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Assuming the earth to be a homogencous s...

Assuming the earth to be a homogencous 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 )is

A

`3 g // (4 pi RG)`

B

` 4 pi g// (3 RG)`

C

` 4 pi Rg (3G)`

D

` 4 pi RG // (3g)`

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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 1: Use the formula for acceleration due to gravity The acceleration due to gravity \( g \) at the surface of the Earth is given by the formula: \[ g = \frac{GM}{R^2} \] where \( M \) is the mass of the Earth and \( R \) is the radius of the Earth. ### Step 2: Rearrange the formula to find the mass \( M \) From the equation above, we can rearrange it to express the mass \( M \) of the Earth: \[ M = \frac{gR^2}{G} \] ### Step 3: Express the mass in terms of density The mass \( M \) can also be expressed in terms of the density \( \rho \) and the volume \( V \) of the Earth. The volume \( V \) of a sphere is given by: \[ V = \frac{4}{3} \pi R^3 \] Thus, we can write: \[ M = \rho V = \rho \left(\frac{4}{3} \pi R^3\right) \] ### Step 4: Set the two expressions for mass equal to each other Now we can set the two expressions for mass equal to each other: \[ \frac{gR^2}{G} = \rho \left(\frac{4}{3} \pi R^3\right) \] ### Step 5: Solve for density \( \rho \) To find the density \( \rho \), we can rearrange the equation: \[ \rho = \frac{gR^2}{G} \cdot \frac{3}{4\pi R^3} \] This simplifies to: \[ \rho = \frac{3g}{4\pi G R} \] ### Final Result Thus, the density 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 1: Use the formula for acceleration due to gravity The acceleration due to gravity \( g \) at the surface of the Earth is given by the formula: \[ g = \frac{GM}{R^2} \] where \( M \) is the mass of the Earth and \( R \) is the radius of the Earth. ...
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