Reconstruct a uniform field from a voltage survey
A local uniform-field region can be described by a linear potential V=ax+3y+C in SI units. Three probes occupy (0,0), (2,0) and (0,1) m. Voltage differences along horizontal and vertical baselines determine the components without calculus: electric work gives Ex=−[V(2,0)−V(0,0)]/(2 m) and Ey=−[V(0,1)−V(0,0)]/(1 m). The minus sign says field points toward decreasing potential.
Learning outcome: Change only C first and retain the unchanged field. Then change a and draw the new normal and equipotential direction with common spatial scales. Compare independent endpoint uncertainty with a common offset, and propose a fourth probe location that tests the uniform-field assumption.
Starting recap
Use signed charge, common coordinate axes, SI units, vector components and algebraic ratios. Separate a source field from probe force and a fitted parameter from independently tested evidence.
All lessons are open directly. Your saved experiments remain when you leave and return.
Try
At a=2 V/m and C=1 V, the three voltages are 1,5,4 V. They imply Ex=−2 and Ey=−3 N/C, magnitude √13. A displacement (3,−2) m gives ΔV=6−6=0 and zero electrostatic work for any test charge.
Open the experimentPredict
Three collinear voltage probes cannot generally determine:
Experiment
Change only C first and retain the unchanged field. Then change a and draw the new normal and equipotential direction with common spatial scales. Compare independent endpoint uncertainty with a common offset, and propose a fourth probe location that tests the uniform-field assumption.
Infer a uniform field from three noncollinear voltages
Worked teaching model · synthetic values · Supplied local planar potential V=a x+3 y+b in SI units. Probes at (0,0),(2,0),(0,1) m have exact coordinates. Compare a common voltage offset with independent ±.1 V per-reading bounds. This is not a global isolated-source potential.
Reset keeps your prediction, captures and practice history.
Parallel equipotentials on common spatial scales
Spatial axes use the same pixels per physical unit, preserving geometry. 1: V minus offset = -3 V (solid).2: V minus offset = 0 V (dashed).3: V minus offset = 3 V (dotted). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Parallel equipotentials on common spatial scales
V minus offset = -3 V
| x (m) | y (m) |
|---|---|
| -2 | 0.333333 |
| 2 | -2.33333 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
V minus offset = 0 V
| x (m) | y (m) |
|---|---|
| -2 | 1.33333 |
| 2 | -1.33333 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
V minus offset = 3 V
| x (m) | y (m) |
|---|---|
| -2 | 2.33333 |
| 2 | -0.333333 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
Voltage differences determine components
Unlike graph quantities rescale independently; read units and values, not screen angles. 1: common-offset voltage map (solid). Joined curves show the supplied model, not additional observations.
Equivalent numerical coordinates for Voltage differences determine components
common-offset voltage map
| x (m) along y=0 | potential (V) |
|---|---|
| 0 | 1 |
| 2 | 5 |
At most 82 representative computed coordinates including endpoints; the plotted curve can use a finer grid. A table of a revealed generator is not independent measurement evidence.
| Quantity | Value | Unit |
|---|---|---|
| Origin voltage | 1 | V |
| x-probe voltage at (2,0) | 5 | V |
| y-probe voltage at (0,1) | 4 | V |
| Recovered electric field x | -2 | N/C |
| Recovered electric field y | -3 | N/C |
| Field magnitude | 3.60555 | N/C |
| Worst-case Ex error from independent voltage bounds | 0.1 | N/C |
| Worst-case Ey error from independent voltage bounds | 0.2 | N/C |
| Potential change along displacement (3,−a) | 0 | V |
A common offset cancels from differences, but independent probe errors do not.
Uniform-field work gives Ex=−[V(2,0)−V(0,0)]/2 and Ey=−[V(0,1)−V(0,0)]. The displacement (3,−a) has zero dot product with the field, so it lies along an equipotential. Independent ±.1 V endpoint errors yield difference bound ±.2 V; divide by each baseline. Collinear probes alone would not identify the perpendicular field component.
Predict before inspecting the values. Save contrasting records with assumptions and one alternative explanation. This virtual display does not certify practical measurement technique.
A common offset cancels from differences, but independent probe errors do not.
Uniform-field work gives Ex=−[V(2,0)−V(0,0)]/2 and Ey=−[V(0,1)−V(0,0)]. The displacement (3,−a) has zero dot product with the field, so it lies along an equipotential. Independent ±.1 V endpoint errors yield difference bound ±.2 V; divide by each baseline. Collinear probes alone would not identify the perpendicular field component.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
Understand
Apply
Public practice checks a specific claim. It does not establish independent mastery.
Which independent observation could reject this model rather than merely refit its parameters?
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.
Save a science backup or import one
Science work is stored locally in this browser, separately from mathematics and AI. It does not sync automatically. Use this science-only backup; this checkout's older all-subject export does not include science.
A legacy file is available only when the complete snapshot fits the 36 MB limit. For larger snapshots, prepare a complete file set below; never discard notebooks to make a smaller file.
Matching imported notebook drafts replace their current drafts. Omitted lessons and known first attempts remain. Export your current work first if you want to retain both drafts.
Complete file sets and course backups
A file set can hold more work than one science file. Keep its manifest and every part together. Each file is limited to 36 MB. This format needs this version of LearnAI or a compatible newer version; older versions can use only the legacy single-file backup above.
The set includes every saved science course and global continuation at this moment. Later edits need a new export. A conflicting tab exports its own visible work, which may differ from saved work in another tab.
0 file(s) selected. File order and filenames do not determine identity. Missing, changed or conflicting parts block the entire restore; no good part is applied by itself.
Science storage: loading. No account or remote computation is required.