Abstract:[1] In this work, we propose a new collocation method for uncertainty quantification in strongly nonlinear problems. Based on polynomial construction, the traditional probabilistic collocation method (PCM) approximates the model output response, which is a function of the random input parameter, from the Eulerian point of view in specific locations. In some cases, especially when the advection dominates, the model response has a strongly nonlinear profile with a discontinuous shock or large gradient. This nonl… Show more
“…For example, it has been demonstrated that the mean and variance of hydraulic head obtained with only the first few leading KL expansion terms (e.g., = 6 for a 1D case) is very close to those obtained from thousands of Monte Carlo simulation with full models [25]. Similar observations are also reported in Li et al [26] and Liao and Zhang [27]. In a quantitative sense, if the polynomial chaos expansion (PCE) is used to construct a surrogate model for the state variables (e.g., hydraulic head) and KL expansion on the model parameter (e.g., log hydraulic conductivity), the number of model evaluation required to obtain the PCE coefficients is ( + )!/ !/ !, where is the degree of PCE.…”
Section: Gaussian Variablessupporting
confidence: 83%
“…The advantage of the proposed method is that KL expansion has the capability to conduct the model dimensionality reduction. If it is further incorporated with polynomial chaos expansion on the state variables, such as hydraulic head in the single-phase flow problem [25], saturation in the multiphase problem [26], and contaminant transport problem [27], the computational cost to perform uncertainty analysis in the hydrological research can be greatly reduced. The proposed KL-based multiscale random fractal field generator provides the foundation to establish a high-efficiency stochastic analysis framework.…”
The traditional geostatistics to describe the spatial variation of hydrogeological properties is based on the assumption of stationarity or statistical homogeneity. However, growing evidences show and it has been widely recognized that the spatial distribution of many hydrogeological properties can be characterized as random fractals with multiscale feature, and spatial variation can be described by power variogram model. It is difficult to generate a multiscale random fractal field by directly using nonstationary power variogram model due to the lack of explicit covariance function. Here we adopt the stationary truncated power variogram model to avoid this difficulty and generate the multiscale random fractal field using Karhunen-Loève (KL) expansion. The results show that either the unconditional or conditional (on measurements) multiscale random fractal field can be generated by using truncated power variogram model and KL expansion when the upper limit of the integral scale is sufficiently large, and the main structure of the spatial variation can be described by using only the first few dominant KL expansion terms associated with large eigenvalues. The latter provides a foundation to perform dimensionality reduction and saves computational effort when analyzing the stochastic flow and transport problems.
“…For example, it has been demonstrated that the mean and variance of hydraulic head obtained with only the first few leading KL expansion terms (e.g., = 6 for a 1D case) is very close to those obtained from thousands of Monte Carlo simulation with full models [25]. Similar observations are also reported in Li et al [26] and Liao and Zhang [27]. In a quantitative sense, if the polynomial chaos expansion (PCE) is used to construct a surrogate model for the state variables (e.g., hydraulic head) and KL expansion on the model parameter (e.g., log hydraulic conductivity), the number of model evaluation required to obtain the PCE coefficients is ( + )!/ !/ !, where is the degree of PCE.…”
Section: Gaussian Variablessupporting
confidence: 83%
“…The advantage of the proposed method is that KL expansion has the capability to conduct the model dimensionality reduction. If it is further incorporated with polynomial chaos expansion on the state variables, such as hydraulic head in the single-phase flow problem [25], saturation in the multiphase problem [26], and contaminant transport problem [27], the computational cost to perform uncertainty analysis in the hydrological research can be greatly reduced. The proposed KL-based multiscale random fractal field generator provides the foundation to establish a high-efficiency stochastic analysis framework.…”
The traditional geostatistics to describe the spatial variation of hydrogeological properties is based on the assumption of stationarity or statistical homogeneity. However, growing evidences show and it has been widely recognized that the spatial distribution of many hydrogeological properties can be characterized as random fractals with multiscale feature, and spatial variation can be described by power variogram model. It is difficult to generate a multiscale random fractal field by directly using nonstationary power variogram model due to the lack of explicit covariance function. Here we adopt the stationary truncated power variogram model to avoid this difficulty and generate the multiscale random fractal field using Karhunen-Loève (KL) expansion. The results show that either the unconditional or conditional (on measurements) multiscale random fractal field can be generated by using truncated power variogram model and KL expansion when the upper limit of the integral scale is sufficiently large, and the main structure of the spatial variation can be described by using only the first few dominant KL expansion terms associated with large eigenvalues. The latter provides a foundation to perform dimensionality reduction and saves computational effort when analyzing the stochastic flow and transport problems.
“…The Karhunen-Loeve expansion method can convert a correlated random function into a polynomial with independent and identically distributed Gaussian random variables [45,46]. Since the log hydraulic conductivity, Y, is heterogeneous and spatial correlated.…”
Section: Unconditional and Conditional Karhunen-loeve Expansion Methodsmentioning
confidence: 99%
“…To obtain the coefficients, the probabilistic collocation method can be used, which is derived on the basis of weighted residual method. Denoting as the differential operator in Equation (1), the stochastic partial differential equation of groundwater flow model can be written as [44,46]:…”
“…An intrusive method to obtain the PCE coefficient has been developed so that the governing equation can be treated as a black box, and any existing solver can be easily adopted. The probabilistic collocation method (PCM) is a non-intrusive method developed by [44] which uses the points of numerical evaluation of the Galerkin integral as collocation points [45,46]. However, the previous response-surface-based inverse modeling methods can only consider a single best model as mentioned before, and thus the model uncertainty has been ignored.…”
Abstract:The characterization of flow in subsurface porous media is associated with high uncertainty. To better quantify the uncertainty of groundwater systems, it is necessary to consider the model uncertainty. Multi-model uncertainty analysis can be performed in the Bayesian model averaging (BMA) framework. However, the BMA analysis via Monte Carlo method is time consuming because it requires many forward model evaluations. A computationally efficient BMA analysis framework is proposed by using the probabilistic collocation method to construct a response surface model, where the log hydraulic conductivity field and hydraulic head are expanded into polynomials through Karhunen-Loeve and polynomial chaos methods. A synthetic test is designed to validate the proposed response surface analysis method. The results show that the posterior model weight and the key statistics in BMA framework can be accurately estimated. The relative errors of mean and total variance in the BMA analysis results are just approximately 0.013% and 1.18%, but the proposed method can be 16 times more computationally efficient than the traditional BMA method.
In this study, an efficient full Bayesian approach is developed for the optimal sampling well location design and source parameters identification of groundwater contaminants. An information measure, i.e., the relative entropy, is employed to quantify the information gain from concentration measurements in identifying unknown parameters. In this approach, the sampling locations that give the maximum expected relative entropy are selected as the optimal design. After the sampling locations are determined, a Bayesian approach based on Markov Chain Monte Carlo (MCMC) is used to estimate unknown parameters. In both the design and estimation, the contaminant transport equation is required to be solved many times to evaluate the likelihood. To reduce the computational burden, an interpolation method based on the adaptive sparse grid is utilized to construct a surrogate for the contaminant transport equation. The approximated likelihood can be evaluated directly from the surrogate, which greatly accelerates the design and estimation process. The accuracy and efficiency of our approach are demonstrated through numerical case studies. It is shown that the methods can be used to assist in both single sampling location and monitoring network design for contaminant source identifications in groundwater.
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