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Sandbox Physics

E59 · Surface spectromicroscopy

LEEM: Measure Island Growth

Can a changing LEEM image tell you a surface island is growing? Only with calibrated contrast. Selecting a different reflected beam can turn the same island from bright to dark without moving its boundary. Recorded electron numbers through a sequence let you estimate its changing area, provided the island shape and the signals from both regions are known.

Record a prescribed island expanding or retreating. Infer its boundary speed from image counts, reverse the selected reflection to test a contrast change, and compare with a stationary island or the retained static energy sweep.

Interactive modelLEEM: Measure Island Growth
Count-derived circular island radius—\text{—}
Fitted boundary speed—\text{—}
Speed difference from known input—\text{—}
Recorded-region image counts—\text{—}
More measurements and target
Conditional counting uncertainty of speed—\text{—}
Fitted initial radius—\text{—}
Selected exposure midpoint—\text{—}
Resolved circular-radius frames—\text{—}
Imaged order—\text{—}
Selected nominal landing energy—\text{—}
Recorded region contrast—\text{—}
Separate micro-LEED counts—\text{—}
First-order propagation threshold: phase A—\text{—}
Assumed image FWHM—\text{—}
Acquisition elapsed time—\text{—}
Experiment target—\text{—}

Physics tutorial

LEEM: Measure Island Growth

BackgroundA low-energy electron image changes when a surface island grows, but it also changes when the microscope selects a different reflected beam. Record a circular island at one fixed energy, infer its area from electron counts, then reverse the selected reflection. The two movies can look very different while giving the same boundary speed.

Why it mattersInfer the signed boundary speed within 10 percent or 0.003 micrometre per second, whichever is larger, with conditional counting uncertainty at most 0.002 micrometre per second and at least 20 resolved radius frames. Keep the complete island and its image blur inside the field. The static energy-sweep preset retains a different target: isolate phase A above 22 eV with aperture radius 0.2–0.5 inverse angstrom, spread at most 0.3 eV, more than 500 region counts and contrast above 0.8.

Start with the essentials

Focus question
Can a changing LEEM image tell you a surface island is growing?
One-sentence intuition
Reflection selection can reverse the brightness of an unchanged boundary. Growth requires a size history with a known contrast calibration.

Core mathematical model

Prescribed circular boundary motion

R(t)=[R0+vbt]+A(t)=πR(t)2\begin{aligned}R(t)&=[R_0+v_bt]_+\\A(t)&=\pi R(t)^2\end{aligned}

The positive-part operation holds the radius at zero after dissolution. The two material states and the boundary speed are assigned inputs; this is a kinematic example, not a thermodynamic growth law.

Area from calibrated image counts

S=∑iNi−nNincTAA^=p2SNinc(TB−TA)R^=A^/π\begin{aligned}S&=\sum_iN_i-nN_{\rm inc}T_A\\\widehat A&=\frac{p^2S}{N_{\rm inc}(T_B-T_A)}\\\widehat R&=\sqrt{\widehat A/\pi}\end{aligned}

The field contains two known material signals. Reversing their contrast changes the sign of the denominator as well as the image. Negative noisy area estimates stay in the fit; a radius is displayed only when the positive area is resolved. The complete island and its blur must remain inside the recorded field.

Average the area over each exposure

R‾=R0+vb(t0+Δt/2)A‾=π(R‾2+vb2Δt212)\begin{aligned}\overline R&=R_0+v_b(t_0+\Delta t/2)\\\overline A&=\pi\left(\overline R^2+\frac{v_b^2\Delta t^2}{12}\right)\end{aligned}

This expression applies when the radius stays positive throughout the exposure. At dissolution the integration is split at zero radius. The count fit uses actual exposure times, with the chosen dead time between frames; it never receives the input speed or geometry mask.

When a diffracted order can propagate

E⊥=E0−ℏ2∣G∣22meE_\perp=E_0-\frac{\hbar^2|\mathbf G|^2}{2m_e}

At normal incidence, an elastic order can leave the surface only if its perpendicular kinetic energy is zero or positive. A relative surface potential changes the local landing energy.

Reflection from a symmetric attractive slab

R=ηsin⁡2(qd)1+ηsin⁡2(qd)R=\frac{\eta\sin^2(qd)}{1+\eta\sin^2(qd)}

This lossless slab has an attractive 10 eV well and can be solved exactly. The phase the wave gathers inside the film makes the reflectivity oscillate.

Mismatch factor and wave number inside the film

η=V024E(E+V0)q=2me(E+V0)ℏ\begin{aligned}\eta&=\frac{V_0^2}{4E(E+V_0)}\\q&=\frac{\sqrt{2m_e(E+V_0)}}{\hbar}\end{aligned}

Thickness, local energy and source-energy averaging each change the intensity curve. One curve therefore does not give a unique thickness for a real material.

Common difficulties

An image change does not identify a growth mechanism

Typical misconceptionIf an island gets brighter, I have measured its growth rate or identified a phase transition.

Better mental modelThe reflection setting, source spread and counting noise also change the image. This example assumes a circular island and known signals for two specified material states. Its fit estimates a boundary speed under those assumptions; it does not identify an unknown phase, recover an arbitrary shape or explain why the material grows.

Run the experiment

  1. 01

    Measure the recorded growth

    Start with the expanding island. Move the selected stored frame in advanced settings, then drag the gold edge handle in the surface detail view to change the initial radius.

    What to observe: Frame selection reuses the recorded counts. Changing the initial condition acquires a new sequence. The circular radius in the image comes from the measured area.
  2. 02

    Reverse contrast without changing the growth law

    Choose Reverse contrast, same growth. Compare the image with the fitted speed and its counting uncertainty.

    What to observe: The island changes from bright to dark, yet a known two-region calibration can still recover its expanding boundary.
  3. 03

    Test noise and a retreating boundary

    Compare the stationary and retreating islands, then reduce exposure time or choose the closed order.

    What to observe: A stationary island can give a small signed apparent speed. A retreating island gives a negative speed. Too little admitted contrast or too few counts prevents a reliable estimate.
  4. 04

    Inspect diffraction as a separate repeat

    Open the micro-LEED data and move its field aperture. Use the static energy-sweep preset to inspect the original fixed domains and energy curves.

    What to observe: The evolving micro-LEED pattern is an independent repeated run of the same prescribed growth, not a transformation of the LEEM image counts or simultaneous acquisition on one camera.
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