📚 Gravitation Question Paper
Answer all questions in 1-2 sentences
| Mass | Weight |
|---|---|
| Quantity of matter in an object | Force of gravity on an object |
| Constant everywhere | Varies with location |
| Scalar quantity (kg) | Vector quantity (N) |
Archimedes' Principle: When an object is fully or partially immersed in a fluid, it experiences an upward force equal to the weight of the fluid displaced by the object.
SI Unit: Pascal (Pa) or N/m²
Sharp objects cut more easily because the same force is concentrated on a smaller area, resulting in greater pressure (P = F/A). Higher pressure makes cutting easier.
Answer in 2-3 sentences with explanation
Where: F = Gravitational force
G = Universal gravitational constant (6.67 × 10⁻¹¹ N·m²/kg²)
M, m = Masses of objects
d = Distance between centers
For an object on Earth's surface:
- M = Mass of Earth
- d = Radius of Earth (R)
- The force is the weight (W)
Therefore: W = G(M × m)/R²
We can write: g = GM/R² (a constant)
Hence: W = mg
Using g = GM/R²:
- Earth: g = 9.8 m/s²
- Moon: g = 1.6 m/s² (Moon has ~1/81 mass of Earth and smaller radius)
A 60 kg person weighs:
- On Earth: W = 60 × 9.8 = 588 N
- On Moon: W = 60 × 1.6 = 96 N (about 1/6 of Earth's weight)
F = (6.67 × 10⁻¹¹) × (6 × 10²⁴ × 7.4 × 10²²) / (3.84 × 10⁸)²
F = (6.67 × 10⁻¹¹) × (4.44 × 10⁴⁷) / (1.47 × 10¹⁷)
F = 2.02 × 10²⁰ N
The gravitational force between Earth and Moon is 2.02 × 10²⁰ N
Upward journey: Gravity acts downward, opposing motion. Velocity decreases continuously until it becomes zero at maximum height.
Downward journey: Gravity acts downward, in the direction of motion. Velocity increases continuously until the object reaches the ground.
Acceleration: Throughout the entire journey, acceleration = -g = -9.8 m/s² (constant, directed downward)
Using Pressure = Force / Area:
- Camel has large feet (large area)
- Despite its heavy weight (large force), the pressure on sand = Weight / Large Area = Small Pressure
Low pressure means the camel doesn't sink deep into the sand, making walking easier.
By Archimedes' principle: Buoyant force = Weight of water displaced
Since average density < water's density → Buoyant force > Weight → Ship floats
1. Weight (W) = mg, acting downward
2. Buoyant force (F_b) = Weight of water displaced, acting upward
Apparent weight = W - F_b
Since F_b > 0, the apparent weight is less than actual weight, making the person feel lighter.
Answer in detail with diagrams and calculations
From Newton's Universal Law of Gravitation:
F = G(M × m)/R²
From Newton's Second Law: F = ma
For an object falling on Earth: a = g (acceleration due to gravity)
Therefore: mg = G(M × m)/R²
Canceling m from both sides:
G = 6.67 × 10⁻¹¹ N·m²/kg²
M = 6 × 10²⁴ kg (Mass of Earth)
R = 6.4 × 10⁶ m (Radius of Earth)
g = (6.67 × 10⁻¹¹ × 6 × 10²⁴) / (6.4 × 10⁶)²
g = (40.02 × 10¹³) / (40.96 × 10¹²)
g = 9.8 m/s²
u = 20 m/s (initial velocity)
v = 0 m/s (at maximum height)
g = 10 m/s² (taking downward as positive)
(a) Maximum Height:
Using v² = u² - 2gs (negative because gravity opposes motion)
0² = 20² - 2(10)s
0 = 400 - 20s
s = 20 m
(b) Time to Maximum Height:
Using v = u - gt
0 = 20 - 10t
t = 2 seconds
(c) Total Time of Flight:
By symmetry, time to come down = time to go up = 2s
Total time = 2 + 2 = 4 seconds
Or using: s = ut - ½gt²
0 = 20t - ½(10)t²
0 = 20t - 5t²
0 = t(20 - 5t)
t = 0 or t = 4 seconds
Tides are caused by gravitational pull of the Moon and Sun on Earth's water bodies.
Moon's Effect (Primary):
- Moon pulls harder on the near side of Earth (closer)
- Pulls less on the far side (farther)
- This difference creates a bulge on the near side (high tide)
- A matching bulge forms on the far side (due to Earth being pulled more than water)
- Results in 2 high tides and 2 low tides per day
Sun's Effect (Secondary):
- Sun also creates tides but with smaller magnitude
- During full and new moon: Sun and Moon align → Spring tides (highest/lowest)
- During quarter moon: Sun and Moon perpendicular → Neap tides (moderate)
| Feature | Gravitational Force | Electrostatic Force |
|---|---|---|
| Law | F = GM₁M₂/r² | F = kq₁q₂/r² |
| Nature | Always attractive | Attractive or repulsive |
| Strength | Very weak (smallest force) | Very strong (10³⁶ times stronger) |
| Medium | Works in vacuum | Works in vacuum |
| Range | Infinite (1/r²) | Infinite (1/r²) |
Why Gravity Seems Weak:
Despite being the weakest fundamental force, gravity dominates at large scales because:
- All mass has gravity (always attractive)
- Charges can cancel (positive/negative)
- Large masses accumulate gravitational effects
For circular orbit, gravitational force provides centripetal force:
F_gravity = F_centripetal
Simplifying: GM/r = v²
v = √(GM/r)
- Orbital velocity depends only on M (central body's mass) and r (orbital radius)
- Independent of orbiting object's mass (m cancels out)
- Larger orbits have lower velocities (v ∝ 1/√r)
- Smaller orbits have higher velocities
Example: Earth orbiting Sun
v_Earth = √(GM_Sun/r_Earth-Sun) = √(6.67×10⁻¹¹ × 2×10³⁰ / 1.5×10¹¹)
v_Earth ≈ 30 km/s
T² ∝ r³ or T = 2π√(r³/GM)
Orbital Velocity:
v = √(GM/r)
Energy in Orbit:
- Kinetic Energy: KE = ½mv² = GMm/(2r)
- Potential Energy: PE = -GMm/r
- Total Energy: E = KE + PE = -GMm/(2r)
Key Characteristics:
1. Constant orbital velocity (v is constant in circular orbit)
2. Constant acceleration (centripetal, towards Earth)
3. Zero total mechanical energy for escape (parabolic orbit)
4. Negative total energy keeps satellite bound (elliptical/circular)
Minimum velocity needed to escape a celestial body's gravitational field to infinity.
Derivation:
At infinity, both KE and PE = 0
Using energy conservation: KE_surface = PE_surface
½mv_e² = GMm/R
- Earth: v_e = 11.2 km/s
- Moon: v_e = 2.4 km/s (1/5 of Earth)
- Sun: v_e = 617 km/s
Applications:
- Rocket launch calculations
- Black hole properties (if R becomes small, v_e > c)
- Planetary atmosphere retention
Using W = mg
On Mercury:
W = 60 × 3.7 = 222 N (about 38% of Earth weight)
On Venus:
W = 60 × 8.9 = 534 N (about 91% of Earth weight)
On Mars:
W = 60 × 3.7 = 222 N (about 38% of Earth weight)
On Jupiter:
W = 60 × 24.8 = 1488 N (about 253% of Earth weight)
Comparison Table:
| Planet | Weight (N) | % of Earth Weight |
|---|---|---|
| Earth | 588 | 100% |
| Mercury | 222 | 38% |
| Venus | 534 | 91% |
| Mars | 222 | 38% |
| Jupiter | 1488 | 253% |
Apply concepts to real-world scenarios
F = G(M₁M₂)/d²
F = (6.67 × 10⁻¹¹) × (60 × 60) / (1)²
F = (6.67 × 10⁻¹¹) × 3600
F = 2.4 × 10⁻⁸ N
This force is extremely tiny!
For comparison:
- Air molecules bump with force ~10⁻²¹ N
- Earth's gravitational pull on person = 588 N
- Ratio: 2.4 × 10⁻⁸ / 10⁻²¹ ≈ 10¹⁴ times larger
Yet even thermal motion of atoms (10⁻²¹ N) completely overwhelms gravitational attraction!
When an object falls through air:
- Initially: Gravitational force > Air resistance → Net downward force
- As velocity increases: Air resistance increases
- At terminal velocity: Gravitational force = Air resistance
- Net force = 0, acceleration = 0
Why different objects reach different terminal velocities:
- Terminal velocity depends on shape, surface area, and mass
- Streamlined objects (like bullets) have higher terminal velocity
- Parachutes (large area) have very low terminal velocity
- Heavier objects reach higher terminal velocity (same shape)
Example:
Raindrops: ~9 m/s
Skydiver (belly-to-earth): ~53 m/s
Skydiver (head-first): ~90 m/s
T² = (4π²/GM) × r³
Rearranging for r:
r³ = (GMT²)/(4π²)
Given:
T = 24 hours = 86,400 seconds
M = 6 × 10²⁴ kg
G = 6.67 × 10⁻¹¹
Calculation:
r³ = (6.67 × 10⁻¹¹ × 6 × 10²⁴ × (86,400)²) / (4π²)
r³ = (6.67 × 10⁻¹¹ × 6 × 10²⁴ × 7.46 × 10⁹) / 39.48
r³ = 7.53 × 10²² m³
r = 4.22 × 10⁷ m = 42,200 km
Distance from Earth's center: 42,200 km
Height above surface: 42,200 - 6,400 = 35,800 km
Reality:
- Earth's gravity still acts on astronauts (provides centripetal force)
- Astronauts' weight = mg is still ~90% of Earth surface value
- This gravitational force keeps them in orbit
Why they appear weightless:
- Space station and astronauts fall together
- Both have same acceleration (g ≈ 8.7 m/s² at ISS altitude)
- No normal force from the station floor
- The sensation of weight comes from normal force, not gravity
Analogy:
In a free-falling elevator, you feel weightless even though Earth's gravity still acts. Both you and elevator fall at acceleration 'g' together.
📊 Answer Summary & Key Concepts
✓ Universal Law
F = G(M₁M₂)/r² is fundamental to understanding all gravitational phenomena. The constant G = 6.67 × 10⁻¹¹ ensures the law is universal.
✓ Acceleration Due to Gravity
g = GM/R² = 9.8 m/s² (Earth surface). Independent of falling object's mass. Varies with location.
✓ Mass vs Weight
Mass (constant, kg) ≠ Weight (varies, N). W = mg. Weight depends on local g value.
✓ Free Fall Motion
Objects fall with constant acceleration g. Uses equations: v = u ± gt, s = ut ± ½gt², v² = u² ± 2gs
✓ Pressure Concept
P = F/A. Pressure increases with force, decreases with area. Sharp objects concentrate force → high pressure.
✓ Buoyancy & Flotation
Buoyant force = Weight of fluid displaced (Archimedes' principle). Objects float if ρ_object < ρ_fluid.
✓ Orbital Motion
Orbital velocity: v = √(GM/r). Period: T² ∝ r³ (Kepler's law). Escape velocity: v_e = √(2GM/R)
✓ Apparent Weightlessness
Objects in free fall (orbit) appear weightless despite gravitational force. Weight = normal force = 0 in orbit, not because gravity is absent.