MadSci Network: Physics |
I guess you are referring to the classical variometer of declination, a device that can measure the horizontal component of the geomagnetic field. The description of such an aparatus is too complex and full of details in order to make an operational instrument, but I'll give you some fundamentals of the method, and a reference where you can find an extensive description of the classical magnetometers. The classical variometers are based on the fact that a magnet of moment M in a field H experiences a torque L such that L = M x H (in vectorial notation) So, a freely suspended magnet with the axis of suspension parallel to the z axis (the vertical) can rotate in the xy plane (horizontal) and the equilibrium position can be reached when a restoring torque is applied to balance the torque L. You can find information about these variometers in Laursen, V. & Olsend, J., 1971, Classical methods of geomagnetic observatories. In Encyclopaedia of Physics, vol. 49/3, Geophysics III. Springer-Verlag, Berlin, Heidelberg, New York. or Jacobs, J.A. (Editor), 1987, Geomagnetism, Vol. 1, Academic Press Limited, 627pp. Best regards Eder C. Molina Dept. of Geophysics Institute of Astronomy and Geophysics University of Sao Paulo - BRASIL eder@iag.usp.br
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