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In the late 17th century, Isaac Newton proposed one of the most important laws in all of physics: a universal law that describes the gravitational attraction between any two masses in the universe. This law unified terrestrial gravity — the force that makes an apple fall — with celestial mechanics — the force that keeps the Moon in orbit around the Earth and the planets in orbit around the Sun.
Newton's law states that every point mass attracts every other point mass with a force that is:
Mathematically:
F=r2GMm
where:
This is a universal law — it applies to every pair of masses in the universe, from atoms to galaxies. The same equation that describes the force between your body and the Earth also describes the force between binary star systems billions of light years away.
flowchart LR
A["Mass M"] -- "F = GMm/r²" --> B["Mass m"]
B -- "F = GMm/r² (equal & opposite)" --> A
subgraph Key["Newton's Third Law Pair"]
C["Same magnitude"]
D["Opposite directions"]
E["Act on different bodies"]
end
The gravitational constant G is one of the fundamental constants of nature. Its value is extremely small:
G=6.674×10−11 N m2 kg−2
This tiny value explains why gravitational forces between everyday objects are imperceptible. Two 1 kg masses placed 1 metre apart attract each other with a force of just 6.674 × 10⁻¹¹ N — far too small to notice. It is only when at least one of the masses is astronomical (like a planet or star) that gravity becomes significant.
G was first measured by Henry Cavendish in 1798 using a torsion balance experiment. His measurement allowed the mass of the Earth to be calculated for the first time, which is why the experiment is sometimes called "weighing the Earth."
It is important to distinguish between G (the universal gravitational constant, always the same everywhere) and g (the gravitational field strength at a particular point, which varies with location).
| Symbol | Name | Value | Units | Constant? |
|---|---|---|---|---|
| G | Universal gravitational constant | 6.674 × 10⁻¹¹ | N m² kg⁻² | Yes — same everywhere |
| g | Gravitational field strength | Varies (9.81 at Earth's surface) | N kg⁻¹ | No — depends on location |
Common exam mistake: Confusing G and g. The constant G is universal and never changes. The field strength g varies with position, mass, and radius of the body you are on. A question asking "what happens to G if you double the mass?" is testing whether you know G is a constant — the answer is nothing.
The inverse square relationship (F ∝ 1/r²) is one of the most important features of Newton's law. It means that:
The inverse square law arises because gravitational influence spreads out over the surface of an expanding sphere. At distance r, the "influence" is distributed over a sphere of area 4πr², so the force per unit area decreases as 1/r².
| Distance multiplier | Force multiplier | Percentage of original |
|---|---|---|
| ×1 (original) | ×1 | 100% |
| ×2 | ×1/4 | 25% |
| ×3 | ×1/9 | 11.1% |
| ×5 | ×1/25 | 4% |
| ×10 | ×1/100 | 1% |
| ×0.5 (halved) | ×4 | 400% |
This relationship is fundamental to understanding how gravity behaves over astronomical distances. The Sun's gravitational pull on Neptune (at 30 AU) is 900 times weaker than its pull on Earth (at 1 AU), because 30² = 900.
F=(3.84×108)26.674×10−11×5.97×1024×7.35×1022
F=1.47×10172.93×1037=1.99×1020 N
This enormous force — about 2 × 10²⁰ N — is what keeps the Moon in orbit.
Two students, each with mass 60 kg, stand 1.5 m apart:
F=1.526.674×10−11×60×60=2.252.40×10−7=1.07×10−7 N
This is about 0.1 micronewtons — completely undetectable without extremely sensitive equipment.
The ISS orbits at approximately 408 km above Earth's surface. Calculate the gravitational force on it (mass ≈ 420,000 kg).
The orbital radius is r = R_Earth + h = 6.37 × 10⁶ + 4.08 × 10⁵ = 6.778 × 10⁶ m
F=r2GMm=(6.778×106)26.674×10−11×5.97×1024×4.20×105
F=4.594×10131.673×1020=3.64×106 N=3.64 MN
The ISS still experiences about 89% of the gravitational force it would feel on the surface. Astronauts appear "weightless" not because gravity is absent, but because they are in free fall — the ISS and everything inside it accelerate together.
Common exam mistake: Students often say astronauts on the ISS are weightless because there is no gravity in space. This is wrong. At ISS altitude, g ≈ 8.7 N kg⁻¹ (about 89% of the surface value). The apparent weightlessness is because the ISS is in continuous free fall around Earth.
An essential point: the gravitational force between two objects is a Newton's third law pair. The Earth pulls on you with a force mg downward, and you pull on the Earth with an equal force mg upward. These forces are equal in magnitude, opposite in direction, and act on different bodies.
The reason the Earth does not noticeably accelerate towards you is that F = ma: the same force on the Earth's enormous mass produces an unimaginably tiny acceleration (about 10⁻²³ m s⁻²).
When more than two masses are present, the total gravitational force on any one mass is the vector sum of the individual forces from all other masses. This is the principle of superposition.
For example, a spacecraft travelling between the Earth and the Moon experiences gravitational pulls from both bodies simultaneously. At each point, the net force is the vector sum of the Earth's pull and the Moon's pull.
Three masses are arranged in a line: mass A (2.0 × 10³⁰ kg) at x = 0, mass B (5.0 × 10²⁰ kg) at x = 1.0 × 10¹¹ m, and mass C (3.0 × 10³⁰ kg) at x = 3.0 × 10¹¹ m. Find the net gravitational force on mass B.
Force on B due to A (towards A, in −x direction):
FBA=(1.0×1011)26.674×10−11×2.0×1030×5.0×1020=1.0×10226.674×1040=6.674×1018 N
Force on B due to C (towards C, in +x direction):
FBC=(2.0×1011)26.674×10−11×3.0×1030×5.0×1020=4.0×10221.001×1041=2.503×1018 N
Net force on B: F_BA − F_BC = 6.674 × 10¹⁸ − 2.503 × 10¹⁸ = 4.17 × 10¹⁸ N towards A.
Superposition is crucial in astrophysics. The orbit of any planet is influenced by the gravitational pull of the Sun and all other planets. These perturbations — small deviations from a perfect elliptical orbit — led to the discovery of Neptune in 1846 when astronomers noticed unexplained anomalies in the orbit of Uranus.
The connection between Newton's law and gravitational field strength is straightforward. If a test mass m is placed in the field of a large mass M at distance r:
F=r2GMm
Dividing both sides by m:
mF=r2GM
But F/m is the definition of gravitational field strength g. Therefore:
g=r2GM
This shows that the field strength at any point depends only on the source mass M and the distance r — it is independent of the test mass. This is a fundamental property of fields: the field exists regardless of whether a test mass is present to detect it.
| Pair of bodies | Force (N) | Comment |
|---|---|---|
| Sun – Earth | 3.54 × 10²² | Keeps Earth in orbit |
| Sun – Jupiter | 4.17 × 10²³ | Largest planet-Sun force |
| Earth – Moon | 1.99 × 10²⁰ | Causes tides |
| Earth – ISS | 3.64 × 10⁶ | Station in free fall |
| You – Earth | ~700 | Your weight |
| You – the person next to you | ~10⁻⁷ | Undetectable |
Edexcel 9PH0 specification Topic 12 — Gravitational Fields opens with Newton's law of universal gravitation F=Gm1m2/r2, the inverse-square dependence on separation, and the recognition that the law applies to every pair of point masses (and to spherically symmetric bodies via the shell theorem). It then develops field strength, potential and orbital motion (refer to the official specification document for exact wording). Newton's law is the foundation statement on which the rest of Topic 12 is built — g=GM/r2 is obtained by dividing F by the test mass, and V=−GM/r is obtained by integrating g from infinity. The law is examined in Paper 2 (9PH0/02), where it routinely appears in calculation questions about planetary, lunar and satellite forces, and in Paper 3 (9PH0/03) synoptic questions linking it to circular motion, energy conservation and Kepler's laws. The Edexcel formula booklet provides F=Gm1m2/r2 explicitly, but candidates must remember the value of G (6.67×10−11 N m2 kg−2) and that the law assumes point-mass (or shell-theorem) geometry.
Question (8 marks):
(a) Calculate the magnitude of the gravitational force between the Earth (mass 5.97×1024 kg) and the Moon (mass 7.35×1022 kg), given a centre-to-centre separation of 3.84×108 m. Use G=6.67×10−11 N m2 kg−2. (3)
(b) The Moon orbits the Earth approximately in a circle of this radius with a period of 27.3 days. Show that the centripetal force required is consistent with the gravitational force found in (a). (4)
(c) State the magnitude and direction of the gravitational force exerted by the Moon on the Earth. (1)
Solution with mark scheme:
(a) Step 1 — apply Newton's law of gravitation.
F=r2Gm1m2=(3.84×108)2(6.67×10−11)(5.97×1024)(7.35×1022)
M1 — correct substitution into F=Gm1m2/r2 with consistent SI units.
Step 2 — evaluate numerator and denominator separately to preserve precision.
Numerator: (6.67×10−11)(5.97×1024)(7.35×1022)≈2.926×1037.
Denominator: (3.84×108)2=1.475×1017.
M1 — correct evaluation of r2. Common slip: forgetting the square, or inputting r in km rather than m.
A1 — F=2.926×1037/1.475×1017=1.98×1020 N (accept 1.97–2.00×1020 N, units required).
(b) Step 1 — express the centripetal force.
The centripetal force required for circular motion of the Moon (mass m) at radius r with angular speed ω=2π/T is:
Fc=mω2r=m(T2π)2r
M1 — correct centripetal-force expression in terms of T and r.
Step 2 — convert the period to seconds.
T=27.3×24×3600=2.359×106 s.
Step 3 — evaluate.
Fc=(7.35×1022)(2.359×1062π)2(3.84×108)
ω=2π/2.359×106=2.664×10−6 rad s−1, so ω2=7.10×10−12 rad2 s−2.
Fc=(7.35×1022)(7.10×10−12)(3.84×108)≈2.00×1020 N.
M1 — correct numerical substitution.
A1 — Fc≈2.0×1020 N, in agreement with (a) to within ∼1%.
A1 (consistency) — explicit comparison statement: "the gravitational force from (a) and the required centripetal force agree to within rounding error, confirming that gravity supplies the centripetal force for the Moon's orbit".
(c) B1 — by Newton's third law, the Moon exerts an equal and opposite force on the Earth: 1.98×1020 N directed from the centre of the Earth toward the centre of the Moon.
Total: 8 marks (M4 A3 B1, split as shown).
Question (6 marks): A spacecraft of mass m=1.20×104 kg lies on the line joining the centres of the Earth and the Moon. The Earth–Moon centre-to-centre distance is d=3.84×108 m. Take ME=5.97×1024 kg and MM=7.35×1022 kg.
(a) Determine the distance x from the centre of the Earth at which the net gravitational force on the spacecraft is zero. (4)
(b) State and justify whether the spacecraft, placed at rest at this point, would remain there. (2)
Mark scheme decomposition by AO:
(a)
(b)
Total: 6 marks split AO1 = 1, AO2 = 3, AO3 = 2. Edexcel uses null-force questions of this kind to combine routine algebra (AO1/AO2) with a higher-tariff stability argument (AO3) — the AO3 mark separates A from A*.
Connects to:
Topic 7 — Electric Fields (Coulomb's law analogy): Coulomb's law F=kQ1Q2/r2 is structurally identical to Newton's gravitational law, with charge Q in place of mass m and k=1/(4πε0) in place of G. The crucial physical difference is that gravity is always attractive (no "negative mass") whereas Coulomb forces can repel. Edexcel routinely asks candidates to compare and contrast — name the analogy and the breaking-point.
Topic 12 — Gravitational Field Strength: g=GM/r2 is Newton's law divided by the test mass. The radial-field formula and the inverse-square decay are inherited directly from F∝1/r2. A confident grasp of Newton's law makes field-strength questions almost mechanical.
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