Radius of core, using densities

In summary: VolumeCore is just the mass of the planet's core in grams. So after all that algebra and substituting in the masses, the radius of the core is 1.206*1026g/cm3.
  • #1
bocobuff
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Homework Statement


A planet with R=4000km and [tex]\rho[/tex]avg=5g/cm3. The planet is made of quartz all the way to the core, which is made of iron. The densities of quart and iron are [tex]\rho[/tex]quartz=2.65g/cm3 and [tex]\rho[/tex]iron=7.874g/cm3. Calculate the radius of the core.


Homework Equations


[tex]\rho[/tex]=M/V
Vsphere=4/3[tex]\pi[/tex]r3


The Attempt at a Solution


I solved for Mplanet=[tex]\rho[/tex]avg=5g/cm3*4/3[tex]\pi[/tex]4000km and got 1.34*1027g. Then with assuming the Mplanet=MTot. Qrtz+MTot. Iron, I tried using various substitutions of my unknowns and I can't get anywhere close to being able to solve for any of them. I know it's some simple calculus, but I am lost and don't remember how to do this. The biggest problem for me is that the radius is cubed and I forgot what to do to solve for that.
Any fresh ideas would help a lot.
Thanks
 
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  • #2
The volume of the planet is equal to the volume of the core plus the volume of the mantle.
That's one equation. Then you have your mass equation.
From these two you can substitute for the volume of the mantle to find the volume of the core and thus arrive at core radius.
 
  • #3
So after a bunch of substitutions and algebra solving for Vcore, I got
Vcore=([tex]\rho[/tex]avg*V[tex]\rho[/tex]planet - [tex]\rho[/tex]mantle*Vplanet) / ([tex]\rho[/tex]core - [tex]\rho[/tex]mantle) and got 1.206*1026g/cm3.
Solving for the radius I got
r=[tex]\sqrt[3]{Vcore/(4pi/3)}[/tex] and got 3.0665*108cm which is 3065km, roughly 75% of the planet's r. Sound right?
 
  • #4
No I don't think so...

VolumePlanet = VolumeMantle + VolumeCore

now

VolumeMantle = VolumePlanet - VolumeCore

so substituing

VolumePlanet = (VolumePlanet - VolumeCore) + VolumeCore

Now why did we do that? Because if we now multiply the volumes by the densities to get the masses, things are much more interesting...

VolumePlanet * DensityAverage= ((VolumePlanet - VolumeCore) * DensityMantle) + (VolumeCore * DensityCore)

Now we know all those numbers except VolumeCore. We are on our way...

I've probably given you too much help but I couldn't see any other way.
 

FAQ: Radius of core, using densities

What is the radius of the Earth's core?

The radius of the Earth's core is approximately 3,485 kilometers.

How is the radius of the core determined?

The radius of the core is determined by using the Earth's average density, which is calculated by dividing the Earth's mass by its volume. This density is then compared to the known densities of different materials found in the Earth's layers to determine the size and composition of the core.

What is the average density of the Earth's core?

The average density of the Earth's core is estimated to be around 13 grams per cubic centimeter.

How does the density of the core affect its radius?

The density of the core directly affects its radius, as a higher density results in a smaller radius and vice versa. This is because the radius is determined by the mass and volume of the core, and density is a measure of how much mass is contained in a certain volume.

Are there any variations in the density and radius of the core?

Yes, there are variations in the density and radius of the core due to its composition and temperature. These variations can affect the Earth's magnetic field and the movement of tectonic plates, and are still being studied by scientists.

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