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Assuming the earth to be a homogeneous s...

Assuming the earth to be a homogeneous sphere of radius `R`, its density in terms of `G` (constant of gravitation) and `g` (acceleration due to gravity on the surface of the earth)

A

`3g//(4piRG)`

B

`4pig//(3RG)`

C

`4piRg//(3G)`

D

`4piRG//(3g)`

Text Solution

AI Generated Solution

The correct Answer is:
To find the density of the Earth in terms of the gravitational constant \( G \) and the acceleration due to gravity \( g \), we can follow these steps: ### Step-by-Step Solution: 1. **Start with the formula for gravitational acceleration**: The acceleration due to gravity \( g \) at the surface of the Earth can be expressed as: \[ g = \frac{G M}{R^2} \] where \( M \) is the mass of the Earth, \( R \) is the radius of the Earth, and \( G \) is the universal gravitational constant. 2. **Express mass \( M \) in terms of density \( \rho \)**: The mass \( M \) of the Earth can be expressed in terms of its density \( \rho \) and volume \( V \): \[ M = \rho V \] For a sphere, the volume \( V \) is given by: \[ V = \frac{4}{3} \pi R^3 \] Therefore, we can write: \[ M = \rho \left(\frac{4}{3} \pi R^3\right) \] 3. **Substitute \( M \) back into the equation for \( g \)**: Substituting the expression for \( M \) into the equation for \( g \): \[ g = \frac{G \left(\rho \frac{4}{3} \pi R^3\right)}{R^2} \] 4. **Simplify the equation**: Simplifying the equation gives: \[ g = \frac{4}{3} \pi G \rho R \] 5. **Rearranging to find \( \rho \)**: To find the density \( \rho \), we rearrange the equation: \[ \rho = \frac{3g}{4 \pi G R} \] ### Final Expression: Thus, the density \( \rho \) of the Earth in terms of \( G \) and \( g \) is: \[ \rho = \frac{3g}{4 \pi G R} \]

To find the density of the Earth in terms of the gravitational constant \( G \) and the acceleration due to gravity \( g \), we can follow these steps: ### Step-by-Step Solution: 1. **Start with the formula for gravitational acceleration**: The acceleration due to gravity \( g \) at the surface of the Earth can be expressed as: \[ g = \frac{G M}{R^2} ...
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