Interactive Laboratories
- 1 Pick a course Hover a course in the list (tap it on a phone) and its labs slide open, grouped by unit.
- 2 Open a lab Or browse every lab below — each one opens right here, in this same layout.
- 3 Drive it Drag, slide, break the presets. It all runs in your browser; nothing is sent anywhere.
Thermodynamics, electric fields & circuits
Twelve simulations and three hands-on bench labs, all on this page. Every lab names the lesson that explains it — check the numbers against the unit notes.
Unit 1 · Thermodynamics
Ideal gas & PV work
Move a piston and a thermostat; the state point traces a PV diagram while W, Q and ΔU add up live.
5 processesFirst law Simulation · on this pageThermal conductivity
Ten materials across a hot–cold slab. Watch P = kAΔT/L respond to every lever.
10 materialsConduction Simulation · on this pageEntropy
Move heat between two reservoirs and check the entropy budget — plus why sixty particles never crowd into one half.
Second lawMultiplicity Simulation · on this pageHeat transfer & calorimetry
Drop two samples into an insulated cup; ΣQ = 0 decides where the mixture settles.
7 materialsmcΔT Bench lab · on this pageBoyle’s law
The hands-on version: procedure, data table and the analysis of pressure against volume.
Write-upExperimental designUnit 2 · Electric force, field & potential
Coulomb force & superposition
Drag two or three point charges and watch each Coulomb force on a chosen charge add tip to tail into the net force.
Vector superpositionInverse square Simulation · Unit 2Field lines & equipotentials
Arrange charges, see field lines and equipotentials cross at right angles, and probe V and E anywhere on the map.
Electric potentialField lines Simulation · Unit 2Charged particle between plates
Fire an electron or proton between charged plates and watch it follow a parabola in the uniform field E = ΔV/d — or hit a plate.
Uniform fieldProjectile motion Simulation · Unit 2Parallel-plate capacitor
Change plate area, gap, dielectric and battery voltage, and see C, Q, ΔV, E and U respond — connected vs. isolated.
CapacitanceConnected vs isolated Bench lab · on this pageMapping equipotentials
Conductive paper and a voltmeter probe: trace equipotentials, draw the field lines, and measure E = ΔV/Δx.
Write-upExperimental designUnit 3 · Electric circuits
Ohm’s law & resistivity
Pick a material, set the wire’s length, diameter and voltage, and watch R = ρL/A set the current on a live I–V line.
R = ρL/AI–V graph Simulation · Unit 3Series vs parallel bulbs
Wire three bulbs four ways, pull any bulb from its socket, and compare each bulb’s ΔV, I and power-proportional glow.
Bulb brightnessOpen circuits Simulation · Unit 3Two-loop circuit solver
An exact two-loop solver with reversible batteries, current arrows that follow the real sign, and a live junction and loop-rule check.
Junction & loop rulesMulti-loop Simulation · Unit 3RC charging & discharging
Throw the switch to charge or discharge a capacitor and watch VC, VR and I evolve, with markers at τ through 5τ.
τ = RCExponential decay Bench lab · on this pageResistivity of a wire
Nichrome on a metre rule: show the wire is ohmic, then get ρ from the slope of R against length.
Write-upData analysis3D labs, unit by unit
Orbit, drag and slice. Every lab names the lesson section that explains it, one click away.
Unit 1 · Vectors & geometry
Vectors in 3D
Drag two vectors through space; the dot product, cross product, sum and difference respond as you move them.
Orbit viewDot & cross Vector benchInto & out of the page
Look straight down the z-axis and see what the sign of a 2D cross product actually means.
Right-hand rule ReferenceVector formula sheet
Every readout on the vector benches, written out as the equations behind it.
Formulas 3D lab · Unit 1Plane explorer
Set a, b, c, d in ax + by + cz = d and watch the normal, the intercepts and the point-to-plane distance.
PlanesDistance 3D lab · Unit 1Quadric surface viewer
Slide a trace plane through each quadric and name the curve it cuts — the exam identification, done live.
TracesSurfaces 3D lab · Unit 1Locate a point three ways
One point, three constructions: Cartesian, cylindrical and spherical, with the conversions worked below.
CoordinatesUnit 2 · Vector functions
Unit 3 · Partial derivatives
Surface, contours & gradient
The same function as a surface and a contour map; the gradient stays perpendicular to the contours and points uphill.
GradientDirectional derivative 3D lab · Unit 3Critical points & the second-derivative test
Tilt the tangent plane until it goes flat, then read the Hessian to tell a bowl from a saddle.
HessianExtremaUnit 4 · Multiple integrals
Riemann boxes under a surface
Slide n up and watch the staircase of boxes melt into the surface, with the sum tracked against the exact value.
Double integrals 3D lab · Unit 4Region explorer: strips & limits
Sweep a strip across a region and read the limits off its ends — then switch the order and see a new description.
Order of integration 3D lab · Unit 4The volume element, edge by edge
A wedge of space with its three edges labelled, showing where r and ρ² sin φ come from.
CylindricalSphericalUnit 5 · Vector fields
Work along a path
Pick a field and a path, drag the endpoints, and see ∫C F·dr computed as you move.
Line integralsConservative fields 3D lab · Unit 5Divergence & curl probe
Drag a probe through the field; a shrinking circle measures flux and circulation, and a paddle wheel spins with the curl.
DivergenceCurlUnit 6 · Surface integrals
Drills, audio & speaking tools
Tense drills that check every answer, and the exam tasks on their own clocks — with text-to-speech audio, writing pads that save your draft, and self-recording.
Tense drills
Present tense, every family
Regular verbs and every irregular family of the present, all 91 verbs.
Presente Drill · Unit 2Preterite & imperfect
The two past tenses side by side, so the forms are automatic before you choose between them.
Past tenses Drill · Unit 2Future & conditional
The irregular stems, in both tenses at once.
Irregular stems Drill · Unit 2Mixed indicative
All five simple indicative tenses across all 91 verbs, mixed.
IndicativeReview Drill · Unit 3Compound tenses, two at a time
Perfect and pluperfect first, then future and conditional perfect with the irregular participles.
Perfect tenses Drill · Unit 3Mixed compound tenses
All five compound indicative tenses at random — name the tense of haber first.
Perfect tensesReview Drill · Unit 4Present subjunctive
The present subjunctive forms, drilled until they are automatic.
Subjunctive Drill · Unit 4Imperfect subjunctive
Both the -ra and the -se forms, behind si-clauses and the sequence of tenses.
Subjunctive Drill · Unit 4Compound subjunctive
Perfect and pluperfect subjunctive with haya and hubiera.
Subjunctive Drill · Unit 4Commands
Affirmative and negative commands.
Imperative Drill · Unit 5Irregular verbs · mixed review
Irregular verbs in the seven tenses you use most in writing, shuffled.
ReviewListening & writing
Listening sources
Two audio passages read aloud by text-to-speech, with questions, answers and a hidden transcript.
Text-to-speechPart B Timed · Unit 6Timed email replies
Two practice emails, fifteen minutes each, in a pad that saves your draft.
Task 1Timer Timed · Unit 6Timed essay with three sources
The full argumentative essay on the exam’s own clock, then the planning notes and an annotated model.
Task 2Timer Timed · Unit 6Timed essay practice
A second essay task: read, listen to the audio, then forty minutes to write.
Task 2AudioSpeaking
Conversation simulator
Five 20-second turns with a partner that talks back, on two worked conversations.
Task 3Audio Speaking · Unit 7Single-turn speaking bank
One 20-second turn at a time, recorded, to drill each conversational function on its own.
Task 3Recorder Speaking · Unit 7Practice conversations
Two more conversations to run cold in the simulator.
Task 3 Speaking · Unit 8Cultural comparison timer & recorder
Six prompts, one per theme: four minutes to prepare, two to present, and a recording to play back.
Task 4RecorderOne lab per unit, from charges to resonance
Fields you can probe, surfaces you can drag, circuits you can scope. Each lab pairs with a unit of the Physics II course.
Fields of continuous charge
Chop a charged rod, ring or disk into pieces, watch each piece’s \(d\mathbf{E}\) add up at a probe, and compare with the exact formula.
SuperpositionRod, ring, disk Unit 2 labGauss’s law: flux through any surface
Drag charges and a Gaussian sphere or cube; the flux, integrated over the whole closed surface, always equals \(Q_{\text{enc}}/\varepsilon_0\).
Electric fluxSphere vs cube Unit 3 labThe potential landscape
Orbit a 3-D surface of \(V(x,y)\) beside its contour map and see \(\mathbf{E} = -\nabla V\) point downhill, across the equipotentials.
3-D surfaceE = −∇V Unit 4 labDielectrics & energy density
Slide a dielectric slab into a capacitor, connected or isolated, and follow charge, field, energy density and the pull on the slab.
DielectricsEnergy density Unit 5 labRC circuit on an oscilloscope
Drive an RC circuit with a square or sine wave and read \(V_C\) and \(V_R\) off a scope — a low-pass and a high-pass filter in one.
OscilloscopeRC filter Unit 6 labCharged particles in magnetic fields
Fire an electron, proton or alpha into \(\mathbf{B}\) (and \(\mathbf{E}\)) in 3-D: circles, helices, \(\mathbf{E}\times\mathbf{B}\) drift and a velocity selector.
Lorentz forceCyclotron motion Unit 7 labMagnetic fields of currents
Wires, loops and solenoids with the field summed piece by piece (Biot–Savart), a probe, and an Ampère loop that checks \(\oint\mathbf{B}\cdot d\mathbf{l} = \mu_0 I_{\text{enc}}\).
Biot–SavartAmpère’s law Unit 8 labFaraday’s law: generators & moving magnets
A magnet through a coil, a rotating-coil generator and a rod on rails, with flux and EMF plotted live and Lenz’s law shown.
Lenz’s lawAC generator Unit 9 labSeries RLC: resonance & phasors
Rotating phasors, time traces and a resonance curve with \(f_0\), the half-power band and the live operating point.
ResonancePhasorsComing soon: labs for Calculus II and for AP Physics 2 Units 4–7.
Ideal gas & PV work
The box on the left holds a fixed amount of monatomic gas (n = 0.10 mol of argon). Move the piston or change the temperature and watch the state point travel across the PV diagram on the right. Pick a process first and the simulation will hold the right quantity constant for you.
Particle speed scales with √T; the piston sets the volume. Colour runs blue (slow) to orange (fast).
Faint curves are isotherms. The dashed one passes through your current state. The orange trail is the path you have taken.
These three accumulate from the moment you last pressed Reset trace, and they always satisfy ΔU = Q + W. Work is integrated numerically as you drag, so it is a real −∫P dV, not a formula for one special case.
- Pick Isothermal and compress. ΔU stays at 0 and Q comes out equal and opposite to W — the gas passes the energy straight through.
- Pick Adiabatic and compress. Q stays 0 and the temperature climbs on its own. That is a diesel engine.
- Run Isochoric: the volume slider locks, no area is swept, and W stays exactly 0.
- Make a closed loop — isobaric out, isochoric down, isobaric back, isochoric up — and check that ΔU returns to 0 while W does not.
Thermal conductivity
A slab bridges a hot and a cold reservoir. The steady-state transfer rate is P = kAΔT/L — proportional to conductivity, area and temperature difference, and inversely proportional to thickness.
Dot speed and count scale with the transfer rate.
- Switch copper to fibreglass with everything else fixed. The rate drops by a factor of about 10 000 — that whole range is why insulation works at all.
- Double the thickness and the rate halves; double the area and it doubles. Thickness and area are equally strong levers, in opposite directions.
- Still air conducts worse than wood. Most insulation is mostly air — the fibres exist to stop it convecting.
Entropy
Move a fixed amount of heat between two reservoirs and watch the entropy budget. The hot side loses Q/TH, the cold side gains Q/TC, and because TC is the smaller denominator the total comes out positive — only in the hot → cold direction.
Bars above the axis are entropy gained, below it lost.
Why it happens: ways to arrange 60 particles between two halves of a box. The marker is your split.
- Switch to cold → hot. Energy is still perfectly conserved — the first law cannot tell the two directions apart. Only the sign of ΔSuniverse rules one out.
- Bring the two temperatures close together. ΔSuniverse shrinks toward zero: a transfer across a vanishing temperature difference is reversible.
- Drag the particle split to 0 or 60. Ω falls to 1 — exactly one arrangement, the lowest possible entropy, and the reason gas never spontaneously crowds into one half.
Heat transfer & calorimetry
Drop two samples into an insulated container. No energy leaves, so ΣQ = 0 and the mixture settles wherever the two mcΔT terms cancel.
Bar height and colour track temperature; bar width tracks heat capacity mc.
No phase changes. If a real mixture would cross 0 °C or 100 °C the answer here is wrong, because latent heat absorbs energy at constant temperature — see the latent heat section. The container is also treated as having zero heat capacity.
- Equal masses of water and copper. The final temperature lands far closer to the water’s start, because water’s c is about 11× larger — it dominates the average.
- Watch ΣQ. It stays at zero no matter what you change; that is the calorimetry equation.
- Lead against water is the most lopsided pairing here: c = 128 against 4186.
Boyle’s law and work from a PV curve
Measure how the pressure of a trapped gas depends on its volume, linearize the result to prove it is a genuine inverse relationship, then integrate your own data to find the work done compressing it. One afternoon, one syringe, and every idea in the unit shows up.
~60 minutes · equipment: minimalContents
Research question
For a fixed quantity of gas held at constant temperature, how does absolute pressure depend on volume — and how much work is required to compress it?
Hypothesis to test: P ∝ 1/V, so a graph of P against 1/V should be a straight line through the origin with slope nRT.
Theory
Starting from PV = nRT, hold n and T fixed and the right-hand side is a constant:
A curved graph is weak evidence: many different relationships produce curves that look alike. Linearizing is the whole method. If P vs 1/V comes out straight, the inverse relationship is confirmed; if it bends, it is not.
The work done on the gas is the area under the PV curve:
You will compute this two ways — numerically from your measured points, and analytically from the formula — and see whether they agree. That comparison is the real payoff of the lab.
Materials
Two versions. Do whichever your equipment allows; the analysis is identical.
Version A — with a pressure sensor (preferred)
- 60 mL plastic syringe with a Luer fitting
- Gas pressure sensor (Vernier, PASCO, or equivalent) with short tubing
- Data logger, tablet, or laptop
- Thermometer for ambient temperature
- Ruler or the syringe’s own graduations
Version B — no sensor, using known masses
- Syringe mounted vertically, nozzle sealed with a cap or plug
- Set of slotted masses (0.5–5 kg total) and a platform that rests on the plunger
- Calipers to measure the plunger diameter (you need the area A)
- Vacuum grease or a drop of oil to reduce plunger friction
In version B, pressure is not measured — it is computed from the force balance on the plunger:
Safety
- Do not compress below about 1/4 of the starting volume. Pressure climbs steeply and a plastic syringe can crack or a fitting can blow off.
- Keep a hand on the plunger at all times when compressed — a released plunger fires outward.
- Never point the nozzle at anyone, and wear eye protection while compressing.
- In version B, load masses gently and centered; an off-center stack tips.
Procedure
- Record the ambient temperature and, if you have a barometer or a weather app, the local atmospheric pressure. Convert the temperature to kelvin immediately so it is not forgotten later.
- Draw the plunger to 30.0 mL with the syringe open, then connect it to the sensor (version A) or cap it (version B). The gas is now sealed.
- With the plunger at rest, record the starting pressure. It should be close to atmospheric — if it is not, your seal is leaking. Fix that before continuing.
- Compress to the next volume on your list. Hold it steady and wait 10–15 seconds before recording the pressure. See the callout below — this step is the difference between a good data set and a bad one.
- Record pressure and volume. Repeat for volumes of 25, 20, 17.5, 15, 12.5, and 10 mL.
- Now reverse: let the plunger back out through the same volumes, recording pressure again. Comparing the two sweeps reveals friction and leaks.
- Repeat the entire run three times and average. If run 3 reads systematically lower than run 1 at every volume, you have a slow leak.
Compressing a gas quickly is adiabatic, not isothermal — the gas heats up and reads high, exactly as described on the first law page. Waiting 10–15 seconds lets that extra energy leak out through the syringe walls so the gas returns to room temperature. Skip the wait and your points will sit systematically above the true isotherm, and the run will not linearize cleanly.
That failure mode is itself a nice observation: watch the pressure reading drift downward for a few seconds after each compression. You are watching a process go from adiabatic to isothermal in real time.
Data table
Print this page or copy the table. Absolute pressure, not gauge.
Ambient temperature: ________ °C = ________ K Atmospheric pressure: ________ kPa
| V (mL) | 1/V (mL−1) | P run 1 (kPa) | P run 2 (kPa) | P run 3 (kPa) | P avg (kPa) | PV (kPa·mL) |
|---|---|---|---|---|---|---|
| 30.0 | 0.0333 | |||||
| 25.0 | 0.0400 | |||||
| 20.0 | 0.0500 | |||||
| 17.5 | 0.0571 | |||||
| 15.0 | 0.0667 | |||||
| 12.5 | 0.0800 | |||||
| 10.0 | 0.1000 |
Analysis
1. The raw PV curve
Plot P (vertical) against V (horizontal). You should get a hyperbola falling to the right — the isotherm from the graph gallery, this time made of your own measurements.
2. Linearize
Plot P against 1/V and fit a straight line. Report the slope with units and the vertical intercept.
- Straight line ⇒ P ∝ 1/V confirmed.
- Slope = nRT, in kPa·mL if you kept those units.
- Intercept should be zero. A noticeably positive one is a real signal, not noise — see part 4.
3. Extract the amount of gas
Convert the slope to SI (1 kPa·mL = 10−3 J) and solve:
Check it against the direct calculation n = PV/RT using your starting state. The two should agree closely — if they do not, suspect the temperature or a unit conversion.
4. Find the dead volume
The syringe graduations do not include the gas sitting in the nozzle, tubing, and sensor cavity. Calling that extra volume Vd, the true relation is
which is why a plot against 1/Vread shows a small positive intercept and a slight bend. To measure Vd, try adding a trial value to every volume and re-plotting; the value that makes the line straightest and drives the intercept to zero is your dead volume. A few tenths of a millilitre up to a couple of millilitres is typical.
5. Work from the area — numerically
Use the trapezoidal rule on your own P–V points. For consecutive points,
Compute the total for the compression from 30.0 mL down to 10.0 mL. Since the gas is being compressed, Won is positive and equals that area.
Because the curve is convex (it bends upward), the trapezoidal rule overestimates the true area — each straight chord sits above the curve. With seven points the error is small, but it is real and it is systematic, so it belongs in your error discussion rather than being hidden in “random uncertainty.” Taking more, closer-spaced points at the high-pressure end, where the curve bends most, shrinks it fastest.
6. Work from the formula — analytically
Compare your numerical area to the isothermal prediction, using the nRT you got from the slope:
Report the percent difference between the two methods.
Sample data & worked analysis
Use this to practice the analysis before you have your own data — or to check your spreadsheet is doing what you think. Taken at 22 °C (295 K).
| V (mL) | 1/V (mL−1) | P (kPa) | PV (kPa·mL) |
|---|---|---|---|
| 30.0 | 0.0333 | 68.5 | 2055 |
| 25.0 | 0.0400 | 81.7 | 2043 |
| 20.0 | 0.0500 | 101.6 | 2032 |
| 17.5 | 0.0571 | 114.5 | 2004 |
| 15.0 | 0.0667 | 133.1 | 1997 |
| 12.5 | 0.0800 | 156.2 | 1953 |
| 10.0 | 0.1000 | 192.4 | 1924 |
Worked analysis of the sample data
Slope. Using the first and last points:
Converting: 1857 kPa·mL = 1.857 J. (Two-point slopes are crude — use a least-squares fit on the real thing.)
Amount of gas.
Dead volume. The data are fit well by
With the dead volume included the corrected slope is 2148 kPa·mL, giving n = 8.8×10−4 mol — about 15% higher than the uncorrected value. Systematic errors matter.
Work, numerically. Trapezoids from 10.0 to 30.0 mL:
10.0→12.5: ½(192.4+156.2)(2.5) = 435.8
12.5→15.0: ½(156.2+133.1)(2.5) = 361.6
15.0→17.5: ½(133.1+114.5)(2.5) = 309.5
17.5→20.0: ½(114.5+101.6)(2.5) = 270.1
20.0→25.0: ½(101.6+ 81.7)(5.0) = 458.3
25.0→30.0: ½( 81.7+ 68.5)(5.0) = 375.5
total = 2210.8 kPa·mL = 2.21 J
So compressing from 30.0 mL to 10.0 mL requires Won = +2.21 J.
Work, analytically. Using the dead-volume-corrected constant:
Percent difference: 0.5%. The numerical result is slightly higher, exactly as the convexity argument predicts. Two independent methods agreeing to half a percent is a strong result — and the direction of the small disagreement is itself explained by the mathematics, which is better than agreement alone.
For scale: 2.2 J is roughly the work of lifting a 250 g apple one metre. You can feel it in your hand as you push the plunger.
Error analysis
Separate the two kinds — AP rubrics award credit for knowing the difference.
| Source | Type | Effect & fix |
|---|---|---|
| Dead volume in tubing and nozzle | Systematic | Every measured V is too small, so PV drifts. Fix by fitting Vd as in part 4, or by using the shortest possible tubing. |
| Compressing too fast (adiabatic heating) | Systematic | Pressures read high; the curve is steeper than the true isotherm. Fix by waiting for equilibrium at every point. |
| Plunger friction | Systematic, direction-dependent | Makes compression readings high and expansion readings low — which is why the two sweeps disagree. Average them, or lubricate the plunger. |
| Slow leak past the seal | Systematic, grows with time | Later runs read low at every volume. Detect by comparing run 1 with run 3; fix the seal rather than averaging it away. |
| Reading the graduations | Random | ±0.25 mL is typical, so it is worst at small volumes — 2.5% at 10 mL versus 0.8% at 30 mL. Repeat and average. |
| Room temperature drift | Random / systematic | nRT is not quite constant across a long session. Record T at the start and end. |
| Trapezoidal approximation | Systematic | Overestimates the area for a convex curve. Shrink it with more points where the curvature is greatest. |
Notice that every systematic error above has a known sign. “Human error” earns nothing on a rubric; “dead volume makes every recorded volume too small, which lowers the apparent PV product most at small volumes” earns full credit. Always state the direction of an error, not just its existence.
Conclusion questions
- Does your P vs 1/V graph support the hypothesis? Cite the shape and the intercept, not just “it looked straight.”
- Your PV column probably drifts in one direction. Which direction, and which systematic error explains that specific direction?
- The gas got warmer as you compressed it, yet you analyzed the data as isothermal. Justify that, referring to what you did in the procedure.
- Using the first law, state the sign of Q for the compression. (You did positive work on the gas and its temperature ended unchanged — so where did the energy go?)
- Sketch your compression on a PV diagram and shade the region whose area you computed. Which page’s gallery figure does it match?
- If you repeated the lab with the syringe in an ice bath at 0 °C, how would the slope of your linearized graph change? By what factor, quantitatively?
- Estimate how much your result would change if the dead volume were twice what you measured. Is this experiment more sensitive to the dead volume or to your reading uncertainty?
Extensions
- Catch the adiabat. Compress the syringe as fast as you can while logging at a high sample rate, then hold. Plot the fast compression and the settled points on the same axes. The fast curve is steeper — you have measured an adiabatic process and an isothermal one on the same apparatus, which is precisely the comparison figure from the notes.
- Charles’s law. Keep the plunger free to move (constant pressure) and put the syringe in water baths at several temperatures. Plot V vs T in kelvin; extrapolate the line to V = 0 and you get an estimate of absolute zero.
- Find kB. Combine your n from the slope with Avogadro’s number to get kB = R/NA, and compare to the accepted value.
- Round trip. Compress, then expand back along a different route by changing the temperature partway. Compute the enclosed area — you have built a (very inefficient) heat engine, and its net work is the loop area from the second law page.
Theory for this lab: Unit 1 · PV diagrams →
Coulomb force & superposition
Drag the point charges around and set their sizes with the sliders. The simulation draws every individual Coulomb force on the charge you pick (dashed) and their vector sum (solid). Each pair obeys F = k|q1q2|/r2 on its own; the other charges change nothing about it. The net force is just the vectors added tip to tail.
Drag any charge. Grid squares are 5 cm. Arrow colour matches the charge that exerts the force (orange +, blue −); the faint arrow drawn from the first tip shows the tip-to-tail sum.
Directions are counter-clockwise from +x (right). Arrow lengths are to scale with one another; the scale rescales so the longest arrow stays readable.
- With two like charges, drag one so the separation doubles. The force drops to a quarter, not a half — that is the inverse square.
- Make q₁ three times bigger than q₂ and switch the test charge between them. The two forces are always equal in size and opposite in direction: Newton’s third law does not care which charge is bigger.
- In three in a line, flip q₃ to positive. The two pushes on the middle charge now oppose each other, and the net force is zero exactly halfway between equal charges.
- In the triangle, the vertical components cancel and the net force on q₃ points parallel to the line from q₁ to q₂. Drag q₃ off the axis of symmetry and watch the cancellation break.
Theory for this lab: Unit 2 · Coulomb’s law →
Field lines & equipotentials
The electric field and the electric potential are two pictures of the same charges. Field lines start on positive charge and end on negative charge; equipotential lines join points at the same V = Σkq/r. Wherever they meet they cross at right angles, and where the equipotentials bunch together the field is strong, because |E| ≈ |ΔV/Δs|.
Drag a charge to move it (that also selects it for the slider below), or drag the green probe — tap empty space to drop the probe there. Orange contours are positive V, blue negative, dashed grey V = 0. The map is 80 cm wide.
Field direction is counter-clockwise from +x. Field lines are drawn in proportion to charge (6 per nC), so line density tracks field strength.
- Slide the probe along one equipotential of the dipole. V stays fixed while the field direction keeps turning — it is always perpendicular to the contour you are on.
- Put the probe at the centre of the dipole. V = 0 there but E is large. Then try the centre of two like charges: now E = 0 but V is not. Zero potential and zero field are different things.
- Between the two rows, the contours are nearly evenly spaced and parallel and E barely changes as you move the probe: a uniform field, with E = ΔV/d.
- Move the probe directly along a field line and watch V. It always falls in the direction the field points.
Theory for this lab: Unit 2 · Electric potential →
Charged particle between plates
Two parallel plates with a potential difference ΔV make a uniform field E = ΔV/d between them. A particle that enters horizontally feels a constant force qE straight across the gap and none along it, so it follows a parabola — exactly like a projectile, with qE/m in place of g.
Drawn to true scale (the faint marks under the plates are centimetres). Small arrows between the plates show the direction of E. Outside the plates there is no field, so the particle leaves in a straight line.
The speed slider covers 0.5–5×10⁷ m/s for the electron and 0.5–5×10⁵ m/s for the proton. Gravity is ignored — at the default settings it is about 10¹⁴ times weaker than the electric force on the electron and 10¹¹ times weaker on the proton.
- Switch electron to proton without touching anything else. The proton bends the other way — opposite charge, so qE flips — and its acceleration is about 1830× smaller because it is that much heavier.
- Flip the plate polarity. The field reverses, and so does the deflection of whichever particle you have chosen.
- Double v₀. The time in the plates halves, so the deflection drops to a quarter: y = ½a(L/v₀)².
- Keep ΔV fixed and halve d. E doubles, so the deflection doubles — and the plates are now closer, so the particle is far more likely to hit one.
Theory for this lab: Unit 2 · Electric field →
Parallel-plate capacitor
Geometry alone sets the capacitance: C = κε0A/d. What happens to Q, ΔV, E and the stored energy when you change that geometry depends on one question: is the battery still connected? Connected, the battery holds ΔV fixed. Disconnected, the charge has nowhere to go, so Q is fixed.
The green readout is the quantity being held fixed. Plate gap and plate width are drawn on different scales so a 1 mm gap stays visible; field-line spacing is inversely proportional to E.
- Connected, double d. C, Q, E and U all halve; ΔV cannot move because the battery pins it.
- Switch to isolated and double d. Now Q is stuck, so ΔV = Q/C doubles, E does not change at all, and U doubles — the extra energy is the work you did pulling the attracting plates apart.
- Isolated, raise κ to 2. ΔV, E and U all halve: the dielectric’s bound charge partly cancels the field. Connected, the same change doubles Q and U instead.
- Charge it, disconnect, then move the battery slider. The capacitor ignores it — it no longer knows the battery exists. Reconnect and charge flows until ΔV matches the battery again.
Theory for this lab: Unit 2 · Capacitors →
Mapping equipotentials and field lines
You cannot see an electric field, but you can measure potential with an ordinary voltmeter. Paint two electrodes onto conductive paper, hunt for points that read the same voltage, and the invisible field draws itself: equipotentials first, field lines at right angles to them, and the field strength from how closely the lines are packed.
~60 minutes · equipment: conductive paper, silver ink, DC supply, voltmeterContents
Research question
What do the equipotentials and field lines look like between two charged electrodes, and does the field between two parallel bars have the uniform magnitude |E| = ΔV/d?
Hypothesis to test: between long parallel electrodes the equipotentials are straight, parallel and evenly spaced, so the potential rises linearly with distance from the negative electrode, with slope equal to the field magnitude.
Theory
An equipotential is a line (in 3-D, a surface) on which every point has the same electric potential. Moving a charge along one takes no work, since W = −qΔV = 0. That forces the field to have no component along the equipotential, so:
- Field lines cross equipotentials at right angles.
- The field points from high potential toward low potential.
- Crowded equipotentials mean a strong field, because the same ΔV is dropped over a shorter distance.
The magnitude of the field is the rate at which the potential changes with distance:
Why conductive paper works. The paper is a weak conductor, so the supply drives a small steady current through it. Inside the paper that current flows along the field lines, and the potential obeys the same equation it would in empty space around the same electrodes (in two dimensions). The paper gives the voltmeter something to touch: a map of V on the paper is a map of the field’s potential.
Materials
- Conductive (carbon-loaded) paper, about 20 cm × 28 cm — ideally with a printed 1 cm grid
- Silver conductive-ink pen for drawing electrodes
- Corkboard or foam board, and metal push pins
- DC power supply, 6–12 V (or a 9 V battery)
- Digital multimeter on the DC volts setting, with a fine-tipped probe
- Connecting leads with alligator clips
- Ruler, and a sheet of ordinary grid paper for recording the map
Safety
- The voltages are low, but never connect the supply leads directly to each other — a short can overheat leads and damage the supply. Always connect through the electrodes.
- Let the silver ink dry completely (at least 15–20 minutes) before powering. Work in a ventilated room and keep the ink off skin.
- Push pins are sharp; press them in with a thumb guard or the back of a ruler.
- Turn the supply off before rearranging any connection.
Procedure
- Draw two straight, parallel bar electrodes 12.0 cm long and 10.0 cm apart in the middle of the conductive paper. Make each line thick, unbroken and evenly inked — gaps and thin patches become extra resistance. Let it dry.
- Pin the paper to the board. Push a metal pin through each electrode and clip a lead to each pin. Connect the leads to the supply and set it to about 10 V.
- Clip the voltmeter’s COM lead to the negative electrode. Touch the probe to the positive electrode and record the reading as ΔVsupply. Touch it to the negative electrode: it should read 0.00 V.
- Center line. Along the line midway between the bar ends (y = 0), record V every 1.0 cm from x = 0 (on the 0 V bar) to x = 10.0 cm (on the positive bar).
- Equipotentials. For each target voltage — 2.00, 4.00, 6.00 and 8.00 V — slide the probe along the lines y = −3.0, 0 and +3.0 cm until the meter reads the target. Record each x. Then find a few more points of each equipotential beyond the ends of the bars (for example y = ±7 cm and ±9 cm) to see how the lines curve.
- Transfer every point to grid paper, with the electrodes drawn in. Join points of equal voltage with a smooth curve and label it.
- Field lines. Starting on the positive electrode, draw lines that cross every equipotential at a right angle and end on the negative electrode. Add arrows pointing from high to low potential.
Pencil graphite conducts. Marking a grid on the conductive paper adds stray conducting paths that bend your equipotentials. Use the paper’s printed grid, or measure positions with a ruler and record them on a separate sheet.
Also, touch the probe lightly. Pressing hard can tear the coating, and a torn spot is an insulating hole that distorts everything around it.
Data table
Supply voltage across electrodes: ________ V Electrode separation d: ________ cm
| x (cm) | V (V) | x (cm) | V (V) |
|---|---|---|---|
| 0.0 | 6.0 | ||
| 1.0 | 7.0 | ||
| 2.0 | 8.0 | ||
| 3.0 | 9.0 | ||
| 4.0 | 10.0 | ||
| 5.0 |
| Target V | x at y = −3.0 cm | x at y = 0 | x at y = +3.0 cm | Spacing to next line (cm) |
|---|---|---|---|---|
| 2.00 V | ||||
| 4.00 V | ||||
| 6.00 V | ||||
| 8.00 V | — |
Analysis
1. The map
Look at your finished drawing. Between the bars, are the equipotentials straight, parallel to the electrodes, and evenly spaced? Where do they start to curve, and which way? Do your field lines meet both electrodes at right angles? (They should — each electrode is itself an equipotential.)
2. Potential vs. position
Plot Table 1 as V (vertical) against x (horizontal). Fit a straight line to the points between the electrodes, leaving out the two points measured on the silver itself. A straight line means the field is uniform.
3. Compare with the parallel-plate prediction
Compute ΔVsupply/d and the percent difference from your slope. Decide whether any gap is random scatter or a systematic effect — and if systematic, which way it points.
4. Field from equipotential spacing
The same field can be read straight off the map. Adjacent equipotentials in Table 2 differ by 2.00 V, so for each gap:
Sample data & worked analysis
Use this to practice before you have your own data. Supply set to 10.0 V; electrodes 10.0 cm apart, 12.0 cm long.
| x (cm) | V (V) | x (cm) | V (V) |
|---|---|---|---|
| 0.0 | 0.00 | 6.0 | 5.93 |
| 1.0 | 1.33 | 7.0 | 6.84 |
| 2.0 | 2.24 | 8.0 | 7.77 |
| 3.0 | 3.18 | 9.0 | 8.68 |
| 4.0 | 4.09 | 10.0 | 10.00 |
| 5.0 | 5.01 |
| Target V | y = −3.0 cm | y = 0 | y = +3.0 cm | Spacing at y = 0 (cm) |
|---|---|---|---|---|
| 2.00 V | 1.73 | 1.74 | 1.76 | 2.16 |
| 4.00 V | 3.91 | 3.90 | 3.89 | 2.18 |
| 6.00 V | 6.07 | 6.08 | 6.09 | 2.17 |
| 8.00 V | 8.26 | 8.25 | 8.24 | — |
Worked analysis of the sample data
Slope (two-point check). Using the outermost interior points, x = 1.0 and 9.0 cm:
Least-squares fit to the nine interior points gives the same slope, 0.919 V/cm, with intercept 0.41 V. Every interior point lies within about 0.01 V of the fitted line — the potential really is linear in x.
Parallel-plate prediction.
Where did the missing voltage go? Extend the fitted line to the electrodes: at x = 0 it gives 0.41 V, and at x = 10.0 cm it gives 0.41 + 0.919 × 10.0 = 9.60 V. So of the 10.0 V supplied, only 9.60 − 0.41 = 9.19 V is actually dropped across the paper between the bars; about 0.4 V is lost at each electrode, in the contact resistance between the silver ink and the carbon coating. Using the voltage that is really across the paper:
Field from the equipotential spacing (Sample Table 2, y = 0):
2.00→4.00 V: 2.00 V / 0.0216 m = 92.6 V/m
4.00→6.00 V: 2.00 V / 0.0218 m = 91.7 V/m
6.00→8.00 V: 2.00 V / 0.0217 m = 92.2 V/m
mean = 92.2 V/m
Agreement with the slope method to within 0.3%, as it should be: they are the same measurement read two ways. And the spacings being equal is itself the evidence of uniformity.
For scale: a proton released in a vacuum field of 91.9 V/m would accelerate at a = eE/mp = (1.60×10−19)(91.9)/(1.67×10−27) = 8.8×109 m/s2 — nearly a billion g, from a field made with a 10 V supply.
Error analysis
Separate the two kinds, and give each systematic error a direction.
| Source | Type | Effect & fix |
|---|---|---|
| Contact resistance at the ink–paper boundary | Systematic | Part of the supply voltage is dropped at the electrodes, so the field across the paper is lower than ΔVsupply/d. Fix: compare with the voltage measured just inside each electrode, or ink the electrodes more heavily. |
| Finite electrode length (edge effects) | Systematic, position-dependent | Near the ends of the bars the equipotentials curve and the field weakens. Measure the uniform field only in the middle region. |
| Non-uniform paper coating | Random across the sheet | Small wiggles in the equipotentials. Repeat on a fresh sheet; average. |
| Probe position | Random | ±1 mm is typical; at 0.92 V/cm that is ±0.09 V, far larger than the meter’s 0.01 V resolution. Use the printed grid and a sharp probe. |
| Electrodes not straight or not parallel | Systematic | Equipotentials tilt and spacings vary along y. Draw the bars against a ruler and measure d at both ends. |
| Voltmeter loading | Systematic, negligible | A digital meter draws almost no current (input resistance ~10 MΩ, far above the paper’s), so it barely disturbs the potentials it measures. |
| Supply drift | Random / systematic | Recheck the electrode voltage at the start and end of the session. |
“The field was lower than expected because of error” earns nothing. “The fitted line does not reach the electrode potentials, so roughly 0.8 V is dropped at the contacts; this lowers the measured field by about 8%, which accounts for the whole discrepancy” earns full credit. Name the effect, give its direction, and check that its size matches.
Conclusion questions
- Explain, using the work done moving a charge along an equipotential, why field lines must cross equipotentials at right angles.
- Where on your map is the field strongest, and where weakest? How can you tell from the equipotentials alone, without drawing a single field line?
- Does your V vs x graph support a uniform field? Cite the shape, the residuals, and the equipotential spacings.
- Your slope and ΔVsupply/d probably disagree. Which is larger, and which systematic error explains that specific direction?
- If this were a vacuum gap with the same potentials, how much work would the field do on a proton moving from the 8.00 V equipotential to the 2.00 V equipotential? Give the answer in joules and in electron-volts. Would it be different for an electron, and how?
- Why is a voltmeter (and not an ammeter) the right instrument for this mapping, and why must it draw very little current?
- Predict how your map would change if the supply were raised to 12 V. Which quantities change, and which stay the same?
Extensions
- A “dipole.” On a fresh sheet, paint two small filled circles 10 cm apart as point-like electrodes. Map the 2, 4, 5, 6 and 8 V equipotentials and compare with the field-line pattern of two opposite charges on the electric field page. The 5 V line should be the perpendicular bisector — and the equipotentials should crowd near each electrode, where the field is strongest.
- Shielding. Paint a closed ring electrode with a small dot electrode outside it, and connect the supply between them. Probe inside the ring: every point reads the same voltage as the ring, so the field inside is zero — the conductor-in-equilibrium result from the conductors & capacitors page.
- Field vs. voltage. Repeat the center-line measurement at 4, 6, 8, 10 and 12 V. Plot the slope against the supply voltage: it should be a straight line through the origin, |E| ∝ ΔV for fixed d.
- Compare with the simulation. Set up the same electrode geometry in the field & equipotential map and lay your hand-drawn map beside it.
Theory for this lab: Unit 2 · Electric potential →
Ohm’s law & resistivity
A uniform wire is connected across a fixed potential difference. Its resistance comes only from what it is made of and its shape, R = ρL/A; the current then follows from I = ΔV/R. Change the material, the length or the thickness and watch the I–V line on the right tilt.
Drawn length and thickness follow the sliders. Electrons drift toward the + terminal, against the conventional current; their speed is log-scaled so that both microamps and kiloamps stay visible.
An ohmic wire gives a straight line through the origin with slope 1/R. The current axis rescales itself, so read the tick labels.
Resistivities are textbook values at 20 °C. The source is ideal, so a short, fat copper wire draws absurd currents here — a real supply (with internal resistance) could not deliver them, and the wire would heat up, raising ρ.
- Double the length: R doubles and I halves. Double the diameter: the area goes up 4×, so R drops to a quarter.
- Swap copper for nichrome with the same shape. R rises about 65× — that is why heating elements are nichrome and house wiring is copper.
- Move only the ΔV slider. The operating point slides along a fixed line: R does not depend on ΔV or I for an ohmic conductor.
- Watch the power: at fixed ΔV, P = (ΔV)²/R, so the lower-resistance wire dissipates more.
Theory for this lab: Unit 3 · Current & resistance →
Series vs parallel bulbs
Three bulbs, one ideal battery, four ways to wire them. Brightness tracks the power each bulb dissipates, P = IΔV. Pull a bulb out of its socket and see which of the others go dark, which get dimmer and which get brighter.
Glow follows each bulb’s power; dot speed is proportional to the branch current, so at every junction the dots coming in match the dots going out. Bulbs are treated as fixed (ohmic) resistors.
| Bulb | R | ΔV | I | P |
|---|---|---|---|---|
| 1 | — | — | — | — |
| 2 | — | — | — | — |
| 3 | — | — | — | — |
For a removed bulb, ΔV is the voltage across its empty socket (what a voltmeter across the gap would read). It shows “—” when the gap is cut off from the battery on both sides and the reading is undefined.
- Set all three resistances equal and compare series with parallel. Each parallel bulb gets the full emf, so it dissipates 9× the power of a series bulb.
- In series, remove any bulb. Every bulb goes out, and the empty socket reads the full emf — the whole battery voltage appears across the gap.
- Pick R1 + (R2 ∥ R3) and remove bulb 3. Req rises, bulb 1 dims, yet bulb 2 gets brighter: it no longer shares the current with bulb 3.
- In parallel, removing a bulb changes nothing for the others (ideal battery), but the battery current drops.
Theory for this lab: Unit 3 · Series & parallel →
Two-loop circuit solver
Two batteries, three resistors, two junctions: the circuit that cannot be reduced to series and parallel pieces. The simulation solves it exactly and then checks its own answer with Kirchhoff’s junction rule and both loop rules, using the actual numbers.
Arrows point the way each current actually flows; thickness is proportional to |I|. Reference directions for the signs: I1 up the left branch, I2 up the right branch, I3 down the middle — a negative value means the arrow has turned round.
Solved by nodal analysis: with V = VA − VB, the junction rule at A reads (±ε1 − V)/R1 + (±ε2 − V)/R2 = V/R3, one equation in one unknown. A negative “delivers” power means that battery is being charged.
- With the defaults, I2 comes out negative: battery 2 is being pushed backwards and absorbs power. Raise ε2 until I2 crosses zero.
- Flip ε2 so the batteries oppose each other around the outer loop. Watch I3 shrink and possibly reverse.
- Set ε1 = ε2 and R1 = R2: by symmetry I1 = I2 = I3/2.
- Make R3 large. The middle branch starves and the circuit becomes one loop with the two batteries in series.
Theory for this lab: Unit 3 · Kirchhoff’s rules →
RC charging & discharging
Throw the switch to connect the capacitor to the battery through a resistor, then throw it the other way to let the capacitor drain through the same resistor. Everything happens on the time scale τ = RC: after one τ the capacitor has gone 63% of the way to where it is heading.
Faint curves are the full prediction for this run; the bold part is the time elapsed. Playback is scaled so one time constant always lasts about 1.5 s on screen — the t readout is the real circuit time. Current is positive when it flows onto the top (+) plate.
—
- Press Charge and read the curves at the τ marker: VC is at 63% of ε and the current has fallen to 37% of its starting value ε/R. By 5τ it is over 99% done.
- At t = 0 the uncharged capacitor acts like a plain wire (all of ε across R); at the end it acts like a break (no current, all of ε across C).
- Press Discharge half-way through a charge. It drains from wherever it got to, and the current runs the other way.
- Double R or double C: τ doubles either way. Only C (and ε) change the final charge and energy; R only changes how long it takes.
Theory for this lab: Unit 3 · RC circuits →
Ohm’s law and the resistivity of a wire
Stretch a length of nichrome wire along a metre rule, push a current through it, and measure the voltage across different lengths. First show the wire obeys Ohm’s law, then turn the slope of a straight-line graph into the resistivity of the alloy — a material constant you can check against a table.
~60 minutes · equipment: standard electricity kit + micrometerContents
Research question
Is a nichrome wire ohmic, and what is the resistivity of nichrome?
Hypotheses to test: (A) at fixed length, ΔV ∝ I, so a graph of ΔV against I is a straight line through the origin; (B) at fixed current, R ∝ L, so a graph of R against L is a straight line whose slope is ρ/A.
Theory
For any conductor, resistance is defined by
For a uniform wire, resistance depends on its geometry and its material:
Using the slope rather than a single R/L value is the point of the method: any constant offset — a contact that sits a few millimetres off the zero mark, for instance — shifts the line up or down but leaves the slope alone.
Nichrome is chosen deliberately. Its resistivity is high (so a metre of thin wire has a measurable resistance of order 10 Ω) and nearly independent of temperature (so the wire stays ohmic even as it warms). Try the same experiment with copper and the resistance is too small to measure well; try it with a bulb filament and it is not ohmic at all.
Materials
- About 1.1 m of bare nichrome wire, roughly 0.3 mm diameter (around 28–30 gauge)
- Metre rule, with the wire taped or clamped taut along it
- Variable DC power supply, 0–12 V (or a battery pack plus a rheostat)
- Ammeter (0–1 A range) and voltmeter (0–5 V range), or two digital multimeters
- Switch, connecting leads, two crocodile clips, and a sliding contact (“jockey”)
- Micrometer screw gauge
Safety
- Keep the current at or below 0.5 A. The wire dissipates a few watts and thin nichrome gets hot enough to burn skin above that.
- Open the switch between readings. This also keeps the wire near room temperature, which keeps its resistance steady.
- Never connect the ammeter across the supply or across the wire — it has almost no resistance and is a short circuit.
- Low-voltage DC only. Do not substitute a mains-powered device for the supply.
Procedure
- Measure the diameter with the micrometer at three points along the wire, and at each point in two perpendicular directions (the wire may not be perfectly round). Check the micrometer’s zero reading first and correct for it. Record all six readings.
- Tape the wire taut along the metre rule, avoiding kinks. Build the circuit in the figure: supply, switch and ammeter in series with the full wire; voltmeter clip fixed at the 0 cm mark.
- Part A. Place the jockey at L = 50.0 cm. Set the supply so the current is 0.100 A, close the switch, and record I and ΔV. Open the switch.
- Repeat for currents of 0.200, 0.300, 0.400 and 0.500 A, opening the switch between readings.
- Part B. Set the current to 0.300 A. Record ΔV with the jockey at L = 20.0, 40.0, 60.0, 80.0 and 100.0 cm. Check that I stays at 0.300 A as you go — it should, since the circuit itself is not changing.
- Press the jockey on lightly and read the voltmeter promptly; dragging it scrapes the wire and changes its cross-section.
- Repeat Part B once more, moving the jockey in the opposite order, and average.
Even nichrome’s resistance creeps up slightly as it heats, and a warm wire also expands and sags. Leaving the switch closed for the whole session turns a clean straight line into a slowly curving one. Switch on, read, switch off.
Data table
Wire diameter readings (mm): ______ ______ ______ ______ ______ ______ Mean d: ______ mm Zero error: ______ mm
Part A — fixed L = 50.0 cm
| I (A) | ΔV (V) | R = ΔV/I (Ω) |
|---|---|---|
| 0.100 | ||
| 0.200 | ||
| 0.300 | ||
| 0.400 | ||
| 0.500 |
Part B — fixed I = 0.300 A
| L (m) | ΔV run 1 (V) | ΔV run 2 (V) | ΔV avg (V) | R (Ω) |
|---|---|---|---|---|
| 0.200 | ||||
| 0.400 | ||||
| 0.600 | ||||
| 0.800 | ||||
| 1.000 |
Analysis
1. Is the wire ohmic?
Plot ΔV (vertical) against I (horizontal) for Part A and fit a straight line. A straight line through the origin confirms ohmic behaviour; its slope is the resistance of 50.0 cm of wire. (With the axes this way round the slope is R; plotted as I vs ΔV it would be 1/R.)
2. Resistance against length
For Part B compute R = ΔV/I at each length, plot R against L, and fit a straight line. Report the slope in Ω/m and the intercept in Ω.
3. Cross-sectional area
4. Resistivity
As a cross-check, compute ρ = RA/L from Part A alone, using the slope of the ΔV–I graph and L = 0.500 m. The two methods should agree.
Sample data & worked analysis
Use this to practice the analysis before you have your own data, or to check your spreadsheet. Micrometer readings (mm): 0.321, 0.318, 0.322, 0.319, 0.320, 0.320; zero error 0.000 mm. Mean d = 0.320 mm.
| I (A) | ΔV (V) | R (Ω) |
|---|---|---|
| 0.100 | 0.69 | 6.90 |
| 0.200 | 1.36 | 6.80 |
| 0.300 | 2.06 | 6.87 |
| 0.400 | 2.74 | 6.85 |
| 0.500 | 3.41 | 6.82 |
| L (m) | ΔV avg (V) | R = ΔV/0.300 (Ω) |
|---|---|---|
| 0.200 | 0.84 | 2.80 |
| 0.400 | 1.65 | 5.50 |
| 0.600 | 2.47 | 8.23 |
| 0.800 | 3.29 | 10.97 |
| 1.000 | 4.10 | 13.67 |
Worked analysis of the sample data
Part A — ohmic check. A least-squares fit of ΔV against I gives
Part B — slope. A least-squares fit of R against L:
Area. d = 0.320 mm = 3.20×10−4 m, so
Resistivity.
Cross-check from Part A.
Uncertainty. The diameter readings span 0.318–0.322 mm, so d = 0.320 ± 0.002 mm (±0.6%). Squaring doubles that: A is uncertain by ±1.3%. The slope’s statistical uncertainty is far smaller (about ±0.2%, the points sit almost exactly on the line), so
Comparison: the accepted value of about 1.10×10−6 Ω·m is 0.6% above our result and inside the uncertainty. The whole experiment’s precision is set by a micrometer reading of a third of a millimetre — the electrical measurements are the easy part.
Error analysis
Separate the two kinds — AP rubrics award credit for knowing the difference.
| Source | Type | Effect & fix |
|---|---|---|
| Diameter measurement | Random (and systematic if zero error ignored) | The dominant uncertainty, doubled by squaring. A micrometer zero error of +0.01 mm would make every A about 6% too large. Take many readings in two orientations; correct for zero error. |
| Clip not exactly at 0 cm | Systematic | Every L is off by the same amount. Shows up as a nonzero intercept on the R–L graph; the slope, and therefore ρ, is unaffected. |
| Wire heating | Systematic | Raises R, most at high current — would bend the Part A line upward at the top. Small for nichrome; minimised by switching off between readings. |
| Non-uniform or kinked wire | Random | Local thin spots raise R for some lengths and not others, scattering the points about the line. Use straight, unscraped wire. |
| Meter calibration | Systematic | A voltmeter reading 1% high makes every R, and ρ, 1% high. Check meters against each other or a known resistor. |
| Meter resolution | Random | ±0.01 V is 1.2% of the smallest reading (0.84 V) but only 0.2% of the largest — another reason to rely on the slope. |
A dirty jockey contact might have a resistance of an ohm or so, but an ideal voltmeter draws essentially no current, so there is no IR drop across that contact and it does not change the reading. That is exactly why voltage is measured with a separate pair of leads instead of across the supply clips. Being able to say why a possible error is negligible earns as much credit as spotting a real one.
Conclusion questions
- Does your Part A graph show the wire is ohmic? Cite the shape and the intercept, not just “it looked straight.”
- Explain why moving the jockey does not change the ammeter reading.
- Your R–L graph probably has a small nonzero intercept. Give one physical cause and explain why it does not affect your value of ρ.
- Which single measurement contributes most to the uncertainty in ρ? Justify with percentages.
- Predict the slope of the R–L graph for a nichrome wire of twice the diameter. By what factor does it change?
- If the same experiment were done with a copper wire of the same diameter, what slope would you expect, and why would it be hard to measure with this equipment?
- Sketch the ΔV–I graph you would get if the wire were replaced with a small filament bulb, and explain its shape using the temperature dependence of resistance.
Extensions
- Test the 1/A dependence. Repeat Part B with two or three other gauges of nichrome. Plot the slope against 1/A; it should be a straight line through the origin with slope ρ.
- Non-ohmic contrast. Replace the wire with a 6 V filament bulb and take ΔV against I from 0 to 6 V. Compute R = ΔV/I at each point and plot it against power to see the filament heating up.
- Temperature coefficient. Coil a length of copper wire in a water bath and measure its resistance from 20 °C to 80 °C. The rise is a few tenths of a percent per degree — a direct look at more lattice collisions.
- Power in the wire. For each Part A reading, compute P = IΔV and confirm it equals I²R — connecting this lab to electric power.
Theory for this lab: Unit 3 · Current & resistance →