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Geothermal gradient - Wikipedia
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Geothermal heating - Wikipedia
WebLa géothermie profonde est une évidence.🌍 Elle est de plus en plus mise en œuvre par les pouvoirs publics de nombreux pays pour alimenter les réseaux de chauffage urbains et diminuer la part des énergies fossiles. Geothermal energy is the thermal energy in the Earth's crust which originates from the formation of the planet and from radioactive decay of materials. The high temperature and pressure in Earth's interior cause some rock to melt and solid mantle to behave plastically. This results in parts of the mantle convecting upward since it is lighter than the surrounding rock. Temperatures at the core–mantle boundary can reach over 4000 °C (7200 °F). Geothermal gradient is the rate of temperature change with respect to increasing depth in Earth's interior. As a general rule, the crust temperature rises with depth due to the heat flow from the much hotter mantle; away from tectonic plate boundaries, temperature rises in about 25–30 °C/km (72–87 °F/mi) of depth near the surface in most of the world. However, in some cases the temperature may drop with increasing depth, especially near the surface, a phenomenon know… h-mtd adapter