2018
DOI: 10.1007/s12217-018-9645-2
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Determination of Diffusion Coefficient in Droplet Evaporation Experiment Using Response Surface Method

Abstract: Evaporation of a liquid droplet resting on a heated substrate is a complex free-surface advection-diffusion problem, in which the main driving force of the evaporation is the vapor concentration gradient across the droplet surface. Given the uncertainty associated with the diffusion coefficient of the vapor in the atmosphere during space evaporation experiments due to the environmental conditions, a simple and accurate determination of its value is of paramount importance for a better understanding of the evap… Show more

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Cited by 8 publications
(6 citation statements)
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“…This temperature difference has two main effects on the evaporation rate and resulting cell sedimentation: i) Surface evaporation occurs as a result of vapor transport at the bio-film/air interface. The vapor transport is highly dependent on the diffusion coefficient of the dissolved gas, where the diffusion coefficient exponentially increases with the temperature [42]. For example, the diffusion coefficient of air is almost five times higher at 60℃ compared to the room temperature.…”
Section: New Surface Morphology For Phase Change Systemsmentioning
confidence: 99%
“…This temperature difference has two main effects on the evaporation rate and resulting cell sedimentation: i) Surface evaporation occurs as a result of vapor transport at the bio-film/air interface. The vapor transport is highly dependent on the diffusion coefficient of the dissolved gas, where the diffusion coefficient exponentially increases with the temperature [42]. For example, the diffusion coefficient of air is almost five times higher at 60℃ compared to the room temperature.…”
Section: New Surface Morphology For Phase Change Systemsmentioning
confidence: 99%
“…Droplet evaporation in terrestrial (normal) gravity conditions involves a complex interaction of diffusion within the substrate, buoyant convection in the gas and liquid phases, contact line evaporation, vapour diffusion, evaporative cooling at the liquid-gas interface, and possible Marangoni effects 11 , 15 24 . Regardless, the main driving force of the evaporation for a sessile droplet is the vapour concentration gradient across the droplet surface 3 , 11 , 25 . Furthermore, albeit a proportionately small region compared with the overall droplet size, the heat and mass transfer at the contact line plays an important role in droplet evaporation dynamics, and this has been shown conclusively in terrestrial gravity conditions 15 , 17 – 19 , 26 .…”
Section: Introductionmentioning
confidence: 99%
“…In microgravity conditions, with the absence of gravity-driven convection, the flow field within an evaporating droplet on a heated substrate is largely determined by Marangoni flow 25 . The main driving evaporation mechanism is the vapour diffusivity at the liquid-gas interface, and since mass diffusion is quite a slow process, this generally leads to lower evaporation rates 5 .…”
Section: Introductionmentioning
confidence: 99%
“…The overlapping air points are then defined to have the saturated humidity at the given temperature condition. Moreover, it is assumed that the main driving force of the liquid mass transfer into vapor at the air-water interface is diffusion driven by the vapor concentration gradient [12].…”
Section: Introductionmentioning
confidence: 99%