Uncertainty quantification and global sensitivity analysis of double-diffusive natural convection in a porous enclosure

被引:20
|
作者
Rajabi, Mohammad Mahdi [1 ]
Fahs, Marwan [2 ]
Panjehfouladgaran, Aref [1 ]
Ataie-Ashtiani, Behzad [3 ,4 ]
Simmons, Craig T. [4 ]
Belfort, Benjamin [2 ]
机构
[1] Tarbiat Modares Univ, Civil & Environm Engn Fac, POB 14115-397, Tehran, Iran
[2] Univ Strasbourg EOST ENGEES, CNRS, LHyGES, 1 Rue Blessig, F-67084 Strasbourg, France
[3] Sharif Univ Technol, Dept Civil Engn, POB 11155-9313, Tehran, Iran
[4] Flinders Univ S Australia, Coll Sci & Engn, Natl Ctr Groundwater Res & Training, GPO Box 2100, Adelaide, SA 5001, Australia
关键词
Double-diffuse convection; Porous media; Uncertainty propagation analysis; Global sensitivity analysis; Polynomial chaos expansion; POLYNOMIAL CHAOS EXPANSION; MIXED CONVECTION; MASS-TRANSFER; COMBINED HEAT; FLOW; TEMPERATURE; PROPAGATION; CAVITY; HETEROGENEITY; PERFORMANCE;
D O I
10.1016/j.ijheatmasstransfer.2020.120291
中图分类号
O414.1 [热力学];
学科分类号
摘要
In this paper, detailed uncertainty propagation analysis (UPA) and variance-based global sensitivity analysis (GSA) are performed on the widely adopted double-diffuse convection (DDC) benchmark problem of a square porous cavity with horizontal temperature and concentration gradients. The objective is to understand the impact of uncertainties related to model parameters on metrics characterizing flow, heat and mass transfer processes, and to derive spatial maps of uncertainty and sensitivity indices which can provide physical insights and a better understanding of DDC processes in porous media. DDC simulations are computationally expensive and UPA and GSA require large number of simulations, so an appropriate strategy is developed to reduce the computational burden. The approach is built on two pillars: (a) an efficient numerical simulator based on the Fourier series method that generates training data, and (b) polynomial chaos expansion (PCE) meta-models that are trained using the simulator data, and then replace the numerical model in UPA and GSA. Assuming that the Rayleigh number (R-a), the solutal to thermal buoyancy ratio (N-b) and the Lewis number (L-e) are the uncertain input variables, the results of UPA show that the zones of high temperature and concentration variability are located in the regions where the flow is mainly driven by the buoyancy effects. GSA indicates that N-b is the most influential parameter affecting the temperature and concentration fields, followed respectively by R-a and L-e. For the heat-driven flow case (N-b > -1), the concentration field is more influenced by L-e than R-a. For deeper understanding of uncertainty propagation, we estimate the bias introduced by replacing uncertain parameters by deterministic values. The resulting spatial maps of the difference between deterministic output and stochastic mean show that a deterministic approach leads to different zones where the temperature, concentration and velocity fields can be either overestimated or underestimated. The conclusions drawn in this work are likely to be helpful in different applications involving DDC in porous enclosures leading to convective circulation cells. (C) 2020 Elsevier Ltd. All rights reserved.
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页数:19
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