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Modeling fault activation due to fluid production: Bayesian update by seismic data

机译:对由于流体产生而引起的断层激活进行建模:地震数据的贝叶斯更新

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The reactivation of faults and the generation of fractures can be caused by stress changes due to injection and/or production of fluids into and/or from the subsurface. The simulation of these processes, which could be associated with (micro-)seismicity, is affected by a high uncertainty. The aim of this work is at developing a mathematical framework to quantify and possibly reduce the prior modeling uncertainties by assimilation of seismic data. The mechanics of fault (re-)activation is simulated by a Finite Element (FE) numerical model where the discontinuous displacements between the fault surfaces are suitably considered using appropriate Interface Elements (IEs). The study is carried out by using a stochastic approach, with a global sensitivity analysis (gSA) based on Sobol' indices initially performed to estimate the influence of the input parameters on the model solution. Then, a Markov Chain Monte Carlo (MCMC) sampling technique based on the generalized Polynomial Chaos expansion (gPC) surrogate solution is used to update the prior information conditioned on seismic observations. The methodology is tested on a 3D synthetic test case. The uncertain input is the natural stress regime and the Mohr-Coulomb parameters characterizing the fault activation criterion. A good reduction of the prior uncertainty is obtained, showing that the assimilation of seismic data can have a promising potential for improving the subsurface characterization.
机译:断层的重新激活和裂缝的产生可能是由于应力的变化引起的,应力的变化是由于流体注入地下和/或从地下产生和/或产生流体引起的。这些过程的模拟(可能与(微)地震有关)受到高度不确定性的影响。这项工作的目的是开发一个数学框架,以通过吸收地震数据来量化并可能减少先前的建模不确定性。断层(重新)激活的机制由有限元(FE)数值模型模拟,其中使用适当的接口元素(IE)适当考虑断层表面之间的不连续位移。该研究是使用随机方法进行的,最初基于Sobol指数进行了全局敏感性分析(gSA),以估计输入参数对模型解的影响。然后,基于广义多项式混沌展开(gPC)替代解决方案的马尔可夫链蒙特卡洛(MCMC)采样技术被用于更新以地震观测为条件的先验信息。该方法已在3D综合测试用例上进行了测试。不确定的输入是自然应力状态和表征故障激活准则的Mohr-Coulomb参数。可以很好地减少先验的不确定性,这表明地震数据的同化可以为改善地下特征提供有希望的潜力。

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