HomePhysicsQ
PhysicsGravitation
The radius of Martian orbit around the Sun is about 4 times the radius of Mercury orbit. The Martian year is 687 Earth days. Then the length of 1 year on Mercury is:
Options
1
124 Earth days
2
88 Earth days
3
225 Earth days
4
172 Earth days
Correct Answer
88 Earth days
Solution
1

Kepler's Third Law: $T^2 \propto R^3$

$$\frac{T_{Mars}^2}{T_{Mercury}^2} = \frac{R_{Mars}^3}{R_{Mercury}^3}$$
2
$$\frac{T_{Mars}}{T_{Mercury}} = \left(\frac{R_{Mars}}{R_{Mercury}}\right)^{3/2} = 4^{3/2} = 8$$$$T_{Mercury} = \frac{T_{Mars}}{8} = \frac{687}{8} \approx \boxed{88 \text{ Earth days}}$$
$$T^2 \propto R^3 \implies T_{Mercury} = \frac{687}{4^{3/2}} = \frac{687}{8} \approx 88 \text{ days}$$
Theory: Gravitation
1. Kepler's Laws of Planetary Motion

Three laws discovered by Johannes Kepler (1609-1619): First law (Law of Ellipses): Every planet orbits the Sun in an ellipse with the Sun at one focus. Second law (Law of Equal Areas): A line joining the planet to the Sun sweeps equal areas in equal times. Consequence: planet moves faster when closer to Sun (perihelion), slower when farther (aphelion). Third law (Harmonic Law): $T^2 \propto R^3$ (for circular orbits $R$ = radius; for elliptical, $R$ = semi-major axis). Newton later derived all three laws from his law of gravitation.

2. Derivation of Kepler Third Law

For a circular orbit of radius $R$: gravitational force = centripetal force: $$ rac{GMm}{R^2} = rac{mv^2}{R}$$ Orbital speed: $v = \sqrt{GM/R}$. Period: $T = rac{2\pi R}{v} = 2\pi R \sqrt{ rac{R}{GM}} = rac{2\pi R^{3/2}}{\sqrt{GM}}$. Therefore: $$T^2 = rac{4\pi^2}{GM} R^3$$ This gives $T^2 \propto R^3$ with proportionality constant $ rac{4\pi^2}{GM}$ (same for all planets orbiting the same central body).

3. Orbital Velocity and Escape Velocity

Orbital velocity at radius $R$: $v_o = \sqrt{GM/R}$. Decreases as $R$ increases (outer planets move slower). For Earth: $v_o pprox 7.9$ km/s at surface level. Escape velocity: $v_e = \sqrt{2GM/R} = \sqrt{2} \, v_o$. Escape velocity from Earth surface: 11.2 km/s. For Moon (small mass, small $g$): 2.38 km/s (no atmosphere because gas molecules can escape). For Jupiter: 59.5 km/s (keeps all gases, has thick atmosphere).

4. Geostationary Satellites

Geostationary orbit: satellite appears stationary relative to Earth. Must be in equatorial plane with $T = 24$ hours. Using Kepler third law: $R_{geo}^3 = rac{GM_E T^2}{4\pi^2}$. $R_{geo} pprox 42,240$ km from Earth's centre $pprox 36,000$ km above surface. Used for: TV broadcasting (INSAT), communication satellites, weather satellites (METEOSAT). GPS satellites: in medium Earth orbit (20,200 km), not geostationary.

5. Energy of a Satellite

For circular orbit of radius $R$: Kinetic energy: $KE = rac{1}{2}mv^2 = rac{GMm}{2R}$. Potential energy: $PE = - rac{GMm}{R}$. Total energy: $E = KE + PE = - rac{GMm}{2R}$. Total energy is negative (bound system). Binding energy = $|E| = rac{GMm}{2R}$. To increase orbit radius: energy must be added (paradox: adding energy decreases orbital speed — that's how Hohmann transfer works). To de-orbit: reduce energy (fire retrorocket).

6. Weightlessness

In a satellite or freely falling body: apparent weight = 0. Both satellite and occupants are in free fall towards Earth (centripetal acceleration = $g$ at that orbit). No normal reaction force → weightlessness. Not because gravity is absent (gravity provides centripetal force). Astronauts in ISS: $g pprox 8.7$ m/s$^2$ (only slightly less than surface). But they're in continuous free fall. Weightlessness causes: bone density loss, muscle atrophy, fluid redistribution. Artificial gravity possible via rotation (centrifugal force simulates gravity).

7. Gravitational Potential Energy

$U = - rac{GMm}{r}$. Zero at infinity, negative everywhere else (bound). Change in PE when moving from $r_1$ to $r_2$: $\Delta U = GMm\left( rac{1}{r_1} - rac{1}{r_2} ight)$. Work done against gravity: $W = \Delta U$ (positive when moving away from Earth). For satellite in orbit: $E = - rac{GMm}{2R}$. For object on Earth surface: $E = - rac{GMm}{R_E}$. Energy needed to launch satellite to orbit: $\Delta E = rac{GMm}{2R} - rac{GMm}{R_E} \cdot ( ext{usually small compared to launch cost})$.

8. Variations of g

Standard $g = 9.8$ m/s$^2$ at sea level. Variation with altitude $h$: $g_h = g\left( rac{R}{R+h} ight)^2 pprox g\left(1 - rac{2h}{R} ight)$ for $h \ll R$. Variation with depth $d$: $g_d = g\left(1 - rac{d}{R} ight)$. At centre of Earth: $g = 0$. Variation with latitude $\phi$: $g_{eff} = g - \omega^2 R\cos^2\phi$. At equator: $g$ is minimum (both altitude and rotation reduce $g$). At poles: $g$ is maximum. Effect of Earth rotation: $g$ at equator $pprox 9.78$ m/s$^2$, at poles $pprox 9.83$ m/s$^2$.

Frequently Asked Questions
1. How is $4^{3/2}$ calculated?
$4^{3/2} = (4^3)^{1/2} = 64^{1/2} = 8$. Or: $4^{3/2} = 4^1 \times 4^{1/2} = 4 \times 2 = 8$. This is a key calculation skill for Kepler's third law problems. General formula: if $R_2/R_1 = k$, then $T_2/T_1 = k^{3/2}$.
2. What is Mercury's orbit like?
Mercury: closest planet to Sun. Average orbital radius $R = 5.79 \times 10^7$ km (0.387 AU). Orbital period 87.97 Earth days. Most eccentric orbit of all planets: varies from 46 to 70 million km from Sun. Mercury also has slowest rotation among planets: 1 Mercurian day = 176 Earth days! It is tidally locked in a 3:2 spin-orbit resonance (3 rotations per 2 orbits). Surface temperature: $-180°C$ to $430°C$ (extreme range due to no atmosphere).
3. Can Kepler's law be applied to satellites?
Yes! Kepler's third law $T^2 = \frac{4\pi^2}{GM_E}R^3$ applies to any satellite orbiting Earth. For geostationary orbit: $T = 86400$ s. $R_{geo} = \left(\frac{GM_E T^2}{4\pi^2}\right)^{1/3}$. Using $GM_E = 4 \times 10^{14}$ m$^3$/s$^2$: $R_{geo} \approx 4.22 \times 10^7$ m = 42,200 km. The Moon also obeys Kepler's third law: $T_{Moon} = 27.3$ days at $R = 3.84 \times 10^5$ km.
4. What is Kepler second law and what does it imply?
Kepler's second law: the radius vector (line from Sun to planet) sweeps equal areas in equal time intervals. Mathematically: $\frac{dA}{dt} = \frac{L}{2m} = $ constant (L = angular momentum, conserved). This means angular momentum is conserved (no torque from central gravitational force). Consequence: planets speed up near perihelion (closest point to Sun) and slow down near aphelion (farthest point). Earth is closest to Sun in January (perihelion) and farthest in July (aphelion) — slightly faster in January.
5. What would happen if planet orbit were twice the radius?
If $R_2 = 2R_1$: $T_2/T_1 = (R_2/R_1)^{3/2} = 2^{3/2} = 2\sqrt{2} \approx 2.83$. So period increases by factor $2\sqrt{2}$. If Earth orbit doubled to $2$ AU: year would be $365 \times 2\sqrt{2} \approx 1031$ Earth days. In this problem: $R_{Mars} = 4R_{Mercury}$, so $T_{Mars} = 4^{3/2} T_{Mercury} = 8 T_{Mercury}$.
Previous Questions
Q.
Two gases pistons radii ratio rA/rB thermodynamics first law
Physics · Answer: rA/rB = 3/4
Q.
Two circular coils radii 1:2 magnetic moment ratio
Physics · Answer: 1:4
Q.
Four thin convex lenses in contact power magnification
Physics · Answer: 4p and m⁴
Q.
Electron velocity selector E perpendicular B 27x10² V/m
Physics · Answer: E ⊥ B, 27×10² V/m
Q.
Pipe open both ends dipped half water fundamental frequency
Physics · Answer: f