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SCIENCE · INVESTIGATE AND EXPLAIN

Separate a vector field from a signed test force

Add source vectors before applying the passive test charge.

Learning outcome: Compare right-source charges −2, 0 and +2 nC at a fixed probe. Construct equal-scale vector arrows at (0,1) before checking the component slices. Then vary only the probe through negative, zero and positive values; retain the unchanged field and changed force. Explain why the displayed component curves are not physical particle trajectories.

Starting recap

Choose source and observer coordinates, integrate normalized charge, and justify symmetry before simplifying field or flux.

All lessons are open directly. Your saved experiments remain when you leave and return.

Try

At (0,1) m, sources +2 nC at (−1,0) and −2 nC at (1,0) have equal positive x contributions and cancelling y contributions. Ex≈12.7103 N/C, Ey = 0. A +1 nC probe feels +1.27103×10⁻⁸ N along x; reversing only the probe reverses its force.

Open the experiment

Predict

If a passive test charge is set to zero, what happens to the field created by the fixed sources?

Experiment

Compare right-source charges −2, 0 and +2 nC at a fixed probe. Construct equal-scale vector arrows at (0,1) before checking the component slices. Then vary only the probe through negative, zero and positive values; retain the unchanged field and changed force. Explain why the displayed component curves are not physical particle trajectories.

Separate source field from passive test force

Worked teaching model · synthetic values · Sources at (−1,0) and (1,0) m; left source +2 nC. Sample at (0,1) m. Passive infinitesimal-probe approximation ignores back reaction; zero test charge does not erase source field. Field slices at y=1 avoid source singularities.

Reset keeps your prediction, captures and practice history.

Source vector map on equal spatial scales

++2 nC−-2 nCx (m); both spatial axes use 90 screen units per metrey (m)−222−2

Arrows share one field scale: 32 screen units represent 35.9502 N/C in this setting. The field scale resets when source charge changes; compare numerical magnitudes across settings. A dot without an arrow indicates zero field. Source singularities are excluded. The probe setting does not change this map.

Field-map positions and components
x (m)y (m)Ex (N/C)Ey (N/C)
-2-2-0.457266-2.4485
-1-21.58879-2.90499
0-23.215480
1-21.588792.90499
2-2-0.4572662.4485
-2-1-4.64989-5.78674
-1-13.21548-16.3674
0-112.71030
1-13.2154816.3674
2-1-4.649895.78674
-20-15.97790
0035.95020
20-15.97790
-21-4.649895.78674
-113.2154816.3674
0112.71030
113.21548-16.3674
21-4.64989-5.78674
-22-0.4572662.4485
-121.588792.90499
023.215480
121.58879-2.90499
22-0.457266-2.4485

Horizontal component along y=1 m

Ex (N/C)x (m)-2212.7103-4.932

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.

Horizontal component along y=1 m: numerical coordinates
x (m)Ex (N/C)
-2-4.64989
-1.93333-4.78336
-1.86667-4.88161
-1.8-4.932
-1.73333-4.9197
-1.66667-4.82785
-1.6-4.6381
-1.53333-4.33163
-1.46667-3.89065
-1.4-3.30049
-1.33333-2.55209
-1.26667-1.6446
-1.2-0.58758
-1.133330.597814
-1.066671.87925
-13.21548
-0.9333334.56029
-0.8666675.86742
-0.87.09554
-0.7333338.21215
-0.6666679.19585
-0.610.0367
-0.53333310.7349
-0.46666711.2987
-0.411.7416
-0.33333312.0797
-0.26666712.3295
-0.212.5063
-0.13333312.6229
-0.066666712.689
012.7103
0.066666712.689
0.13333312.6229
0.212.5063
0.26666712.3295
0.33333312.0797
0.411.7416
0.46666711.2987
0.53333310.7349
0.610.0367
0.6666679.19585
0.7333338.21215
0.87.09554
0.8666675.86742
0.9333334.56029
13.21548
1.066671.87925
1.133330.597814
1.2-0.58758
1.26667-1.6446
1.33333-2.55209
1.4-3.30049
1.46667-3.89065
1.53333-4.33163
1.6-4.6381
1.66667-4.82785
1.73333-4.9197
1.8-4.932
1.86667-4.88161
1.93333-4.78336
2-4.64989

Vertical component along y=1 m

Ey (N/C)x (m)-2216.3706-16.3706

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.

Vertical component along y=1 m: numerical coordinates
x (m)Ey (N/C)
-25.78674
-1.933336.41909
-1.866677.11483
-1.87.87476
-1.733338.69702
-1.666679.57616
-1.610.5019
-1.5333311.4583
-1.4666712.4225
-1.413.3648
-1.3333314.2487
-1.2666715.033
-1.215.6745
-1.1333316.1318
-1.0666716.3706
-116.3674
-0.93333316.1129
-0.86666715.6134
-0.814.8893
-0.73333313.972
-0.66666712.8994
-0.611.7114
-0.53333310.4456
-0.4666679.13457
-0.47.80381
-0.3333336.47166
-0.2666675.14948
-0.23.84252
-0.1333332.55117
-0.06666671.2722
00
0.0666667-1.2722
0.133333-2.55117
0.2-3.84252
0.266667-5.14948
0.333333-6.47166
0.4-7.80381
0.466667-9.13457
0.533333-10.4456
0.6-11.7114
0.666667-12.8994
0.733333-13.972
0.8-14.8893
0.866667-15.6134
0.933333-16.1129
1-16.3674
1.06667-16.3706
1.13333-16.1318
1.2-15.6745
1.26667-15.033
1.33333-14.2487
1.4-13.3648
1.46667-12.4225
1.53333-11.4583
1.6-10.5019
1.66667-9.57616
1.73333-8.69702
1.8-7.87476
1.86667-7.11483
1.93333-6.41909
2-5.78674
Calculated values under the declared model
QuantityValueUnit
Source field x component12.7103N/C
Source field y component0N/C
Passive probe force x1.27103e-8N
Passive probe force y0N
Field magnitude12.7103N/C

Changing only the passive test charge changes force, not the source field.

Each vector contribution uses kq displacement/r³. Sum components before taking a magnitude. The displayed two curves are component slices, not field lines or trajectories.

Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.

Changing only the passive test charge changes force, not the source field.

Each vector contribution uses kq displacement/r³. Sum components before taking a magnitude. The displayed two curves are component slices, not field lines or trajectories.

Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.

Understand

Define the passive probe assumption

The electric field is the force per positive test charge in the limit that the probe does not substantially disturb the sources. Writing E = F/q does not mean E depends on whichever test charge is chosen. At q = 0 use the independently specified source field rather than dividing zero force by zero charge.

Sum the source displacement vectors

A source q at rsource contributes E = kq(robs−rsource)/|robs−rsource|³. The denominator contains the cube because the numerator still contains a vector of length r. Adding these components implements superposition. Negative q reverses the contribution. Never sum magnitudes first when source directions differ.

Read maps and field lines honestly

A vector map attaches a local direction and scaled magnitude to sample points. A field-line diagram draws curves tangent to that field and uses line density only as a relative-strength convention. Lines are not trajectories of a massive particle, whose initial velocity also matters. The two graphs here are Ex(x,1) and Ey(x,1), not field lines. Singular source locations are excluded by sampling a line one metre above them.

Distinguish source materials

In electrostatic equilibrium the electric field inside conducting material is zero, and the surface field has no tangential component; otherwise mobile charge would keep moving. Excess charge resides at its surface. Insulators can retain assigned volume charge and nonzero interior fields. A hollow cavity, a conducting material region and an insulating volume are different domains; later spherical examples compare them explicitly.

Worked original case

At (0,1) m, sources +2 nC at (−1,0) and −2 nC at (1,0) have equal positive x contributions and cancelling y contributions. Ex≈12.7103 N/C, Ey = 0. A +1 nC probe feels +1.27103×10⁻⁸ N along x; reversing only the probe reverses its force.

Investigation

Compare right-source charges −2, 0 and +2 nC at a fixed probe. Construct equal-scale vector arrows at (0,1) before checking the component slices. Then vary only the probe through negative, zero and positive values; retain the unchanged field and changed force. Explain why the displayed component curves are not physical particle trajectories.

Public numerical transfer practice

Try a new practice case

Change the right source to +2 nC. At (0,1) m, what is Ey divided by k×(1 nC)/(1 m)²?

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 evidence boundary

Original cases and teaching checked 30 October 2026 against the current official calculus-based electricity and magnetism framework and OpenStax electric fields. All displayed records are generated or supplied, not learner measurements. No charging, mains connection, high-voltage equipment, physical circuit or material handling is requested. Public feedback and retained self-reports are practice evidence, not independent mastery, performed laboratory time or AP authorization.

Apply

If a passive test charge is set to zero, what happens to the field created by the fixed sources?

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

Which source, boundary or independence assumption would have to change before the conclusion changes?

Continue

Completion requires a saved prediction, at least one capture and a reflection. Presence checks do not grade your reasoning.

Skipping retains experiments and awards no mastery.

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