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Effect of ambient temperature on the micro-explosion characteristics of soybean oil droplet: The phenomenon of evaporation induced vapor cloud
•Soybean oil droplet shows four-staged evaporation characteristics at high temperatures.•The micro-explosion strength increases with the increase of ambient temperature.•Evaporation induced vapor cloud was first observed at 973 K.•Homogenous and heterogeneous nucleation were observed at 873 K, 923 K...
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Published in: | International journal of heat and mass transfer 2019-08, Vol.139, p.736-746 |
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Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | •Soybean oil droplet shows four-staged evaporation characteristics at high temperatures.•The micro-explosion strength increases with the increase of ambient temperature.•Evaporation induced vapor cloud was first observed at 973 K.•Homogenous and heterogeneous nucleation were observed at 873 K, 923 K and 973 K.
Micro-explosion characteristics of soybean oil droplet were investigated using high speed backlight imaging technique at ambient temperature 873 K, 923 K and 973 K. Experimental results indicate that soybean oil droplet underwent transient heating phase, micro-explosion evaporation phase, equilibrium evaporation phase, and residue evaporation phase at all the studied temperatures. The evaporation rate of equilibrium evaporation phase is increased when the temperature increased. However, a decrease for the evaporation rate of residue evaporation phase. Homogeneous and heterogeneous nucleation are observed at all temperatures, homogeneous nucleation lead to strong micro-explosion and heterogeneous nucleation lead to weak micro-explosion. Moreover, micro-explosion strength increased when the ambient increased. It was found that the micro-explosion occurred at the end of droplet evaporation, this is one of the reasons for the poor atomization characteristics of bio-oil in the engine. More importantly, the evaporation induced vapor cloud is observed at 973 K, this is mainly due to the non-isothermal condensation caused by Stefan outflow. |
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ISSN: | 0017-9310 1879-2189 |
DOI: | 10.1016/j.ijheatmasstransfer.2019.04.038 |