Classical-Mechanics · Unit 12 · Video 3 · Interactive Practice
| Formula | Name | What it takes |
|---|---|---|
| Two particles | Both masses and both positions | |
| particles | ; holds component by component | |
| Continuous body | The denominator is just | |
| Linear mass density | Trades mass for a length element |
Key Insight: All three are the same mass-weighted average of position. The only hard part of the continuous case is that the integration variable is mass, not length — so you must trade for before the integral can be evaluated.
Each position is weighted by its own mass, so the balance point drifts toward the heavier particle.
The Moon pulls the balance point off the Earth's center — far enough to reach the surface?
💡 The balance point only breaks the surface if the Moon is about times heavier: setting gives .
Piling mass toward one end drags the balance point with it; only the density inside the integral changes.
Problem 1 · Two Masses on a Line
Given: at and at on the -axis — find .
Both particles lie on one axis, so the vector definition reduces to its -component:
Check the two limits. Equal masses would give the midpoint m; letting would give m. The answer m lies between the midpoint and the heavy particle, exactly where a weighted average belongs.
Problem 2 · Moving the Origin
Given: the Earth–Moon system with , and . With the origin at the Earth's center the answer was . Now put the origin at the Moon's center, with pointing toward the Earth — find in this frame.
The origin is ours to choose, and the choice kills whichever term sits at the origin. Placing it on the Moon makes , so
Consistency check: , the full separation. The balance point never moved — only the ruler did. Notice too that the Earth-based calculation is the easier one, because the small mass carries the surviving term.
Problem 3 · A Rod Whose Density Grows Linearly
Given: a thin rod of length and total mass lying from to , with linear mass density — find the constant and the center of mass.
What is ?
Where is ?
Step 1 — fix from the total mass.
The units check: mass over length, kilograms per meter.
Step 2 — integrate for the center of mass.
Sanity check. For the same two integrals give : the uniform rod () balances at , this rod () at , and the video's rod () at . Steeper density, later balance point.
Problem 4 · A Rod Plus a Bead
Given: a uniform rod of mass and length lying from to , with a point particle of mass glued to its right end at — find the center of mass of the combined system.
Step 1 — collapse the rod. The uniform rod's own integral was done in the video: it balances at its midpoint, so for this purpose it is a particle of mass at .
Step 2 — two particles.
Step 3 — read the answer. The bead drags the balance point from out to , exactly the distance the quadratic density managed by smearing the extra mass along the rod instead of concentrating it at the end.
The general rule this uses: in , each "particle" may be an entire extended body, entered as its total mass located at its own center of mass. That is what makes multi-part systems tractable without ever redoing the integral.
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