Reconcile orbital energy with angular momentum
Use two conserved quantities without mistaking an eccentric orbit for a circular one.
Learning outcome: Compare f=.5,1,1.25,1.5 at r0=4. Compute E and L independently, classify the orbit and test whether a finite second turning radius exists. Explain why changing K around a bound eccentric orbit does not imply energy loss. For the circular case, derive a period ratio for a changed radius without using a full numerical trajectory.
Starting recap
State the reference axis and system, distinguish time and angle integrals, and verify an accessible and supported motion branch.
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At r0=4 and f=1, v=sqrt(3), K=3 J, U=−6 J, E=−3 J and L=8sqrt(3) kg m²/s. At the same radius with f=.5, E=−5.25 J, L=4sqrt(3) and the other turning radius is 4/7 m in the ideal point-source model.
Open the experimentPredict
In an ideal eccentric bound orbit, which pair remains constant about the central source?
Experiment
Compare f=.5,1,1.25,1.5 at r0=4. Compute E and L independently, classify the orbit and test whether a finite second turning radius exists. Explain why changing K around a bound eccentric orbit does not imply energy loss. For the circular case, derive a period ratio for a changed radius without using a full numerical trajectory.
Compare satellite energy and angular-momentum constraints
Worked teaching model · synthetic values · Ideal dominant spherical central source GM=12 m³/s² and satellite mass 2 kg; initial radial speed zero,positive tangential speed. Point-source field assumed throughout,zero U at infinity. Bound/unbound classification and turning radius only, not a full timed trajectory or real launch.
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Effective radial potential
Axes rescale independently. Curves join sampled coordinates; a joining segment is not additional measured evidence. Read physical units rather than screen angles or apparent slopes.
Effective radial potential: numerical coordinates
| radius (m) | effective energy (J) |
|---|---|
| 0.4 | 240 |
| 0.79 | 46.531 |
| 1.18 | 14.1339 |
| 1.57 | 4.18678 |
| 1.96 | 0.249896 |
| 2.35 | -1.52105 |
| 2.74 | -2.3656 |
| 3.13 | -2.76822 |
| 3.52 | -2.94421 |
| 3.91 | -2.99841 |
| 4.3 | -2.9854 |
| 4.69 | -2.93507 |
| 5.08 | -2.86441 |
| 5.47 | -2.78334 |
| 5.86 | -2.69776 |
| 6.25 | -2.6112 |
| 6.64 | -2.52577 |
| 7.03 | -2.44269 |
| 7.42 | -2.36267 |
| 7.81 | -2.28605 |
| 8.2 | -2.21297 |
| 8.59 | -2.14344 |
| 8.98 | -2.07737 |
| 9.37 | -2.01465 |
| 9.76 | -1.95512 |
| 10.15 | -1.89861 |
| 10.54 | -1.84496 |
| 10.93 | -1.794 |
| 11.32 | -1.74556 |
| 11.71 | -1.69948 |
| 12.1 | -1.65562 |
| 12.49 | -1.61385 |
| 12.88 | -1.57401 |
| 13.27 | -1.53601 |
| 13.66 | -1.49971 |
| 14.05 | -1.46503 |
| 14.44 | -1.43185 |
| 14.83 | -1.40009 |
| 15.22 | -1.36966 |
| 15.61 | -1.34049 |
| 16 | -1.3125 |
| Quantity | Value | Unit |
|---|---|---|
| Initial tangential speed | 1.73205 | m/s |
| Initial gravitational potential | -6 | J |
| Initial kinetic energy | 3 | J |
| Total mechanical energy | -3 | J |
| Angular momentum magnitude | 13.8564 | kg m²/s |
| Bound orbit under point-source assumptions | 1 | flag |
| Circular period at selected radius | 14.5104 | s |
| Other radial turning point | 4 | m |
The supplied state is circular: K,U,E and angular momentum remain constant.
A central gravitational force exerts zero torque about the source. At turning points radial speed is zero; equating E to L²/(2mr²)−GMm/r gives the second radius for bound states. This optional exact turning-point calculation is not a full timed orbit. Any finite source surface or additional interaction can invalidate the point-source continuation.
Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.
The supplied state is circular: K,U,E and angular momentum remain constant.
A central gravitational force exerts zero torque about the source. At turning points radial speed is zero; equating E to L²/(2mr²)−GMm/r gives the second radius for bound states. This optional exact turning-point calculation is not a full timed orbit. Any finite source surface or additional interaction can invalidate the point-source continuation.
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Which conclusions survive if there is atmospheric drag, and which conservation assumptions fail?
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