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The Sun is a yellow dwarf of spectral class G2V, the central star of our system. Its mass is about 2×10³⁰ kg. In the core, at a temperature of 15 million kelvin, thermonuclear fusion occurs: the proton-proton chain turns hydrogen into helium-4, releasing neutrinos and gamma rays. Energy is transferred first by radiation, and closer to the surface by convection. The visible surface (photosphere) has a temperature of 5778 K and is covered with granules — convective cells. Above it are the chromosphere and corona, heated to millions of degrees (the heating mechanism is not fully clear). The Sun's activity follows an 11-year cycle, which affects the number of sunspots and flare frequency.

History

The Sun was worshipped since ancient times. In the 19th century, Joseph Fraunhofer discovered dark lines in its spectrum, and in 1925, Cecilia Payne-Gaposchkin proved that the Sun consists mainly of hydrogen. In the 20th century, physicists uncovered the source of its energy — thermonuclear fusion.

How it works

In the Sun's core, under enormous pressure and temperature, hydrogen nuclei fuse into helium, releasing energy. This energy slowly pushes through the star's bulk to the surface and is radiated into space. Thus the Sun has been shining for 4.6 billion years and will last about as long again.

💡 The Sun loses mass at a rate of about 4 million tons per second due to radiation and the solar wind, but even over billions of years this will amount to a minuscule fraction of a percent.
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Scientists
Joseph von FraunhoferCecilia Payne-Gaposchkin
Related tags
gravityheliummagnetic reconnectionnuclear fusionSolar windspectroscopystar formationstellar evolution
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Stefan–Boltzmann law

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