Step 1: Understanding the Concept:
Orbital speed near the surface: \(v_0 = \sqrt{GM/R}\). Express \(M\) in terms of density \(\rho\) and \(R\).
Step 2: Detailed Explanation:
\(M = \dfrac{4}{3}\pi R^3 \rho\), so:
\[
v_0 = \sqrt{\frac{G \cdot \frac{4}{3}\pi R^3 \rho}{R}} = \sqrt{\frac{4\pi G\rho}{3}}\cdot R
\]
Applying Newton’s second law to a circular orbit, we have
\[
\frac{mv^2}{r} = \frac{4\pi^2 r m}{T^2} = \frac{G M m}{r^2}
\]
where \( m \) is the mass of satellite, and \( v \) is the orbital speed.
\( T \) is the time period
\[
T = \frac{2\pi r^{3/2}}{\sqrt{G M}}
\]
For
\[
r \approx R
\]
and
\[
M = \frac{4}{3} \pi R^3 \rho \quad (\rho = \text{density of planet})
\]
\[
T = \sqrt{\frac{3 \pi}{\rho G}}
\]
i.e. is independent of \( R \).
Step 3: Final Answer:
orbital speed \(\propto R^0\) (independent of radius for given density).