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cossatot | 1 year ago
The belts themselves are an effect of Earth's magnetic field, which I believe is particularly strong because of flow within the Earth's liquid iron-nickel outer core. (I had long believed that the spinning of the inner core was the primary contributor but given a surface-level skim of the literature that doesn't seem to be the case; convection seems to be more of a driver.)
I think perhaps many otherwise similar planets don't have a liquid iron core, so they may not have the strong radiation belts that shield life from the solar wind. Of course I am not sure what fraction of otherwise-similar planets have liquid iron cores, but Mars for example does not seem to. It is probably a function of the size of a planet (governing the pressure distribution in the interior), the ratio of iron to other elements, the temperature field (a function of the amount of radiogenic elements in the planet and its age), and perhaps other factors. Other planets may not be hot enough to have a liquid iron core at the right pressures, or be too massive (too much pressure) at the right temperatures, etc.
groos|1 year ago
But there is one more factor. In the absence of a magnetic field, gas molecules can dissociate from being hit with the particles from the solar wind. E.g., water can dissociate into oxygen and hydrogen, and hydrogen having a relatively high RMS velocity readily leaks out to space. The remaining oxygen is too reactive to remain and then forms carbonates in rocks and carbon dioxide in the atmosphere. This is, from what I read, the explanation for the atmospheres of both Mars and Venus, which have only a small to non-existent magnetic field.
So yes, a magnetic field seems to be essential to holding a life-friendly atmosphere.
s1artibartfast|1 year ago
perihelions|1 year ago
dekhn|1 year ago
doctoboggan|1 year ago
jordanb|1 year ago