TY - GEN
T1 - Experimental quantification of partial melting in a single frozen drop
AU - Yan, Sihong
AU - Palacios, Jose
N1 - Funding Information:
This project was funded by NASA Research Grant and Cooperative Agreement Number NNX12AK16A. The authors would like to acknowledge our valuable interaction with NASA Glenn Research Center engineers, especially Richard E. Kreeger. His guidance and support of this project were critical for the completion of the research. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily indicate the views of the U.S. Federal Government or NASA.
Publisher Copyright:
© 2016, American Institute of Aeronautics and Astronautics Inc, AIAA.
PY - 2016
Y1 - 2016
N2 - The visualization and quantification of the melting process of a single frozen droplet was conducted. Luminescent dye and high-speed camera visualization were used to monitor the partial melting state of an ultrasonically levitated frozen drop exposed to warm environments. Rhodamine B was dissolved (0.01% mass fraction) in the water used to create a droplet. The Droplet was placed at the node of the wave created by the acoustic levitator and frozen via convective cooling. When the cold air flow was turned off, the partial melting of the droplet began. Water droplets with a diameter ranging approximately between 300μm to 1800μm were tested. Four environmental melting temperatures were tested: 5°C, 15°C, 25°C and 35°C. A laser beam was pointed at the partially melted drop to enhance the luminesce behavior of the Rhodamine B molecules in the water. The luminescence of the ink in the melted water allowed for the discretization between frozen ice and melted water. The variation of percentage of partial melting of the drop with time was recorded. The correlation between the rate of melting, environmental temperature, and diameter of the frozen droplets is reported and discussed in this paper. It is confirmed that the time rate of melting is inversely proportional to the diameter of the ice crystals and directly proportional to the environmental temperature. An empirical fit to predict the percentage of partial melting with respect to temperature and droplet diameter was experimentally acquired.
AB - The visualization and quantification of the melting process of a single frozen droplet was conducted. Luminescent dye and high-speed camera visualization were used to monitor the partial melting state of an ultrasonically levitated frozen drop exposed to warm environments. Rhodamine B was dissolved (0.01% mass fraction) in the water used to create a droplet. The Droplet was placed at the node of the wave created by the acoustic levitator and frozen via convective cooling. When the cold air flow was turned off, the partial melting of the droplet began. Water droplets with a diameter ranging approximately between 300μm to 1800μm were tested. Four environmental melting temperatures were tested: 5°C, 15°C, 25°C and 35°C. A laser beam was pointed at the partially melted drop to enhance the luminesce behavior of the Rhodamine B molecules in the water. The luminescence of the ink in the melted water allowed for the discretization between frozen ice and melted water. The variation of percentage of partial melting of the drop with time was recorded. The correlation between the rate of melting, environmental temperature, and diameter of the frozen droplets is reported and discussed in this paper. It is confirmed that the time rate of melting is inversely proportional to the diameter of the ice crystals and directly proportional to the environmental temperature. An empirical fit to predict the percentage of partial melting with respect to temperature and droplet diameter was experimentally acquired.
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M3 - Conference contribution
AN - SCOPUS:84979917074
SN - 9781624104336
T3 - 8th AIAA Atmospheric and Space Environments Conference
BT - 8th AIAA Atmospheric and Space Environments Conference
PB - American Institute of Aeronautics and Astronautics Inc, AIAA
T2 - 8th AIAA Atmospheric and Space Environments Conference, 2016
Y2 - 13 June 2016 through 17 June 2016
ER -