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    Disintegration of Pairs of Drops Raised to Equal and Opposite Potentials

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 001::page 66
    Author:
    Azad, A. K.
    ,
    Latham, J.
    DOI: 10.1175/1520-0469(1968)025<0066:DOPODR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In order to assess quantitatively the role of drop disintegrations in producing the electrification of warm clouds, it is necessary to establish the electrohydrodynamical equations governing the stability of drops subjected to electrical forces. In the present paper a theoretical and experimental study is presented of the disintegration of drops raised to equal and opposite potentials. In his theoretical treatment of the deformation and disintegration of individual water drops of undistorted radius R0 raised to a potential V, Taylor assumed that the drop retained a spheroidal shape until the instability point was reached and that the equations of equilibrium between the stresses due to surface tension T, the potential V, and the difference between the external and internal pressures was satisfied at the poles and the equator. He showed that since there is no stationary value for V as the elongation a/b increases, the only stable condition is when the drop is stable and V(πR0T)?½ < 4. Taylor's spheroidal assumption has been applied to the problem of the deformation and disintegration of pairs of drops raised to equal and opposite potentials. In this case directionality is imposed upon the problem by the attractive forces between the drops which provide a contribution, increasing with decreasing separation, to the outwardly-directed stresses in their surfaces. Stationary values of V were found to exist at values of a/b > 1, and the corresponding values of V(πR0T)?½ were less than 4.0 by a factor which increased rapidly as the initial separation was decreased. These critical values of V(πR0T)?½ at the disintegration point ranged from Rayleigh's value of 4.0 at infinite separations to 3.117, 6.842 ? 10?1, 2.880 ? 10?2 and 8.654 ? 10?4 for initial separations of 10, 1, 0.1 and 0.01 radii, respectively. These values of V(πR0T)?½ are slightly reduced for larger drops owing to the influence of the hydrostatic pressure difference between their vertical extremities. These calculations were tested experimentally on suspended drops of water, aniline and benzene, and good agreement was obtained in all cases. High speed photographs indicated that the process of disintegration was similar to that observed by Taylor, with an extremely rapid transformation (<10?8 sec) from an approximately spheroidal shape to a conical profile. Measurements taken from the photographs demonstrated that the radius of curvature and the elongation of a drop at the moment of disintegration agreed quite closely with the predicted values.
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      Disintegration of Pairs of Drops Raised to Equal and Opposite Potentials

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4151053
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    contributor authorAzad, A. K.
    contributor authorLatham, J.
    date accessioned2017-06-09T14:14:17Z
    date available2017-06-09T14:14:17Z
    date copyright1968/01/01
    date issued1968
    identifier issn0022-4928
    identifier otherams-15387.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151053
    description abstractIn order to assess quantitatively the role of drop disintegrations in producing the electrification of warm clouds, it is necessary to establish the electrohydrodynamical equations governing the stability of drops subjected to electrical forces. In the present paper a theoretical and experimental study is presented of the disintegration of drops raised to equal and opposite potentials. In his theoretical treatment of the deformation and disintegration of individual water drops of undistorted radius R0 raised to a potential V, Taylor assumed that the drop retained a spheroidal shape until the instability point was reached and that the equations of equilibrium between the stresses due to surface tension T, the potential V, and the difference between the external and internal pressures was satisfied at the poles and the equator. He showed that since there is no stationary value for V as the elongation a/b increases, the only stable condition is when the drop is stable and V(πR0T)?½ < 4. Taylor's spheroidal assumption has been applied to the problem of the deformation and disintegration of pairs of drops raised to equal and opposite potentials. In this case directionality is imposed upon the problem by the attractive forces between the drops which provide a contribution, increasing with decreasing separation, to the outwardly-directed stresses in their surfaces. Stationary values of V were found to exist at values of a/b > 1, and the corresponding values of V(πR0T)?½ were less than 4.0 by a factor which increased rapidly as the initial separation was decreased. These critical values of V(πR0T)?½ at the disintegration point ranged from Rayleigh's value of 4.0 at infinite separations to 3.117, 6.842 ? 10?1, 2.880 ? 10?2 and 8.654 ? 10?4 for initial separations of 10, 1, 0.1 and 0.01 radii, respectively. These values of V(πR0T)?½ are slightly reduced for larger drops owing to the influence of the hydrostatic pressure difference between their vertical extremities. These calculations were tested experimentally on suspended drops of water, aniline and benzene, and good agreement was obtained in all cases. High speed photographs indicated that the process of disintegration was similar to that observed by Taylor, with an extremely rapid transformation (<10?8 sec) from an approximately spheroidal shape to a conical profile. Measurements taken from the photographs demonstrated that the radius of curvature and the elongation of a drop at the moment of disintegration agreed quite closely with the predicted values.
    publisherAmerican Meteorological Society
    titleDisintegration of Pairs of Drops Raised to Equal and Opposite Potentials
    typeJournal Paper
    journal volume25
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1968)025<0066:DOPODR>2.0.CO;2
    journal fristpage66
    journal lastpage75
    treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 001
    contenttypeFulltext
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