Given the mass and composition of a planet, can one determine what the radius should be?

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I'm trying to auto-generate random solar systems, and I'm basically just allocating 2% of the total system mass to planets (and moons). It provides interesting results, I always have a few gas giants, I often have many Mars-and-Mercury-massed planets.



But to calculate surface gravity, I need a radius.



This largely depends on the planet's composition... which can be quite varied (and depends quite a bit on where it formed, how it formed, etc).



But if I have a planet with 0.7 Earth mass, and 35% of that is iron/nickel (or siderophile), and 50% lithophile, and so on, can a decent estimate of radius be determined?



Do I need the breakdown on composition to be per atomic element, or can this give decent ballpark numbers if I have the mass as the ratio of lithophile/siderophile/chalcophile/volatiles?



My understanding of physics in this arena is... inadequate. I do not believe it's enough to simply look up the density of these elements on Wikipedia and calculate backwards from volume. Certainly an iron core compresses a bit such that the density is quite higher than that of an iron ingot on the surface?










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  • You may wish to look into hydrostatic equilibrium. Disclaimer: it is not simple if you want to do this exactly.
    – Joe Bloggs
    1 hour ago










  • @JoeBloggs Ahhh! Friends don't link friends to mobile Wikipedia! If you are on a cell phone you will be auto-redirected from the normal to mobile version...
    – kingledion
    12 mins ago















up vote
6
down vote

favorite
2












I'm trying to auto-generate random solar systems, and I'm basically just allocating 2% of the total system mass to planets (and moons). It provides interesting results, I always have a few gas giants, I often have many Mars-and-Mercury-massed planets.



But to calculate surface gravity, I need a radius.



This largely depends on the planet's composition... which can be quite varied (and depends quite a bit on where it formed, how it formed, etc).



But if I have a planet with 0.7 Earth mass, and 35% of that is iron/nickel (or siderophile), and 50% lithophile, and so on, can a decent estimate of radius be determined?



Do I need the breakdown on composition to be per atomic element, or can this give decent ballpark numbers if I have the mass as the ratio of lithophile/siderophile/chalcophile/volatiles?



My understanding of physics in this arena is... inadequate. I do not believe it's enough to simply look up the density of these elements on Wikipedia and calculate backwards from volume. Certainly an iron core compresses a bit such that the density is quite higher than that of an iron ingot on the surface?










share|improve this question























  • You may wish to look into hydrostatic equilibrium. Disclaimer: it is not simple if you want to do this exactly.
    – Joe Bloggs
    1 hour ago










  • @JoeBloggs Ahhh! Friends don't link friends to mobile Wikipedia! If you are on a cell phone you will be auto-redirected from the normal to mobile version...
    – kingledion
    12 mins ago













up vote
6
down vote

favorite
2









up vote
6
down vote

favorite
2






2





I'm trying to auto-generate random solar systems, and I'm basically just allocating 2% of the total system mass to planets (and moons). It provides interesting results, I always have a few gas giants, I often have many Mars-and-Mercury-massed planets.



But to calculate surface gravity, I need a radius.



This largely depends on the planet's composition... which can be quite varied (and depends quite a bit on where it formed, how it formed, etc).



But if I have a planet with 0.7 Earth mass, and 35% of that is iron/nickel (or siderophile), and 50% lithophile, and so on, can a decent estimate of radius be determined?



Do I need the breakdown on composition to be per atomic element, or can this give decent ballpark numbers if I have the mass as the ratio of lithophile/siderophile/chalcophile/volatiles?



My understanding of physics in this arena is... inadequate. I do not believe it's enough to simply look up the density of these elements on Wikipedia and calculate backwards from volume. Certainly an iron core compresses a bit such that the density is quite higher than that of an iron ingot on the surface?










share|improve this question















I'm trying to auto-generate random solar systems, and I'm basically just allocating 2% of the total system mass to planets (and moons). It provides interesting results, I always have a few gas giants, I often have many Mars-and-Mercury-massed planets.



But to calculate surface gravity, I need a radius.



This largely depends on the planet's composition... which can be quite varied (and depends quite a bit on where it formed, how it formed, etc).



But if I have a planet with 0.7 Earth mass, and 35% of that is iron/nickel (or siderophile), and 50% lithophile, and so on, can a decent estimate of radius be determined?



Do I need the breakdown on composition to be per atomic element, or can this give decent ballpark numbers if I have the mass as the ratio of lithophile/siderophile/chalcophile/volatiles?



My understanding of physics in this arena is... inadequate. I do not believe it's enough to simply look up the density of these elements on Wikipedia and calculate backwards from volume. Certainly an iron core compresses a bit such that the density is quite higher than that of an iron ingot on the surface?







planets gravity






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edited 3 hours ago









kingledion

66k22217376




66k22217376










asked 3 hours ago









John O

1965




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  • You may wish to look into hydrostatic equilibrium. Disclaimer: it is not simple if you want to do this exactly.
    – Joe Bloggs
    1 hour ago










  • @JoeBloggs Ahhh! Friends don't link friends to mobile Wikipedia! If you are on a cell phone you will be auto-redirected from the normal to mobile version...
    – kingledion
    12 mins ago

















  • You may wish to look into hydrostatic equilibrium. Disclaimer: it is not simple if you want to do this exactly.
    – Joe Bloggs
    1 hour ago










  • @JoeBloggs Ahhh! Friends don't link friends to mobile Wikipedia! If you are on a cell phone you will be auto-redirected from the normal to mobile version...
    – kingledion
    12 mins ago
















You may wish to look into hydrostatic equilibrium. Disclaimer: it is not simple if you want to do this exactly.
– Joe Bloggs
1 hour ago




You may wish to look into hydrostatic equilibrium. Disclaimer: it is not simple if you want to do this exactly.
– Joe Bloggs
1 hour ago












@JoeBloggs Ahhh! Friends don't link friends to mobile Wikipedia! If you are on a cell phone you will be auto-redirected from the normal to mobile version...
– kingledion
12 mins ago





@JoeBloggs Ahhh! Friends don't link friends to mobile Wikipedia! If you are on a cell phone you will be auto-redirected from the normal to mobile version...
– kingledion
12 mins ago











1 Answer
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Mass, density and radius are related



Let $m$ be the mass of a planet.



For a given a density $rho$, the relationship between mass and volume is
$$beginalign
V &= frac43pi r^3\
m &= rho V = frac43pirho r^3
endalign$$



The bottom equation gives you your relations. Of the two variables you are interested in, mass ($m$) and radius ($r$), the solutions in terms of one another are:



$$beginalign
m&=frac43pirho r^3\
r&=sqrt[3]frac3m4pirho
endalign$$



Be careful with units! Always convert mass to kg, radius to m, and density to kg/m$^3$ to be safe.



What should density be?



Since you need density in both these equations, what are some reasonable densities for a planet?



Object/Planet Density (kg/m^3)
Earth's Inner Core 12800
Earth's Outer Core 9900
Earth 5510
Mercury 5430
Venus 5240
Mars 3930
Vesta (densest asteroid) 3420
Luna 3340
Ceres (largest asteroid) 2080
Ganymede 1940
Titan 1880
Neptune 1640
Jupiter 1330
Uranus 1270
A small chunk of water ice 934
Saturn 690


A lot goes into planetary density, and that could totally be its own question. Mass drives density; the bigger a planet the more gravity will compress it. Mercury has more iron (relatively) than Earth, but is less dense because Earth's gravity compresses its core more. But these values are some guidelines for solving the above equations.






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    1 Answer
    1






    active

    oldest

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    1 Answer
    1






    active

    oldest

    votes









    active

    oldest

    votes






    active

    oldest

    votes








    up vote
    6
    down vote













    Mass, density and radius are related



    Let $m$ be the mass of a planet.



    For a given a density $rho$, the relationship between mass and volume is
    $$beginalign
    V &= frac43pi r^3\
    m &= rho V = frac43pirho r^3
    endalign$$



    The bottom equation gives you your relations. Of the two variables you are interested in, mass ($m$) and radius ($r$), the solutions in terms of one another are:



    $$beginalign
    m&=frac43pirho r^3\
    r&=sqrt[3]frac3m4pirho
    endalign$$



    Be careful with units! Always convert mass to kg, radius to m, and density to kg/m$^3$ to be safe.



    What should density be?



    Since you need density in both these equations, what are some reasonable densities for a planet?



    Object/Planet Density (kg/m^3)
    Earth's Inner Core 12800
    Earth's Outer Core 9900
    Earth 5510
    Mercury 5430
    Venus 5240
    Mars 3930
    Vesta (densest asteroid) 3420
    Luna 3340
    Ceres (largest asteroid) 2080
    Ganymede 1940
    Titan 1880
    Neptune 1640
    Jupiter 1330
    Uranus 1270
    A small chunk of water ice 934
    Saturn 690


    A lot goes into planetary density, and that could totally be its own question. Mass drives density; the bigger a planet the more gravity will compress it. Mercury has more iron (relatively) than Earth, but is less dense because Earth's gravity compresses its core more. But these values are some guidelines for solving the above equations.






    share|improve this answer


























      up vote
      6
      down vote













      Mass, density and radius are related



      Let $m$ be the mass of a planet.



      For a given a density $rho$, the relationship between mass and volume is
      $$beginalign
      V &= frac43pi r^3\
      m &= rho V = frac43pirho r^3
      endalign$$



      The bottom equation gives you your relations. Of the two variables you are interested in, mass ($m$) and radius ($r$), the solutions in terms of one another are:



      $$beginalign
      m&=frac43pirho r^3\
      r&=sqrt[3]frac3m4pirho
      endalign$$



      Be careful with units! Always convert mass to kg, radius to m, and density to kg/m$^3$ to be safe.



      What should density be?



      Since you need density in both these equations, what are some reasonable densities for a planet?



      Object/Planet Density (kg/m^3)
      Earth's Inner Core 12800
      Earth's Outer Core 9900
      Earth 5510
      Mercury 5430
      Venus 5240
      Mars 3930
      Vesta (densest asteroid) 3420
      Luna 3340
      Ceres (largest asteroid) 2080
      Ganymede 1940
      Titan 1880
      Neptune 1640
      Jupiter 1330
      Uranus 1270
      A small chunk of water ice 934
      Saturn 690


      A lot goes into planetary density, and that could totally be its own question. Mass drives density; the bigger a planet the more gravity will compress it. Mercury has more iron (relatively) than Earth, but is less dense because Earth's gravity compresses its core more. But these values are some guidelines for solving the above equations.






      share|improve this answer
























        up vote
        6
        down vote










        up vote
        6
        down vote









        Mass, density and radius are related



        Let $m$ be the mass of a planet.



        For a given a density $rho$, the relationship between mass and volume is
        $$beginalign
        V &= frac43pi r^3\
        m &= rho V = frac43pirho r^3
        endalign$$



        The bottom equation gives you your relations. Of the two variables you are interested in, mass ($m$) and radius ($r$), the solutions in terms of one another are:



        $$beginalign
        m&=frac43pirho r^3\
        r&=sqrt[3]frac3m4pirho
        endalign$$



        Be careful with units! Always convert mass to kg, radius to m, and density to kg/m$^3$ to be safe.



        What should density be?



        Since you need density in both these equations, what are some reasonable densities for a planet?



        Object/Planet Density (kg/m^3)
        Earth's Inner Core 12800
        Earth's Outer Core 9900
        Earth 5510
        Mercury 5430
        Venus 5240
        Mars 3930
        Vesta (densest asteroid) 3420
        Luna 3340
        Ceres (largest asteroid) 2080
        Ganymede 1940
        Titan 1880
        Neptune 1640
        Jupiter 1330
        Uranus 1270
        A small chunk of water ice 934
        Saturn 690


        A lot goes into planetary density, and that could totally be its own question. Mass drives density; the bigger a planet the more gravity will compress it. Mercury has more iron (relatively) than Earth, but is less dense because Earth's gravity compresses its core more. But these values are some guidelines for solving the above equations.






        share|improve this answer














        Mass, density and radius are related



        Let $m$ be the mass of a planet.



        For a given a density $rho$, the relationship between mass and volume is
        $$beginalign
        V &= frac43pi r^3\
        m &= rho V = frac43pirho r^3
        endalign$$



        The bottom equation gives you your relations. Of the two variables you are interested in, mass ($m$) and radius ($r$), the solutions in terms of one another are:



        $$beginalign
        m&=frac43pirho r^3\
        r&=sqrt[3]frac3m4pirho
        endalign$$



        Be careful with units! Always convert mass to kg, radius to m, and density to kg/m$^3$ to be safe.



        What should density be?



        Since you need density in both these equations, what are some reasonable densities for a planet?



        Object/Planet Density (kg/m^3)
        Earth's Inner Core 12800
        Earth's Outer Core 9900
        Earth 5510
        Mercury 5430
        Venus 5240
        Mars 3930
        Vesta (densest asteroid) 3420
        Luna 3340
        Ceres (largest asteroid) 2080
        Ganymede 1940
        Titan 1880
        Neptune 1640
        Jupiter 1330
        Uranus 1270
        A small chunk of water ice 934
        Saturn 690


        A lot goes into planetary density, and that could totally be its own question. Mass drives density; the bigger a planet the more gravity will compress it. Mercury has more iron (relatively) than Earth, but is less dense because Earth's gravity compresses its core more. But these values are some guidelines for solving the above equations.







        share|improve this answer














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        edited 2 hours ago

























        answered 3 hours ago









        kingledion

        66k22217376




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