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Integration of microseismic monitoring data into coupled flow and geomechanical models with ensemble Kalman filter

机译:使用集成卡尔曼滤波器将微地震监测数据集成到耦合流动和地质力学模型中

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摘要

Hydraulic stimulation of low-permeability rocks in enhanced geothermal systems, shale resources, and CO2 storage aquifers can trigger microseismic events, also known as microearthquakes (MEQs). The distribution of microseismic source locations in the reservoir may reveal important information about the distribution of hydraulic and geomechanical rock properties. In this paper, we present a framework for conditioning heterogeneous rock permeability and geomechanical property distributions on microseismic data. To simulate the multiphysics processes in these systems, we combine a fully coupled flow and geomechanical model with the Mohr-Coulomb type rock failure criterion. The resulting multiphysics simulation constitutes the forecast model that relates microseismic source locations to reservoir rock properties. We adopt this forward model in an ensemble Kalman filter (EnKF) data assimilation framework to jointly estimate reservoir permeability and geomechanical property distributions from injection-induced microseismic response measurements. We show that integration of a large number of spatially correlated microseismic data with practical ensemble sizes can lead to severe underestimation of ensemble spread, and eventually ensemble collapse. To mitigate the variance underestimation issue, two low-rank data representation schemes are presented and discussed. In the first approach, microseismic data are projected onto a low-dimensional subspace defined by the left singular vectors of the perturbed observation matrix. The second method uses a coarser grid for representing the microseismic data. A series of numerical experiments is presented to evaluate the performance of the proposed methods and to illustrate their applicability for assimilating microseismic data into coupled flow and geomechanical forward models to estimate multiphysics rock properties.
机译:在增强的地热系统,页岩资源和二氧化碳存储含水层中对低渗透率岩石进行水力刺激会触发微地震事件,也称为微地震(MEQ)。储层中微震源位置的分布可能揭示有关水力和岩石力学岩石特性分布的重要信息。在本文中,我们提供了一个基于微震数据处理非均质岩石渗透率和岩土力学特性分布的框架。为了模拟这些系统中的多物理场过程,我们将完全耦合的流动和岩土力学模型与Mohr-Coulomb型岩石破坏准则相结合。由此产生的多物理场模拟构成了将微震源位置与储层岩石特性相关联的预测模型。我们在集合卡尔曼滤波器(EnKF)数据同化框架中采用此正演模型,以便根据注入诱发的微地震响应测量值来共同估算储层渗透率和地质力学特性分布。我们显示大量空间相关的微地震数据与实际合奏大小的集成可能导致对合奏传播的严重低估,并最终导致合奏崩溃。为了缓解方差低估问题,提出并讨论了两种低秩数据表示方案。在第一种方法中,微地震数据被投影到由扰动观测矩阵的左奇异矢量定义的低维子空间上。第二种方法使用较粗糙的网格表示微地震数据。提出了一系列数值实验,以评估所提出方法的性能,并说明它们在将微地震数据吸收到耦合流动模型和地质力学正演模型中以估计多物理场岩石特性时的适用性。

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