首页> 外文会议>International High-Level Radioactive Waste Management 2019 >KALMAN CALIBRATION APPROACH TO ASSESS HYDRAULIC IMPACT INDUCED BY THE CONSTRUCTION AND OPERATION OF THE PLANNED IHLRW REPOSITORY - CIGEO (FRANCE)
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KALMAN CALIBRATION APPROACH TO ASSESS HYDRAULIC IMPACT INDUCED BY THE CONSTRUCTION AND OPERATION OF THE PLANNED IHLRW REPOSITORY - CIGEO (FRANCE)

机译:卡尔曼校准方法,以评估因ILHLRW储罐的建造和运营而引起的液压影响-CIGEO(法国)

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摘要

Prediction of hydraulic perturbations induced by theconstruction and the operation of deep geologicalradioactive waste repository is need to support: (i) theengineering and monitoring operations, and (ii) theassessment of the consequences on groundwaterresources. Andra (French National Radioactive WasteManagement Agency) has developed a three-dimensionalhigh-resolution numerical model of variably saturatedflow in order:1. to understand the local flow behavior and to improvethe characterization of lithological structures andheterogeneities of the Oxfordian aquifer system atMeuse/Haute-Marne site.2. to assess 3D extension of the perturbation and estimategroundwater volumes drained by underground ramps andshafts.Novel calibration method was applied to reproduce themonitored transient flow and map the heterogeneity of theOxfordian aquifer formation affected by undergroundstructures (shafts). Simulations of the predictive transientflow behavior induced by the construction and theoperation of the planned repository allow the assessmentof the extension of perturbation and the estimation ofdrained water discharge. Robustness of the numericalmodel as well as reliability of the prediction resultsdepend on the quality of the transient flow calibrationbased on inverse approach, called “Iterative EnsembleSmother (IES)” for parameter estimation. By assimilatingall monitoring data at once, the ensemble smootherallows the estimation of poorly known parameters bysampling of an approximate Gaussian posteriordistribution which unknown moments estimated fromupdated realizations. Computation of Kalman gain matrixdepends on covariance matrices approximated from theensemble describing a linear relationship between theupdated realizations and the observed data.
机译:需要对由深部地质放射性废物处置库的建设和运行引起的水力扰动进行预测,以支持:(i)工程和监测操作,以及(ii)对地下水的影响\ r \ n资源。法国国家放射性废物管理局的安德拉(Andra)已按以下顺序开发了可变饱和\ r \ n流量的三维\ r \ n高分辨率数值模型:\ r \ n1。 \ r \ n2在Meuse / Haute-Marne站点了解牛津含水层系统的岩性结构和\ r \ n非均质性,以了解其局部流动行为并改善其特性。来评估扰动的3D扩展并估算地下坡道和竖井所排放的地下水量。\ n \ n采用新颖的标定方法来再现\ r \监测的瞬态流量并绘制\ r \的异质性受地下\ r \ n结构(竖井)影响的牛津含水层构造。通过对计划的储存库的建造和运行所引起的预测瞬态水流行为进行模拟,可以评估扰动的扩展和排水的估计。数值\ r \ n模型的稳健性以及预测结果的可靠性\ r \ n取决于基于逆向方法的瞬态流量校准的质量\ r \ n,称为“迭代集成\ r \ nSmother(IES)”作为参数估计。通过一次吸收所有监控数据,该集成器可以更平滑地允许通过对近似高斯后验分布进行采样,从而对未知参数进行估算,未知分布是根据更新的实现来估算的。卡尔曼增益矩阵的计算依赖于从方差近似的协方差矩阵,该方差矩阵描述了更新的实现与观测数据之间的线性关系。

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    French National Agency for Radioctive Waste Management: Andra, 1/7 rue Jean Monnet, 92298 Châtenay-Malabry, Cedex, France. Abdelhakim.Benabderrahmane@andra.fr;

    Centre of Hydrogeology and Geothermics (CHYN), University of Neuchâtel, Rue Emile Argand 11, 2000 Neuchâtel, Switzerland;

    Centre of Hydrogeology and Geothermics (CHYN), University of Neuchâtel, Rue Emile Argand 11, 2000 Neuchâtel, Switzerland;

    Laboratoire de Mécanique des Sols (EPFL - LMS), Ecole Polytechnique Fédérale de Lausanne, CH - 1015 Lausanne, Switzerland;

    Centre of Hydrogeology and Geothermics (CHYN), University of Neuchâtel, Rue Emile Argand 11, 2000 Neuchâtel, Switzerland;

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