Abstract: An antenna system for radiating information in the ELF range is disclosed and comprises an extended conductor sized to produce a corona at the operating voltage. In the preferred embodiment, "ultra-thin" wire is used as the antenna element for weight savings and is lofted by means of a tether line which absorbs the stresses. Means are provided for helically winding the antenna element around the tether line.

Abstract: The separation of isotopes is accomplished by scattering a beam of particles from a standing electromagnetic wave. The particles may consist of either atoms or molecules, each having a desired isotope and at least one other. The particle beam is directed in a normal direction against the standing wave, which may be a light wave. The particles; that is, the atomic or molecular quantum-mechanical waves, see basically a diffraction grating corresponding to the troughs and peaks of the electromagnetic wave. The frequency of the electromagnetic wave substantially corresponds to an internal energy level-transition of the desired isotope. Accordingly, the desired isotope is spatially separated by being scattered or diffracted.

Abstract: A vertical dipole antenna for the ELF (extremely low frequency) range. The antenna provides a series resonant circuit consisting of an inductor and the distributed capacitance of the conductor such as a wire which may be carried by lighter-than-air craft. The lighter-than-air craft may be conductive, in which case it contributes to the capacitance or the capacitance may be solely represented by the wire. The antenna may be frequency or phase modulated. In case of frequency modulation the frequency of the generator must be changed accordingly so that the series resonant circuit remains resonant at the frequency to be radiated. The antenna can be readily moved. A plurality of antennas may be provided to form a super-radiant array.

Abstract: There is disclosed a method and apparatus for measuring electromagnetic conductivity within a medium to thereby derive a measurement of the rate of propagation of a magnetic field therein. If one then measures the return time of a pulse transmitted in the medium when a conductivity anomaly is encountered which creates a reflection, a magnetic diffusion radar can be calibrated. This technique enables one to measure the conductivity of a propagation medium such as salt water, earth or the like for any desired purpose such as determining the salinity of sea water or river water. More particularly, however, this enables one to make such a measurement in order to provide an electromagnetic anomaly detector such as is used in metal locaters, mine detectors, and in geophysical prospecting or exploration.