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Concept
Courant tellurique
Résumé
A telluric current (from Latin tellūs, "earth"), or Earth current, is an electric current that flows underground or through the sea, resulting from natural and human-induced causes. These currents are extremely low frequency and traverse large areas near or at the Earth's surface. The Earth's crust and mantle are host to telluric currents, with around 32 mechanisms generating them, primarily geomagnetically-induced currents caused by changes in the Earth's magnetic field due to solar wind interactions with the magnetosphere or solar radiation's effects on the ionosphere. These currents exhibit diurnal patterns, flowing towards the Sun during the day and towards the poles at night.
Both telluric and magnetotelluric methods exploit these currents for subsurface exploration, aiding in activities like geothermal and mineral exploration, petroleum prospecting, fault zone mapping, groundwater assessment, and the study of tectonic plate boundaries. The phenomenon has also captured the imagination of authors, finding its way into fiction. In Umberto Eco's Foucault's Pendulum, the search for a mystic center of the Earth connects to telluric currents, while Thomas Pynchon's Mason & Dixon incorporates them as enigmatic communication conduits alongside Hollow Earth theories. These fictional representations mirror the scientific intrigue and creative potential linked with telluric currents.
Telluric currents are phenomena observed in the Earth's crust and mantle. In September 1862, an experiment to specifically address Earth currents was carried out in the Munich Alps (Lamont, 1862). Including minor processes, there are at least 32 different mechanisms which cause telluric currents. The strongest are primarily geomagnetically induced currents, which are induced by changes in the outer part of the Earth's magnetic field, which are usually caused by interactions between the solar wind and the magnetosphere or solar radiation effects on the ionosphere. Telluric currents flow in the surface layers of the Earth.
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