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SCIENCE · INVESTIGATE AND EXPLAIN

Differentiate ring potential without losing the reference distinction

Potential contributions add as scalars, which can make source integration simpler than vector field integration. Every element of a uniform ring is the same distance from an axial point. With Q=2 nC, V(z)=18/√(R²+z²) V when the reference is zero at infinity. This finite-source reference is legitimate because the potential tends to zero at large distance.

Learning outcome: Predict the center field from symmetry, then verify by differentiating the potential. At z=1 m compare h=0.1,0.2,0.4 m and retain signed errors. On paper add the same 5 V offset to both sampled potentials and show the cancellation before discussing independent error bounds.

Starting recap

Review oriented normals, definite integrals, source volume measures and partial derivatives as one-coordinate rates. Potential differences use an explicit reference and field work uses a signed line integral.

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Try

For R=1 m, center potential is 18 V while center field is zero. At z=1 m, V=18/√2≈12.727922 V and exact E=9/√2≈6.363961 N/C. Compare symmetric half-spacings 0.1 and 0.2 m against that analytic derivative; their disagreement is discretization evidence, not a change in source charge.

Open the experiment

Predict

Which statement about the ring center is correct?

Experiment

Predict the center field from symmetry, then verify by differentiating the potential. At z=1 m compare h=0.1,0.2,0.4 m and retain signed errors. On paper add the same 5 V offset to both sampled potentials and show the cancellation before discussing independent error bounds.

Differentiate a source potential and audit a finite difference

Worked teaching model · synthetic values · Uniform ring Q=2 nC, potential V(z)=18/sqrt(R²+z²) V with infinity reference. Evaluate axial field at z=1 m by analytic derivative and symmetric finite difference. Added gauge offsets cancel in the difference; finite spacing gives truncation error, not a physical field change.

Reset keeps your prediction, captures and practice history.

Ring potential with infinity reference

potential (V)axial coordinate (m)-22180

Unlike graph quantities rescale independently; read units and values, not screen angles. 1: source-integrated scalar potential (solid). Joined curves show the supplied model, not additional observations.

Equivalent numerical coordinates for Ring potential with infinity reference

source-integrated scalar potential

axial coordinate (m)potential (V)
-28.049845
-1.958.2137
-1.98.383436
-1.858.559307
-1.88.741573
-1.758.930501
-1.79.126362
-1.659.329431
-1.69.539981
-1.559.758284
-1.59.984604
-1.4510.21919
-1.410.46229
-1.3510.7141
-1.310.97479
-1.2511.24451
-1.211.52332
-1.1511.81122
-1.112.10811
-1.0512.41379
-112.72792
-0.9513.04999
-0.913.37929
-0.8513.71491
-0.814.05564
-0.7514.4
-0.714.74617
-0.6515.09199
-0.615.43487
-0.5515.77189
-0.516.09969
-0.4516.41459
-0.416.71258
-0.3516.98945
-0.317.24087
-0.2517.46257
-0.217.65045
-0.1517.80085
-0.117.91067
-0.0517.97754
018
0.0517.97754
0.117.91067
0.1517.80085
0.217.65045
0.2517.46257
0.317.24087
0.3516.98945
0.416.71258
0.4516.41459
0.516.09969
0.5515.77189
0.615.43487
0.6515.09199
0.714.74617
0.7514.4
0.814.05564
0.8513.71491
0.913.37929
0.9513.04999
112.72792
1.0512.41379
1.112.10811
1.1511.81122
1.211.52332
1.2511.24451
1.310.97479
1.3510.7141
1.410.46229
1.4510.21919
1.59.984604
1.559.758284
1.69.539981
1.659.329431
1.79.126362
1.758.930501
1.88.741573
1.858.559307
1.98.383436
1.958.2137
28.049845

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.

Calculated quantities under the declared measurement model
QuantityValueUnit
Potential at ring center18V
Axial field at ring center0N/C
Potential at z equals 112.72792V
Analytic axial field at z equals 16.363961N/C
Symmetric finite-difference field6.330798N/C
Signed derivative approximation error-0.03316259N/C

A nonzero potential can have zero gradient; gauge offsets change neither field nor potential differences.

All ring elements lie at the same axial distance, so V=KQ/√(R²+z²) with zero at infinity. Taking −dV/dz gives KQz/(R²+z²)^(3/2). At the center V=KQ/R while E=0 by symmetry. A symmetric finite difference approximates the derivative at z=1; changing its spacing changes truncation error, not the underlying field. Adding any constant to both sampled potentials cancels exactly algebraically.

Predict before inspecting the values. Save contrasting records with assumptions and one alternative explanation. This virtual display does not certify practical measurement technique.

A nonzero potential can have zero gradient; gauge offsets change neither field nor potential differences.

All ring elements lie at the same axial distance, so V=KQ/√(R²+z²) with zero at infinity. Taking −dV/dz gives KQz/(R²+z²)^(3/2). At the center V=KQ/R while E=0 by symmetry. A symmetric finite difference approximates the derivative at z=1; changing its spacing changes truncation error, not the underlying field. Adding any constant to both sampled potentials cancels exactly algebraically.

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

Understand

Define the geometry and reference

Potential contributions add as scalars, which can make source integration simpler than vector field integration. Every element of a uniform ring is the same distance from an axial point. With Q=2 nC, V(z)=18/√(R²+z²) V when the reference is zero at infinity. This finite-source reference is legitimate because the potential tends to zero at large distance.

Derive the integral or gradient

Take the negative derivative to recover Ez=18z/(R²+z²)^(3/2). At the center V=18/R is nonzero but its derivative and field are zero. At z=1 m, a symmetric estimate is −[V(1+h)−V(1−h)]/(2h). That is an approximation to the local derivative, not the exact finite-interval field unless the relevant potential is linear.

Check the inference boundary

Changing h changes truncation error. Adding a common potential offset to both readings cancels algebraically, but separate reading errors are divided by the spacing and can grow important as h shrinks. The displayed packet is noise-free; it does not quietly assign a confidence interval or declare the smallest step always best for real measurements.

Worked original case

For R=1 m, center potential is 18 V while center field is zero. At z=1 m, V=18/√2≈12.727922 V and exact E=9/√2≈6.363961 N/C. Compare symmetric half-spacings 0.1 and 0.2 m against that analytic derivative; their disagreement is discretization evidence, not a change in source charge.

Investigation

Predict the center field from symmetry, then verify by differentiating the potential. At z=1 m compare h=0.1,0.2,0.4 m and retain signed errors. On paper add the same 5 V offset to both sampled potentials and show the cancellation before discussing independent error bounds.

Changed-case practice

Try the changed case before feedback

For R=2 m and Q=2 nC, find the center potential with zero at infinity in volts.

This practice is public and unsaved. A matching number does not verify understanding. Retain your explanation, assumptions and changed-case evidence in the separate course workspace.

Sources and boundaries

Original calculations checked 30 October 2026 against the primary explanation. All source distributions, fields and readings are hypothetical. This is not a physical high-voltage or electrical handling activity, and public numerical feedback does not establish independent mastery. Preserve first predictions, critique, revision and newly assigned work in the separate retained course workspace.

Apply

Which statement about the ring center is correct?

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

Which geometry, calibration or source assumption could fail while an exact arithmetic fit remains possible?

Continue

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