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According to Kepler\'s third law, the time period $T$ of a planet is related to the semi-major axis $R$ of its orbit as:

R
Solution written and verified by Roshan, science educator with 5 years of experience teaching NEET and JEE aspirants. Last reviewed September 2026.
Options
1
$T \propto R^2$
2
$T \propto R^{3/2}$
3
$T \propto R^{1/2}$
4
$T \propto R^3$
Correct Answer
$T \propto R^{3/2}$
Solution
1

Kepler\'s 3rd law: $T^2 \propto R^3$

2

Taking square root: $T \propto R^{3/2}$

Derivation: $T = 2\pi\sqrt{R^3/GM} \propto R^{3/2}$

Answer: $T \propto R^{3/2}$

Kepler\'s 3rd law: $T^2 \propto R^3$ or $T \propto R^{3/2}$
$T = 2\pi\sqrt{R^3/GM}$
Theory: Gravitation / Kepler
1. Kepler's Laws — Detailed

1st law (Ellipse law): Each planet orbits the Sun in an ellipse with Sun at one focus. Eccentricity $e$: circle $e=0$, ellipse $0

2. Artificial Satellites

Circular orbit: $v_o = \sqrt{GM/r}$, $T = 2\pi\sqrt{r^3/GM}$. Near Earth: $T \approx 84$ min, $v \approx 7.9$ km/s. Geostationary: $T = 24$ h, $r = 42,164$ km from Earth centre, $v \approx 3.07$ km/s; used for communication, weather. Polar orbit: passes over poles, can scan entire Earth surface over time. GPS: 24 satellites at altitude 20,200 km, $T = 12$ h.

3. Gravitational Field and Potential

Gravitational field: $g = GM/r^2$ (directed toward mass). Gravitational potential: $V = -GM/r$ (always negative). Relation: $g = -dV/dr$. Gravitational PE: $U = mV = -GMm/r$. Potential energy at surface: $U = -GMm/R$. Total energy of satellite in circular orbit: $E = KE + PE = \frac{GMm}{2r} - \frac{GMm}{r} = -\frac{GMm}{2r}$ (always negative → bound system).

4. Weightlessness and Microgravity

Weightlessness in orbit: apparent weight = $m(g - a_{centripetal}) = 0$ when $a_{centripetal} = g$ (satellite is in free fall). Not due to absence of gravity (gravity is still present at orbital altitude). True weightlessness: at very large distances from all masses. Effects: no buoyancy, no convection, no sedimentation → unique environment for science experiments, crystal growth, biology research aboard ISS.

5. Kepler's Third Law and How It Is Used

The law states $T^2 \propto a^3$, where a is the semi-major axis of the orbit. Because the constant of proportionality depends only on the central mass, the law lets you compare two satellites of the same planet without knowing G or M at all: $(T_1/T_2)^2 = (r_1/r_2)^3$. This is why most exam questions on Kepler are ratio questions — they are solvable in one line once you write both sides as a ratio rather than computing each period separately.

6. Deriving Kepler's Third Law from Newton's Law

For a circular orbit, equating gravitational and centripetal force gives $GMm/r^2 = m\omega^2r$ with $\omega = 2\pi/T$. Rearranging yields $T^2 = \frac{4\pi^2}{GM}r^3$, which is exactly Kepler's third law with the constant now identified. This derivation is worth being able to reproduce, because it shows that Kepler's empirical laws are consequences of Newton's law of gravitation rather than independent facts.

7. The Law of Areas and Angular Momentum

Kepler's second law says the line joining a planet to the Sun sweeps equal areas in equal times. The reason is that gravity is a central force, so it exerts no torque about the Sun, and the planet's angular momentum $L = mvr$ is therefore conserved. The areal velocity equals $L/2m$, a constant. This is why a planet moves fastest at perihelion and slowest at aphelion — the same conservation law, seen from a different angle.

Where students lose the mark

Using the radius instead of the semi-major axis. For a circular orbit they are the same, but for an elliptical orbit the third law needs the semi-major axis, not the perihelion or aphelion distance.

Forgetting that Kepler's laws apply to any central-force orbit. They hold for a satellite around the Earth and a moon around Jupiter just as they do for planets around the Sun — only the constant changes.

Frequently Asked Questions
1. What are Kepler's three laws? ⌄
1st (Ellipse): planets move in elliptical orbits with Sun at one focus. 2nd (Equal Areas): radius vector sweeps equal areas in equal times (L=const). 3rd (Harmonic): T² ∝ a³ where a = semi-major axis. For circular orbits: T ∝ R^(3/2).
2. How is T∝R^(3/2) derived? ⌄
For circular orbit: $GMm/R^2 = mv^2/R$ → $v = \sqrt{GM/R}$. $T = 2\pi R/v = 2\pi R/\sqrt{GM/R} = 2\pi\sqrt{R^3/GM} = \frac{2\pi}{\sqrt{GM}} R^{3/2} \propto R^{3/2}$.
3. What is the significance of Kepler's 3rd law? ⌄
Same constant $T^2/R^3 = 4\pi^2/GM$ for all planets around same star. If $T$ and $R$ known for two planets: $T_1^2/R_1^3 = T_2^2/R_2^3$. Used to find masses of planets (from satellite orbit data) and to verify Newton\'s law of gravitation.
4. What is the orbital speed of a satellite? ⌄
$v = \sqrt{GM/R}$. For near-Earth satellite ($R \approx R_E = 6400$ km): $v \approx 7.9$ km/s. Orbital period of near-Earth satellite: $T = 2\pi R_E/v \approx 5400$ s $\approx 90$ min. Geostationary orbit: $T = 24$ h, $R \approx 42,000$ km.
5. What is the relation between orbital speed and escape speed? ⌄
$v_{escape} = \sqrt{2GM/R} = \sqrt{2} \cdot v_{orbital}$. Escape speed is $\sqrt{2}$ times the orbital speed at the same radius. To escape from orbit: need to increase speed by factor $\sqrt{2}-1 \approx 41\%$.
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