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My idea is a carbon planet 50 % larger than Earth and with 5 times its mass (approximately), but I set these values ​​after investigating those of several discovered exoplanets and none of them is considered a carbon planet, they are probably more similar to Earth in terms of their internal composition.

I understand that the planets of carbon could have a mantle of carbides instead of one of silicates as with Earth; and if they are massive enough, they could have a diamond layer near their core. Would there be any significant change with the mass of the planet considering an internal composition like this? I mean, I understand that the mass of exoplanets is estimated considering an internal composition like that of the Earth, but the fact that the planet has, for example, a mantle of carbides instead of one of silicates, would the mass be different?

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  • $\begingroup$ Are you asking about mass estimation based on measured radius? $\endgroup$ – Arkenstein XII Aug 14 at 3:57
  • $\begingroup$ That's right. Also considered the influence of the internal composition (carbon or silicon), if any. $\endgroup$ – URIZEN Aug 14 at 4:08
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    $\begingroup$ Generally, volume scales as radius cubed ($r^3$). Assuming the same density, mass scales with volume. Replacing Si with C, the mass ratio is 12:28, based on atomic masses, so about half the mass. In your case, $1.5^3*12/28$ times Mass of the Earth should give a rough approximation $\endgroup$ – nzaman Aug 14 at 6:21
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Short version:

It'll be heavier than an Earth-like world the same size but we can't actually work out how heavy.

Long version: Carbon Planets aren't really made of carbon, they just have enough carbon, as a molar fraction, that it can't all react with the available oxygen and hydrogen so you can get pure carbon that can't be oxidised into CO, CO2 or the CO3-2 Carbonate ion or converted into simple organic compounds like CH4. So as well as borate, carbonate and silicate rocks, which will be holding most of the world's oxygen, there would also be some borides, carbides and silicides but not necessarily in large volumes and they'll tend to be in the mantle as they're much denser than their oxygen bearing counterparts.

Given the rarefaction process that needs to occur to form a Carbon Planet they're going to be quite dense, since they lack not only hydrogen and oxygen, and thus water, but also light halogens and also some of the lighter metals like lithium. There will be relatively more heavy metals and more of them will be in their pure (unoxidised) state so they'll pack together tighter under pressure, especially when hot. The mantle will be denser so the diamond belt (this is about 900km down on Earth), where diamond becomes the most stable form of pure carbon, will be closer to the crust but they're a bit less likely to migrate to the surface because the mantle is denser.

Overall mass is impossible to make an exact quantitative call on; the world will certainly be denser than Earth but it already would have been because it's bigger, therefore more massive, and therefore has higher core pressure and density. It will also have a higher pressure/depth gradient due to the reduced level of oxygen in the mantle increasing its density. Density gradients are never more than estimates and have proved extremely problematic to calculate let alone predict based on composition. So we can't really work out a solid figure for the average planetary density and thus get a good prediction for total mass.

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