2013
DOI: 10.1016/j.jnnfm.2012.10.008
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Thermal instabilities in a yield stress fluid: Existence and morphology

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Cited by 41 publications
(55 citation statements)
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“…Unyielded regions may be further categorized as being stationary or in motion, with the former typically abutting a wall of the flow domain. This paper is motivated by the recent experimental study of Davaille et al (2013) in which thermal plumes are induced in a stationary viscoplastic fluid reservoir (rectangular tank), by means of localized heating applied at the lower wall of the tank. In natural convection, buoyancy forces resulting from thermal expansion induce fluid motion.…”
Section: Introductionmentioning
confidence: 99%
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“…Unyielded regions may be further categorized as being stationary or in motion, with the former typically abutting a wall of the flow domain. This paper is motivated by the recent experimental study of Davaille et al (2013) in which thermal plumes are induced in a stationary viscoplastic fluid reservoir (rectangular tank), by means of localized heating applied at the lower wall of the tank. In natural convection, buoyancy forces resulting from thermal expansion induce fluid motion.…”
Section: Introductionmentioning
confidence: 99%
“…A review of the vast body of research on Newtonian plumes can be found in Ribe, Davaille & Christensen (2007). To the best of authors' knowledge, the first experimental studies of viscoplastic plumes were conducted very recently by Davaille et al (2013).…”
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confidence: 99%
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“…Finally, a number of authors have recently studied the onset of natural convection experimentally using solutions of Carbopol (e.g. Darbouli et al 2013;Davaille et al 2013;Kebiche, Castelain & Burghelea 2014). …”
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confidence: 99%
“…Whether time-invariant or not, and whether coupled to the flow or independently prescribed, the body force determines how the momentum balance is affected by purely viscous stresses, yield stress and the body force, and hence allows for different dynamic behaviours; e.g. recent studies have illustrated the possibility of delayed flow 55 onset when the driving force is the buoyancy due to temperature differences in the domain [6,7,8]. In naturally convecting flows, the forcing is coupled with the flow field.…”
Section: Introductionmentioning
confidence: 99%