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Water-Cut Forecasting and Permeability Inversion From Time-Lapse Seismic using a Stream-Line Technique

机译:流线技术从时移地震中进行含水预测和渗透率反演

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In this paper, we describe an algorithm, which predictsrnsaturation development through the a-priori unknownrnpermeability field using the saturation history of the field.rnFurthermore, the algorithm allows estimation of thernunderlying permeability field. The field’s saturation history isrnderived from time-lapse 3-D seismic data. Time-lapse seismicrnis used to monitor the reservoir during production. Assumingrnseismic repeatability, it is possible to couple seismic changesrnto dynamic reservoir properties changes induced byrnproduction. Successive seismic data set give direct informationrnover the speed at which the saturation front propagatesrnthrough the a-priori unknown permeability field. Thernpropagation speed of the saturation front contains usefulrninformation about the fluid flow velocity field in the observedrnmedium. It enables us to forecast the development of thernsaturation contours in time, which is easily translated intornwater-cut profiles. In addition, a relation between the velocityrnmap and desired reservoir parameters (e.g. permeability) canrnbe established using an inversion technique.rnA streamline technique is used to verify that eachrnsimulated saturation contour matches the a-priori knownrncontour it is based on. In a number of test cases we createdrnrandomly exponential correlated heterogeneous permeabilityrnfields. We verified the algorithm by comparing the forecastedrnresults with the real simulated results. A sensitivity analysisrnwas performed to study the number of saturation fronts (i.e.rnrepeat 3D surveys) required to yield reliable results. Thernproposed approach offers the advantage of invertingrnpermeability via a rather simple, but reliable method usingrntime-lapse seismic data.
机译:在本文中,我们描述了一种算法,该算法利用该场的饱和历史来预测先验未知渗透率场的饱和度发展。此外,该算法还可以估算基础渗透率场。该字段的饱和度历史记录是根据延时的3-D地震数据得出的。延时地震记录仪在生产过程中用于监控储层。假设地震可重复性,则有可能将地震变化与生产引起的动态储层物性变化耦合起来。连续的地震数据集给出了有关饱和锋面通过先验未知渗透率场传播的速度的直接信息。饱和前沿的传播速度包含有关被观测介质中流体流速场的有用信息。它使我们能够及时预测饱和度等值线的发展,可以轻松地将其转换为含水切面。另外,可以使用反演技术来建立速度图和期望的储层参数(例如渗透率)之间的关系。流线技术用于验证每个模拟的饱和度轮廓是否与其所基于的先验已知轮廓相匹配。在许多测试案例中,我们创建了随机指数相关的非均质渗透率场。我们通过将预测结果与实际仿真结果进行比较来验证算法。进行了敏感性分析以研究产生可靠结果所需的饱和前沿数量(即rnrepeat 3D测量)。所提出的方法通过使用时移地震数据的相当简单但可靠的方法提供了反渗透性的优点。

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