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Scale and Process Dependent Model Errors in Seismic History Matching

机译:地震历程匹配中规模和过程相关的模型误差

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Time-Lapse (4D) seismic data offers spatial and dynamic information about changes in reservoir fluid properties and can be used to constrain flow simulation models thereby improving confidence in the reservoir characterisation and its predicted behaviour. To address this, we have developed a method of quantitatively integrating 4D seismic data in an automated history matching workflow. Appropriately parameterised flow simulations are converted to predictions of 4D signatures by a petro-elastic transform and suitable rescaling before a misfit is calculated by comparison to observed data. Model parameters are then updated using a quasi-global stochastic inversion method. This process is affected by scale and process dependent model errors. Flow simulations are often created such that computer resources are optimised and some level of accuracy is sacrificed. To speed up simulations, some form of upscaling is required to capture two-phase flow properties such as relative permeability but also to represent geological heterogeneity. The upscaling may be over-simplified or ignored. In addition, simplifications to the flow processes may be made, for example by using streamline methods. Finally, the petro-elastic transform contributes to the model errors due to assumptions about saturation distributions and cross-scaling is required because modelled and observed seismic are obtained for different volumes. We present an analysis of the above model errors that occur using a synthetic geo-model based on a North Sea reservoir. We show that the model error depends on the rock physics parameters as well as the underlying geo-model. When the 4D signature is dominated by pressure effects, the model error is negligible in our case. We describe how the model error affects the history matching process due to biasing. The latter results in a best set of model parameters which may be different from that obtained by upscaling while the uncertainty estimator is also changed. We compare the effect of the model error to other errors such as observed data errors. Finally, we describe how the model error is addressed in the misfit calculation to improve the history matching process and reduce the biasing effect.
机译:时移(4D)地震数据可提供有关储层流体性质变化的空间和动态信息,并可用于约束流动模拟模型,从而提高对储层表征及其预测行为的信心。为了解决这个问题,我们开发了一种在自动历史匹配工作流程中定量集成4D地震数据的方法。在通过与观察到的数据进行比较来计算失配之前,通过岩弹性转换和适当的重新缩放将适当参数化的流量模拟转换为4D签名的预测。然后,使用准全局随机反演方法更新模型参数。此过程受比例尺和与过程相关的模型误差的影响。通常创建流程模拟,以便优化计算机资源并牺牲一定程度的准确性。为了加快模拟速度,需要某种形式的放大以捕获两相流动特性(例如相对渗透率),也要表现出地质异质性。升级可能被过度简化或忽略。另外,可以例如通过使用流线型方法来简化流程。最后,由于关于饱和度分布的假设,石油弹性变换会导致模型误差,因为需要针对不同的体积获得建模和观测到的地震,因此需要进行跨比例缩放。我们对上述模型误差进行了分析,这些误差是使用基于北海水库的综合地理模型发生的。我们表明模型误差取决于岩石物理参数以及基础的地质模型。当4D签名受压力效应支配时,在我们的情况下,模型误差可以忽略不计。我们描述了由于偏倚,模型错误如何影响历史匹配过程。后者导致最佳模型参数集,该模型参数集可能不同于通过升标获得的模型参数,而不确定性估计量也发生了变化。我们将模型错误的影响与其他错误(例如观察到的数据错误)进行比较。最后,我们描述了如何在失配计算中解决模型错误,以改善历史匹配过程并减少偏差影响。

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