Equipotential surface


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Related to Equipotential surface: electric dipole
Translations
Äquipotentialfläche
References in periodicals archive ?
2 show the correspondence of the mesopause with the main equipotential surface [40; [infinity]] = 90 km of the fundamental field F, calibrated on the electron wavelength.
The geoid is defined as an equipotential surface of the constant gravity potential W,
Conducted Current Density, I, is the vector quantity of current passing through a unit area of an equipotential surface; it is the product of the electrical conductivity and the electric field intensity.
Although the rotation of Venus [31] is retrograde, its rotation period of 5816.66728 hours fits perfectly with the main temporal equipotential surface [65; [infinity]] of the electron F:
(2.3) it follows that if the fluid surface is the equipotential surface [W.sub.2] = const, then the function V(p) is constant.
Accordingly, the equipotential surfaces of the Earth are curved (Fig.
Two equipotential surfaces of equal and opposite potentials are thus generated defines the profile of the biconical antenna.
Geopotential numbers are determined in GRS 80 normal field, applying the new European gravity system and evaluating non-linearity of GRS 80 normal field equipotential surfaces (Moritz 1988).

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