Calculating the Radius of Earth's Iron Core: A Simple Model Approach

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SUMMARY

The discussion focuses on calculating the radius of Earth's iron core using a model that incorporates constant mass densities for both the core and surrounding rock. The densities are specified as ρ0 = 8.90×103 kg/m3 for the iron core and ρ1 = 3.80×103 kg/m3 for the rock. The total mass of the Earth is expressed in terms of the core radius 'a' and the Earth's radius R = 6.40×106 m. The gravitational field g(r) is derived using the gravitational potential Φ and Newton's law of gravity, leading to the calculation of g(a).

PREREQUISITES
  • Understanding of gravitational potential and field concepts
  • Familiarity with Newton's law of gravity
  • Knowledge of spherical mass distributions
  • Basic calculus for deriving functions
NEXT STEPS
  • Study the derivation of gravitational potential using the equation Φ=-G∫(ρ(r')/r)dv'
  • Learn about mass density calculations in spherical coordinates
  • Explore the application of Newton's law of gravity in different contexts
  • Investigate the implications of varying density profiles in planetary models
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Students in physics or earth sciences, educators teaching gravitational concepts, and researchers modeling planetary interiors will benefit from this discussion.

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Homework Statement


Consider a simple model for the interior of the Earth: there is a spherical iron core with constant mass density ρ0 and radius a; outside the core is "rock" with constant density ρ1. Use these values for the densities: ρ0= 8.90×103 kg/m3 and ρ1= 3.80×103 kg/m3. The radius of the Earth is R = 6.40×106 m.

Calculate the radius a of the iron core.

Derive the graviational field g(r) as a function of r. Find g(a).

Homework Equations



\Phi=-G\int(\rho(r')/r)dv'

g=-\nabla\Phi

The Attempt at a Solution



I really am unsure as where to go with this one. I have the mass of the core as a ratio of the densities, but from there I am stuck.
 
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The problem suggests that you consider that the Earth is comprised of a central iron core of some radius r with a given density, surrounded by a concentric shell of another density out to a radius R. You should be able to write an expression for the total mass of the Earth that depends upon r and R.

What you known is that the acceleration due to gravity at the Earth's surface (radius R) is given by Newton's law of gravity (can you write the appropriate expression given M and R?). You know the value of g. You know R.

Plug in the mass expression from above into the Newton's law formula for g. Solve for the iron core radius.

As for g(r), you will need to consider Newton's gravitation law again, and deal with the mass contained in the spherical volume below radius "r".
 
The book claims the answer is that all the magnitudes are the same because "the gravitational force on the penguin is the same". I'm having trouble understanding this. I thought the buoyant force was equal to the weight of the fluid displaced. Weight depends on mass which depends on density. Therefore, due to the differing densities the buoyant force will be different in each case? Is this incorrect?

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