Physics / Modern physics / Photoelectric effect
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EXPERIMENT 01 · LIGHT & MATTER

The photoelectric effect.

Practise the undergraduate photoelectric effect experiment.
When light meets metal, something remarkable happens.
Explore the physics. Make the measurements. Discover the constant.

◷   Work at your own pace↗   Undergraduate physics◎   Interactive experiment
YOUR VIRTUAL WORKBENCH

A little light. A big discovery.

LIVE SIMULATION
EMITTING METALCOLLECTORINCIDENT PHOTONSElectrons are emitted
Photon Electronλ = 450 nm
PHOTON ENERGY2.76 eV
PHOTOCURRENT0.00 nA
MAX. KINETIC ENERGY0.48 eV
CHANGE & OBSERVE
450 nm
200 nm · UV800 nm · IR
50%
DimBright
+0.00 V
−5 V · retarding+2 V · collecting

A negative collector voltage pushes emitted electrons back toward the metal.

↳
Same light. Different questions.

Try increasing intensity. Watch the current change, then compare the maximum electron energy.

THE QUESTION WE’RE ASKING

Can we measure a quantum of action?

Measure stopping potential at several light frequencies. The gradient of your graph reveals Planck’s constant—the link between a photon’s frequency and its energy.

TRY THIS FIRST

Make a prediction.

At a fixed colour, will brighter light give each emitted electron more maximum kinetic energy?

About this simulation & its limits

This is an ideal, single-photon teaching model. Photon energy is hc/λ; maximum electron energy is hf − φ. The emission threshold is exact. The current uses an illustrative energy distribution: for retarding voltage its collected fraction is (1 − |V|/Kmax)² up to the stopping voltage. Saturation current scales with photon flux at fixed conversion efficiency. Particle motion is schematic, slowed down, and not to scale. Material work functions are representative values, not calibrated photocell specifications. Contact potentials, leakage, dark current, surface contamination, space charge and instrument noise are omitted. The 0.01 V control spacing limits recorded voltage resolution. A real experiment needs its own apparatus manual, calibration and uncertainty analysis.

FROM INTUITION TO EQUATIONS

Understand every piece.

Open a concept to follow the explanation deeper. Then return to the workbench and test it.

EINSTEIN’S PHOTOELECTRIC EQUATION
hf = φ + Kmax

Incoming photon energy = escape energy + maximum electron kinetic energy

01What is the photoelectric effect?

Light incident on a suitable material can eject electrons. In this experiment, light illuminates a metal cathode inside an evacuated photocell. We infer electron motion from the collected current.

Observe two different things

Emission means electrons leave the surface. Detection means electrons arrive at the collector. A retarding field can prevent detection while emission continues.

Why was this surprising?

The threshold frequency and the dependence of maximum electron energy on frequency challenged a simple classical wave explanation in which energy transfer would depend on light intensity. Einstein’s photon model accounts for these observations.

02Frequency, wavelength & intensity

Frequency f counts oscillations per second (Hz). Wavelength λ is the distance between wave crests. In vacuum they obey c = fλ. Intensity is optical power per unit area.

c = fλ

Shorter wavelength means higher frequency. Convert nanometres to metres before calculating: 1 nm = 10⁻⁹ m. At 400 nm, f ≈ 7.49 × 10¹⁴ Hz.

Does intensity count photons?

For monochromatic light, photon arrival rate per unit area is intensity divided by hf. At a fixed frequency, more intensity means more photons. At fixed optical intensity, increasing frequency actually reduces photon flux. Current also depends on collection and conversion efficiency.

03Photons & their energy

A photon is one quantum of electromagnetic energy. Its energy depends on frequency, not on how bright the source looks. The same colour can be delivered as a faint beam or a bright beam.

Ephoton = hf = hc / λ

Using h = 6.62607015 × 10⁻³⁴ J s and c = 299792458 m/s gives energy in joules. Divide by e = 1.602176634 × 10⁻¹⁹ C to express the energy in electronvolts.

What is an electronvolt?

One electronvolt is the energy change of an elementary charge across one volt: 1 eV = 1.602176634 × 10⁻¹⁹ J. It is an energy unit, whereas a volt is a potential-difference unit.

04Work function & the surface

The work function φ is the minimum energy needed to remove an electron from the material into vacuum. It depends on material and surface condition. A photon must supply at least this escape energy.

φ = escape-energy threshold

For our representative sodium surface, φ = 2.28 eV. A 450 nm photon supplies about 2.76 eV, leaving a maximum of about 0.48 eV for electron motion.

Why “maximum” electron energy?

Electrons do not all escape with the same kinetic energy. Their initial states and energy losses differ. Einstein’s relation specifies the upper end of the emitted energy distribution; this is what stopping potential probes.

05Threshold frequency & wavelength

The ideal emission threshold occurs when the photon has just enough energy to overcome the work function. Below the threshold frequency, increasing intensity cannot produce emission within this single-photon model.

f₀ = φ / h · λ₀ = hc / φ

Emission requires f > f₀, equivalently λ < λ₀ for positive electron kinetic energy. Sodium’s representative threshold wavelength here is about 544 nm.

Are there exceptions at very high intensity?

Multiphoton and other strong-field processes can occur outside the ordinary low-intensity photoelectric experiment. They are excluded from this model. Exactly at threshold the ideal maximum kinetic energy is zero.

06Einstein’s energy balance

A photon transfers its energy in one absorption event. Some energy is needed for escape; the remaining energy sets the maximum kinetic energy of an emitted electron.

Kmax = hf − φ

Above threshold, increasing frequency increases Kmax. Increasing intensity at fixed frequency increases the number of absorption events but does not increase Kmax.

Why isn’t negative Kmax shown?

When hf < φ, the negative algebraic result signals that emission is energetically forbidden. It does not describe an emitted electron with negative kinetic energy. The workbench shows zero and a no-emission message.

07Voltage & stopping potential

A negative collector voltage produces an electric field that opposes electrons travelling from cathode to collector. Increase its magnitude until even the fastest electrons cannot cross.

eVₛ = Kmax

Here e is the positive elementary-charge magnitude and Vₛ is the positive magnitude of the stopping voltage. The control displays signed collector voltage; the notebook records its magnitude.

Why must we find the first zero?

Every sufficiently negative voltage also gives zero collected current. Only the boundary between nonzero and zero collection estimates stopping potential. Bracket that boundary instead of choosing an arbitrary zero-current voltage.

08Photocurrent & current–voltage behaviour

Photocurrent is collected charge per unit time. For emission above threshold, increasing intensity at fixed wavelength generally raises the saturation current. A retarding voltage rejects progressively more emitted electrons.

I = collected charge / time

At sufficient collecting voltage, all available photoelectrons are collected in the ideal model. Increasing voltage further then produces no extra photoelectrons.

How realistic is our current curve?

Its shape is illustrative. We assume constant conversion efficiency and a simple energy distribution. Actual curves depend on geometry, electron energies, electrode contact potentials, space charge and dark current. Only the ideal stopping boundary follows directly from Einstein’s relation.

09Measure Planck’s constant with a graph

Rearrange the energy equation to express stopping potential as a straight-line function of frequency. Use several frequencies with the same emitting surface.

Vₛ = (h/e)f − φ/e

The gradient m equals h/e, so h = em. The vertical intercept b equals −φ/e. With frequency in Hz, the gradient has units V s and h has units J s.

What if frequency is displayed in 10¹⁴ Hz?

The chart uses scaled axis labels for readability. The fit converts its gradient back to V s before calculating h. If you calculate manually from the displayed axis, divide the graphical gradient by 10¹⁴.

10Uncertainty, residuals & honest conclusions

Repeated readings reveal random scatter. Instrument resolution, wavelength bandwidth and calibration contribute uncertainty. A systematic voltage offset can shift the intercept even when the gradient looks reasonable.

residual = observed Vₛ − fitted Vₛ

Look for a pattern in residuals, repeat measurements, and report assumptions. A small difference from the accepted h does not by itself prove a precise or accurate measurement.

What does this virtual experiment establish?

Its readings are generated from a model that already contains the accepted value of h. Fitting them practises measurement and analysis; it is not independent evidence for the value of h. In a physical lab, use the actual setup’s documented corrections and uncertainty budget.

BEFORE YOU TOUCH A CONTROL

Meet your apparatus.

The workbench uses an ideal photocell arrangement. Your university’s equipment may measure stopping voltage differently.

01 / ILLUMINATE

Monochromatic light source

Provides light with a known wavelength. In a physical lab, a lamp with filters or a suitable spectral source can select different wavelengths. Know the wavelength and its bandwidth before converting it to frequency.

Why one wavelength at a time?

A broad spectrum contains photons with different energies. High-frequency components can dominate the stopping voltage, making a single-frequency interpretation misleading.

02 / EMIT

Evacuated photocell

Light strikes a photosensitive cathode (K), releasing electrons when photon energy is sufficient. The collector (A) receives electrons that cross the gap. Evacuation reduces collisions with gas.

Why does the material matter?

Its work function sets the escape-energy threshold. Real surfaces and contact potentials affect measurements; changing metals is an exploration control here, not a required step in the Planck-constant procedure.

03 / CONTROL

Variable bias & voltmeter

The collector voltage is measured relative to the emitting cathode. Negative voltage retards electrons. The stopping potential Vₛ is the positive magnitude of the negative voltage required to stop even the most energetic electrons.

What sign goes in my graph?

Record Vₛ = |Vcollector|, not a negative value. For the ideal setup, eVₛ = Kmax. Use volts on the vertical axis.

04 / DETECT

Sensitive current meter

A nanoammeter measures the charge arriving per second. As retarding voltage increases in magnitude, fewer emitted electrons reach the collector, and the photocurrent falls.

Does zero current mean no emission?

No. Electrons may still leave the cathode and return to it. Zero collected current at stopping potential is different from no emission below threshold.

◎
Bring this understanding into your real lab.

Check the actual instrument manual for connections, polarity, zeroing, light-source handling and the specified stopping-voltage method. Never look into UV sources or laser beams.

GUIDED PRACTICE

One careful measurement at a time.

Aim: determine Planck’s constant from stopping potential versus frequency. Use the same target material throughout one data set.

TURN OBSERVATIONS INTO EVIDENCE

Your measurements tell a story.

Plot stopping potential Vₛ against frequency f. Collect at least three distinct wavelengths for a fit; five or more give a better opportunity to assess scatter.

Stopping potential vs frequency

YOUR OBSERVATIONS

Your recorded measurements will appear here.

LINEAR FIT · Vₛ = mf + b

Find Planck’s constant.

Record three or more different wavelengths to calculate a best-fit line.

h = e × gradient

Reference: h = 6.62607015 × 10⁻³⁴ J s
e = 1.602176634 × 10⁻¹⁹ C

#Materialλ (nm)f (10¹⁴ Hz)Vₛ (V)Remove

No measurements yet. Find a stopping voltage on the workbench, then record it.

Interpret the result, including its limitations

The fit is ordinary least squares with equal weight for each voltage reading. Percentage difference from the reference value is not the same as experimental uncertainty. Inspect residuals and repeat measurements. In this ideal model, the first zero-current setting is rounded by the 0.01 V step; the measured crossing lies between the last nonzero setting and the first zero setting. Real instruments add wavelength bandwidth, dark current, contact potentials, calibration effects and a less definite zero. A small percentage difference here demonstrates the model and your method, not an independent physical measurement of h. A negative fitted intercept gives φ = −eb in joules, or numerically −b in eV.

EXPLAIN IT IN YOUR OWN WORDS

Ready for the lab?

Test the ideas behind your measurements. Choose an answer to see why it works.

Prepare for your viva

Explain why a zero current can occur even while electrons are being emitted. Describe which variable you would change to measure h, which you would hold fixed, and how you would identify a systematic offset in stopping voltage.

WORKED EXAMPLE · SIMULATED DATA

Photoelectric effect: sample lab report

Demonstration report—not a record of a physical experiment.

These five readings were generated with OpenLab’s ideal sodium model and the first zero-current setting at 0.01 V spacing. Use this as a format and calculation guide. Replace the observations with your own measurements and follow your department’s reporting requirements.

Student: __________________Student ID: __________________Course / section: __________________Date performed: __________________Lab partner: __________________Instructor: __________________

1. Title and aim

Determination of Planck’s constant using the photoelectric effect. Measure stopping potential at several known light frequencies for one emitting material, fit a straight line, and estimate Planck’s constant. Estimate the effective work function and threshold frequency from the intercept.

2. Abstract

Five simulated stopping potentials were obtained for wavelengths from 500 to 300 nm at fixed target material and 50% intensity. Linear regression gave a gradient of 4.15224 × 10⁻¹⁵ V s and intercept −2.28878 V, yielding h = 6.65263 × 10⁻³⁴ J s. The estimate differs by 0.401% from the reference value. These values demonstrate the analysis procedure; the simulator itself uses the reference h and is not an independent measurement.

3. Apparatus and settings

  • OpenLab ideal photoelectric simulator; sodium target with representative work function φ = 2.28 eV.
  • Monochromatic source: selected wavelengths 500, 450, 400, 350 and 300 nm; intensity fixed at 50%.
  • Evacuated photocell, collector-bias control and sensitive current meter represented schematically.
  • Collector voltage range: −5 to +2 V; control spacing: 0.01 V. There is no simulated instrument noise.
  • A real laboratory additionally needs the actual photocell, specified light source / filters, variable supply, voltmeter, current meter, connecting leads and the instrument manual.

4. Theory and working equations

A photon carries energy hf. Emission occurs when this energy can overcome the surface work function. The most energetic emitted electrons satisfy Einstein’s energy balance. A retarding voltage stops collection when its electric potential-energy barrier equals that maximum kinetic energy.

hf = φ + Kmax   ·   Kmax = eVs
Vs = (h/e)f − φ/e   ·   f = c/λ

Vs is a positive magnitude. The collector control is negative at the stopping point. For a fit Vs = mf + b with f in Hz, h = em and φ = −eb in joules. Numerically, φ in eV equals −b in volts. Threshold frequency f₀ = −b/m.

Constants: c = 299792458 m s⁻¹; e = 1.602176634 × 10⁻¹⁹ C; reference h = 6.62607015 × 10⁻³⁴ J s. The SI values of these constants are exact; the fitted estimate is limited by the observations.

5. Procedure

  1. Select sodium, set intensity to 50%, and set collector voltage to 0 V.
  2. Select 500 nm and check that emission produces a nonzero current.
  3. Make the collector voltage increasingly negative until the collected current first becomes zero.
  4. Increase voltage one 0.01 V step toward zero to verify that current returns. Return to the first zero-current step.
  5. Record the wavelength, frequency, last nonzero voltage and current, first zero voltage, and Vs.
  6. Repeat at 450, 400, 350 and 300 nm while keeping material and intensity fixed.
  7. Plot Vs against f, perform a least-squares fit, calculate h, and inspect residuals and measurement limitations.

6. Observations: raw and derived readings

The current values below are calculated from the simulator’s illustrative current curve. Tiny nonzero currents appear as “<0.01 nA” on the workbench; extra digits here explain the bracket and do not represent real meter precision. One bracket per wavelength is used; no repeated physical trials are claimed.

Table 1. Simulated stopping-boundary observations; sodium, intensity 50%.
No.λ (nm)f (10¹⁴ Hz)Last nonzero V (V)Current there (nA)First zero V (V)Current (nA)Vₛ (V)
15005.995849−0.190.026132−0.2000.20
24506.662055−0.470.001199−0.4800.48
34007.494811−0.810.001221−0.8200.82
43508.565499−1.260.000028−1.2701.27
53009.993082−1.850.000015−1.8601.86

Download these sample observations as CSV ↓

7. Worked calculation for one reading

For λ = 400 nm = 400 × 10⁻⁹ m:

f = 299792458 / (400 × 10⁻⁹) = 7.49481145 × 10¹⁴ Hz
Vs = |−0.82| = 0.82 V
Kmax, inferred = eVs = 1.31378484 × 10⁻¹⁹ J = 0.82 eV

The boundary is bracketed by −0.81 V with a small nonzero current and −0.82 V with zero current. Thus 0.81 V < Vs,true ≤ 0.82 V for this ideal monotonic model. The notebook records the upper endpoint, 0.82 V.

8. Graph and least-squares calculation

Let x = f / (10¹⁴ Hz) and y = Vs. Fit y = ax + b using all five readings, rather than only two selected points.

0.00.51.01.52.0678910Frequency (10¹⁴ Hz)Stopping potential (V)

Orange points: simulated observations. Green line: equal-weight least-squares fit.

Table 2. Calculation table; energy inferred from recorded Vₛ.
λ (nm)xx²xyeVₛ (10⁻¹⁹ J)Fitted Vₛ (V)Residual (V)
5005.99584935.9502071.1991700.3204350.200848-0.000848
4506.66205544.3829723.1977860.7690450.477473+0.002527
4007.49481156.1721996.1457451.3137850.823254-0.003254
3508.56549973.36777010.8781832.0347641.267829+0.002171
3009.99308299.86168718.5871322.9800491.860597-0.000597
x̄ = 7.74225919   ·   ȳ = 0.926000 V
Σ(x − x̄)² = 10.02194676
Σ(x − x̄)(y − ȳ) = 4.16135725
a = Σ(x − x̄)(y − ȳ) / Σ(x − x̄)² = 0.415224442
b = ȳ − ax̄ = -2.288775250 V

The displayed frequency axis is scaled. Therefore m = a / 10¹⁴ = 4.152244415 × 10⁻¹⁵ V s.

h = em = (1.602176634 × 10⁻¹⁹)(4.152244415 × 10⁻¹⁵)
h = 6.652628981 × 10⁻³⁴ J s
φfit = −b = 2.288775250 eV
f₀ = −b/m = 5.512139992 × 10¹⁴ Hz
λ₀ = c/f₀ ≈ 543.877 nm

9. Uncertainty and percentage difference

Percentage difference = |hfit − hreference| / hreference × 100 = 0.4008%. This is a comparison with a reference, not an uncertainty estimate.

Fit scatter only: for n = 5, Σr² = 2.27609 × 10⁻⁵ V². The residual standard deviation is s = √[Σr²/(n − 2)] = 0.00275444 V. The slope standard error on the scaled axis is sa = s/√Σ(x − x̄)² = 0.00087008, yielding sh = esa/10¹⁴ = 1.39402 × 10⁻³⁶ J s.

The regression-only result can be written h = (6.653 ± 0.014) × 10⁻³⁴ J s, where ± denotes one slope standard error. It assumes independent, equal-variance voltage errors and exact frequencies. These assumptions do not describe a complete uncertainty budget for these deterministic rounded data.

Resolution and endpoint bias: the true boundary lies in a 0.01 V interval. Recording its first zero-current endpoint biases each observation upward by between 0 and 0.01 V. Under a uniform-within-bracket approximation, a midpoint estimate would subtract 0.005 V and have standard uncertainty 0.01/√12 ≈ 0.00289 V. Subtracting the same 0.005 V from every reading changes the intercept, but not the fitted slope. This report retains the notebook’s endpoint convention.

In a physical lab, include wavelength uncertainty and bandwidth, voltage calibration, current-meter zero, dark current, contact potentials, surface condition and repeatability. They are omitted from this demonstration; the quoted fit error must not be reported as the full physical uncertainty.

10. Results and discussion

  • Estimated Planck’s constant: 6.653 × 10⁻³⁴ J s; regression-only standard error: 0.014 × 10⁻³⁴ J s.
  • Fitted effective work function: 2.289 eV; threshold frequency: 5.512 × 10¹⁴ Hz.
  • Stopping potential increases approximately linearly with frequency, consistent with the model’s energy balance.
  • The small residuals arise from the voltage step and first-zero convention. They do not demonstrate realistic instrument performance.
  • The fitted work function differs from the model input 2.28 eV because of rounding and the endpoint convention.

11. Precautions and sources of error

Keep the same emitting surface for all readings. Use one known wavelength at a time, distinguish a tiny current from exactly zero in this simulation, bracket the stopping boundary, and maintain a consistent sign convention. In a real laboratory, zero and calibrate instruments, account for background current, follow the equipment manual, and avoid direct exposure to UV sources or laser beams.

12. Conclusion

This worked example shows how stopping-potential observations lead to a graph-based estimate of Planck’s constant. The five simulated readings yield 6.653 × 10⁻³⁴ J s, differing by 0.401% from the reference. The exercise demonstrates the method and its analysis; because the simulator contains the reference constant, it does not independently verify its value.

Review the photoelectric-effect theory →   Try your own measurements →