Newton’s Revolution

From Patterns to Physics

Dr. Anna Rosen

February 4, 2026

The Apple and the Moon

Does the force that pulls an apple to the ground…

also reach up to the Moon?

The Moon Is Falling

The Moon IS falling toward Earth.

Right now. Continuously. Every second.

But it’s moving sideways so fast that it keeps missing.

That combination of falling + moving sideways is what we call an orbit.

The Moon’s Orbit: Velocity + Inward Force

Two ideas at once:

  • Sideways velocity carries the Moon forward
  • Gravity pulls inward

The path curves because both happen continuously.

Earth with a Moon moving along an elliptical path, showing tangent velocity arrows and inward gravitational force arrows.
Credit: cococubed.com

Newton’s Cannon

Multiple projectile paths around Earth showing impacts, bound orbits, and unbound escape trajectories.
Credit: cococubed.com

Fire fast enough to fall around Earth instead of hitting it.

Today’s Learning Objectives

By the end of today, you can:

  • State Newton’s three laws and use \(F = ma\)
  • Explain why circular motion needs centripetal acceleration
  • State universal gravitation and the inverse-square rule

Today’s Learning Objectives (continued)

By the end of today, you can:

  • Distinguish mass from weight
  • Explain why astronauts float (free fall, not zero gravity)
  • Connect Newton’s gravity to Kepler’s three laws
  • Use orbital motion to infer mass of a central object

Where We Left Off (Lecture 5)

Kepler discovered three empirical laws:

  1. Orbits are ellipses with the Sun at one focus
  2. Planets sweep equal areas in equal times
  3. \(P^2 \propto a^3\) (period-distance relation)

These describe what planets do.

But Kepler couldn’t explain why.

Part 1: The Rules of Motion

Newton’s Three Laws

Newton’s First Law: Inertia

An object at rest stays at rest. An object in motion stays in motion — unless acted upon by a net force.

Key insight: Things don’t change their motion on their own.

If something speeds up, slows down, or changes direction — a net force caused it.

First Law Example: Deep Space

A spacecraft in deep space fires its engines briefly, then shuts them off. What happens next?

  • It gradually slows down and stops
  • It continues at constant velocity indefinitely
  • It starts drifting toward the nearest star
  • It needs to keep firing to maintain speed

Newton’s Second Law: F = ma

\[\vec{F}_{net} = m\vec{a}\]

Net force tells matter how to accelerate.

Mass tells matter how much to resist.

A vector has magnitude and direction. The arrows show direction.

Units: force in N, mass in kg, acceleration in \(\mathrm{m/s^2}\).

More net force, more acceleration.

More mass, less acceleration.

Quick Check: F = ma

The same force is applied to a bowling ball and a tennis ball. Which experiences greater acceleration?

  • The bowling ball (more mass)
  • The tennis ball (less mass)
  • Both experience the same acceleration
  • Neither accelerates

Critical Insight: Direction Changes = Acceleration

Constant speed ≠ constant velocity

Acceleration happens when either changes:

  • Speeding up
  • Slowing down
  • Changing direction at constant speed

A planet moving in a circle at constant speed is accelerating because its direction constantly changes!

Quick Check: Circular Motion

A car drives around a circular track at a constant speedometer reading of 60 mph. Is the car accelerating?

  • No — the speed is constant
  • Yes — the direction is constantly changing
  • Only if the driver presses the gas pedal
  • Only if there’s friction

Centripetal Acceleration

For circular motion at speed \(v\) and radius \(r\):

\[a_c = \frac{v^2}{r}\]

This acceleration points toward the center.

The force required:

\[F_c = ma_c = \frac{mv^2}{r}\]

What Provides the Centripetal Force?

Centripetal force is not a new type of force.

It’s whatever force happens to be pulling the object toward the center:

  • For planets: gravity
  • For a ball on a string: tension
  • For a car turning: friction between tires and road

Circular Motion Needs an Inward Force

If the inward force vanishes, the object keeps moving straight.

That is Newton’s First Law in action.

Two panels: a ball on a string moving in a circle with an inward force, and after the string breaks the ball moves straight.
Credit: cococubed.com

Quick Check: Centripetal Force

A planet orbits the Sun in a nearly circular orbit. What force provides the centripetal acceleration?

  • The planet’s inertia
  • The planet’s momentum
  • Gravity from the Sun
  • The planet’s rotational spin

Newton’s Third Law: Action-Reaction

For every force, there is an equal and opposite reaction force.

Examples:

  • You push on the ground; the ground pushes back on you
  • Earth pulls on the Moon; the Moon pulls on Earth
  • The Sun pulls on Jupiter; Jupiter pulls on the Sun

The Astronomical Payoff

Jupiter pulls on the Sun with the same force the Sun pulls on Jupiter.

But the Sun is about 1000 times more massive, so it accelerates about 1000 times less.

The Sun wobbles — just barely.

This tiny stellar wobble is one major way we detect exoplanets!

Center of Mass: The Real Pivot Point

The center of mass is the balance point of a system. If you could put your finger exactly there, the system would not tip.

For a star–planet pair, both objects orbit this point, not each other. The more massive object sits closer to it, so its orbit is smaller — that is the wobble we detect.

Diagram showing a star and a planet connected by a line with a marked center of mass between them; both bodies trace orbits around that point.
Credit: cococubed.com

Quick Check: Third Law

Earth exerts a gravitational force on the Moon. The Moon exerts a force on Earth that is:

  • Much weaker, because the Moon is smaller
  • Much stronger, because Earth is closer
  • Exactly equal in magnitude, opposite in direction
  • Zero, because the Moon is in space

Part 2: Universal Gravitation

One equation rules all

Predict First!

If you double your distance from Earth’s center, gravity becomes…

  • 1/2 as strong
  • 1/4 as strong
  • 1/8 as strong

Newton’s Law of Universal Gravitation

\[F_g = \frac{Gm_1m_2}{r^2}\]

Part Meaning
\(G\) Universal constant (\(6.67 \times 10^{-11}\ \mathrm{N\,m^2/kg^2}\))
\(m_1 m_2\) Force depends on both masses
\(r^2\) Force weakens with distance squared

The Gravity Equation in Pictures

Gravity depends on:

  • Both masses (\(m_1, m_2\))
  • Distance squared (\(r^2\))

Closer or more massive means stronger force.

Two masses labeled M1 and M2 separated by distance d with the formula F = G M1 M2 / d^2 shown between them.
Credit: cococubed.com

The Inverse-Square Law

\(r^2\) in the denominator” is profound:

Distance change Force change
Double the distance Force drops to 1/4
Triple the distance Force drops to 1/9
\(10\times\) the distance Force drops to 1/100

Why Inverse-Square?

As distance grows, the same influence spreads over a larger sphere.

Area grows like \(r^2\), so strength drops like \(1/r^2\).

Concentric spheres shown as circles at distances r, 2r, and 3r around a source. Labels show per-area strength decreasing as 1, 1/4, and 1/9 because surface area grows like r squared.

What to notice: inverse-square comes from spreading over spherical area — double distance means 4× the area and 1/4 the per-area strength. (Credit: Illustration: A. Rosen (SVG))

Quick Check: Inverse-Square

The Moon is about 60 Earth radii from Earth’s center. The Moon experiences gravitational acceleration that is:

  • 60 times weaker
  • 360 times weaker
  • 3,600 times weaker
  • The same strength

Mass vs. Weight

A critical distinction

The Distinction

Quantity What it measures Changes with location?
Mass (\(m\)) Resistance to acceleration (inertia) No — same everywhere
Gravitational force (\(F_g\)) Force from gravity Yes — depends on local \(g\)
Apparent weight What you feel (scale reading) Yes — depends on gravity AND motion

Quick Check: Mass vs. Weight

An astronaut has mass 70 kg on Earth. On the Moon (about \(1/6\) of Earth’s \(g\)), their:

  • Mass decreases to about 12 kg
  • Weight is about 1/6, but mass stays 70 kg
  • Both mass and scale reading stay the same
  • Mass increases because there’s less gravity

Why Astronauts Float

Fixing the biggest misconception

The Wrong Answer

Misconception: “Astronauts float because there’s no gravity in space.”

At ISS altitude (~400 km), Earth’s gravity is still ~90% as strong as at the surface!

The Right Answer

Astronauts float because they’re in free fall.

The ISS and everyone inside are falling toward Earth together.

But moving sideways so fast they keep missing.

Everything falls together at the same rate, so nothing pushes back on you.

That means no sensation of weight.

Free Fall Feels Weightless

You feel weight when a surface pushes back on you.

In orbit, everything falls together, so there is no push.

Two panels: standing on Earth shows gravity down and a normal force up; in orbit, gravity still acts but there is no normal force because everything falls together.

What to notice: weight is the floor’s push (normal force) — in free fall there is gravity but no supporting push, so you feel weightless. (Credit: Illustration: A. Rosen (SVG))

Free fall = apparent weightlessness

Not because gravity is gone — because everything is falling together.

Quick Check: Weightlessness

An astronaut floats inside the ISS, 400 km above Earth. Earth’s gravitational pull on the astronaut is:

  • Zero — that’s why they float
  • About 90% of what it would be on Earth’s surface
  • Exactly the same as on Earth’s surface
  • Much stronger than on Earth’s surface

Part 3: Newton Explains Kepler

From patterns to physics

The Big Picture

Kepler’s Law Newton’s Explanation
Orbits are ellipses Inverse-square force implies conic sections
Equal areas in equal times Central force implies angular momentum conservation
\(P^2 \propto a^3\) Inverse-square gives this exact exponent

Kepler said “here’s what happens.”

Newton said “here’s why it must happen.”

Explaining Kepler I: Ellipses

Question: Why are orbits ellipses?

Newton’s Answer:

Any object moving under an inverse-square central force traces a conic section.

  • Not enough energy to escape: ellipse
  • Just enough energy to escape: parabola
  • More than escape energy: hyperbola

Orbits Are Conic Sections

Energy decides the shape:

  • Ellipse: bound
  • Parabola: just escapes
  • Hyperbola: unbound
Two-part diagram showing orbit curves around a planet and a cone section graphic labeling circle, ellipse, parabola, and hyperbola.
Credit: cococubed.com

Quick Check: First Law Explained

Newton explained that planetary orbits are ellipses because:

  • Planets were created in elliptical paths
  • Inverse-square gravity mathematically produces conic sections
  • Ellipses are the simplest possible curves
  • The Sun’s rotation shapes the orbits

Explaining Kepler II: Equal Areas

Question: Why do planets sweep equal areas in equal times?

Newton’s Answer:

Gravity is a central force — always pointing toward the Sun.

Central forces conserve angular momentum.

If \(L\) is constant and you get closer (\(r\) smaller), you must move faster (\(v\) larger).

Equal Areas = Variable Speed

In the same time interval:

  • Near perihelion: fast, short arc
  • Near aphelion: slow, long arc

Areas match because speed changes.

Elliptical orbit with two red swept areas at perihelion and aphelion labeled as equal for the same time interval.
Credit: cococubed.com

The Ice Skater (Again)

Arms in: spins faster

(smaller \(r\))

Arms out: spins slower

(larger \(r\))

Conservation of angular momentum.

Same physics for planets: closer is faster, farther is slower.

Quick Check: Second Law Explained

Newton explained Kepler’s Second Law (equal areas) as a consequence of:

  • The inverse-square nature of gravity
  • Conservation of angular momentum because gravity is a central force
  • The fact that planets have elliptical orbits
  • Energy conservation

Explaining Kepler III: \(P^2 \propto a^3\)

Question: Why this exact relationship?

Newton’s Answer:

For a force \(F \propto 1/r^n\), the period-distance relationship is:

\[P^2 \propto a^{n+1}\]

  • If \(n = 2\) (inverse-square): \(P^2 \propto a^3\) (matches Kepler)
  • If \(n = 1\): \(P^2 \propto a^2\) (does not match)
  • If \(n = 3\): \(P^2 \propto a^4\) (does not match)

Newton’s Improved Version

\[P^2 = \frac{4\pi^2}{G(M + m)} a^3\]

What’s new compared to Kepler:

  • The constant includes \(G\) and the total mass
  • Works for any gravitational system, not just our Solar System
  • We can solve for mass!

Motion Reveals Mass

Rearranging Newton’s version:

\[M \approx \frac{4\pi^2 a^3}{G P^2}\]

Measure orbital period and distance. Calculate central mass.

This is how we “weigh” the Sun, black holes, and galaxies.

We never touch them — we just watch how things move around them.

Quick Check: Weighing the Sun

How do astronomers determine the mass of the Sun?

  • By measuring how bright it is
  • By measuring Earth’s orbital period and distance
  • By sending a spacecraft to collect a sample
  • By measuring the Sun’s size

Quick Check: Different Stars

Two planets orbit at the same distance. Star A: \(2M_\odot\). Star B: \(0.5M_\odot\). Which planet has the shorter orbital period?

  • Planet A
  • Planet B
  • Both have the same period
  • Cannot tell without planet masses

Part 4: Synthesis

From empirical to physical

From Kepler to Newton

Kepler (Empirical) Newton (Physical)
Describes what planets do Explains why they do it
Patterns from data Mechanisms from principles
Limited to observed systems Universal — applies everywhere
Can predict within Solar System Can predict anywhere gravity acts

One Equation Rules All

\[F = \frac{Gm_1m_2}{r^2}\]

With this single equation, Newton explained:

  • Why apples fall
  • Why the Moon orbits Earth
  • Why planets orbit the Sun
  • Why all three of Kepler’s laws hold
  • How to weigh objects we’ll never touch

Key Takeaways (1/2)

  1. Newton’s Three Laws: (1) Inertia, (2) \(F = ma\), (3) Action-Reaction

  2. Circular motion = acceleration (direction changes), requiring centripetal force

  3. Universal Gravitation: \(F = GMm/r^2\) — inverse-square law

  4. Mass vs. Weight: Mass is intrinsic; weight depends on local gravity

Key Takeaways (2/2)

  1. Astronauts float because of free fall, not because gravity is absent.

  2. Newton explains Kepler:

    • Ellipses: inverse-square force implies conic sections
    • Equal areas: central force implies angular momentum conservation
    • \(P^2 \propto a^3\): inverse-square gives the exponent
  3. Motion reveals mass: \(M \approx 4\pi^2 a^3/(G P^2)\)

The Course Connection

Motion reveals mass — the foundation for nearly everything else:

  • Stars: Binary star orbits, stellar masses
  • Galaxies: Rotation curves, dark matter
  • Black holes: Orbiting stars, invisible mass
  • Exoplanets: Stellar wobbles, planet detection

Coming Up: Light as Information

Next lecture: Light is our only messenger from the cosmos.

We’ll learn to decode what light tells us:

  • How fast is it moving? (wavelength)
  • How hot is it? (spectrum)
  • What is it made of? (spectral lines)

Next Steps

Reading: Lecture 7 Reading Companion

Demo: Binary Orbits (motion reveals mass)

../../../demos/binary-orbits/

Questions?

Kepler gave us the patterns.

Newton gave us the physics.

Next: Light gives us the information.

Appendix: Optional Numericals

Use as backup or post-lecture reference.

Numerical Verification

Newton’s claim: the Moon is falling

The Moon IS Falling: Calculation

Newton’s claim: The same gravity that pulls apples pulls the Moon.

Test: Calculate the Moon’s centripetal acceleration and compare to surface gravity.

Given data:

  • Earth-Moon distance: \(r = 384,400\) km \(= 3.844 \times 10^8\) m
  • Moon’s orbital period: \(P = 27.3\) days
  • Earth’s radius: \(R_E = 6,371\) km
  • Surface gravity: \(g = 9.81\ \mathrm{m/s^2}\)

Step 1: Find the Moon’s Orbital Speed

The Moon travels a circular path of circumference \(2\pi r\) in time \(P\).

Convert period to seconds:

\[P = 27.3 \text{ days} \times \frac{24 \text{ hr}}{1 \text{ day}} \times \frac{3600 \text{ s}}{1 \text{ hr}} = 2.36 \times 10^6 \text{ s}\]

Calculate orbital speed:

\[v = \frac{2\pi r}{P} = \frac{2\pi \times 3.844 \times 10^8 \text{ m}}{2.36 \times 10^6 \text{ s}}\]

\[v = \frac{2.415 \times 10^9 \text{ m}}{2.36 \times 10^6 \text{ s}} = 1,023 \text{ m/s} \approx 1.0 \text{ km/s}\]

Step 2: Calculate Centripetal Acceleration

\[a_c = \frac{v^2}{r} = \frac{(1,023 \text{ m/s})^2}{3.844 \times 10^8 \text{ m}}\]

\[a_c = \frac{1.047 \times 10^6 \text{ m}^2/\text{s}^2}{3.844 \times 10^8 \text{ m}} = 2.72 \times 10^{-3} \text{ m/s}^2\]

Unit check: \(\frac{\text{m}^2/\text{s}^2}{\text{m}} = \frac{\text{m}}{\text{s}^2}\) (acceleration)

The Moon’s acceleration toward Earth is \(a_c = 0.00272\ \mathrm{m/s^2}\).

Compare to surface gravity: \(g = 9.81\ \mathrm{m/s^2}\).

Step 3: Test the Inverse-Square Law

If gravity follows \(1/r^2\), then at the Moon’s distance:

\[\frac{a_{\text{Moon}}}{g_{\text{surface}}} = \frac{1}{(\text{distance ratio})^2}\]

Calculate distance ratio:

\[\frac{r_{\text{Moon}}}{R_E} = \frac{3.844 \times 10^8 \text{ m}}{6.371 \times 10^6 \text{ m}} = 60.3\]

The Moon is 60.3 Earth radii away.

Predicted acceleration ratio:

\[\frac{a_{\text{Moon}}}{g} = \frac{1}{(60.3)^2} = \frac{1}{3636} = 2.75 \times 10^{-4}\]

Step 4: Compare Prediction to Measurement

Predicted (from inverse-square):

\[a_{\text{predicted}} = \frac{g}{3636} = \frac{9.81}{3636} = 2.70 \times 10^{-3} \text{ m/s}^2\]

Measured (from orbital motion):

\[a_{\text{measured}} = 2.72 \times 10^{-3} \text{ m/s}^2\]

Match! Difference < 1%

The same gravity that pulls apples pulls the Moon.

This was Newton’s triumph: unifying terrestrial and celestial physics.

Verifying ISS “Weightlessness”

Claim: At ISS altitude (400 km), gravity is still ~90% of surface value.

Calculate:

\[r_{\text{ISS}} = R_E + h = 6,371 + 400 = 6,771 \text{ km}\]

\[\frac{g_{\text{ISS}}}{g_{\text{surface}}} = \left(\frac{R_E}{r_{\text{ISS}}}\right)^2 = \left(\frac{6,371}{6,771}\right)^2\]

\[= (0.941)^2 = 0.885 = 88.5\%\]

Gravity at ISS altitude is 88.5% of surface gravity!

Astronauts float because they’re falling, not because gravity is gone.

Weighing the Sun: Full Calculation

Given:

  • Earth’s orbital period: \(P = 365.25\) days \(= 3.156 \times 10^7\) s
  • Earth’s orbital radius: \(a = 1.496 \times 10^{11}\) m (1 AU)
  • \(G = 6.674 \times 10^{-11}\ \mathrm{N\,m^2/kg^2}\)

From Newton’s form of Kepler III:

\[M_\odot = \frac{4\pi^2 a^3}{G P^2}\]

\[M_\odot = \frac{4\pi^2 (1.496 \times 10^{11})^3}{(6.674 \times 10^{-11})(3.156 \times 10^7)^2}\]

Weighing the Sun: Unit Analysis

\[M_\odot = \frac{4\pi^2 a^3}{G P^2}\]

Numerator units:

\[[\text{m}^3] \quad \text{(since } a^3 \text{ is in meters cubed)}\]

Denominator units:

\[\left[\frac{\text{N} \cdot \text{m}^2}{\text{kg}^2}\right] \times [\text{s}^2] = \left[\frac{\text{kg} \cdot \text{m/s}^2 \cdot \text{m}^2}{\text{kg}^2}\right] \times [\text{s}^2] = \frac{\text{m}^3}{\text{kg}}\]

Result units:

\[\frac{\text{m}^3}{\text{m}^3/\text{kg}} = \text{kg}\]

Weighing the Sun: Result

Calculating numerator:

\[4\pi^2 (1.496 \times 10^{11})^3 = 4\pi^2 \times 3.348 \times 10^{33} = 1.322 \times 10^{35} \text{ m}^3\]

Calculating denominator:

\[(6.674 \times 10^{-11})(3.156 \times 10^7)^2 = 6.674 \times 10^{-11} \times 9.96 \times 10^{14}\] \[= 6.65 \times 10^{4} \text{ m}^3/\text{kg}\]

Final result:

\[M_\odot = \frac{1.322 \times 10^{35}}{6.65 \times 10^{4}} = 1.99 \times 10^{30} \text{ kg}\]

The Sun’s mass is \(2 \times 10^{30}\) kg — determined just by watching Earth orbit!

Deeper Dive

Escape velocity and orbital energy

Escape Velocity

Question: How fast must you launch an object so it never falls back?

Energy conservation:

\[\frac{1}{2}mv^2 - \frac{GMm}{r} = 0\]

(Kinetic energy at launch = gravitational potential energy to escape)

Solving for escape velocity:

\[v_{\text{escape}} = \sqrt{\frac{2GM}{r}}\]

Escape Velocity in One Picture

Add energy and the orbit stretches.

Add enough and the path becomes unbound.

Earth with a rocket in low orbit, a higher elliptical orbit after a burn, and an open escape path after a stronger burn.
Credit: cococubed.com

Earth’s Escape Velocity: Calculation

\[v_{\text{escape}} = \sqrt{\frac{2GM_E}{R_E}}\]

Given:

  • \(G = 6.674 \times 10^{-11}\ \mathrm{N\,m^2/kg^2}\)
  • \(M_E = 5.97 \times 10^{24}\) kg
  • \(R_E = 6.371 \times 10^6\) m

\[v_{\text{escape}} = \sqrt{\frac{2 \times 6.674 \times 10^{-11} \times 5.97 \times 10^{24}}{6.371 \times 10^6}}\]

\[= \sqrt{\frac{7.97 \times 10^{14}}{6.371 \times 10^6}} = \sqrt{1.25 \times 10^8} \text{ m}^2/\text{s}^2\]

\[v_{\text{escape}} = 11,200 \text{ m/s} = \boxed{11.2 \text{ km/s}}\]

Escape Velocities Across the Solar System

Object Mass (Earth = 1) Radius (Earth = 1) \(v_{\text{escape}}\)
Moon 0.012 0.27 2.4 km/s
Earth 1 1 11.2 km/s
Jupiter 318 11.2 59.5 km/s
Sun 333,000 109 618 km/s

Circular Orbital Velocity

For a circular orbit, set gravitational force = centripetal force:

\[\frac{GMm}{r^2} = \frac{mv^2}{r}\]

Solving for orbital velocity:

\[v_{\text{circular}} = \sqrt{\frac{GM}{r}}\]

Key relationship:

\[v_{\text{escape}} = \sqrt{2} \times v_{\text{circular}}\]

To escape, you need only 41% more speed than circular orbit speed!