Gravitational potential for various matter configurations

AI Thread Summary
The discussion focuses on calculating the gravitational potential and field for different configurations of Earth: constant density, thin shell, and linear density. For a constant density, the potential outside is given by V = -GM/r, leading to a gravitational field of g = -GM/r². To find the potential inside the Earth, it is suggested to integrate over thin shells of radius dr. The approach emphasizes the need to consider contributions from all shells to accurately compute the gravitational potential within the Earth. Overall, the calculations highlight fundamental principles of gravitational theory in varying matter configurations.
Afonso Campos
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Homework Statement



Consider the Earth as

1. with a constant density of matter,
2. as a thin shell empty sphere and
3. with a constant linear density of matter ##\rho(r) = \rho_{0}r##.

In all cases, calculate the gravitational potential and the gravitational field everywhere and make a sketch.

Homework Equations



The Attempt at a Solution



1. The gravitational potential outside the Earth is equal to the gravitational potential of a point particle of the mass of the Earth, that is,

$$V = - \frac{GM}{r}.$$

Therefore, the gravitational field is simply

$$g = - \nabla V = - \frac{GM}{r^{2}}.$$

To compute the gravitational potential within the Earth, do I have to slice up the Earth into thin shells of radius ##dr## and integrate over shells which contribute to the potential?
 
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Afonso Campos said:
To compute the gravitational potential within the Earth, do I have to slice up the Earth into thin shells of radius ##dr## and integrate over shells which contribute to the potential?
Right.
 
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