(Low Energy) Ion Scattering Spectroscopy (ISS) / (LEIS)

Technique Overview

Ion Scattering Spectroscopy (ISS), also known as Low Energy Ion Scattering (LEIS), is a highly surface-sensitive analytical technique used to study the composition and structure of materials. It involves directing a beam of low-energy ions, typically noble gases like helium, at a surface and has a pobing depth of around 1-2 atomic layers. These ions scatter upon hitting the surface atoms, and the kinetic energy of the scattered ions is measured. Each element at the surface produces a distinct peak in the energy spectrum due to differences in mass and momentum transfer. ISS is extremely sensitive to the topmost atomic layer, making it ideal for analyzing surface composition. It is primarily used to determine the elemental composition of atoms at the outermost surface.

 

Applications and Fields

Thin film analysis

Adsorbate analysis

Terminating layer annalysis

Ion scattering spectroscopy (ISS), also known as low energy ion scattering (LEIS), is a surface technique which involves probing the outermost surface layers of a solid using elastic collisions of ions. While ISS is generally be used to provide surface identities and ratios, it may also be used in a semi-quantitative manner through comparison with standard samples. Originally involving high energy (MeV) ions (and often referred to as Rutherford Backscattering Spectroscopy or RBS), the ISS technique was refined to utilise lower energy ions to be more readily available in laboratories. It was the discovery that ion-surface collisions could be described kinematically by a simple two body elastic collision model that allowed for facile determination of surface composition:

The extreme surface sensitivity of ISS allows it to offer additional structural information, complementary to that of pure XPS analysis and it has found use in many fields. While ISS remains a valuable tool in materials analysis, care needs to be taken over sample choice and preparation. For example, ‘rough’ surfaces such as silicas commonly used in heterogeneous catalysis may exhibit broadened peaks in eventual ISS profiles. To overcome this, compacting samples into pellets may improve surface suitability, however, care must be taken so as not to alter the material properties. Furthermore, ion scattering may have limitations depending on sample composition, since preferential sputtering can lead to erroneously low concentrations of easily sputtered components such as sodium.

Ion Scattering Spectroscopy (ISS) works by directing a beam of low-energy ions, typically noble gases like helium, at the surface of a material. When these ions collide with the surface atoms, they scatter. The kinetic energy of the scattered ions is then measured. Each element at the surface produces a distinct peak in the energy spectrum due to differences in mass and momentum transfer.

The dependence of peak energy position on atomic mass in ISS. E0 = primary ion EkE1 = primary ion Ek following a scattering process at θ° to initial trajectory, m1 = mass of primary ion, m2 = mass of target atom.

Ions can be detected either using an XPS analyser with a reversed polarity (ISS), or with a dedicated cylindrical mirror analyzer (LEIS).1 ISS may be incorporated into a standard XPS system, and is commonly found on instruments from most manufacturers – however LEIS requires a dedicated standalone instrument.

When running an ISS experiment on an XPS instrument, it is typically performed in the 1-3 keV region (the energy span of the analyzer). Helium ions are lighter, and therefore do not provide as large an energy separation for heavier elements – so it is often advised to use Argon gas lines instead if one wishes to distinguish two heavy elements. The penalty of this is increased intrinsic sputtering of the surface.

General Analysis

ISS data is output in the same format as XPS data, with kinetic energy on the X-axis instead of binding energy. As such, standard XPS fitting softwares such as CasaXPS, or Avantage can be used for analysis.

Care should be taken with background selection – since ISS data is subject to the same inelastic background considerations as XPS data.2

Qualitative Analysis

If one simple wishes to observe the elemental identity of the terminating layer – then the peak assignment is a relatively trivial affair, requiring only the angle and the energy of the ion beam.

Energy Ratio = Kinetic Energy / Ion Beam Energy

(Ion gun angle = 130 degrees)

These ratios will be consistent for a given ion gun angle, and can be computed using the binary collision model above.

Quantitative Analysis

Quantitative analysis of scattered ions is possible by the following relationship:

Yi = ni . ( δσi / δω ) . Pi+ . cR

Where:

Yi = Detected ion yield

ni = Atomic surface concentration

δσi / δω = Differential scattering cross section

Pi+ = Ion fraction of backscattered projectiles

c = instrument factor (solid angle of acceptance, transmission function)

R = Roughness factor

 

For more information – see the practical guide to interpreting low energy ion scattering (LEIS) spectra article from Stanislav Průša et al.

CasaXPS is capable of handling ISS data, and has inbuilt background functions suitable for analysis.

Owing to its enhanced surface sensitivity in comparison to XPS, which has an information depth of as much as 9–10 nm (using a typical Al kα X-ray source), ISS has found much use in extracting qualitative information on elemental distributions in the very uppermost atomic layers of a sample. The ability to probe only a single monolayer allows for a more sophisticated analysis of the atomic arrangement at the surface and near surface.

This information is of critical concern in fields such as heterogeneous catalysis, wherein performance and activity are directed by surface interactions of reactants onto active sites. Ceria based mixed oxides for example, possess unique surface properties which render them highly useful in a variety of applications. Surface segregation of either dopant or ceria, determined by ISS, has enabled a deeper understanding of how different thermal treatments or synthesis methods affect the resultant materials properties as catalysts, ion conductors and oxygen storage.

Furthermore, since this is in effect an ion bombardment technique, the correct experimental parameters may induce sputtering of the surface of a material (even at low accelerating voltages), successive ISS spectra may therefore reveal an elemental gradient, affording further information which with knowledge of sputtering yields (or in comparison with alternative methods of probing the depth distribution of the outer surface) may even be used to prepare a incredibly surface sensitive elemental depth profile.

ISS may also be used to determine changes to the outermost surface following chemical or physical processing and has been used to study systems undergoing many common processes such as thermal treatments, hydrogen reduction or exposure to gases or vapours such as O2 and H2O, and has also been used to study particle sintering.

When considering nanoparticle or thin-film growth over a substrate (of non-matching identities), knowledge of nucleation and growth modes permits sophisticated and precise control over nanomaterial synthesis. ISS analysis combined with XPS affords a simple methodology for modelling the growth based on the calculated surface coverage or peak intensity relative ratios.

Many detailed models have been developed to understand the varying growth mechanisms of particles on films.4

ISS may be used during temperature profiles much in the same way as XPS, to observe structural changes as a function of increased temperature.

With careful consideration of intrinsic sputtering rates, and adsorbate removal rates, this technique has been shown to resolve CO adsorption sites from Pd nanocluster samples.5

ISS is ideal for studying SMSI formations, given the extreme surface sensitivity of the technique. The formation of an ultra-thin overlayer (e.g. TiO2 over Ag nanoparticles)6 results in a markedly different ISS signal.

  1. Průša, Stanislav, et al. “A practical guide to interpreting low energy ion scattering (LEIS) spectra.” Applied Surface Science 657 (2024): 158793. Read it online here.
  2. ISS Surface Insight Note
  3. Cushman, Cody V., et al. “Low energy ion scattering (LEIS). A practical introduction to its theory, instrumentation, and applications.” Analytical Methods 8.17 (2016): 3419-3439. Read it online here.
  4. James, Trevor E., et al. “Energetics of Cu adsorption and adhesion onto reduced CeO2 (111) surfaces by calorimetry.” The Journal of Physical Chemistry C 119.30 (2015): 17209-17217. Read it online here.
  5. Kaden, William E., et al. “CO adsorption and desorption on size-selected Pdn/TiO2 (110) model catalysts: Size dependence of binding sites and energies, and support-mediated adsorption.” The Journal of chemical physics 136.20 (2012). Read it online here.
  6. Grünert, Wolfgang, et al. “Structural properties of Ag/TiO2 catalysts for acrolein hydrogenation.” The Journal of Physical Chemistry B 108.18 (2004): 5709-5717. Read it online here.