Classical-Mechanics · Unit 12 · Video 3 · Interactive Practice

Where a System Really Balances: Center of Mass from Two Particles to a Rod

IKey Formulas

FormulaNameWhat it takes
Rcm=m1r1+m2r2m1+m2\vec{R}_{\text{cm}} = \dfrac{m_1\vec{r}_1 + m_2\vec{r}_2}{m_1 + m_2}Two particlesBoth masses and both positions
Rcm=1msysi=1Nmiri\vec{R}_{\text{cm}} = \dfrac{1}{m_{\text{sys}}}\displaystyle\sum_{i=1}^{N} m_i\vec{r}_iNN particlesmsys=imim_{\text{sys}} = \sum_i m_i; holds component by component
Rcm=bodyrdmbodydm\vec{R}_{\text{cm}} = \dfrac{\int_{\text{body}} \vec{r}\,'\,dm}{\int_{\text{body}} dm}Continuous bodyThe denominator is just MM
dm=λ(x)dxdm = \lambda(x')\,dx'Linear mass densityTrades 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 dmdm for λ(x)dx\lambda(x')\,dx' before the integral can be evaluated.

IITwo Particles, One Weighted Average

Each position is weighted by its own mass, so the balance point drifts toward the heavier particle.

IIIThe Earth–Moon Balance Point

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 1.41.4 times heavier: setting mmrem/(me+mm)=REm_m r_{em}/(m_e + m_m) = R_E gives mm=meRE/(remRE)=1.01×1023 kgm_m = m_e R_E/(r_{em} - R_E) = 1.01 \times 10^{23}\ \text{kg}.

IVFrom a Density Law to the Balance Point

Piling mass toward one end drags the balance point with it; only the density inside the integral changes.

VQuiz Questions

Problem 1 · Two Masses on a Line

Given: m1=3.0 kgm_1 = 3.0\ \text{kg} at x1=2.0 mx_1 = 2.0\ \text{m} and m2=5.0 kgm_2 = 5.0\ \text{kg} at x2=10.0 mx_2 = 10.0\ \text{m} on the xx-axis — find xcmx_{\text{cm}}.

✅ Correct! The heavier particle claims 5/85/8 of the weight, so the balance point sits 5.05.0 m from m1m_1 and only 3.03.0 m from m2m_2.
❌ That is the geometric midpoint. (x1+x2)/2(x_1 + x_2)/2 is the center of mass only when m1=m2m_1 = m_2; here m2m_2 is heavier, so the point must slide toward it.
❌ The weights are attached to the wrong particles. You computed (m2x1+m1x2)/(m1+m2)(m_2x_1 + m_1x_2)/(m_1+m_2) — each position must be multiplied by its own mass.
❌ You stopped at the numerator. 56 kgm56\ \text{kg}\cdot\text{m} is the mass-weighted sum; dividing by the total mass 8.08.0 kg is what turns it back into a position.
❌ Not quite. Use xcm=(m1x1+m2x2)/(m1+m2)x_{\text{cm}} = (m_1x_1 + m_2x_2)/(m_1+m_2) with numerator 3.0(2.0)+5.0(10.0)=563.0(2.0) + 5.0(10.0) = 56.
Show solution

Both particles lie on one axis, so the vector definition reduces to its xx-component:

xcm=m1x1+m2x2m1+m2=(3.0)(2.0)+(5.0)(10.0)3.0+5.0=6.0+50.08.0=568.0=7.0 mx_{\text{cm}} = \frac{m_1x_1 + m_2x_2}{m_1 + m_2} = \frac{(3.0)(2.0) + (5.0)(10.0)}{3.0 + 5.0} = \frac{6.0 + 50.0}{8.0} = \frac{56}{8.0} = 7.0\ \text{m}

Check the two limits. Equal masses would give the midpoint 6.06.0 m; letting m10m_1 \to 0 would give 10.010.0 m. The answer 7.07.0 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 me=5.98×1024 kgm_e = 5.98 \times 10^{24}\ \text{kg}, mm=7.34×1022 kgm_m = 7.34 \times 10^{22}\ \text{kg} and rem=3.84×108 mr_{em} = 3.84 \times 10^{8}\ \text{m}. With the origin at the Earth's center the answer was 4.66×106 m4.66 \times 10^{6}\ \text{m}. Now put the origin at the Moon's center, with ı^\hat{\imath} pointing toward the Earth — find RcmR_{\text{cm}} in this frame.

✅ Correct! The same physical point, described from a new origin: 4.66×106+3.79×108=3.84×108 m=rem4.66 \times 10^{6} + 3.79 \times 10^{8} = 3.84 \times 10^{8}\ \text{m} = r_{em}.
❌ The point does not move, but its coordinate does. 4.66×106 m4.66 \times 10^{6}\ \text{m} is its distance from the Earth's center; from the Moon it is almost the whole separation away.
❌ That is the midpoint rem/2r_{em}/2. The midpoint would be the answer only for two equal masses; here the Earth outweighs the Moon by more than 8080 times.
❌ Check the direction. The center of mass lies between the two bodies, so the two distances must add to remr_{em}, not overshoot it.
❌ Not quite. With the origin on the Moon, the Moon's term dies instead: Rcm=merem/(me+mm)R_{\text{cm}} = m_e r_{em}/(m_e + m_m).
Show solution

The origin is ours to choose, and the choice kills whichever term sits at the origin. Placing it on the Moon makes rm=0\vec{r}_m = \vec{0}, so

Rcm=mere+mmrmme+mm=meremme+mmı^\vec{R}_{\text{cm}} = \frac{m_e\vec{r}_e + m_m\vec{r}_m}{m_e + m_m} = \frac{m_e r_{em}}{m_e + m_m}\,\hat{\imath} =(5.98×1024)(3.84×108)6.05×1024=2.30×10336.05×1024=3.79×108 m= \frac{(5.98 \times 10^{24})(3.84 \times 10^{8})}{6.05 \times 10^{24}} = \frac{2.30 \times 10^{33}}{6.05 \times 10^{24}} = 3.79 \times 10^{8}\ \text{m}

Consistency check: 3.79×108+4.66×106=3.84×108 m3.79 \times 10^{8} + 4.66 \times 10^{6} = 3.84 \times 10^{8}\ \text{m}, 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 LL and total mass MM lying from x=0x' = 0 to x=Lx' = L, with linear mass density λ(x)=λ0x/L\lambda(x') = \lambda_0 x'/Lfind the constant λ0\lambda_0 and the center of mass.

What is λ0\lambda_0?

Where is RcmR_{\text{cm}}?

✅ Correct! A linear density piles less mass to the right than a quadratic one, so the balance point stops at 2L/32L/3, short of the 3L/43L/4 of the video's rod.
❌ That is the uniform rod's density. M/LM/L is the average density; λ0\lambda_0 here is the peak value at x=Lx' = L, and it must be larger than the average.
❌ That is the λx2\lambda \propto x'^2 answer. 0Lx2dx=L3/3\int_0^L x'^2\,dx' = L^3/3 gives λ0=3M/L\lambda_0 = 3M/L; for λx\lambda \propto x' the integral is L2/2L^2/2 instead.
❌ Not quite. Fix λ0\lambda_0 by demanding that the density integrate to the total mass: 0Lλ0x/Ldx=M\int_0^L \lambda_0 x'/L\,dx' = M.
❌ That is the uniform rod. The mass here is not spread evenly, so the balance point cannot stay at the midpoint.
❌ Right number, wrong end. L/3L/3 is the distance from the heavy end; measured from x=0x' = 0 as asked, the center of mass is at LL/3=2L/3L - L/3 = 2L/3.
❌ That belongs to the quadratic rod. 3L/43L/4 comes from λx2\lambda \propto x'^2; a gentler linear pile-up cannot drag the balance point that far.
❌ Not quite. Evaluate Rcm=1M0Lxλ(x)dxR_{\text{cm}} = \frac{1}{M}\int_0^L x'\lambda(x')\,dx', where the integrand is proportional to x2x'^2.
Show solution

Step 1 — fix λ0\lambda_0 from the total mass.

M=bodydm=0Lλ0xLdx=λ0LL22=λ0L2λ0=2MLM = \int_{\text{body}} dm = \int_0^L \frac{\lambda_0 x'}{L}\,dx' = \frac{\lambda_0}{L}\cdot\frac{L^2}{2} = \frac{\lambda_0 L}{2} \quad\Longrightarrow\quad \lambda_0 = \frac{2M}{L}

The units check: mass over length, kilograms per meter.

Step 2 — integrate for the center of mass.

Rcm=1M0Lxλ0xLdx=λ0ML0Lx2dx=λ0MLL33R_{\text{cm}} = \frac{1}{M}\int_0^L x'\,\frac{\lambda_0 x'}{L}\,dx' = \frac{\lambda_0}{ML}\int_0^L x'^2\,dx' = \frac{\lambda_0}{ML}\cdot\frac{L^3}{3} =1ML2MLL33=2L3= \frac{1}{ML}\cdot\frac{2M}{L}\cdot\frac{L^3}{3} = \frac{2L}{3}

Sanity check. For λxn\lambda \propto x'^n the same two integrals give Rcm=n+1n+2LR_{\text{cm}} = \frac{n+1}{n+2}L: the uniform rod (n=0n = 0) balances at L/2L/2, this rod (n=1n = 1) at 2L/32L/3, and the video's rod (n=2n = 2) at 3L/43L/4. Steeper density, later balance point.

Problem 4 · A Rod Plus a Bead

Given: a uniform rod of mass MM and length LL lying from x=0x = 0 to x=Lx = L, with a point particle of mass MM glued to its right end at x=Lx = Lfind the center of mass of the combined system.

✅ Correct! And it is the same 3L/43L/4 as the rod with λx2\lambda \propto x'^2 — two very different bodies can share a balance point, because only the mass distribution decides.
❌ That is the bare rod. The glued particle carries as much mass as the entire rod, so it must pull the balance point to the right of L/2L/2.
❌ You placed the rod's mass at its far end. A body enters as its total mass sitting at its own center of mass — the rod acts as MM at L/2L/2, not at LL.
❌ Wrong total mass. Dividing by MM instead of 2M2M puts the answer at 3L/23L/2, off the end of the rod entirely — a weighted average can never leave the segment joining the parts.
❌ Not quite. Replace the rod by a single particle of mass MM at x=L/2x = L/2, then apply the two-particle definition.
Show solution

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 MM at x=L/2x = L/2.

Step 2 — two particles.

xcm=M(L2)+M(L)M+M=32ML2M=3L4x_{\text{cm}} = \frac{M\left(\frac{L}{2}\right) + M(L)}{M + M} = \frac{\frac{3}{2}ML}{2M} = \frac{3L}{4}

Step 3 — read the answer. The bead drags the balance point from L/2L/2 out to 3L/43L/4, exactly the distance the quadratic density λx2\lambda \propto x'^2 managed by smearing the extra mass along the rod instead of concentrating it at the end.

The general rule this uses: in imiri\sum_i m_i\vec{r}_i, 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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