Special Issue: Ground Magnetic Observations: New technologies and the role in understanding the Earth System
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Theodolite-borne vector Overhauser magnetometer: DIMOVER
Earth, Planets and Space volume 58, pages 711–716 (2006)
Abstract
This report covers results of the long-term research directed at developing an absolute vector proton magnetometer based on the switching of bias magnetic fields. The distinctive feature is the attempt of the installation of a miniature Overhauser sensor and optimized Garret solenoid directly on the telescope of the theodolite. Thus this design (Declination Inclination Modulus Overhauser magnetometer: DIMOVER) will complement the universally recognised DIflux absolute device by adding full vector measurement capability. Preliminary designs, which also can be interesting to the experts in vector proton magnetometers, are presented.
References
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Lauridsen, K. E., Experiences with the DI-fluxgate Magnetometer Inclusive Theory of the Instrument and Comparison with Other Methods, Danish Meteorological Institute Geophysical Papers, R–71, 1985.
Serson, P. H., Method of making an electromagnetic measurement, Ottawa, Ontario, Canada, CANADIAN PATENT No. 654, 552, Issued Dec. 1962, CLASS 324-1.
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Sapunov, V., Rasson, J., Denisov, A. et al. Theodolite-borne vector Overhauser magnetometer: DIMOVER. Earth Planet Sp 58, 711–716 (2006). https://doi.org/10.1186/BF03351972
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DOI: https://doi.org/10.1186/BF03351972