Classical-Mechanics Β· Unit 23 Β· Video 3 Β· Interactive Practice

What Changes Angular Momentum: Torque, Conservation, and a Meteor Grazing Earth

IKey Formulas

FormulaNameWhat it needs
τ⃗S=r⃗S×F⃗=dL⃗Sdt\vec{\boldsymbol{\tau}}_S = \vec{\mathbf{r}}_S \times \vec{\mathbf{F}} = \dfrac{d\vec{\mathbf{L}}_S}{dt} Torque law (one particle) Differentiate L⃗S=r⃗S×p⃗\vec{\mathbf{L}}_S = \vec{\mathbf{r}}_S \times \vec{\mathbf{p}} about a fixed point SS: the term v⃗×mv⃗=0⃗\vec{\mathbf{v}} \times m\vec{\mathbf{v}} = \vec{\mathbf{0}} drops out and dp⃗dt=F⃗\frac{d\vec{\mathbf{p}}}{dt} = \vec{\mathbf{F}}, the net force
Ο„βƒ—S=0βƒ—β€…β€Šβ‡’β€…β€ŠLβƒ—S,f=Lβƒ—S,i\vec{\boldsymbol{\tau}}_S = \vec{\mathbf{0}} \;\Rightarrow\; \vec{\mathbf{L}}_{S,f} = \vec{\mathbf{L}}_{S,i} Conservation of angular momentum A fixed point SS about which the total torque vanishes; about another point the torque generally does not
Jβƒ—S=∫titfΟ„βƒ—S dt=Ξ”Lβƒ—S\vec{\mathbf{J}}_S = \displaystyle\int_{t_i}^{t_f} \vec{\boldsymbol{\tau}}_S\,dt = \Delta\vec{\mathbf{L}}_S Angular impulse The torque about SS over the interval; the rotational twin of ∫F⃗ dt=Ξ”pβƒ—\int \vec{\mathbf{F}}\,dt = \Delta\vec{\mathbf{p}}
mvih=mvpRE,h=RE2+2GMEREvi2m v_i h = m v_p R_E, \quad h = \sqrt{R_E^2 + \dfrac{2GM_E R_E}{v_i^2}} Meteor grazing Earth (Example 19.4) Angular momentum about Earth's centre plus mechanical energy 12mvi2=12mvp2βˆ’GmMERE\tfrac{1}{2}mv_i^2 = \tfrac{1}{2}mv_p^2 - \tfrac{GmM_E}{R_E}; hh is the impact parameter

Key Insight: Gravity on the meteor always points at Earth's centre, so its moment arm about that one point is zero. The meteor's speed and direction both change, yet Lβƒ—S\vec{\mathbf{L}}_S about Earth's centre does not β€” and that single fixed number, βˆ’hmvi k^-h m v_i\,\hat{\mathbf{k}}, ties the far-away approach to the moment of closest approach.

IIVisualization 1 β€” Choosing the Point

The same gravitational force exerts zero torque about Earth's centre and a nonzero torque about almost any other point.

IIIVisualization 2 β€” How Far to the Side Can the Line Be?

For a given speed far away, which impact parameter hh makes the meteor just graze the surface?

IVVisualization 3 β€” Angular Impulse Is the Area Under the Torque

Each second of torque adds Ο„z Δt\tau_z\,\Delta t to LzL_z, so the net change is the signed area under Ο„z(t)\tau_z(t).

VQuiz Questions

Problem 1 Β· Torque from Angular Momentum

Given: about a fixed point SS, a particle's angular momentum is Lβƒ—S(t)=(3t2+2) k^Β kgβ‹…m2/s\vec{\mathbf{L}}_S(t) = (3t^2 + 2)\,\hat{\mathbf{k}}\ \text{kg}\cdot\text{m}^2/\text{s} with tt in seconds β€” find the zz-component of the total torque about SS at t=2Β st = 2\ \text{s}.

βœ… Correct! The torque is the rate of change: Ο„S,z=dLS,zdt=6t=12Β Nβ‹…m\tau_{S,z} = \frac{dL_{S,z}}{dt} = 6t = 12\ \text{N}\cdot\text{m} at t=2Β st = 2\ \text{s}.
❌ That is LS,z(2)L_{S,z}(2) itself. 3(2)2+2=143(2)^2 + 2 = 14 is the angular momentum at that instant; the torque law asks for its time derivative.
❌ Evaluate the derivative at t=2 st = 2\ \text{s}. ddt(3t2+2)=6t\frac{d}{dt}(3t^2 + 2) = 6t, not the constant 66.
❌ Check the power rule. ddt(3t2)=6t\frac{d}{dt}(3t^2) = 6t, which is 1212 at t=2t = 2; 2424 is 6t26t^2.
❌ Not quite. Use Ο„βƒ—S=dLβƒ—S/dt\vec{\boldsymbol{\tau}}_S = d\vec{\mathbf{L}}_S/dt and differentiate 3t2+23t^2 + 2.
Show solution

The torque law about a fixed point SS is τ⃗S=dL⃗Sdt\vec{\boldsymbol{\tau}}_S = \dfrac{d\vec{\mathbf{L}}_S}{dt}, so componentwise

Ο„S,z=ddt(3t2+2)=6t.\tau_{S,z} = \frac{d}{dt}\left(3t^2 + 2\right) = 6t.

At t=2Β st = 2\ \text{s}: Ο„S,z=6(2)=12Β Nβ‹…m\tau_{S,z} = 6(2) = 12\ \text{N}\cdot\text{m}. The constant 22 is the angular momentum at t=0t = 0 and contributes nothing to the rate of change.

Problem 2 Β· Which Quantity Stays Fixed?

Given: a satellite moves on an elliptical orbit around Earth; Earth is fixed, sits at one focus of the ellipse, and exerts the only force β€” which quantity is constant along the orbit?

βœ… Correct! Gravity points along βˆ’r^-\hat{\mathbf{r}} from Earth's centre, so rβƒ—SΓ—Fβƒ—=0βƒ—\vec{\mathbf{r}}_S \times \vec{\mathbf{F}} = \vec{\mathbf{0}} about that point and Lβƒ—S\vec{\mathbf{L}}_S is constant β€” exactly the meteor's argument.
❌ The speed changes. Constant LS=r mvβŠ₯L_S = r\,m v_\perp means the satellite moves faster where rr is small; energy conservation says the same thing, since U=βˆ’GmME/rU = -GmM_E/r varies along the orbit.
❌ Wrong point. The force's line of action passes through the focus where Earth sits, not through the centre of the ellipse, so everywhere except at the two ends of the major axis gravity has a nonzero moment arm about the centre and exerts a torque there.
❌ There is a net force. Fβƒ—=dpβƒ—/dtβ‰ 0βƒ—\vec{\mathbf{F}} = d\vec{\mathbf{p}}/dt \neq \vec{\mathbf{0}}, so pβƒ—\vec{\mathbf{p}} keeps changing direction (and size).
❌ Not quite. Look for the fixed point about which the torque is zero.
Show solution

Take SS at Earth's centre. The only force is Fβƒ—=βˆ’GmMEr2 r^\vec{\mathbf{F}} = -\dfrac{GmM_E}{r^2}\,\hat{\mathbf{r}} and the position vector is rβƒ—S=r r^\vec{\mathbf{r}}_S = r\,\hat{\mathbf{r}}, so they are anti-parallel:

Ο„βƒ—S=r r^Γ—(βˆ’GmMEr2 r^)=0βƒ—β€…β€Šβ‡’β€…β€ŠLβƒ—S=constant.\vec{\boldsymbol{\tau}}_S = r\,\hat{\mathbf{r}} \times \left(-\frac{GmM_E}{r^2}\,\hat{\mathbf{r}}\right) = \vec{\mathbf{0}} \;\Rightarrow\; \vec{\mathbf{L}}_S = \text{constant}.

About the centre of the ellipse the line of action generally misses the point, so the torque there is not zero. Linear momentum changes because the net force is not zero, and the speed changes because the potential energy does.

Problem 3 Β· The Grazing Meteor in Numbers

Given: a meteor approaches from very far away with vi=8.0Β km/sv_i = 8.0\ \text{km/s}; RE=6.37Γ—106Β mR_E = 6.37 \times 10^{6}\ \text{m} and GME=3.99Γ—1014Β m3/s2GM_E = 3.99 \times 10^{14}\ \text{m}^3/\text{s}^2 β€” find the impact parameter hh for which it just grazes Earth, and its speed vpv_p at the grazing point.

What is h?

What is v_p?

βœ… Correct! hβ‰ˆ1.72 REh \approx 1.72\,R_E: a line aimed well outside Earth's disc still hits, and the meteor arrives at 13.8Β km/s13.8\ \text{km/s} with the same angular momentum it started with.
❌ Missing the factor 2. Multiplying the energy equation by 2 gives vi2=vp2βˆ’2GMEREv_i^2 = v_p^2 - \frac{2GM_E}{R_E}, so the extra term is 2GMEREvi2\frac{2GM_E R_E}{v_i^2}, not GMEREvi2\frac{GM_E R_E}{v_i^2}.
❌ That ignores gravity. h=REh = R_E is the answer for a straight line; gravity bends the path inward, so the grazing line lies farther out.
❌ The terms add under the square root. h2=RE2+2GMEREvi2h^2 = R_E^2 + \frac{2GM_E R_E}{v_i^2}; you added RER_E to 2GMEvi2\frac{2GM_E}{v_i^2} instead.
❌ Check h. Solve h2=RE2+2GMERE/vi2h^2 = R_E^2 + 2GM_ER_E/v_i^2 with viv_i in m/s.
❌ Ratio upside down. mvih=mvpREm v_i h = m v_p R_E gives vp=vih/REv_p = v_i h / R_E, and h>REh > R_E makes vpv_p larger than viv_i.
❌ Constant angular momentum is not constant speed. The moment arm shrinks from hh to RER_E, so vp=vih/REv_p = v_i h/R_E must grow.
❌ That is the escape speed 2GME/RE\sqrt{2GM_E/R_E}. Energy gives vp2=vi2+2GMEREv_p^2 = v_i^2 + \frac{2GM_E}{R_E} β€” the meteor also keeps its initial vi2v_i^2.
❌ Check v_p. Use vp=vih/REv_p = v_i h / R_E from angular momentum.
Show solution

Angular momentum about Earth's centre (zero torque there): mvih=mvpREm v_i h = m v_p R_E, so vp=vih/REv_p = v_i h/R_E.

Energy (potential energy β†’0\to 0 far away): 12mvi2=12mvp2βˆ’GmMERE\tfrac{1}{2}m v_i^2 = \tfrac{1}{2}m v_p^2 - \dfrac{GmM_E}{R_E}. Substituting vpv_p, cancelling mm and multiplying by 2:

h2=RE2+2GMEREvi2=(6.37Γ—106)2+2(3.99Γ—1014)(6.37Γ—106)(8.0Γ—103)2h^2 = R_E^2 + \frac{2GM_E R_E}{v_i^2} = (6.37\times10^{6})^2 + \frac{2(3.99\times10^{14})(6.37\times10^{6})}{(8.0\times10^{3})^2} h2β‰ˆ4.06Γ—1013+7.94Γ—1013=1.20Γ—1014Β m2β€…β€Šβ‡’β€…β€Šhβ‰ˆ1.10Γ—107Β mβ‰ˆ1.72 RE.h^2 \approx 4.06\times10^{13} + 7.94\times10^{13} = 1.20\times10^{14}\ \text{m}^2 \;\Rightarrow\; h \approx 1.10\times10^{7}\ \text{m} \approx 1.72\,R_E.

Then vp=vi hREβ‰ˆ(8.0Β km/s)(1.72)β‰ˆ13.8Β km/sv_p = v_i\,\dfrac{h}{R_E} \approx (8.0\ \text{km/s})(1.72) \approx 13.8\ \text{km/s}.

Check with energy alone: vp2=vi2+2GMEREβ‰ˆ64.0+125.3=189.3Β km2/s2v_p^2 = v_i^2 + \dfrac{2GM_E}{R_E} \approx 64.0 + 125.3 = 189.3\ \text{km}^2/\text{s}^2, so vpβ‰ˆ13.8Β km/sv_p \approx 13.8\ \text{km/s} βœ“

Problem 4 Β· Angular Impulse from a Changing Torque

Given: a particle has LS,z=5Β kgβ‹…m2/sL_{S,z} = 5\ \text{kg}\cdot\text{m}^2/\text{s} about a fixed point SS at t=0t = 0; from t=0t = 0 to t=3Β st = 3\ \text{s} the total torque about SS is Ο„S,z(t)=(4βˆ’2t)Β Nβ‹…m\tau_{S,z}(t) = (4 - 2t)\ \text{N}\cdot\text{m} β€” find LS,zL_{S,z} at t=3Β st = 3\ \text{s}.

βœ… Correct! JS,z=∫03(4βˆ’2t) dt=3Β Nβ‹…mβ‹…sJ_{S,z} = \int_0^3 (4 - 2t)\,dt = 3\ \text{N}\cdot\text{m}\cdot\text{s}, so LS,zL_{S,z} rises from 55 to 88.
❌ The torque is not constant. Ο„S,z(3)β‹…3=βˆ’6\tau_{S,z}(3)\cdot 3 = -6 uses the final torque for the whole interval; integrate instead.
❌ The torque is not constant. Ο„S,z(0)β‹…3=12\tau_{S,z}(0)\cdot 3 = 12 uses the initial torque for the whole interval; the torque falls to zero at t=2Β st = 2\ \text{s} and then turns negative.
❌ That is Ξ”LS,z\Delta L_{S,z}, not LS,zL_{S,z}. The angular impulse is the change; add it to the initial 5Β kgβ‹…m2/s5\ \text{kg}\cdot\text{m}^2/\text{s}.
❌ Not quite. Integrate the torque over the interval and add the result to LS,z(0)L_{S,z}(0).
Show solution

The angular impulse about SS equals the change in angular momentum about SS:

JS,z=∫03(4βˆ’2t) dt=[4tβˆ’t2]03=12βˆ’9=3Β Nβ‹…mβ‹…s.J_{S,z} = \int_0^{3} (4 - 2t)\,dt = \Big[4t - t^2\Big]_0^{3} = 12 - 9 = 3\ \text{N}\cdot\text{m}\cdot\text{s}. LS,z(3)=LS,z(0)+JS,z=5+3=8Β kgβ‹…m2/s.L_{S,z}(3) = L_{S,z}(0) + J_{S,z} = 5 + 3 = 8\ \text{kg}\cdot\text{m}^2/\text{s}.

Geometrically: the positive area from 00 to 2Β s2\ \text{s} is 44, the negative area from 22 to 3Β s3\ \text{s} is βˆ’1-1, net +3+3.

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