2015
DOI: 10.1016/j.ijheatmasstransfer.2014.12.027
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Dynamics and stability of moving fronts of water evaporation in a porous medium

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Cited by 29 publications
(13 citation statements)
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“…Under such conditions, the intensity of moisture evaporation is described by a simple Arrhenius dependence. But in fact the evaporation of moisture flows in a very narrow zone, constantly moving along the particle (the front of evaporation) [27]. At the same time, the velocity of this front depends greatly on the temperature of its surface.…”
Section: A Brief Review Of the Mathematical Models Of The Wood Particmentioning
confidence: 99%
“…Under such conditions, the intensity of moisture evaporation is described by a simple Arrhenius dependence. But in fact the evaporation of moisture flows in a very narrow zone, constantly moving along the particle (the front of evaporation) [27]. At the same time, the velocity of this front depends greatly on the temperature of its surface.…”
Section: A Brief Review Of the Mathematical Models Of The Wood Particmentioning
confidence: 99%
“…This is because that the phase transition (in particular evaporation) occurs in a very narrow (much less than the linear dimension of the particle) constantly moving zone (front of evaporation) [13,14]. The models [15][16][17][18][19][20], describing the phase transitions (such as evaporation) have been developed at present, but most of them are based on the considerably simplifying assumptions of modeling procedure.…”
Section: Introductionmentioning
confidence: 99%
“…Очевидно, что указанные граничные условия выполняются, пока поверхность фазового перехода не достигла верхней или нижней границы малопроницаемого слоя. Подобная постановка задачи была сформулирована в [8][9][10]18], а в работе [9] приведена и практическая интерпретация поставленной задачи.…”
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“…Устойчивость плоской поверхности фазового перехода по отношению к бесконечно малым возмущениям изучалась в [9,10]. При этом, как показано в [8,9,18], устойчивая по отношению к малым возмущениям плоская поверхность фазового перехода может быть неустойчива по отношению к локализованным конечным возмущениям. Если пористая среда несмачиваема, то могут одновременно существовать два стационарных решения с разной локализацией разрыва, соответствующего плоскому фронту фазового перехода.…”
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