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Red dwarfs are M-class stars (mass from 0.075 to 0.5 solar masses) with surface temperatures of 2000–3500 K. Their luminosity ranges from hundredths to a few percent of the Sun's. Thanks to full convection in their interiors, hydrogen is consumed extremely sparingly, so their lifetime exceeds the age of the Universe, and no red dwarf has yet left the main sequence. Many have planets, and terrestrial-type planets often lie in the habitable zone.

History

The first red dwarfs were observed as early as the 19th century. In the early 20th century, astronomers identified them as a separate class of low-mass stars. For a long time, it was believed that they could not have planets with life, but modern discoveries have shown otherwise.

How it works

Inside a red dwarf, hydrogen turns into helium, releasing energy, but the reactions proceed slowly due to low core temperature and pressure. Unlike the Sun, the star's material is fully mixed: hydrogen from outer layers constantly flows into the core, and helium does not accumulate. Hence, the star shines stably for trillions of years.

💡 The closest red dwarf, Proxima Centauri, has an Earth-sized planet in the habitable zone, despite frequent powerful flares from the star.
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Scientists
Henri PoincaréSubrahmanyan Chandrasekhar
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biosignatureselectromagnetismexoplanetgravitymagnetic reconnectionnuclear fusionspectroscopystar formation
Laws
virial theorem

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