Integrate magnetic motion and recover a Hall sign
For B along +z and signed omega = (q/m)B, the Lorentz equations are dvx/dt = omega vy, dvy/dt = −omega vx and dvz/dt = 0.
Learning outcome: Compare negative, neutral and positive q/m. Derive the position functions by integration and check their initial values. Retain the no-work dot product and distinguish transverse from three-dimensional motion. Independently derive the Hall polarity under one reversal and explain the one-carrier assumption.
Starting recap
Integrate magnetic sources, preserve cross-product direction and test the symmetry and calibration needed for a field inference.
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Try
At q/m = +1 C/kg and B = 2 T, omega = 2 rad/s, transverse radius is 1.5 m and period pi s. Initial acceleration is (0,−6,0) m/s². Reversing q/m reverses circulation while radius, period and speed stay unchanged.
Open the experimentPredict
In a pure uniform magnetic field, which quantity is constant for this isolated classical body?
Experiment
Compare negative, neutral and positive q/m. Derive the position functions by integration and check their initial values. Retain the no-work dot product and distinguish transverse from three-dimensional motion. Independently derive the Hall polarity under one reversal and explain the one-carrier assumption.
Integrate magnetic deflection without inventing work
Worked teaching model · synthetic values · Hypothetical classical body starts at origin with velocity (3,0,2) m/s in constant B along z. No electric field, radiation or material collision. Zero charge-to-mass setting is the neutral straight-path limit; no species identification claimed.
Reset keeps your prediction, captures and practice history.
Equal-scale transverse trajectory
The same metres-per-pixel scale is used on x and y. The particle starts at the origin moving toward positive x; the solid dot marks one eighth of the displayed time interval. Its z coordinate increases as 2t and is not plotted here. The transverse circle is the projection of a helix, not a loss of kinetic energy.
Axis half-span: 3 m over 140 pixels. Displayed duration: 3.1416 s. One-eighth-time position: (1.0607, -0.43934) m.
Transverse x coordinate
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.
Transverse x coordinate: numerical coordinates
| time (s) | x (m) |
|---|---|
| 0 | 0 |
| 0.0523599 | 0.156793 |
| 0.10472 | 0.311868 |
| 0.15708 | 0.463525 |
| 0.20944 | 0.610105 |
| 0.261799 | 0.75 |
| 0.314159 | 0.881678 |
| 0.366519 | 1.0037 |
| 0.418879 | 1.11472 |
| 0.471239 | 1.21353 |
| 0.523599 | 1.29904 |
| 0.575959 | 1.37032 |
| 0.628319 | 1.42658 |
| 0.680678 | 1.46722 |
| 0.733038 | 1.49178 |
| 0.785398 | 1.5 |
| 0.837758 | 1.49178 |
| 0.890118 | 1.46722 |
| 0.942478 | 1.42658 |
| 0.994838 | 1.37032 |
| 1.0472 | 1.29904 |
| 1.09956 | 1.21353 |
| 1.15192 | 1.11472 |
| 1.20428 | 1.0037 |
| 1.25664 | 0.881678 |
| 1.309 | 0.75 |
| 1.36136 | 0.610105 |
| 1.41372 | 0.463525 |
| 1.46608 | 0.311868 |
| 1.51844 | 0.156793 |
| 1.5708 | 8.49831e-16 |
| 1.62316 | -0.156793 |
| 1.67552 | -0.311868 |
| 1.72788 | -0.463525 |
| 1.78024 | -0.610105 |
| 1.8326 | -0.75 |
| 1.88496 | -0.881678 |
| 1.93732 | -1.0037 |
| 1.98968 | -1.11472 |
| 2.04204 | -1.21353 |
| 2.0944 | -1.29904 |
| 2.14675 | -1.37032 |
| 2.19911 | -1.42658 |
| 2.25147 | -1.46722 |
| 2.30383 | -1.49178 |
| 2.35619 | -1.5 |
| 2.40855 | -1.49178 |
| 2.46091 | -1.46722 |
| 2.51327 | -1.42658 |
| 2.56563 | -1.37032 |
| 2.61799 | -1.29904 |
| 2.67035 | -1.21353 |
| 2.72271 | -1.11472 |
| 2.77507 | -1.0037 |
| 2.82743 | -0.881678 |
| 2.87979 | -0.75 |
| 2.93215 | -0.610105 |
| 2.98451 | -0.463525 |
| 3.03687 | -0.311868 |
| 3.08923 | -0.156793 |
| 3.14159 | -1.69966e-15 |
Transverse y coordinate
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.
Transverse y coordinate: numerical coordinates
| time (s) | y (m) |
|---|---|
| 0 | 0 |
| 0.0523599 | -0.00821716 |
| 0.10472 | -0.0327786 |
| 0.15708 | -0.0734152 |
| 0.20944 | -0.129682 |
| 0.261799 | -0.200962 |
| 0.314159 | -0.286475 |
| 0.366519 | -0.385283 |
| 0.418879 | -0.496304 |
| 0.471239 | -0.618322 |
| 0.523599 | -0.75 |
| 0.575959 | -0.889895 |
| 0.628319 | -1.03647 |
| 0.680678 | -1.18813 |
| 0.733038 | -1.34321 |
| 0.785398 | -1.5 |
| 0.837758 | -1.65679 |
| 0.890118 | -1.81187 |
| 0.942478 | -1.96353 |
| 0.994838 | -2.1101 |
| 1.0472 | -2.25 |
| 1.09956 | -2.38168 |
| 1.15192 | -2.5037 |
| 1.20428 | -2.61472 |
| 1.25664 | -2.71353 |
| 1.309 | -2.79904 |
| 1.36136 | -2.87032 |
| 1.41372 | -2.92658 |
| 1.46608 | -2.96722 |
| 1.51844 | -2.99178 |
| 1.5708 | -3 |
| 1.62316 | -2.99178 |
| 1.67552 | -2.96722 |
| 1.72788 | -2.92658 |
| 1.78024 | -2.87032 |
| 1.8326 | -2.79904 |
| 1.88496 | -2.71353 |
| 1.93732 | -2.61472 |
| 1.98968 | -2.5037 |
| 2.04204 | -2.38168 |
| 2.0944 | -2.25 |
| 2.14675 | -2.1101 |
| 2.19911 | -1.96353 |
| 2.25147 | -1.81187 |
| 2.30383 | -1.65679 |
| 2.35619 | -1.5 |
| 2.40855 | -1.34321 |
| 2.46091 | -1.18813 |
| 2.51327 | -1.03647 |
| 2.56563 | -0.889895 |
| 2.61799 | -0.75 |
| 2.67035 | -0.618322 |
| 2.72271 | -0.496304 |
| 2.77507 | -0.385283 |
| 2.82743 | -0.286475 |
| 2.87979 | -0.200962 |
| 2.93215 | -0.129682 |
| 2.98451 | -0.0734152 |
| 3.03687 | -0.0327786 |
| 3.08923 | -0.00821716 |
| 3.14159 | 0 |
Transverse trajectory with independently scaled plot axes
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.
Transverse trajectory with independently scaled plot axes: numerical coordinates
| x (m) | y (m) |
|---|---|
| 0 | 0 |
| 0.117689 | -0.004624 |
| 0.234652 | -0.0184675 |
| 0.350168 | -0.0414451 |
| 0.463525 | -0.0734152 |
| 0.574025 | -0.114181 |
| 0.680986 | -0.16349 |
| 0.783748 | -0.22104 |
| 0.881678 | -0.286475 |
| 0.974172 | -0.359391 |
| 1.06066 | -0.43934 |
| 1.14061 | -0.525828 |
| 1.21353 | -0.618322 |
| 1.27896 | -0.716252 |
| 1.33651 | -0.819014 |
| 1.38582 | -0.925975 |
| 1.42658 | -1.03647 |
| 1.45855 | -1.14983 |
| 1.48153 | -1.26535 |
| 1.49538 | -1.38231 |
| 1.5 | -1.5 |
| 1.49538 | -1.61769 |
| 1.48153 | -1.73465 |
| 1.45855 | -1.85017 |
| 1.42658 | -1.96353 |
| 1.38582 | -2.07403 |
| 1.33651 | -2.18099 |
| 1.27896 | -2.28375 |
| 1.21353 | -2.38168 |
| 1.14061 | -2.47417 |
| 1.06066 | -2.56066 |
| 0.974172 | -2.64061 |
| 0.881678 | -2.71353 |
| 0.783748 | -2.77896 |
| 0.680986 | -2.83651 |
| 0.574025 | -2.88582 |
| 0.463525 | -2.92658 |
| 0.350168 | -2.95855 |
| 0.234652 | -2.98153 |
| 0.117689 | -2.99538 |
| 1.83697e-16 | -3 |
| -0.117689 | -2.99538 |
| -0.234652 | -2.98153 |
| -0.350168 | -2.95855 |
| -0.463525 | -2.92658 |
| -0.574025 | -2.88582 |
| -0.680986 | -2.83651 |
| -0.783748 | -2.77896 |
| -0.881678 | -2.71353 |
| -0.974172 | -2.64061 |
| -1.06066 | -2.56066 |
| -1.14061 | -2.47417 |
| -1.21353 | -2.38168 |
| -1.27896 | -2.28375 |
| -1.33651 | -2.18099 |
| -1.38582 | -2.07403 |
| -1.42658 | -1.96353 |
| -1.45855 | -1.85017 |
| -1.48153 | -1.73465 |
| -1.49538 | -1.61769 |
| -1.5 | -1.5 |
| -1.49538 | -1.38231 |
| -1.48153 | -1.26535 |
| -1.45855 | -1.14983 |
| -1.42658 | -1.03647 |
| -1.38582 | -0.925975 |
| -1.33651 | -0.819014 |
| -1.27896 | -0.716252 |
| -1.21353 | -0.618322 |
| -1.14061 | -0.525828 |
| -1.06066 | -0.43934 |
| -0.974172 | -0.359391 |
| -0.881678 | -0.286475 |
| -0.783748 | -0.22104 |
| -0.680986 | -0.16349 |
| -0.574025 | -0.114181 |
| -0.463525 | -0.0734152 |
| -0.350168 | -0.0414451 |
| -0.234652 | -0.0184675 |
| -0.117689 | -0.004624 |
| -3.67394e-16 | 0 |
| Quantity | Value | Unit |
|---|---|---|
| Signed cyclotron angular frequency | 2 | rad/s |
| Neutral straight-path flag | 0 | flag |
| Transverse radius when charged, zero placeholder if neutral | 1.5 | m |
| Period when charged, zero placeholder if neutral | 3.14159 | s |
| Constant speed | 3.60555 | m/s |
| Initial acceleration x | 0 | m/s² |
| Initial acceleration y | -6 | m/s² |
| Magnetic acceleration dot velocity at sampled time | 0 | m²/s³ |
Magnetic force rotates the transverse velocity while leaving speed and parallel velocity unchanged.
Equations dvx/dt = omega vy and dvy/dt = −omega vx give vx=3cos(omega t), vy=−3sin(omega t), with vz=2 m/s. The work rate q(v cross B) dot v vanishes. Displayed radius and period are explicitly not applicable in the neutral branch; zero placeholders are not physical zero radius or zero period. The coordinate plot may rescale axes independently; use the equal-scale diagram and coordinates for geometry.
Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.
Magnetic force rotates the transverse velocity while leaving speed and parallel velocity unchanged.
Equations dvx/dt = omega vy and dvy/dt = −omega vx give vx=3cos(omega t), vy=−3sin(omega t), with vz=2 m/s. The work rate q(v cross B) dot v vanishes. Displayed radius and period are explicitly not applicable in the neutral branch; zero placeholders are not physical zero radius or zero period. The coordinate plot may rescale axes independently; use the equal-scale diagram and coordinates for geometry.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
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Which source geometry, material response or independent measurement assumption limits this magnetic inference?
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