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Geothermal energy is a renewable resource that draws on the Earth's internal heat to provide both electricity and direct heating, with a long history of human use and a contemporary role that continues to expand.

Geothermal energy refers to thermal energy extracted from the Earth's crust, originating from both the planet's formation and ongoing radioactive decay. It can be accessed through naturally occurring hot springs, engineered reservoirs, or shallow ground heat for heating and cooking.

Modern geothermal systems tap underground reservoirs of hot water or steam through wells, bringing heat to the surface for electricity generation, direct heating, or geothermal heat pumps.

People have used geothermal heat for thousands of years. Hot springs were used for bathing as early as Paleolithic times. The Romans used geothermal waters for public baths and underfloor heating. The oldest geothermal district heating system began operating in Chaudes-Aigues, France, in the 15th century. Industrial use began in the 19th century, when geyser steam was used to extract boric acid from volcanic mud.

Geothermal power plants convert underground heat into electricity. They operate most effectively where hot water or steam is located close to the surface, often near tectonic plate boundaries. Geothermal plants produce constant, weather-independent power, and costs have fallen significantly since the 1980s. Internationally, Indonesia and Kenya are major producers, with Kenya generating 45% of its electricity from geothermal sources.

Geothermal heating takes two main forms: direct use and district heating, and geothermal heat pumps (GHPs).

Hot water from shallow reservoirs is piped directly into buildings or used for industrial processes such as food drying and greenhouse heating. Reykjavik, Iceland, is a leading example of city-scale geothermal district heating.

Geothermal heat pumps use the stable temperature of shallow ground to heat and cool buildings efficiently. They work by transferring heat between the ground and indoor spaces.

Geothermal systems include direct use systems (which tap naturally warm water near the surface), geothermal power plants (which require high-temperature water or steam), and geothermal heat pumps (which use shallow ground temperatures for heating and cooling).

Today, geothermal energy supports electricity generation, residential and commercial heating and cooling, industrial processes (drying, pasteurizing, mining), agricultural applications (greenhouses, aquaculture), and spas and recreational uses. Worldwide, an additional 28 GW of geothermal heat is used for non-electric applications.

Geothermal energy is considered renewable because the Earth continuously produces internal heat. Resources are vast - more than sufficient to meet global energy needs if accessed effectively.

Environmental impacts include low emissions (geothermal plants emit far less carbon dioxide than fossil fuels), a small land footprint (facilities require less space than solar or wind installations), water use (some systems require water for reinjection or cooling), induced seismicity (enhanced geothermal systems can trigger small earthquakes due to fluid injection), and localized impacts (potential release of trace gases or minerals from underground reservoirs). Overall, geothermal energy is among the cleanest and most reliable renewable energy sources, with manageable environmental impacts when properly regulated.

 

 

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