仿真方法应用于预测孔隙率和渗透性分布。来自前向地层模型的合成阱日志作为辅助数据,以控制储层模型中的孔隙度和渗透性表示。建立一个符合不同地点数据的水库模型,具有高水平的不确定性。因此,产生适当的地层框架以引导岩散和相关孔隙率渗透性模拟至关重要。本任务采用的工作流程由三部分组成:首先,使用SCHlumberger开发的地质过程建模(GPM?)软件,模拟了20个沉积物运输和沉积的沉积。其次,使用Petrel中的物业计算器工具估计地层模型中的岩石缩略图单位的程度和比例Δ.最后,将孔隙率和渗透率值分配给前向地层模型中的相应岩散单元,以产生前向地层基孔隙率和渗透性模型。结果表明,正向地层基锂外模型,取决于沉积物扩散速率,海平面变化,泥沙运动,波条工艺和构造事件。该观察结果与自然发生,其中海平面,沉积物供应和容纳控制地层序列的变化,因此相片分布在地质盆地。验证Wells VP1和VP2在比较原始的基于地层的孔隙率模型后显示出一个值得注意的匹配。然而,在渗透率估计中记录了显着的差异。这些结果表明,前锋地层建模方法可以是对基于地统计学的工作流程的实际补充,以便现实地预测孔隙率和渗透性。

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