This is the atmospheric layer that covers the surface of the Sun and other stars, and most of the light energy that these stars radiate into space is emitted directly from here. The atoms involved in absorbing and emitting radiant energy are mainly negative hydrogen (neutral hydrogen ions with one electron added to them, giving them a negative charge). This thickness is small compared to the size of the star, except for supergiants. For the Sun, it is about 500 kilometers, which is only about 0.06% of the solar radius. When the temperature of the photosphere is high, it mainly emits ultraviolet light, and when it is low, it emits infrared light. Stars can be seen to be bluish-white or reddish, which is due to differences in the temperature of the photosphere. [Hiei Eijiro] [References] | |Source: Shogakukan Encyclopedia Nipponica About Encyclopedia Nipponica Information | Legend |
太陽や恒星の表面を覆う大気層であり、これらの星々が宇宙空間に放射している光のエネルギーの大部分の量が、ここから直接放出されている。放射エネルギーの吸収・放射に関与している原子は、おもに負水素(中性な水素に電子1個が加わり負の電荷を帯びたイオン)である。この厚みは、超巨星を除いて、星の大きさに比べて小さい。太陽では約500キロメートルで太陽半径の約0.06%にすぎない。光球の温度が高いと紫外線をおもに放射し、低温の場合は赤外線を放射する。恒星には青白いものや赤みがかったものが見られるが、これは光球の温度の違いによる。 [日江井榮二郎] [参照項目] | |出典 小学館 日本大百科全書(ニッポニカ)日本大百科全書(ニッポニカ)について 情報 | 凡例 |
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