2010
DOI: 10.1016/j.ijthermalsci.2010.03.009
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Transient and steady natural convection from a heat source embedded in thermally stratified porous layer

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Cited by 9 publications
(2 citation statements)
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“…Combined thermally draft stream past a semi endless vertical plate entrenched in situations absorbent area integrates the unpredictable permeableness by Darcy's modeling premeditated through Mohammadein as well as El‐Shaer 1 . Zhang et al 2 provided short‐lived as well as reliable natural convection stream entrenched in a soaked spongy stratum. The possessions of combined quantities on sturdy magnetohydrodynamic (MHD) mutual natural and strained thermal draft discharge past a semi‐infinite perpendicular smooth plate were deliberated by Alam et al 3 The features of heat radiating transport have been researched through Brewster 4 .…”
Section: Introductionmentioning
confidence: 99%
“…Combined thermally draft stream past a semi endless vertical plate entrenched in situations absorbent area integrates the unpredictable permeableness by Darcy's modeling premeditated through Mohammadein as well as El‐Shaer 1 . Zhang et al 2 provided short‐lived as well as reliable natural convection stream entrenched in a soaked spongy stratum. The possessions of combined quantities on sturdy magnetohydrodynamic (MHD) mutual natural and strained thermal draft discharge past a semi‐infinite perpendicular smooth plate were deliberated by Alam et al 3 The features of heat radiating transport have been researched through Brewster 4 .…”
Section: Introductionmentioning
confidence: 99%
“…Mixed convective flow past a semi-infinite vertical plate embedded in a porous medium incorporating the variable permeability in Darcy's model studied by Mohammadein and El-Shaer [1]. Zhang et al [2] presented transient and steady natural convection from a heat source embedded in a saturated porous layer. The effects of Dufour and Soret numbers on steady combined free-forced convective and mass transfer flow past a semi-infinite vertical flat plate in the presence of a uniform transverse magnetic field studied by Alam et al [3].…”
Section: Introductionmentioning
confidence: 99%