Classical-Mechanics Β· Unit 24 Β· Video 4 Β· Interactive Practice

Orbit Plus Spin: Angular Momentum Splits at the Center of Mass, and the Earth Carries Four Million Times More in Its Orbit

IKey Formulas

FormulaNameWhat it says
Lβƒ—Stotal=Lβƒ—Sorbital+Lβƒ—cmspin\vec{\mathbf{L}}_S^{\text{total}} = \vec{\mathbf{L}}_S^{\text{orbital}} + \vec{\mathbf{L}}_{cm}^{\text{spin}}Orbit–spin splitHolds for any system of particles and any point SS
L⃗Sorbital=r⃗S,cm×p⃗sys\vec{\mathbf{L}}_S^{\text{orbital}} = \vec{\mathbf{r}}_{S,cm}\times\vec{\mathbf{p}}_{\text{sys}},  p⃗sys=mTV⃗cm\ \vec{\mathbf{p}}_{\text{sys}} = m_T\vec{\mathbf{V}}_{cm}Orbital angular momentumThe system as one particle of mass mTm_T at the center of mass; depends on SS
Lβƒ—cmspin=βˆ‘irβƒ—cm,iΓ—mivβƒ—cm,i=Icm ω⃗cm\vec{\mathbf{L}}_{cm}^{\text{spin}} = \sum_i \vec{\mathbf{r}}_{cm,i}\times m_i\vec{\mathbf{v}}_{cm,i} = I_{cm}\,\vec{\boldsymbol{\omega}}_{cm}Spin angular momentumMotion relative to the center of mass; no SS in it (second form: rigid body about a symmetry axis)
LSorbitalLcmspin=52 rs,e2Re2 TspinTorbitβ‰ˆ3.77Γ—106\dfrac{L_S^{\text{orbital}}}{L_{cm}^{\text{spin}}} = \dfrac{5}{2}\,\dfrac{r_{s,e}^2}{R_e^2}\,\dfrac{T_{\text{spin}}}{T_{\text{orbit}}} \approx 3.77\times10^{6}Earth: orbit vs spinUniform sphere, circular orbit; the squared distance ratio dominates

Key Insight: The two cross terms vanish because, measured from the center of mass, the mass-weighted positions and velocities both sum to zero: βˆ‘imirβƒ—cm,i=0βƒ—\sum_i m_i\vec{\mathbf{r}}_{cm,i} = \vec{\mathbf{0}} and βˆ‘imivβƒ—cm,i=0βƒ—\sum_i m_i\vec{\mathbf{v}}_{cm,i} = \vec{\mathbf{0}}.

IIVisualization 1 β€” Orbital Depends on S, Spin Does Not

For a spinning body sliding in a straight line, the particle-by-particle sum always equals orbital plus spin.

IIIVisualization 2 β€” Why the Orbit Wins by Millions

With the mass cancelled, the ratio is a product of three factors; on a log scale they add.

πŸ’‘ All three bodies are modelled as uniform spheres, Icm=25mR2I_{cm} = \tfrac{2}{5}mR^2; Jupiter is centrally condensed (Icmβ‰ˆ0.25 mR2I_{cm} \approx 0.25\,mR^2), so its true ratio is about 1.61.6 times larger.

IVVisualization 3 β€” Sidereal Day and Solar Day

Because the Earth also moves along its orbit, facing the Sun again takes longer than one turn against the stars.

VQuiz Questions

Problem 1 Β· Orbit Plus Spin for a Disk

Given: A uniform disk of mass 2 kg2\ \text{kg} and radius 0.5 m0.5\ \text{m} spins at 4 rad/s4\ \text{rad/s} about its symmetry axis (vertical, through its center). Its center moves at 3 m/s3\ \text{m/s} in a straight horizontal line that passes 2 m2\ \text{m} from a point SS in the same plane. Seen from above, both the spin and the motion of the center about SS are counterclockwise. Find the magnitude of L⃗Stotal\vec{\mathbf{L}}_S^{\text{total}}.

βœ… Correct! Orbital 1212 plus spin 11, both along the same vertical direction, gives 13Β kgΒ m2/s13\ \text{kg m}^2/\text{s}.
❌ Not quite. 1212 is only the orbital piece d mTVcmd\,m_T V_{cm}; the disk's rotation about its own center adds spin.
❌ Check the moment of inertia. A uniform disk about its symmetry axis has Icm=12MR2I_{cm} = \tfrac{1}{2}MR^2, not MR2MR^2.
❌ Check the directions. Both motions are counterclockwise seen from above, so both vectors point up and add.
❌ Not quite. Compute Lorbital=d mTVcmL^{\text{orbital}} = d\,m_T V_{cm} and Lspin=IcmΟ‰L^{\text{spin}} = I_{cm}\omega separately, then add.
Show solution

Orbital: the center moves on a straight line at perpendicular distance d=2Β md = 2\ \text{m} from SS, so

LSorbital=d mTVcm=(2)(2)(3)=12Β kgΒ m2/s.L_S^{\text{orbital}} = d\,m_T V_{cm} = (2)(2)(3) = 12\ \text{kg m}^2/\text{s}.

Spin: for a uniform disk about its symmetry axis,

Lcmspin=Icm ω=12(2)(0.5)2(4)=1Β kgΒ m2/s.L_{cm}^{\text{spin}} = I_{cm}\,\omega = \tfrac{1}{2}(2)(0.5)^2(4) = 1\ \text{kg m}^2/\text{s}.

Both are counterclockwise seen from above, so both point up:

LStotal=12+1=13Β kgΒ m2/s.L_S^{\text{total}} = 12 + 1 = 13\ \text{kg m}^2/\text{s}.

Problem 2 Β· A Straight Path Still Carries Orbital Angular Momentum

Given: A puck, a uniform disk of mass 3Β kg3\ \text{kg} and radius 0.10Β m0.10\ \text{m}, slides along the xx-axis with Vβƒ—cm=4 i^Β m/s\vec{\mathbf{V}}_{cm} = 4\,\hat{\mathbf{i}}\ \text{m/s} while spinning counterclockwise (seen from +z+z) at 20Β rad/s20\ \text{rad/s}. Find its angular momentum about S=(0,β€‰βˆ’1.5Β m)S = (0,\,-1.5\ \text{m}) and about Sβ€²=(5Β m, 0)S' = (5\ \text{m},\,0), which lies on its path.

Angular momentum about S

Angular momentum about Sβ€² (on the path)

βœ… Correct! The orbital piece βˆ’18 k^-18\,\hat{\mathbf{k}} depends on the point; the spin +0.3 k^+0.3\,\hat{\mathbf{k}} is the same about both.
❌ Check the direction of the orbital piece. rβƒ—S,cm\vec{\mathbf{r}}_{S,cm} points up (+j^+\hat{\mathbf{j}}) and pβƒ—sys\vec{\mathbf{p}}_{\text{sys}} points along +i^+\hat{\mathbf{i}}; j^Γ—i^=βˆ’k^\hat{\mathbf{j}}\times\hat{\mathbf{i}} = -\hat{\mathbf{k}}.
❌ Check the spin's direction. Counterclockwise seen from +z+z means the spin is along +k^+\hat{\mathbf{k}}, opposite to the orbital piece here.
❌ A straight path still has orbital angular momentum. About a point off the line, rβƒ—S,cmΓ—pβƒ—sysβ‰ 0βƒ—\vec{\mathbf{r}}_{S,cm}\times\vec{\mathbf{p}}_{\text{sys}} \neq \vec{\mathbf{0}}.
❌ Only the orbital piece vanishes. On the path rβƒ—Sβ€²,cm\vec{\mathbf{r}}_{S',cm} is parallel to pβƒ—sys\vec{\mathbf{p}}_{\text{sys}}, but the spin has no SS in it and is still there.
❌ The orbital piece depends on the point. Only zero total momentum makes Lβƒ—\vec{\mathbf{L}} the same about every point; here pβƒ—sysβ‰ 0βƒ—\vec{\mathbf{p}}_{\text{sys}} \neq \vec{\mathbf{0}}.
❌ Check the value about S. Add the orbital piece rβƒ—S,cmΓ—pβƒ—sys\vec{\mathbf{r}}_{S,cm}\times\vec{\mathbf{p}}_{\text{sys}} and the spin Icmω k^I_{cm}\omega\,\hat{\mathbf{k}}.
❌ Check the value about Sβ€². On the path, rβƒ—Sβ€²,cm\vec{\mathbf{r}}_{S',cm} is parallel to pβƒ—sys\vec{\mathbf{p}}_{\text{sys}}.
Show solution

Spin (the same about every point): Icm=12(3)(0.10)2=0.015Β kgΒ m2I_{cm} = \tfrac{1}{2}(3)(0.10)^2 = 0.015\ \text{kg m}^2, so

Lβƒ—cmspin=(0.015)(20) k^=0.3 k^Β kgΒ m2/s.\vec{\mathbf{L}}_{cm}^{\text{spin}} = (0.015)(20)\,\hat{\mathbf{k}} = 0.3\,\hat{\mathbf{k}}\ \text{kg m}^2/\text{s}.

Orbital about SS: with the puck at (x,0)(x, 0), rβƒ—S,cm=x i^+1.5 j^\vec{\mathbf{r}}_{S,cm} = x\,\hat{\mathbf{i}} + 1.5\,\hat{\mathbf{j}} and pβƒ—sys=12 i^Β kgΒ m/s\vec{\mathbf{p}}_{\text{sys}} = 12\,\hat{\mathbf{i}}\ \text{kg m/s}:

Lβƒ—Sorbital=(x i^+1.5 j^)Γ—12 i^=18 (j^Γ—i^)=βˆ’18 k^Β kgΒ m2/s,\vec{\mathbf{L}}_S^{\text{orbital}} = (x\,\hat{\mathbf{i}} + 1.5\,\hat{\mathbf{j}})\times 12\,\hat{\mathbf{i}} = 18\,(\hat{\mathbf{j}}\times\hat{\mathbf{i}}) = -18\,\hat{\mathbf{k}}\ \text{kg m}^2/\text{s},

the same at every xx. Total: Lβƒ—S=βˆ’18 k^+0.3 k^=βˆ’17.7 k^Β kgΒ m2/s\vec{\mathbf{L}}_S = -18\,\hat{\mathbf{k}} + 0.3\,\hat{\mathbf{k}} = -17.7\,\hat{\mathbf{k}}\ \text{kg m}^2/\text{s}.

About Sβ€²S': rβƒ—Sβ€²,cm=(xβˆ’5) i^\vec{\mathbf{r}}_{S',cm} = (x - 5)\,\hat{\mathbf{i}} is parallel to pβƒ—sys\vec{\mathbf{p}}_{\text{sys}}, so the orbital piece is zero and Lβƒ—Sβ€²=+0.3 k^Β kgΒ m2/s\vec{\mathbf{L}}_{S'} = +0.3\,\hat{\mathbf{k}}\ \text{kg m}^2/\text{s}.

Problem 3 Β· Orbit Versus Spin for Mars

Given: Mars orbits the Sun on a (nearly) circular orbit of radius 2.28Γ—1011Β m2.28\times10^{11}\ \text{m} with period 687Β d687\ \text{d}, has mean radius 3.39Γ—106Β m3.39\times10^{6}\ \text{m}, and spins once every 24Β hΒ 37Β min24\ \text{h}\ 37\ \text{min} relative to the stars. Model Mars as a uniform sphere. Find LSorbital/LcmspinL_S^{\text{orbital}}/L_{cm}^{\text{spin}} with SS at the Sun.

βœ… Correct! About 1717 million: Mars is farther out than the Earth and smaller, so its squared distance ratio is even larger.
❌ A factor is missing. The 25\tfrac{2}{5} in IcmI_{cm} sits in the denominator of the ratio, so it contributes 52\tfrac{5}{2}.
❌ The factor is upside down. 25\tfrac{2}{5} belongs to the spin, which is in the denominator, so the ratio carries 52\tfrac{5}{2}, not 25\tfrac{2}{5}.
❌ Square the distance ratio. Orbital goes as mr2Ο‰orbitm r^2\omega_{\text{orbit}} and spin as 25mR2Ο‰spin\tfrac{2}{5}mR^2\omega_{\text{spin}}, so the ratio has (r/R)2(r/R)^2.
❌ Not quite. Use LorbitalLspin=52 r2R2 TspinTorbit\dfrac{L^{\text{orbital}}}{L^{\text{spin}}} = \dfrac{5}{2}\,\dfrac{r^2}{R^2}\,\dfrac{T_{\text{spin}}}{T_{\text{orbit}}}.
Show solution

Divide Lorbital=mr2 2Ο€TorbitL^{\text{orbital}} = m r^2\,\dfrac{2\pi}{T_{\text{orbit}}} by Lspin=25mR2 2Ο€TspinL^{\text{spin}} = \tfrac{2}{5}mR^2\,\dfrac{2\pi}{T_{\text{spin}}}; the mass and 2Ο€2\pi cancel:

LSorbitalLcmspin=52 r2R2 TspinTorbit.\frac{L_S^{\text{orbital}}}{L_{cm}^{\text{spin}}} = \frac{5}{2}\,\frac{r^2}{R^2}\,\frac{T_{\text{spin}}}{T_{\text{orbit}}}.

Distance factor: r/R=2.28Γ—1011/3.39Γ—106=6.73Γ—104r/R = 2.28\times10^{11}/3.39\times10^{6} = 6.73\times10^{4}, squared 4.52Γ—1094.52\times10^{9}.

Period factor: Tspin=24Β hΒ 37Β min=88,620Β sT_{\text{spin}} = 24\ \text{h}\ 37\ \text{min} = 88{,}620\ \text{s} and Torbit=687Γ—86,400Β s=5.94Γ—107Β sT_{\text{orbit}} = 687 \times 86{,}400\ \text{s} = 5.94\times10^{7}\ \text{s}, so Tspin/Torbit=1.49Γ—10βˆ’3T_{\text{spin}}/T_{\text{orbit}} = 1.49\times10^{-3}.

LSorbitalLcmspin=2.5Γ—4.52Γ—109Γ—1.49Γ—10βˆ’3β‰ˆ1.69Γ—107.\frac{L_S^{\text{orbital}}}{L_{cm}^{\text{spin}}} = 2.5 \times 4.52\times10^{9} \times 1.49\times10^{-3} \approx 1.69\times10^{7}.

Problem 4 Β· The Solar Day on Venus

Given: Venus spins once relative to the stars every 243.0243.0 Earth days, but in the sense opposite to its orbital motion, and it orbits the Sun once every 224.7224.7 Earth days. Find the length of its solar day (Sun overhead to Sun overhead).

βœ… Correct! With the spin opposite to the orbit, the orbital motion brings the Sun round to meet the marker sooner, so the solar day is shorter than the sidereal one.
❌ Not quite. The solar day differs from both periods: the direction to the Sun turns at 2Ο€/Torbit2\pi/T_{\text{orbit}} while the planet turns at 2Ο€/Tsidereal2\pi/T_{\text{sidereal}} against the stars.
❌ That is the Earth's rule. Subtracting the rates applies when spin and orbit are in the same sense; for Venus they are opposite, so the rates add.
Show solution

Relative to the stars, the planet turns at Ο‰spin=2Ο€/Tsidereal\omega_{\text{spin}} = 2\pi/T_{\text{sidereal}}, while the direction from the planet to the Sun turns at Ο‰orbit=2Ο€/Torbit\omega_{\text{orbit}} = 2\pi/T_{\text{orbit}} in the orbital sense.

For the Earth the two are in the same sense, so a marker gains on the Sun at Ο‰spinβˆ’Ο‰orbit\omega_{\text{spin}} - \omega_{\text{orbit}} (that is the extra degree per day). For Venus they are opposite, so it gains at Ο‰spin+Ο‰orbit\omega_{\text{spin}} + \omega_{\text{orbit}}:

1Tsolar=1Tsidereal+1Torbit=1243.0Β d+1224.7Β d\frac{1}{T_{\text{solar}}} = \frac{1}{T_{\text{sidereal}}} + \frac{1}{T_{\text{orbit}}} = \frac{1}{243.0\ \text{d}} + \frac{1}{224.7\ \text{d}} Tsolar=(243.0)(224.7)243.0+224.7Β dβ‰ˆ116.7Β d.T_{\text{solar}} = \frac{(243.0)(224.7)}{243.0 + 224.7}\ \text{d} \approx 116.7\ \text{d}.

Using the Earth's rule, 1/Tsolar=1/Tsiderealβˆ’1/Torbit1/T_{\text{solar}} = 1/T_{\text{sidereal}} - 1/T_{\text{orbit}}, would give a negative rate with magnitude 1/2984Β dβˆ’11/2984\ \text{d}^{-1}, which is wrong here.

Solved: 0 / 4