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Reading Time: 6 min
Last Updated: March 9, 2026
Main Ideas: 5
Reading Time: 6 min
Last Updated: March 9, 2026
Main Ideas: 5

Topic 2.6 Notes – Gravitational Force

Verified for 2027 AP® Physics C: Mechanics Exam
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You’ll move from the force between two point masses to modeling gravity as a field, then to weight, apparent weight, mass types, and finally how gravity behaves inside spherical objects. This is where Newton’s law starts connecting to orbits and energy later on.

1. Newton’s Law of Universal Gravitation

Every mass attracts every other mass.

F⃗g=Gm1m2r2r^ \vec{F}_{g} = G \frac{m_{1} m_{2}}{r^{2}}\hat{r}

  • G=6.67×10−11 N⋅m2/kg2G = 6.67 \times 10^{-11}\ \text{N}\cdot\text{m}^{2}/\text{kg}^{2}
  • rr is the distance between centers of mass
  • Direction r^ \hat{r} : along the line connecting the centers
  • The force is always attractive

Patterns you must recognize instantly

  • F∝m1F \propto m_{1}
  • F∝m2F \propto m_{2}
  • F∝1r2F \propto \frac{1}{r^{2}}

If distance doubles, force becomes 1/41/4.
If one mass triples, force triples.

Here’s the geometry the equation assumes. The force on each mass points along the line connecting their centers, and the two forces are equal in magnitude and opposite in direction.

Study guide illustration

Mutual gravitational forces between two masses

For spherically symmetric objects (planets, stars), you treat them like point masses located at their centers. That shortcut becomes crucial later for orbits.

2. Gravitational Field and Weight

Instead of always thinking about two objects pulling on each other, it’s often cleaner to say a mass creates a gravitational field around it.

Gravitational Field

g⃗=F⃗gm \vec{g} = \frac{\vec{F}_{g}}{m}

For a mass MM:

g⃗=GMr2r^ \vec{g} = G \frac{M}{r^{2}}\hat{r}

  • Units: N/kg=m/s2 \text{N/kg} = \text{m/s}^{2}
  • Direction: toward the mass
  • If gravity is the only force, then a⃗=g⃗ \vec{a} = \vec{g}

That last idea is huge. Field strength numerically equals free-fall acceleration.

Weight

Weight is the gravitational force from a large astronomical body.

Fweight=mg F_{\text{weight}} = mg

  • Mass stays the same everywhere.
  • Weight changes with location.
  • Near Earth’s surface, g≈9.8≈10 N/kg g \approx 9.8 \approx 10\ \text{N/kg} .

When Can You Treat Gravity as Constant?

Near Earth’s surface, changes in height are tiny compared to Earth’s radius. That means:

  • rr barely changes
  • gg is approximately constant
  • FgF_{g} is approximately constant

That’s why projectile motion uses constant gg.
This approximation breaks down for satellites or large altitude changes.

3. Apparent Weight and Noninertial Frames

What a scale reads is normal force, not mgmg.

Let upward be positive. Apply ∑F=ma \sum F = ma .

SituationAccelerationNormal Force (Apparent Weight)
At rest / constant velocitya=0a = 0N=mgN = mg
Accelerating upwarda>0a > 0N=m(g+a)N = m(g + a)
Accelerating downwarda>0a > 0 downwardN=m(g−a)N = m(g - a)
Free falla=ga = g downwardN=0N = 0

If N=0N = 0, you feel weightless.

Astronauts in orbit are weightless because gravity is the only force acting. They’re in continuous free fall.

Equivalence Principle

Inside a closed box, you cannot distinguish between:

  • Being at rest in a gravitational field
  • Accelerating upward in deep space

Acceleration and gravity are locally indistinguishable. This idea shows up conceptually on exams more than computationally.

4. Inertial Mass vs Gravitational Mass

Two roles for mass:

Inertial Mass mim_{i}

From Newton’s second law:

F=mia F = m_{i} a

Measures resistance to acceleration.

Gravitational Mass mgm_{g}

From the gravitational law:

Fg=Gmg1mg2r2 F_{g} = G \frac{m_{g1} m_{g2}}{r^{2}}

Determines strength of gravitational attraction.

The Big Experimental Result

mi=mg m_{i} = m_{g}

Because they’re equal:

  • All objects fall with the same acceleration (ignoring air).
  • gg does not depend on the object’s mass.

That equality is not assumed lightly. It’s experimentally verified.

5. Gravity from Spherical Mass Distributions

The total gravitational force from a distributed object is the vector sum of forces from tiny mass pieces. For spherical symmetry, Newton’s shell theorem simplifies everything.

No derivation required for AP.

Thin Spherical Shell

The figure below summarizes the key results for both a thin shell and a solid sphere. Focus first on the thin shell cases.

Study guide illustration

Newton’s shell theorem: shell vs. solid sphere

  • Outside → behaves like all mass at center
    F=GMmr2F = G \frac{Mm}{r^{2}}
  • Inside → F=0F = 0

Forces cancel perfectly inside.

Solid Sphere with Uniform Density

Now focus on the solid sphere cases in the same figure.

Outside behaves like a point mass.

Inside is more interesting.

Only mass at radius ≤r \le r contributes.

mpartial=43πr3ρ m_{\text{partial}} = \frac{4}{3}\pi r^{3} \rho

Force becomes:

F=GMmR3r F = G \frac{Mm}{R^{3}} r

So inside:

F∝r F \propto r

  • Zero at center
  • Increases linearly
  • Maximum at surface

That linear dependence is mathematically identical to a spring force. If you drilled through Earth (uniform density assumption), motion would be simple harmonic motion.

Key Takeaways

Gravitational force depends on distance between centers of mass, not surfaces.
Field strength gg equals the acceleration of free fall at that location.
Near Earth’s surface, treating gg as constant is an approximation based on rr barely changing.
Apparent weight equals the normal force, which changes whenever there is vertical acceleration.
Weightlessness means N=0N = 0, not Fg=0F_{g} = 0.
Equality of inertial and gravitational mass explains why acceleration due to gravity is mass-independent.
Inside a uniform sphere, gravitational force is proportional to rr, which leads to simple harmonic motion behavior.

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