2015
DOI: 10.1016/j.ijheatmasstransfer.2014.08.015
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Highly efficient and local projection-based stabilized finite element method for natural convection problem

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Cited by 21 publications
(8 citation statements)
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“…For natural convection problem, which has a wide range of applications in many research fields (Wu et al , 2017b, 2016), the density difference in the fluid occurring due to temperature gradient is the driving mechanism of fluid motion[1]. In case that the density variation is small, it can be modeled by using a Boussinesq approximation, which treats the density as a constant but with an added buoyancy force, and most literature studies the constant density natural convection based on the Boussinesq approximation (Boland and Layton, 1990; Du et al , 2015; Feng et al , 2011; Huang et al , 2015, 2013, 2012; Liao, 2012, 2010; Si et al , 2014; Szumbarski et al , 2014; Su et al , 2017a, 2017b, 2014a, 2014b; Sun et al , 2011; Davis, 1983; Wang et al , 2018a, 2018b; Wu et al , 2015b, 2017a, 2016; Zhang et al , 2016, 2018]). However, in most geophysical flows and many other situations, fluid motion is usually driven by large temperature differences, which results in a considerable density change and the Boussinesq approximation is no longer valid.…”
Section: Introductionmentioning
confidence: 99%
“…For natural convection problem, which has a wide range of applications in many research fields (Wu et al , 2017b, 2016), the density difference in the fluid occurring due to temperature gradient is the driving mechanism of fluid motion[1]. In case that the density variation is small, it can be modeled by using a Boussinesq approximation, which treats the density as a constant but with an added buoyancy force, and most literature studies the constant density natural convection based on the Boussinesq approximation (Boland and Layton, 1990; Du et al , 2015; Feng et al , 2011; Huang et al , 2015, 2013, 2012; Liao, 2012, 2010; Si et al , 2014; Szumbarski et al , 2014; Su et al , 2017a, 2017b, 2014a, 2014b; Sun et al , 2011; Davis, 1983; Wang et al , 2018a, 2018b; Wu et al , 2015b, 2017a, 2016; Zhang et al , 2016, 2018]). However, in most geophysical flows and many other situations, fluid motion is usually driven by large temperature differences, which results in a considerable density change and the Boussinesq approximation is no longer valid.…”
Section: Introductionmentioning
confidence: 99%
“…As we know, the above bilinear and trilinear forms have following important estimates (Su et al, 2017;Huang et al, 2012Huang et al, , 2015Layton and Tobiska, 1998;Luo, 2006;Su et al, 2014aSu et al, , 2014b are two fixed positive constants depending only on X.…”
Section: Penalized Finite Element Methodsmentioning
confidence: 99%
“…In fact, in many engineering applications, especially in relation to heat losses from thermal storage systems such as solar collectors, nuclear reactor design, buildings and aircraft cabin insulation, the problem is researched to find means to improve the insulating properties of fluid layers. In [59,60], for the natural convection heat transfer, numerical investigation of this problem is presented. Now, we will test this problem for the Darcy-Brinkman model, which describes double-diffusive phenomena and comes from the combined heat and mass transfer.…”
Section: The Partitioned Square Enclosure Problemmentioning
confidence: 99%