THE BIVORTEX QUADRUPOLE FIELD
Copyright 2004 George William Kelly

The bivortex particle can be visualized with an ordinary apple as its model.

Imagine the apple as rotating, or spinning. The subparticles that compose this apple bivortex particle flow along field lines that collectively form the shape of the apple. Indeed, the flowing particles constitute the field lines of the bivortex. On the upper half (the stem end) of the apple the subparticles flow into the vortex at the apple's north pole. On the lower half of the apple subparticles flow into the vortex at the apple's south pole. The subparticles spiral into the vortex counterclockwise at the north pole and clockwise at the south pole, in keeping with the Coriolis effect that has long been observed in the earth's weather patterns. Both streams flow into the axial tube (the core of the apple) that connects the two vortexes. At the centerpoint of the tube the two highly focused streams of subparticles collide. The explosions from these collisions radiate subparticles outward from the center of the bivortex apple. The attraction of the rapidly spinning tube, however, pulls these subparticles back to the tube's wall in successive field line arches, either northward or southward from the equatorial plane. The effect is to create the apple's equatorial bulge. Since the escape potential of these radiated subparticles is greatest at the equatorial plane, the field line arches become larger and larger approaching the equatorial surface of the apple.

The flow of bivortex subparticles described above suggests that the apple bivortex field must be a quadrupole field. This differs sharply from the view that the Earth is a dipole magnet whose field lines emerge from one pole and converge at the opposite pole. The dipole concept has been around since the days of William Gilbert and Michael Faraday. It is familiar to schoolchildren who have conducted the famous bar-magnet-with-iron-filings experiment. The field lines of the bivortex, however, emerge as oppositely directed loops from the equatorial plane. These matching sets of bivortex quadrupole field lines diverge in radial succession along the equatorial plane or disk. The northward hemispherical flow lines converge at the north pole, and the southward hemispherical flow lines converge at the south pole. If the Earth is a bivortex body, the Earth should have a quadrupole field instead of a dipole field.

The bivortex quadrupole field flow pattern follows the same pattern as that obtained with a Helmholtz Coil. In the Helmholtz Coil the flow is inward at both poles and outward at the equator. Similarly in the bivortex field there is a helical flow of subparticles down the bivortex tube from both poles toward the center of the tube. The helical flow essentially forms the cylindrical wall of the bivortex tube. The turns or coils of the helices pack closer and closer together as they approach the centerpoint of the tube. They become more perpendicular to the bivortex rotational axis than when they entered as stretched-out spirals. When they reach the center, they radiate outward in a flattened spiral flow along the equatorial plane, gradually spiraling again toward the poles to complete the spheroidal form of the bivortex body.
- posted by George William Kelly @ 3:02 PM