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Sandbox Physics

E59 · Surface spectromicroscopy

LEEM: Surface Reflection & Diffraction

Sweep low-energy electrons across a two-domain surface. Select a reflected order to form an image, inspect stored region intensity curves and record a separate micro-LEED pattern with a field aperture. Find contrast reversals and the energy where a diffracted order can propagate.

Interactive modelLEEM: Surface Reflection & Diffraction
Imaged order—\text{—}
Selected nominal landing energy—\text{—}
Stored region image counts—\text{—}
Phase A / B recorded contrast—\text{—}
Separate micro-LEED counts—\text{—}
First-order propagation threshold: phase A—\text{—}
Assumed image FWHM—\text{—}
Total image-stack exposure—\text{—}
Experiment target—\text{—}

Physics tutorial

LEEM: Surface Reflection & Diffraction

BackgroundSweep low-energy electrons across a two-domain surface. Select a reflected order to form an image, inspect stored region intensity curves and record a separate micro-LEED pattern with a field aperture. Find contrast reversals and the energy where a diffracted order can propagate.

Why it mattersTarget: select the phase-A first order above 22 eV with a reciprocal aperture radius from 0.2 to 0.5 inverse angstrom. Keep source spread at or below 0.3 eV, select only phase A, acquire more than 500 region counts and obtain recorded domain contrast above 0.8. A bright-field image cannot complete this dark-field task.

Start with the essentials

Focus question
Can one diffracted beam isolate a surface domain?
One-sentence intuition
The diffraction-plane contrast aperture and real-space field aperture perform different selections. Energy-dependent intensity is a measurement that needs a scattering model, not a direct height map.

Core mathematical model

Propagating diffraction order

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

At normal incidence an elastic order requires nonnegative perpendicular kinetic energy. A relative surface potential changes local landing energy.

Symmetric attractive slab

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

The exactly soluble lossless slab has an attractive 10 eV well; the phase inside the film produces reflectivity oscillations.

Mismatch and internal wave number

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 set different intensity curves. No unique real-material thickness inversion follows.

Common difficulties

Brightness needs a model

Typical misconceptionA bright region directly reveals its physical cause.

Better mental modelThe diffraction-plane contrast aperture and real-space field aperture perform different selections. Energy-dependent intensity is a measurement that needs a scattering model, not a direct height map.

Run the experiment

  1. 01

    Predict contrast reversal

    In bright field, move through the energy stack and compare the two recorded domain curves.

    What to observe: The brighter domain changes with energy; brightness alone does not label thickness.
  2. 02

    Select an order and a region

    Choose the phase-A dark-field preset. Move the field aperture from the left to the right domain.

    What to observe: The image selects an angular order; the independent micro-LEED exposure selects a real-space region.
  3. 03

    Check propagation and precision

    Compare closed-order, wide-aperture, mirror and low-count presets.

    What to observe: A closed order stays dark. A wide aperture mixes domains, while low counts undermine an otherwise correct selection.