Bayesian calibration of a large-scale geothermal reservoir model by a new adaptive delayed acceptance Metropolis Hastings algorithm

被引:110
作者
Cui, T. [1 ]
Fox, C. [2 ]
O'Sullivan, M. J. [1 ]
机构
[1] Univ Auckland, Dept Engn Sci, Auckland 1141, New Zealand
[2] Univ Otago, Dept Phys, Dunedin 9016, New Zealand
关键词
MONTE-CARLO METHODS; PILOT POINT METHODOLOGY; INVERSE PROBLEMS; UNCERTAINTY QUANTIFICATION; DIFFERENTIAL EVOLUTION; AUTOMATED CALIBRATION; TRANSMISSIVITY FIELDS; PARAMETER-ESTIMATION; STATISTICAL-ANALYSIS; GLOBAL OPTIMIZATION;
D O I
10.1029/2010WR010352
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The aim of this research is to estimate the parameters of a large-scale numerical model of a geothermal reservoir using Markov chain Monte Carlo (MCMC) sampling, within the framework of Bayesian inference. All feasible parameters that are consistent with the measured data are summarized by the posterior distribution, and hence parameter estimation and uncertainty quantification are both given by calculating expected values of statistics of interest over the posterior distribution. It appears to be computationally infeasible to use the standard Metropolis-Hastings algorithm (MH) to sample the high dimensional computationally expensive posterior distribution. To improve the sampling efficiency, a new adaptive delayed-acceptance MH algorithm (ADAMH) is implemented to adaptively build a stochastic model of the error introduced by the use of a reduced-order model. This use of adaptivity differs from existing adaptive MCMC algorithms that tune proposal distributions of the Metropolis-Hastings algorithm (MH), though ADAMH also implements that technique. For the 3-D geothermal reservoir model we present here, ADAMH shows a great improvement in the computational efficiency of the MCMC sampling, and promising results for parameter estimation and uncertainty quantification are obtained. This algorithm could offer significant improvement in computational efficiency when implementing sample-based inference in other large-scale inverse problems.
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页数:26
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