HR: 16:40h
AN: SA54A-02 INVITED [Abstracts]
TI: Laboratory Experiments of Helicity or Vortex Generation in an Electric Quadrupole: Simulation of Tonadoes with and without Lightning
AU: * Kikuchi, H
EM: hkikuchi@mars.dti.ne.jp
AF: Institute for Environmental Electromagnetics, 3-8-18, Komagome, Toshima-ku, Tokyo, 170,
Japan
AB:
Laboratory Experiments of Helicity or Vortex Generation in an Electric Quadrupole: Simulation of Tornadoes with
and without Lightning
H. Kikuchi
Institute for Environmental Electromagnetics
3-8-18, Komagome, Toshima-ku, Tokyo 170, Japan
e-mail: hkikuchi@mars.dti.ne.jp
Abstract
Usually the source-origins of helicity or vortex generation have been considered to be thermohydrodynamic in the
hydrodynamic (HD) regime and/or magnetohydrodynamic in the magnetohydrodynamic (MHD) regime. It has
been shown, however, by the present author that an electric quadrupole is also capable for helicity or vortex
generation and a new electric helic- ity defined as hE= v·E (v: flow velocity; E: electric field) has been
introduced. Accordingly, we have now three kinds of helicity, namely fluid, magnetic, and electric helicity. In many
cases of atmospheric and space electricity phenomena in nature, electric helicity or vortex generation of electric
origin is involved as typically seen in tornadic thunderstorms. Conventional theory of tornadoes, however, space-
charge and electric fields have never been considered properly so far, surprisingly in spite of their effects of
significance, because of no theorv for such cases, although those effects have been recognized implicitly by field
experiments. This paper fills up these demands by newly introducing the concept of 'Electric Helicity' based
on 'Electrohydrodynamics' (EHD) established and developed over the last more than two decades and such a
whole theory is applied to tornadioes with and without lightning. Further, experimental evidence of this theory is
presented for the first time by using a 'universal electric-cusp type plasma reactor' designed more than a
decade ago [1]. This device is composed of two positive and negative electrodes of lead spheres 1.5 cm in
diameter suspended 2~5 cm above a copper plane on which a semispherical lead 1.25 cm in diameter or its
modified object is placed. A whole setup is arranged in a wooden box whose back and both sides are covered by
black papers to prevent scattered and reflected light while its front side is open. We are particularly focusing on
'significance of electric quadrupole(s) in helicity and vortex generation',taking photos of wind flows with the
use of a bunch of incense sticks burned and placed on the semispherical lead at the cusp center in the reactor.
With increasing both electrode voltages from zero to a certain kV, ascending straight wind flows turn to be
cyclonic separately toward the both electrodes. As soon as electric discharge from both electrodes to object starts
at a certain breakdown voltage, typically 20~30 kV, wind flows suddenly turn to be violent and wind flows toward
negative electrode are still cyclonic but wind flows toward positive electrode become anticyclonic. These results
are shown by a number of photos taken and provide at the same time 'laboratory simulation of tonadoes with
and without lightning'.
[1] Kikuchi, H. Electrohydrodynamics in Dusty and Dirty Plasmas, Kluwer Academic Publishers, Dordrecht/The
Netherlands, 2001, pp.93-94.
DE: 0499 New fields (not classifiable under other headings)
DE: 0654 Plasmas
DE: 1704 Atmospheric sciences
DE: 2411 Electric fields (2712)
SC: SPA-Aeronomy [SA]
MN: 2007 Joint Assembly