{"title":"Determination of the Mechanism of Droplets Post-impact Atomisation in Water Sprays at Temperatures Bellow the Critical Nukiyama and Leidenfrost Values","authors":"V. Stamatov, L. Stamatova","doi":"10.15866/IREPHY.V11I5.14261","DOIUrl":null,"url":null,"abstract":"Several non-intrusive laser diagnostic techniques (PIV, Marker Nephelometry and PLIF) were applied to study spray impact morphology: droplets velocity and size prior and after the impact, the number of droplets in the impact and post-impact zones, and the presence of vorticity fields in the impact area, at a temperature lower than the critical Nukiyama and Leidenfrost temperatures. The experimental results suggest that the process of droplet post-impact atomisation follows a hydrodynamic mechanism in which the first droplets that hit the wall form a liquid film. Later, the film breaks up because of the impact of the next incident dropletsm. As a result, a small number of relatively large post-impact droplets of low velocity is formed and pushed away from the zone of impact.","PeriodicalId":448231,"journal":{"name":"International Review of Physics","volume":"32 4","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2017-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Review of Physics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15866/IREPHY.V11I5.14261","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Several non-intrusive laser diagnostic techniques (PIV, Marker Nephelometry and PLIF) were applied to study spray impact morphology: droplets velocity and size prior and after the impact, the number of droplets in the impact and post-impact zones, and the presence of vorticity fields in the impact area, at a temperature lower than the critical Nukiyama and Leidenfrost temperatures. The experimental results suggest that the process of droplet post-impact atomisation follows a hydrodynamic mechanism in which the first droplets that hit the wall form a liquid film. Later, the film breaks up because of the impact of the next incident dropletsm. As a result, a small number of relatively large post-impact droplets of low velocity is formed and pushed away from the zone of impact.