Integrate material resistance without confusing graph slopes
Resistivity describes a specified material state; resistance also depends on geometry.
Learning outcome: Compare uniform and linearly varying resistivity with the same rho0. Derive the cumulative voltage curve, then differentiate it. Predict both graph slopes. Finally use the supplied temperature and nonlinear packets to identify where a fixed-parameter ohmic model is no longer appropriate.
Starting recap
Integrate current or resistance, preserve node topology and derive transient state with a signed energy account.
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Try
For rho0 = 2 micro-ohm m, alpha = 1, A = 1 mm² and L = 1 m, R = 3 ohm. At 10 V, I = 10/3 A. The I-versus-V slope is 1/3 A/V; local field grows from 20/3 to 40/3 V/m while its integrated drop remains 10 V.
Open the experimentPredict
An I-versus-V graph has slope 0.25 A/V for a fixed ohmic component. What is its resistance?
Experiment
Compare uniform and linearly varying resistivity with the same rho0. Derive the cumulative voltage curve, then differentiate it. Predict both graph slopes. Finally use the supplied temperature and nonlinear packets to identify where a fixed-parameter ohmic model is no longer appropriate.
Integrate a spatially varying resistivity
Worked teaching model · synthetic values · Uniform area 1 mm² and length 1 m; rho(x) = rho0(1 + alpha x/L). Maintained 10 V, steady current, prescribed local temperature/material state. No self-heating feedback solved. Material resistivity is not the same quantity as whole-object resistance.
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Cumulative resistor potential drop
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.
Cumulative resistor potential drop: numerical coordinates
| distance (m) | potential drop (V) |
|---|---|
| 0 | 0 |
| 0.0166667 | 0.112037 |
| 0.0333333 | 0.225926 |
| 0.05 | 0.341667 |
| 0.0666667 | 0.459259 |
| 0.0833333 | 0.578704 |
| 0.1 | 0.7 |
| 0.116667 | 0.823148 |
| 0.133333 | 0.948148 |
| 0.15 | 1.075 |
| 0.166667 | 1.2037 |
| 0.183333 | 1.33426 |
| 0.2 | 1.46667 |
| 0.216667 | 1.60093 |
| 0.233333 | 1.73704 |
| 0.25 | 1.875 |
| 0.266667 | 2.01481 |
| 0.283333 | 2.15648 |
| 0.3 | 2.3 |
| 0.316667 | 2.44537 |
| 0.333333 | 2.59259 |
| 0.35 | 2.74167 |
| 0.366667 | 2.89259 |
| 0.383333 | 3.04537 |
| 0.4 | 3.2 |
| 0.416667 | 3.35648 |
| 0.433333 | 3.51481 |
| 0.45 | 3.675 |
| 0.466667 | 3.83704 |
| 0.483333 | 4.00093 |
| 0.5 | 4.16667 |
| 0.516667 | 4.33426 |
| 0.533333 | 4.5037 |
| 0.55 | 4.675 |
| 0.566667 | 4.84815 |
| 0.583333 | 5.02315 |
| 0.6 | 5.2 |
| 0.616667 | 5.3787 |
| 0.633333 | 5.55926 |
| 0.65 | 5.74167 |
| 0.666667 | 5.92593 |
| 0.683333 | 6.11204 |
| 0.7 | 6.3 |
| 0.716667 | 6.48981 |
| 0.733333 | 6.68148 |
| 0.75 | 6.875 |
| 0.766667 | 7.07037 |
| 0.783333 | 7.26759 |
| 0.8 | 7.46667 |
| 0.816667 | 7.66759 |
| 0.833333 | 7.87037 |
| 0.85 | 8.075 |
| 0.866667 | 8.28148 |
| 0.883333 | 8.48981 |
| 0.9 | 8.7 |
| 0.916667 | 8.91204 |
| 0.933333 | 9.12593 |
| 0.95 | 9.34167 |
| 0.966667 | 9.55926 |
| 0.983333 | 9.7787 |
| 1 | 10 |
| Quantity | Value | Unit |
|---|---|---|
| Integrated resistance | 3 | ohm |
| Steady current | 3.33333 | A |
| Slope of I versus applied voltage | 0.333333 | A/V |
| Slope of voltage versus I | 3 | V/A |
| Local field at source end | 6.66667 | V/m |
| Local field at far end | 13.3333 | V/m |
A constant current can coexist with a varying local electric field when resistivity changes along a uniform section.
Add infinitesimal series drops: dV = I rho(x) dx/A and R = integral rho(x) dx/A. The I-versus-V slope is conductance, so resistance is its reciprocal. These parameters describe a fixed material/temperature state; ordinary ohmic behavior at fixed temperature does not imply temperature-independent resistivity in all circumstances.
Derive before checking. Retain contrasting captures and explain one assumption that could fail; calculated evidence is not actual laboratory work.
A constant current can coexist with a varying local electric field when resistivity changes along a uniform section.
Add infinitesimal series drops: dV = I rho(x) dx/A and R = integral rho(x) dx/A. The I-versus-V slope is conductance, so resistance is its reciprocal. These parameters describe a fixed material/temperature state; ordinary ohmic behavior at fixed temperature does not imply temperature-independent resistivity in all circumstances.
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