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    Experimental Study of Drop Impact on Deep-Water Surface in the Presence of Wind

    Source: Journal of Physical Oceanography:;2018:;volume 048:;issue 002::page 329
    Author:
    Liu, Xinan
    DOI: 10.1175/JPO-D-17-0172.1
    Publisher: American Meteorological Society
    Abstract: AbstractThe effects of wind on the impact of a single water drop on a deep-water surface are studied experimentally in a wind tunnel. Experiments are performed by varying impacting drop diameters, ranging from 2.5 to 4.1 mm and wind speeds up to 6.7 m s?1. The sequence of splashing events that occurred during drop impacts is recorded with a backlit, cinematic shadowgraph technique. The experimental results show that for low wind speeds, an asymmetrical crown forms on the leeward of the periphery of the colliding region after the drop hits the water surface, while a wave swell forms on the windward. Secondary droplets are generated from the crown rim. For high wind speeds with large drop diameters, ligaments are generated from the crown rim on the leeward of the drop impact site. The ligaments grow, coalesce, and fragment into secondary droplets. It is found that both the drag force and surface tension play important roles in the evolution process of the ligaments. The nondimensional K number (K = WeOh?0.4, where We is the Webber number and Oh is the Ohnesorge number) is used to describe the splashing-deposition limit of drop impact. The threshold value of this K number changes with the wind velocity and/or drop impact angle.
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      Experimental Study of Drop Impact on Deep-Water Surface in the Presence of Wind

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4260908
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    contributor authorLiu, Xinan
    date accessioned2019-09-19T10:02:38Z
    date available2019-09-19T10:02:38Z
    date copyright1/8/2018 12:00:00 AM
    date issued2018
    identifier otherjpo-d-17-0172.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4260908
    description abstractAbstractThe effects of wind on the impact of a single water drop on a deep-water surface are studied experimentally in a wind tunnel. Experiments are performed by varying impacting drop diameters, ranging from 2.5 to 4.1 mm and wind speeds up to 6.7 m s?1. The sequence of splashing events that occurred during drop impacts is recorded with a backlit, cinematic shadowgraph technique. The experimental results show that for low wind speeds, an asymmetrical crown forms on the leeward of the periphery of the colliding region after the drop hits the water surface, while a wave swell forms on the windward. Secondary droplets are generated from the crown rim. For high wind speeds with large drop diameters, ligaments are generated from the crown rim on the leeward of the drop impact site. The ligaments grow, coalesce, and fragment into secondary droplets. It is found that both the drag force and surface tension play important roles in the evolution process of the ligaments. The nondimensional K number (K = WeOh?0.4, where We is the Webber number and Oh is the Ohnesorge number) is used to describe the splashing-deposition limit of drop impact. The threshold value of this K number changes with the wind velocity and/or drop impact angle.
    publisherAmerican Meteorological Society
    titleExperimental Study of Drop Impact on Deep-Water Surface in the Presence of Wind
    typeJournal Paper
    journal volume48
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-17-0172.1
    journal fristpage329
    journal lastpage341
    treeJournal of Physical Oceanography:;2018:;volume 048:;issue 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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