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Quantifying remaining oil saturation using time-lapse seismic amplitude changes at fluid contacts

机译:使用流体接触处的延时地震振幅变化来量化剩余油饱和度

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Our study shows that time-lapse changes in the amplitude of the seismic reflection at an oil-water contact (OWC) and/or produced OWC can be used to estimate directly the displacement efficiency of water displacing oil, E-D, without the need of a rock and fluid physics model. From this value, it is possible to determine the remaining oil saturation if required. A preliminary application is performed using several published literature examples, which are reinterpreted to assess the average E-D and ensure that the theory is consistent with expectations. Next, a North Sea field model with a known E-D is used to create fluid-flow predictions and the corresponding synthetic time-lapse seismic data. Application to these data again confirms the basic principles of the method and defines the accuracy when applied to 4D seismic data. Finally, an observed 4D seismic dataset from a producing field in the North Sea is analysed. The results suggest a displacement efficiency of between 21 and 65 with an accuracy of 3 due to data non-repeatability (with a NRMS of between 11 and 13). Given an average irreducible water saturation of 0.32, this calculates the remaining oil saturations at between 24 and 53 for this field. A prerequisite for use of the proposed OWC approach is that a discrete contact be interpreted on either the 3D or 4D seismic datasets. Therefore, successful application of this technique requires moderate- to high-quality seismic data and a fairly thick reservoir sequence without significant structural complexity.
机译:我们的研究表明,油水接触处地震反射振幅的延时变化(OWC)和/或产生的OWC可用于直接估计水置换油的驱替效率E-D,而无需岩石和流体物理模型。如果需要,可以根据该值确定剩余油饱和度。使用几个已发表的文献示例进行初步应用,重新解释这些示例以评估平均 E-D 并确保理论与预期一致。接下来,使用具有已知 E-D 的北海场模型来创建流体流动预测和相应的合成延时地震数据。对这些数据的应用再次证实了该方法的基本原理,并定义了应用于四维地震数据时的精度。最后,分析了来自北海生产油田的观测到的四维地震数据集。结果表明,由于数据不可重复性(NRMS在11%至13%之间),位移效率在21%至65%之间,精度为3%。假设平均不可还原水饱和度为0.32,则计算出该油田的剩余油饱和度在24%至53%之间。使用所提出的 OWC 方法的先决条件是在 3D 或 4D 地震数据集上解释离散接触。因此,该技术的成功应用需要中等到高质量的地震数据和相当厚的储层序列,而没有明显的结构复杂性。

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