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On an Alternative Implementation of the Iterative Ensemble Smoother and its Application to Reservoir Facies Estimation

机译:在迭代集合的替代实施中,迭代集合更顺畅及其在水库相片估算中的应用

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For data assimilation problems there are different ways in using available observations. While certain data assimilation algorithms, for instance, the ensemble Kalman filter (EnKF, see. for example. Aanonsen et al., 2009) assimilate the observations sequentially in time, other data assimilation algorithms may instead collect the observations at different time instants and assimilate them simultaneously. In general such algorithms can be classified as smoothers. In this aspect, the ensemble smoother (ES, see, for example, Evensen and van Leeuvven, 2000) can be considered as an smoother counterpart of the EnKF. The EnKF has been widely used for reservoir data assimilation problems since its introduction to the community of petroleum engineering (Nasvdal et al.. 2002). The applications of the ES to reservoir data assimilation problems are also investigated recently. Compared to the EnKF, the ES has certain technical advantages, including, for instance, avoiding the restarts associated with each update step in the EnKF and also having fewer variables to update, which may result in a significant reduction in simulation time, while providing similar assimilation results to those obtained by the EnKF (Skjervheim and Evensen, 2011). To further improve the performance of the ES, some iterative ensemble smoothers are suggested in the literature, in which the iterations are carried out in the forms of certain iterative optimization algorithms, e. g.. the Gaussian-Newton (Chen and Oliver, 2012) or the Levenberg-Marquardt method (Chen and Oliver. 2013; Emerick and Reynolds. 2012), or in the context of adaptive Gaussian mixture (AGM, see Stordal and Lorentzen. 2013). In this contribution we show that the iteration formulae used in Chen and Oliver (2013): Emerick and Reynolds (2012) can also be derived from the regularized Levenberg-Marquardt (REM) algorithm in inverse problems theory (Engl et al.. 2000). with certain linearization approximations introduced to the RLM. This does not only lead to an alternative theoretical tool in understanding and analyzing the behaviour of the aforementioned iterative ES, but also provide insights and guidelines for further developments of the iterative ES algorithm. As an example, we show that an alternative implementation of the iterative ES can be derived based on the RLM algorithm. For illustration, we apply this alternative algorithm to a facies estimation problem previously investigated in Lorentzen et al. (2012). and compare its performance to that of the (approximate) iterative ES used in Chen and Oliver (2013).
机译:对于数据同化问题,有不同的方法使用可用的观察。虽然某些数据同化算法,例如,Ensemble Kalman滤波器(ENKF,参见。例如,AANONSEN等人,2009)在时间顺序同化观察,其他数据同化算法可以在不同的时间瞬间收集观察结果并同化他们同时。通常,这种算法可以被归类为smoothers。在这方面,集合更顺畅(ES,例如,Evensen和Van Leeuvven,2000)可以被视为ENKF的更顺畅。自从其对石油工程社区引入以来,ENKF已广泛用于水库数据同化问题(NASVDAL等人2002)。最近还调查了ES到水库数据同化问题的应用。与ENKF相比,ES具有某些技术优点,包括例如,避免了与ENKF中的每个更新步骤相关联的重启,并且还可以使更新的变量较少,这可能导致模拟时间显着降低,同时提供类似的同化结果对由ENKF(Skjervheim和Evensen,2011)获得的结果。为了进一步提高ES的表现,文献中提出了一些迭代的集合SmoOthers,其中迭代以某种迭代优化算法的形式进行,即,e。 G ..高斯 - 牛顿(陈和奥利弗,2012年)或Levenberg-Marquardt方法(陈和奥利弗。2013; Emerick和Reynolds。2012),或在适应性高斯混合物(AGM,见Stordal和Lorentzen的背景下。 2013)。在这一贡献中,我们展示了陈和奥利弗(2013)中使用的迭代公式:Emerick和Reynolds(2012)也可以从正面问题理论(Engl等,2000)中的正则化的Levenberg-Marquardt(REM)算法得出。具有某些线性化近似引入RLM。这不仅导致替代理论工具,在理解和分析上述迭代es的行为,还提供了迭代es算法的进一步发展的见解和准则。作为示例,我们表明可以基于RLM算法导出迭代es的替代实现。出于说明,我们将该替代算法应用于先前在Lorentzen等人的面部估计问题。 (2012)。并将其对陈和奥利弗(2013)使用的(近似)迭代ES的性能进行比较。

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