Astralis-7, a tidally locked planet orbiting a K-type star at 0.4 AU, is a world of contrasts. Its day side is scorched by the relentless heat of its star, while its night side is plunged into frigid darkness. But between these two extremes is a habitable zone, where liquid water could flow and life could potentially thrive.
Tidal forces are more constant for planets with low eccentricity. This is because the distance between the planet and its star does not vary as much throughout the orbit. For planets with high eccentricity, the tidal forces vary as the planet moves around its orbit, which can make it more difficult for tidal locking to occur. In the case of ASTRALIS-7, its near-zero eccentricity means that the tidal forces exerted by its star are very constant. This allows the tidal forces to slow down Stellar's rotation until it matches its orbital period, resulting in tidal locking.
A perfect 0.8 solar mass of a k-type star and the corresponding distance of the planet from star of 0.4 AU justifies tidal locking
Astralis-7 iron-rich core is a dense and powerful heart, providing geothermal energy and regulating the planet's climate.
Astralis-7 iron-rich core generates a strong magnetic field. This magnetic field protects the planet from harmful radiation from its star, such as solar flares and coronal mass ejections. Harmful radiation can damage DNA and disrupt essential biological processes, making it difficult for life to survive.
Nitrogen serves as the atmospheric foundation, playing a vital role in plant protein synthesis. Bacteria fix it into the soil, forming nitrates essential for amino acids. Oxygen facilitates respiration by oxidizing respiratory substrates for energy release. Carbon dioxide acts as a greenhouse gas, reflecting heat to prevent daytime overheating and trapping it to establish convection currents and winds from the day side to the night side. Water vapor aids in distributing heat, maintaining slightly higher temperatures on the night side for the sustenance of life. Sulfur dioxide originates from sulfur-producing reactions in volcanic craters and geothermal springs.
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