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Honors Physics Unit 7 Review: Newton's Law of Gravitation

This unit explains why the Moon, planets, and satellites move the way they do, starting with Kepler's patterns and ending with Newton's and Einstein's explanations for them. By the end, you should be able to calculate gravitational force, field strength, orbital speed, and orbital period, and explain what makes an orbit fast or slow.

Read the big ideas first, then work through each topic's notes and try the check-yourself question before moving on.

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What is Honors Physics unit 7?

Gravity is the same force whether it pulls an apple off a tree or holds Jupiter in orbit. This unit connects those two scales. You'll use the centripetal force ideas from circular motion and the energy and momentum ideas from earlier units, now applied to planets and satellites.

Honors Physics Unit 7 covers gravitation in two parts. First come Kepler's laws: orbits are ellipses with the Sun at one focus, planets sweep out equal areas in equal times, and T2T^2 is proportional to a3a^3. Second is Newton's law of universal gravitation, F=Gm1m2r2F = G\frac{m_1 m_2}{r^2}, which you use to find gravitational force, field strength g=GMr2g = \frac{GM}{r^2}, circular orbital speed v=GM/rv = \sqrt{GM/r}, and orbital period. The unit closes with how Einstein's general relativity describes gravity as the curvature of spacetime and where it improves on Newton.

Gravity weakens with the square of the distance between centers.

Doubling the center-to-center distance cuts the force to one quarter, and tripling it cuts the force to one ninth. For spherical bodies, measure rr between their centers. An object on Earth's surface sits at r=6.37×106r = 6.37 \times 10^6 m from Earth's center, not zero.

An orbit is free fall with enough sideways speed to keep missing the ground.

For a circular orbit around a much more massive body, gravity provides the centripetal force. Setting GMmr2=mv2r\frac{GMm}{r^2} = \frac{mv^2}{r} gives v=GM/rv = \sqrt{GM/r}, so the satellite's mass cancels. Around the same central body, closer circular orbits are faster and have shorter periods.

Newton's law works in many cases, and Einstein's theory improves on it.

General relativity treats gravity as mass and energy curving spacetime. In weak fields and at low speeds, its predictions are close to Newton's. It becomes necessary near black holes, for GPS clock corrections, and for small effects like the precession of Mercury's orbit.

One simple force law explains motion on Earth and in the sky.

Before Newton, falling objects and planetary orbits seemed to follow different rules. Newton's 1687 law of universal gravitation showed that the same inverse square attraction causes both, and Kepler's laws fall out of it as consequences. Einstein's theory changed the description of gravity, but it agrees closely with Newton's predictions when gravity is weak and speeds are low.

Honors Physics unit 7 topics

Unit 7 review notes

7.1

Kepler's Laws of Planetary Motion

Kepler's three laws describe how planets move, and Newton later showed that all three follow from gravity. Johannes Kepler worked them out in the early 1600s using Tycho Brahe's careful observations of Mars.

The first law says orbits are ellipses with the Sun at one focus. For a noncircular ellipse, the other focus is empty; for a circle, both foci coincide at the center. Eccentricity ee measures how stretched the ellipse is. A circle has e=0e = 0, and Earth's orbit (e≈0.017e \approx 0.017) is very close to one.

The second law says a line from the Sun to a planet sweeps out equal areas in equal times. So a planet moves fastest at perihelion (its closest point) and slowest at aphelion (its farthest point). The reason is conservation of angular momentum. Gravity points straight at the Sun, so it exerts no torque about the Sun.

The third law links orbit size to orbit time with T2∝a3T^2 \propto a^3, where aa is the semi-major axis. Newton's version is T2=4π2GMa3T^2 = \frac{4\pi^2}{GM}a^3, where MM is the mass of the central body. The orbiting body's mass drops out as long as it's much smaller than MM.

Worked example. Mars has a semi-major axis of a=1.52a = 1.52 AU. For an object much less massive than the Sun, measuring TT in years and aa in AU gives approximately T2=a3T^2 = a^3. So T2=1.523=3.51T^2 = 1.52^3 = 3.51, and T=3.51=1.87T = \sqrt{3.51} = 1.87 years. The measured value is 687 days, or 1.88 years, so the law holds up.

  • Ellipse: An oval-shaped closed curve with two focus points, where the Sun sits at one focus of a planet's orbit.
  • Eccentricity: A number from 0 to just under 1 for closed orbits that tells how stretched an ellipse is, with 0 meaning a perfect circle.
  • Semi-major axis: Half the longest diameter of an ellipse. For an orbit, it is also the average of the closest and farthest distances from the central body.
  • Perihelion and aphelion: The closest and farthest points of an orbit around the Sun, where the planet moves fastest and slowest.

Check yourself: A planet orbits a star with the same mass as the Sun at a semi-major axis of 4 AU. What is its orbital period? (Answer: T2=43=64T^2 = 4^3 = 64, so T=8T = 8 years.)

7.2

Newton's Law of Universal Gravitation and Einstein's Theory of General Relativity

Newton's law of universal gravitation says masses attract one another. For point masses or nonoverlapping spherical bodies with spherically symmetric mass distributions, F=Gm1m2r2F = G\frac{m_1 m_2}{r^2}, where G=6.67×10−11G = 6.67 \times 10^{-11} N·m²/kg² and rr is the distance between their centers. If you double the distance, the force drops to one quarter, which is why it's called an inverse square law. The force is always attractive and equal on both objects, so Earth pulls on you exactly as hard as you pull on Earth.

Divide the force on a test mass by that mass to get gravitational field strength, measured in N/kg, equivalent to m/s². Outside a spherically symmetric body of mass MM, its field has magnitude g=GMr2g = \frac{GM}{r^2}. For a circular orbit around a much more massive body, gravity supplies the centripetal force, so GMmr2=mv2r\frac{GMm}{r^2} = \frac{mv^2}{r} gives v=GM/rv = \sqrt{GM/r}.

Worked example. The ISS orbits about 420 km up, so r=6.37×106+0.42×106=6.79×106r = 6.37\times10^6 + 0.42\times10^6 = 6.79\times10^6 m. Earth's GM=(6.67×10−11)(5.97×1024)=3.98×1014GM = (6.67\times10^{-11})(5.97\times10^{24}) = 3.98\times10^{14} m³/s². Then g=3.98×1014(6.79×106)2=8.6g = \frac{3.98\times10^{14}}{(6.79\times10^6)^2} = 8.6 m/s², about 88% of surface gravity. Astronauts float because they and the station are falling together, not because gravity is gone. Their orbital speed is v=3.98×1014/6.79×106≈7.7v = \sqrt{3.98\times10^{14} / 6.79\times10^6} \approx 7.7 km/s.

Einstein's general relativity (1915) describes gravity as mass and energy curving spacetime instead of a force acting at a distance. It agrees closely with Newton in weak fields at low speeds. It also explains the extra precession of Mercury's orbit beyond Newtonian predictions and predicts how much light bends around massive objects.

  • Gravitational constant (G): The universal constant 6.67×10−116.67 \times 10^{-11} N·m²/kg² that sets the strength of gravity in Newton's law.
  • Gravitational field strength: The gravitational force per kilogram at a location, equal to the free-fall acceleration there. Outside a spherically symmetric body, its field has magnitude g=GM/r2g = GM/r^2.
  • Inverse square law: A relationship where a quantity is proportional to 1/r21/r^2, so doubling the distance makes it four times smaller.
  • Spacetime curvature: Einstein's description of gravity, where mass and energy bend space and time so that objects follow curved paths.

Check yourself: What is the gravitational field strength at a point two Earth radii from Earth's center? (Answer: The distance doubled, so gg is one quarter of 9.8 m/s², about 2.45 m/s².)

QuestionNewton's gravityEinstein's general relativity
What is gravity?An attractive force between massesThe curvature of spacetime caused by mass and energy
How fast do gravitational effects travel?Instantly (action at a distance)At the speed of light, as gravitational waves
Where does it work well?Weak fields and low speeds, like everyday motion and most orbitsIn tested cases including strong gravity and high speeds, though it is not a complete theory of quantum gravity
Mercury's orbitPredicts slightly too little precessionMatches the observed precession
Light passing a starPredicts little or no bendingCorrectly predicts gravitational lensing

Key terms

TermDefinition
Newton's law of universal gravitationThe rule that masses attract one another. For point masses or nonoverlapping spherically symmetric bodies, the force has magnitude $F = G\frac{m_1 m_2}{r^2}$ and acts along the line between their centers.
Gravitational field strengthThe gravitational force per unit mass at a point, measured in N/kg. Outside a spherically symmetric body, its field has magnitude $g = GM/r^2$. Near Earth's surface, $g$ is about 9.8 N/kg.
Kepler's first lawEach planet moves in an elliptical orbit with the Sun at one focus.
Kepler's second lawA line from the Sun to a planet sweeps out equal areas in equal times, so planets move faster when closer to the Sun.
Kepler's third lawThe square of the orbital period is proportional to the cube of the semi-major axis, $T^2 \propto a^3$.
Orbital speedThe speed needed for a circular orbit, $v = \sqrt{GM/r}$, which gets smaller as the orbit gets larger.
Escape velocityThe minimum speed needed to reach arbitrarily far from an isolated body without further thrust. From Earth's surface, it is about 11.2 km/s when air resistance and other bodies' gravity are ignored.
General relativityEinstein's 1915 theory that describes gravity as the curvature of spacetime by mass and energy.

Mistakes to avoid in Newton's Law of Gravitation

Measuring r from the surface instead of the center

Problems often give altitude, like a satellite 420 km above Earth. Newton's law needs the center-to-center distance, so add Earth's radius first: r=6.37×106+4.2×105r = 6.37\times10^6 + 4.2\times10^5 m. Using the altitude alone gives a force that is hundreds of times too big.

Thinking double the distance means half the force

Gravity depends on 1/r21/r^2, not 1/r1/r. Doubling the distance divides the force by 4, and tripling it divides by 9. Set up a ratio like F2F1=(r1r2)2\frac{F_2}{F_1} = \left(\frac{r_1}{r_2}\right)^2 to check yourself quickly.

Believing astronauts float because there's no gravity in space

At the ISS, gravity is still about 8.6 m/s², roughly 88% of what you feel on the ground. Astronauts feel weightless because they and the station are in free fall together, so nothing pushes up on them. Gravity is what keeps the station in orbit at all.

Assuming a heavier satellite needs a different orbital speed

In v=GM/rv = \sqrt{GM/r} and T2=4π2GMa3T^2 = \frac{4\pi^2}{GM}a^3, MM is the central body's mass. These formulas assume the satellite is much less massive than the central body. A bolt and a space station in circular orbits at the same radius around the same body have the same orbital speed.

Study unit 7 other ways

Ready to review Unit 7?Start with the notes, check the topic cards, and use the practice or resource links when they are available for this course.