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    Electric Potential of a Rubbed Ice Surface

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 006::page 1259
    Author:
    Takahashi, Tsutomu
    DOI: 10.1175/1520-0469(1969)026<1259:EPOARI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The electric potential of an ice surface rubbed by a single crystal ice piece was investigated both theoretically and experimentally. The negative electric potential on the rubbed ice surface increased with increasing number of dislocations on the ice surface. In order to explain this negative electric potential of a rubbed ice surface, it was assumed that negatively electrified dislocations and positively electrified D-defects were produced in pairs by rubbing. In the steady state, a potential difference is set up at the surface such that the surface becomes negative because of the much greater mobility of D-defects than dislocation. On the bases of some theoretical arguments it is predicted that the surface potential is ?58 mV when the dislocation density at the ice surface is one order of magnitude larger than that in the interior of the ice. It is thought that these phenomena are of basic importance in the generation of positive electric charge of graupel pellets and hail at colder temperatures.
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      Electric Potential of a Rubbed Ice Surface

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4151414
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    contributor authorTakahashi, Tsutomu
    date accessioned2017-06-09T14:15:10Z
    date available2017-06-09T14:15:10Z
    date copyright1969/11/01
    date issued1969
    identifier issn0022-4928
    identifier otherams-15711.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151414
    description abstractThe electric potential of an ice surface rubbed by a single crystal ice piece was investigated both theoretically and experimentally. The negative electric potential on the rubbed ice surface increased with increasing number of dislocations on the ice surface. In order to explain this negative electric potential of a rubbed ice surface, it was assumed that negatively electrified dislocations and positively electrified D-defects were produced in pairs by rubbing. In the steady state, a potential difference is set up at the surface such that the surface becomes negative because of the much greater mobility of D-defects than dislocation. On the bases of some theoretical arguments it is predicted that the surface potential is ?58 mV when the dislocation density at the ice surface is one order of magnitude larger than that in the interior of the ice. It is thought that these phenomena are of basic importance in the generation of positive electric charge of graupel pellets and hail at colder temperatures.
    publisherAmerican Meteorological Society
    titleElectric Potential of a Rubbed Ice Surface
    typeJournal Paper
    journal volume26
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1969)026<1259:EPOARI>2.0.CO;2
    journal fristpage1259
    journal lastpage1265
    treeJournal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 006
    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
    yabeshDSpacePersian