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SCIENCE · INVESTIGATE AND EXPLAIN

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 experiment

Predict

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.

xy

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

x (m)time (s)03.141591.5-1.5

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)
00
0.05235990.156793
0.104720.311868
0.157080.463525
0.209440.610105
0.2617990.75
0.3141590.881678
0.3665191.0037
0.4188791.11472
0.4712391.21353
0.5235991.29904
0.5759591.37032
0.6283191.42658
0.6806781.46722
0.7330381.49178
0.7853981.5
0.8377581.49178
0.8901181.46722
0.9424781.42658
0.9948381.37032
1.04721.29904
1.099561.21353
1.151921.11472
1.204281.0037
1.256640.881678
1.3090.75
1.361360.610105
1.413720.463525
1.466080.311868
1.518440.156793
1.57088.49831e-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

y (m)time (s)03.141590-3

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)
00
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
3.141590

Transverse trajectory with independently scaled plot axes

y (m)x (m)-1.51.50-3

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)
00
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
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-1.06066-2.56066
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-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-160
Calculated values under the declared model
QuantityValueUnit
Signed cyclotron angular frequency2rad/s
Neutral straight-path flag0flag
Transverse radius when charged, zero placeholder if neutral1.5m
Period when charged, zero placeholder if neutral3.14159s
Constant speed3.60555m/s
Initial acceleration x0m/s²
Initial acceleration y-6m/s²
Magnetic acceleration dot velocity at sampled time0m²/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.

Understand

Write the coupled velocity equations

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. With initial velocity (3,0,2) m/s, vx = 3cos(omega t), vy = −3sin(omega t) and vz = 2. Integrating positions gives x = 3sin(omega t)/omega, y = 3[cos(omega t) − 1]/omega and z = 2t for nonzero omega.

Recover the neutral limit safely

If q/m = 0, use x = 3t, y = 0 and z = 2t directly. Do not divide by zero or draw a fictitious zero-radius orbit. For a charged body, transverse radius is 3/|omega| and period 2pi/|omega|. The zero placeholders in the neutral ledger are explicitly not physical radius or period. A field-parallel velocity creates a helix, not a closed three-dimensional circle.

Prove the energy statement

Magnetic power is q(v cross B) dot v = 0, so speed remains sqrt(13) m/s in this pure magnetic packet. The field changes direction of motion but not kinetic energy. An electric field, radiation or collision would change the account and is excluded here. This conclusion does not mean every macroscopic current-driven device has no source energy transfer.

Derive a Hall equilibrium with explicit polarity

Let conventional current density J point +x and applied B point +z in a single-carrier conductor. Mean carrier drift is vd = J/(nq). The transverse equilibrium is EHall = −vd cross B, so Ey = vd B. If the upper edge is at larger y by width w, Vupper − Vlower = −Ey w. Electron carriers have negative vd, giving negative Ey and a positive upper-minus-lower potential in this stated geometry. A reversal of either J or B reverses the Hall voltage.

Check a signed original Hall packet

Use the supplied carrier density n = 1×10²⁸ per m³, electron charge −e, J = 1×10⁶ A/m², B = 0.5 T and width 0.01 m. Then vd ≈ −6.24151×10⁻⁴ m/s, Ey ≈ −3.12075×10⁻⁴ V/m and Vupper − Vlower ≈ +3.12075 microvolt. A positive-carrier model with the same n and J predicts the opposite sign. Multiple carriers or uncertain contact polarity would require a richer model; this is not a material-identification guarantee.

Worked original case

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.

Investigation

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.

Changed-case practice

Try a new practice case

For q/m = −2 C/kg and B = 3 T, what is transverse radius with the stated 3 m/s transverse speed, in metres?

This public, unsaved check is not a secure assessment. Explain the source integral, symmetry or charge boundary in the retained course evidence workspace.

Sources and model boundary

Original teaching checked 31 October 2026 against the current official framework, Unit 12. The displayed magnetic calculations use the stipulated introductory approximation mu0 = 4pi×10⁻⁷ SI, not a claim that this is exact in modern SI. All apparatus and records are virtual, supplied or generated. No real magnet handling, electrical current setup, particle apparatus or material operation is requested. Public feedback and retained reports are practice evidence, not independent mastery or performed laboratory time.

Supplemental primary teaching reference: The Hall effect. The supplied cases, derivations and diagrams here are original; the source’s older exact-mu0 convention and classical spin language are not adopted literally.

Apply

In a pure uniform magnetic field, which quantity is constant for this isolated classical body?

Public practice checks a specific claim. It does not establish independent mastery.

Which source geometry, material response or independent measurement assumption limits this magnetic inference?

Continue

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