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Measuring the Earth’s magnetic field in a laboratory
Physics Education, 2008Two methods for measuring the Earth's magnetic field are described. In the former, according to Gauss, the Earth's magnetic field is compared with that of a permanent magnet; in the latter, a well-known method, the comparison is made with the magnetic field generated by a current.
CARTACCI, ANNA MARIA, STRAULINO, SAMUELE
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Fall in Earth's Magnetic Field Is Erratic
Science, 2006Earth's magnetic field has decayed by about 5% per century since measurements began in 1840. Directional measurements predate those of intensity by more than 250 years, and we combined the global model of directions with paleomagnetic intensity measurements to estimate the fall in strength for this earlier period (1590 to 1840 A.D.).
David, Gubbins +2 more
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2023
Abstract Legendary anecdotes relate how Greco-Roman and Chinese societies may have first become aware of magnetism. For centuries it was thought to be a celestial power, but scientists learned through experimental investigations how magnetism is related to electrical currents.
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Abstract Legendary anecdotes relate how Greco-Roman and Chinese societies may have first become aware of magnetism. For centuries it was thought to be a celestial power, but scientists learned through experimental investigations how magnetism is related to electrical currents.
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The Room with the Weakest Magnetic Field on Earth
Scientific American, 2015The article discusses a room at the Technical University of Munich in Germany which is designed to contain the weakest magnetic field in the solar system. Physicists will be able to use the room for research on topics such as antimatter, magnetic monopoles, dark matter, and the role of magnetic fields in animal navigation.
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Magnetic disturbances and the Earth's magnetic field
Journal of Geophysical Research, 1961An attempt is made to explain the origin of the observed magnetic field of the earth as being due to a current system circulating in the core, the current system in its turn being maintained by world-wide magnetic disturbances. The mantle behaves as a semiconductor, and the conduction electron density is given by the Boltzmann distribution law.
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Reversals of the Earth's Magnetic Field
Scientific American, 1967A, Cox, R R, Doell, G B, Dalrymple
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Electric Field Control of the Magnetic Weyl Fermion in an Epitaxial SrRuO3 (111) Thin Film
Advanced Materials, 2021Weinan Lin, Liang Liu, Xinyu Shu
exaly

