Gravitational Force Calculator
Calculate the gravitational force between any two masses using Newton's Law of Universal Gravitation (F=Gm₁m₂/r²), find your weight on all planets and the Moon, determine surface gravity, and calculate g-force and impact force — with full step-by-step working throughout.
Newton's Law of Universal Gravitation — F=Gm₁m₂/r²
Enter your mass or Earth weight to see how much you would weigh on every planet, the Moon, and the Sun. Your mass stays constant — only weight changes with planet gravity.
Your Weight on Other Planets — W = m × g_planet
| Body | g (m/s²) | Weight (N) | Weight (lbf) | vs Earth | Description |
|---|
Surface Gravity (Gravitational Field Strength)
G-Force — Acceleration in Units of Gravity
| Situation | G-Force | Effect |
|---|---|---|
| Standing still | 1 g | Normal |
| Sneeze | 2.9 g | Brief, harmless |
| Roller coaster | 3–5 g | Thrilling |
| Fighter jet turn | 5–9 g | G-suit needed |
| Car crash (minor) | 10–20 g | Injury risk |
| Ejector seat | 14–16 g | Survivable |
| Fatal crash | >50 g | Usually fatal |
| Bullet fired | 30,000 g | Instantaneous |
Impact Force — F = mv²/(2d)
Newton's Law of Universal Gravitation — F = Gm₁m₂/r²
This gravitational force calculator uses Newton's Law of Universal Gravitation to compute the attractive force between any two masses. The fundamental formula F=Gm₁m₂/r² tells us that every object with mass attracts every other object with mass — from two hydrogen atoms to the Earth and Moon. Newton's Law of Universal Gravitation is one of the most powerful and universal equations in all of physics.
The gravitational constant G = 6.674×10⁻¹¹ N·m²/kg² is a fundamental constant — the same everywhere in the universe. Two key facts about gravitational force: (1) it is always attractive — gravity never repels, unlike electric and magnetic forces; (2) it obeys the inverse square law — doubling the distance decreases the gravitational force by a factor of 4. The gravitational force F=Gm₁m₂/r² acts equally on both objects (Newton's 3rd law).
Why G is so small: gravity is the weakest of the four fundamental forces. The gravitational force between two 1 kg balls at 1 m apart is only 6.674×10⁻¹¹ N — thousands of billions of times weaker than the electromagnetic force between two electrons. Yet gravity dominates the universe at large scales because it acts over infinite range and is always attractive (unlike charges which can cancel). The gravitational force from F=Gm₁m₂/r² between Earth (5.972×10²⁴ kg) and the Moon (7.342×10²² kg) reaches 1.978×10²⁰ N.
Mathematical equation for gravity: F = Gm₁m₂/r² where G=6.674×10⁻¹¹ N·m²/kg², masses in kg, distance in meters, force in Newtons. The force of attraction formula shows that two objects attract each other gravitationally with equal and opposite forces — Earth pulls the Moon and the Moon pulls Earth with the same gravitational force magnitude.
What Two Factors Affect Gravitational Force?
Exactly two factors affect gravitational force — no more, no less. This is one of the most commonly tested facts about Newton's Law of Universal Gravitation:
- Factor 1: The masses of the two objects (m₁ and m₂). Gravitational force is directly proportional to each mass. Double m₁ → force doubles. Double both masses → force quadruples. Gravitational force and mass are directly proportional: F ∝ m₁ × m₂.
- Factor 2: The distance between the centers of the two objects (r). Gravitational force is inversely proportional to the SQUARE of the distance. This is the factor that most students get wrong. Double r → force decreases by factor 4 (not 2). Triple r → force decreases by factor 9. The relationship between distance and gravity follows F ∝ 1/r².
No other factors affect the strength of gravitational force — not temperature, color, composition, density, or anything else. A steel sphere and a wooden sphere of the same mass feel identical gravitational attraction. To increase the amount of gravitational force between two objects: increase either mass, or decrease the distance between them. These are the only two ways to change the gravitational force between two objects.
| Change | Effect on F=Gm₁m₂/r² | Reason |
|---|---|---|
| Double m₁ | F × 2 | F ∝ m₁ |
| Double m₂ | F × 2 | F ∝ m₂ |
| Double both masses | F × 4 | F ∝ m₁m₂ |
| Double distance r | F ÷ 4 | F ∝ 1/r² |
| Triple distance r | F ÷ 9 | F ∝ 1/r² |
| Half the distance | F × 4 | F ∝ 1/r² |
Weight — The Measure of Gravitational Force on an Object
Weight is gravitational force: W = mg. A measure of the force of gravity on an object, weight is what the gravitational force calculator computes when you enter your mass and the local surface gravity. Weight has units of Newtons (SI) or pound-force (lbf). The measure of the pull of gravity on an object is your weight — and it changes depending on which planet you stand on.
The critical distinction: mass (kg) is the amount of matter — it never changes. Weight (N or lbf) is the gravitational force on that mass — it changes with location. A 70 kg person has a mass of 70 kg everywhere in the universe. Their weight in Newtons: 686.5 N on Earth (9.807 m/s²), 260.5 N on Mars (3.721 m/s²), 113.4 N on the Moon (1.62 m/s²). In everyday language "weight" often means mass, but in physics: weight = force = gravitational force exerted on an object = F_g. 1 kg on Earth weighs 9.807 N = 2.205 lbf. Gravity in Newtons at Earth's surface: g = 9.807 N/kg.
Weight on Other Planets — Your Weight Across the Solar System
Your weight on other planets differs because each planet has a different surface gravity g = GM/r². The weight on other planets formula is: W_planet = m × g_planet. Your mass is constant; only gravity changes. This is the physical meaning of F=Gm₁m₂/r² applied at a planet's surface.
- Weight on Mars: Mars surface gravity = 3.721 m/s² (38% of Earth). 70 kg → 260.5 N (58.6 lbf). How much would I weigh on Mars: multiply your Earth weight by 0.3795. A 100 lb person weighs 37.95 lbs on Mars.
- Weight on Jupiter: Jupiter surface gravity = 24.79 m/s² (2.528× Earth). 70 kg → 1735 N (390 lbf). Jupiter's enormous gravity means you would feel very heavy — 2.5× your Earth weight. How much would a 100 lb person weigh on Jupiter: 252.8 lbs.
- Weight on the Moon: Moon surface gravity = 1.62 m/s² (16.5% of Earth). Apollo astronauts bounced in their suits because they felt so light. 70 kg on Earth = 113.4 N on the Moon. Weight on Earth vs Moon: 6.05:1 ratio.
- Which planet would you weigh the least on: Pluto — g=0.62 m/s², only 6.3% of Earth gravity. A 100 lb person would weigh just 6.3 lbs on Pluto.
- How much would I weigh on the Sun: Sun surface gravity = 274 m/s² (27.94× Earth). A 70 kg person would weigh 19,180 N = 4,313 lbf. How much would a 100 lb person weigh on Venus: g_Venus=8.87 m/s², ratio=0.905, weight=90.5 lbs.
- Weight on Neptune: g = 11.15 m/s² (1.137× Earth) — actually stronger than Earth despite being an ice giant.
Surface Gravity Formula — g = GM/r²
Surface gravity is derived from Newton's Law of Universal Gravitation. At the surface of a planet with mass M and radius r, a small mass m feels a gravitational force F = GMm/r². The gravitational acceleration (surface gravity) is g = F/m = GM/r². This is the gravitational field strength formula — units m/s² = N/kg.
Example 1 — Surface gravity of Mars from M and r
- g = GM/r² = 6.674×10⁻¹¹ × 6.4171×10²³ / (3.3895×10⁶)²
- = 4.280×10¹³ / 1.149×10¹³ = 3.725 m/s² (actual: 3.721 m/s²)
- Relative to Earth: 3.721/9.807 = 0.3795 g
Example 2 — Saturn's surprising surface gravity
- g = GM/r² = 6.674×10⁻¹¹ × 5.683×10²⁶ / (5.823×10⁷)² = 10.44 m/s²
- Saturn is 95× Earth's mass but only 1.065g surface gravity — because Saturn is very large and very low density (density < water)
Example 3 — Custom planet: M=3×10²⁴ kg, r=5000 km
- g = 6.674×10⁻¹¹ × 3×10²⁴ / (5×10⁶)² = 2.002×10¹⁴ / 2.5×10¹³ = 8.01 m/s²
G-Force — Acceleration Measured in Units of Gravity
G-force (n) is acceleration expressed in multiples of standard gravity: n = a/g₀ where g₀ = 9.80665 m/s². At 1g: normal standing. At 0g: weightlessness (free fall or orbit). Negative g: upside-down, blood rushes to head. The g force calculator computes this from acceleration, velocity change, or circular motion.
- From acceleration: n = a/9.807. Example: a=50 m/s² → n=5.10g (fighter pilot maneuver zone)
- From velocity change (crash): n = Δv/(g₀×Δt). Car at 60→0 km/h in 0.3s: a=16.67/0.3=55.6 m/s², n=5.66g
- Centripetal: n = v²/(r×g₀). Racing car at 200 km/h around r=100m: n=(55.56²/100)/9.807=3.15g
Physical effects: at 4-5g, blood pools in legs, vision grays. Above 9g sustained without G-suit: loss of consciousness. Car crashes: 10-50g depending on speed and crumple. This g acceleration calculator helps understand acceleration in physically meaningful terms.
Impact Force — How Hard Does a Falling Object Hit?
Impact force depends on mass, fall height, and — critically — stopping distance. The shorter the stopping distance, the greater the impact force. This is why car crumple zones, helmets, airbags, and padded floors save lives: they increase stopping distance, reducing the peak impact force. The formula: F = mv²/(2d), where v = √(2gh) for a fall from height h.
Example 1 — 5kg object falls 10m, stops over 5cm
- v = √(2×9.807×10) = 14.007 m/s
- F = 5×14.007²/(2×0.05) = 5×196.2/0.1 = 9,810 N
- G-force: 9810/(5×9.807) = 200.1g!
Example 2 — 80kg person falls 2m, stops over 5cm
- v = √(2×9.807×2) = 6.264 m/s
- F = 80×39.24/(0.1) = 31,392 N = 7,057 lbf
- G-force = 40.1g — severely injurious
Example 3 — Car 1500kg at 60km/h, crumple zone 0.5m
- v = 60 km/h = 16.667 m/s
- F = 1500×16.667²/(2×0.5) = 1500×277.8/1.0 = 416,700 N = 41.7 tonnes-force
- G-force = 28.3g — why seatbelts are essential
Common Mistakes in Gravitational Force Calculations
Mistake 1 — Confusing mass (kg) and weight (N)
- ❌ Wrong: "I weigh 70 kg on Mars" — your mass is 70 kg on Mars, not your weight
- ✅ Correct: Mass = 70 kg everywhere. Weight on Mars = 70×3.721 = 260.5 N. Weight measures the gravitational force exerted on an object.
Mistake 2 — Forgetting to SQUARE the distance in F=Gm₁m₂/r²
- ❌ Wrong: F = G×m₁×m₂/r (dividing by r instead of r²)
- ✅ Correct: F = G×m₁×m₂/r² — the denominator is r SQUARED. This is the most common arithmetic error in Newton's law calculations.
Mistake 3 — Using diameter instead of radius (or center-to-center distance)
- ❌ Wrong: Using the surface-to-surface distance as r
- ✅ Correct: r is the distance between CENTERS of mass. For two touching spheres of radii r₁ and r₂: r = r₁ + r₂. For Earth-Moon: r is center-to-center = 3.844×10⁸ m.
Mistake 4 — Wrong value of G (sign of exponent)
- ❌ Wrong: G = 6.674×10¹¹ (positive exponent)
- ✅ Correct: G = 6.674×10⁻¹¹ N·m²/kg² (negative exponent). Getting this wrong gives an answer 10²² times too large.
Mistake 5 — Thinking gravity depends on composition or density
- ❌ Wrong: "A denser material has stronger gravitational pull"
- ✅ Correct: Gravitational force depends ONLY on mass and distance (the two factors that affect gravitational force). A steel sphere and a wooden sphere of identical mass exert exactly the same gravitational force. Density and composition are irrelevant to F=Gm₁m₂/r².
Worked Examples — 8 Complete Problems
1. Earth-Moon gravitational force
- F = G×m₁×m₂/r² = 6.674×10⁻¹¹×5.972×10²⁴×7.342×10²²/(3.844×10⁸)²
- = 6.674×10⁻¹¹×4.383×10⁴⁷/1.478×10¹⁷ = 1.978×10²⁰ N
2. Two 1kg balls at 1m — gravity is weak!
- F = 6.674×10⁻¹¹×1×1/1² = 6.674×10⁻¹¹ N (67 picoNewtons)
3. 70kg person on Earth — their weight IS gravitational force
- W = m×g = 70×9.807 = 686.5 N = 154.3 lbf
4. 70kg person on Mars — weight on Mars
- W = 70×3.721 = 260.5 N = 58.6 lbf (38% of Earth weight)
5. Surface gravity of Mars from M and r
- g = GM/r² = 6.674×10⁻¹¹×6.417×10²³/(3.390×10⁶)² = 3.721 m/s²
6. G-force: car crash 60→0 km/h in 0.3s
- Δv = 60 km/h = 16.67 m/s; a = 16.67/0.3 = 55.56 m/s²
- n = 55.56/9.807 = 5.67g (fighter pilot zone — dangerous!)
7. Impact force: 80kg person falls 2m, stops over 5cm
- v = √(2×9.807×2) = 6.264 m/s; F = 80×39.24/0.1 = 31,392 N
8. 100 lb person on Venus (how much would a 100 lb person weigh on Venus?)
- Mass = 100 lbf / 2.2046 = 45.36 kg
- W_Venus = 45.36 × 8.87 = 402.3 N = 90.5 lbf (90.5% of Earth weight)
Frequently Asked Questions — Gravitational Force
Related Calculators
| Planet | g (m/s²) | g/g_E |
|---|---|---|
| ☿ Mercury | 3.70 | 0.378 |
| ♀ Venus | 8.87 | 0.905 |
| 🌍 Earth | 9.807 | 1.000 |
| 🌙 Moon | 1.62 | 0.165 |
| ♂ Mars | 3.721 | 0.379 |
| ♃ Jupiter | 24.79 | 2.528 |
| ♄ Saturn | 10.44 | 1.065 |
| ⛢ Uranus | 8.69 | 0.886 |
| ♆ Neptune | 11.15 | 1.137 |
| ♇ Pluto | 0.62 | 0.063 |
| ☀ Sun | 274.0 | 27.94 |
| Planet | Mass (kg) | Radius (km) | g (m/s²) | g/g_Earth |
|---|---|---|---|---|
| ☿ Mercury | 3.301×10²³ | 2,440 | 3.70 | 0.378 |
| ♀ Venus | 4.868×10²⁴ | 6,052 | 8.87 | 0.905 |
| 🌍 Earth | 5.972×10²⁴ | 6,371 | 9.807 | 1.000 |
| 🌙 Moon | 7.342×10²² | 1,737 | 1.62 | 0.165 |
| ♂ Mars | 6.417×10²³ | 3,390 | 3.721 | 0.379 |
| ♃ Jupiter | 1.898×10²⁷ | 69,911 | 24.79 | 2.528 |
| ♄ Saturn | 5.683×10²⁶ | 58,232 | 10.44 | 1.065 |
| ⛢ Uranus | 8.681×10²⁵ | 25,362 | 8.69 | 0.886 |
| ♆ Neptune | 1.024×10²⁶ | 24,622 | 11.15 | 1.137 |
| ♇ Pluto | 1.303×10²² | 1,188 | 0.62 | 0.063 |
| ☀ Sun | 1.989×10³⁰ | 695,700 | 274.0 | 27.94 |
| Factor | Effect on F=Gm₁m₂/r² | Formula |
|---|---|---|
| Mass of objects | Double m₁ → F doubles | F ∝ m₁ × m₂ |
| Distance between objects | Double r → F decreases by 4× | F ∝ 1/r² |
| Property | Value |
|---|---|
| Symbol | G |
| Value | 6.67430×10⁻¹¹ N·m²/kg² |
| SI units | N·m²/kg² |
| First measured by | Henry Cavendish (1798) |
| Uncertainty | ±0.00015×10⁻¹¹ (most uncertain fundamental constant) |
| Standard gravity g₀ | 9.80665 m/s² (exact SI) |
| Term | Definition | Unit | Changes with location? |
|---|---|---|---|
| Mass | Amount of matter | kg | No — constant everywhere |
| Weight | Gravitational force on mass (W=mg) | N (or lbf) | Yes — varies by planet |
| G-force | Acceleration in units of g | dimensionless | Yes |
| g (surface gravity) | Gravitational field strength = GM/r² | m/s² = N/kg | Yes — by planet |
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Shahid Ali
Shahid Ali is the creator and lead developer of SciSolveLab, a platform dedicated to making complex scientific and mathematical computations accessible. With a deep background in physics, thermodynamics, and wave mechanics, Shahid's work is driven by the belief that robust, accurate mathematical tools should be just a click away for students, engineers, and researchers.