Analytical Ion Microbeam


Method

Normally ion beams have a size in the mm range but they can also be focussed to µm beamsizes using slits as object and a set of magnetic quadrupole lenses. The ion beam current for ion microbeams is much less than for mm-sized ion beams because of the small size of the object slits, needed for a small beamsize. The ion beam can be scanned over the sample magnetically of electrostatically to obtain laterally resolved information, e.g. elemental distribution maps.

Foto: Prinzip Ionenmikrostrahl ©Copyright: Dr. Frans Munnik

Schematic of a MeV ion microbeam, object and aperture are slits, the lens consists typically of a set of quadrupole magnets, the sample should be mounted in the target plane.

All Ion Beam Analysis (IBA) methods can also be applied with a ion microbeam but PIXE is most often used because PIXE is a very sensitive technique when 2-3 MeV proton beams are used. It is also important to have large solid angles for the detectors or use multiple detectors to improve the sensitivity because of the low beam currents available. Multiple techniques like PIXE, RBS, PIGE are often used simultaneously to obtain a maximum of information from one measurement.

Advantages

  • Quantitative determination of concentrations based on IBA techniques is available at the micrometer scale.
  • Light elements can be analysed by PIGE, NRA or RBS in the energy region of elevated non-Rutherford cross sections.
  • Some of the methods like RBS and NRA are depth sensitive.

Limitations

  • The beamsize is typically several µm and it is difficult to focuse sub-µm because MeV ions are much more rigid then keV electrons.
  • Measurements in vacuum, in air is possible but with larger beam size of tens of µm.
  • Some damage can occur, especially for fragile samples.

Analytical Ion Microbeam setup at HZDR

The ion microbeam is connected to the 3 MV Tandetron of the Ion Beam Center and typically a 3 MeV proton beam is used, which is very suitable for PIXE and non-Rutherford RBS. The following methods are available: PIXE, RBS, PIGE, NRA, STIM (Scanning Transmission Ion Microscopy). Quantitative elemental concentration maps can be obtained from PIXE measurements using the software package GeoPIXE, available at the HZDR.

Foto: Ionenmikrostrahl am 3 MV Tandetron ©Copyright: Dr. Frans Munnik

Ion Microbeam setup at the 3 MV Tandetron

Samples

A wide variety of samples from many fields of application can be analysed, such as minerals for Geoscience, aerosol filters for environmental science, coatings and thin films in tribology (science of wear, friction and lubrication), biomedical devices like stents.

  • Flat samples with size of max. 25x25 mm² and a maximum thickness of 5 mm can be mounted with double sided tape on the sample holder.
  • Samples with a diameter of ≤ 10 mm and a maximum thickness of 15 mm can be mounted at recesses on the side of the sample holder.
  • Point measurements can be performed on irregular samples, whereas a flat (small) surface is required for elemental imaging.

Application 1: Analysis of individual aerosol particles

  • Aerosol particles have a direct impact on air quality, cloud nucleation, radiation balance, public health, etc.
  • These particles can be collected on filter materials with an impactor.
  • Particle Induced X-Ray Emission (PIXE) is a non-destructive and undemanding technique for elemental analysis that is suitable for offline filter analysis.
  • Rutherford Backscattering Spectrometry (RBS) is a non-destructive technique that can provide offline elemental depth information.
  • With an ion microbeam, laterally resolved elemental maps can be made, making the analysis of individual particles possible.

Samples:

  • Mineral/Saharan dust particles collected on filter tape of quartz fibres coated with Teflon using a Aethalometer AE33.
Foto: Drei Kollektorstellen mit Mineralstaubpartikeln auf einem AE33-Filterband. ©Copyright: Dr. Rok Podlipec

Three collector spots of mineral dust particles on AE33 filter tape.

Measurements:

  • Ions: H+ (protons)
  • Energy: 3 MeV
  • Beam size: 6x4 μm²
  • Maps: 256x256 points with a step size of 1 µm
  • Detection: characteristics X-rays with a Ketek Silicon drift detector
                     backscattered protons with a silicon strip detector

Spectra with regions for maps:

Foto: PIXE-Spektrum eines Scans von Sahara Staubpartikeln gesammelt auf Filterband ©Copyright: Dr. Frans Munnik

PIXE spectrum of a scan of saharan dust particles collected on filter tape. The grouped lines show the characteristic X-rays of the elements that are used for making maps.

Foto: RBS-Spektrum eines Scans von Sahara Staubpartikeln gesammelt auf Filterband ©Copyright: Dr. Frans Munnik

RBS spectrum of a scan of saharan dust particles collected on filter tape. The regions are used to select events for maps. Surf. denotes a region near the sample surface, below and deeper is at larger depths in the sample.


Elemental maps:

Foto: Mit PIXE gewonnene Elementkarten von Aerosolpartikeln ©Copyright: Dr. Frans Munnik

Elemental maps obtained with PIXE showing aerosol particles

  • Large high intensity areas in the Fe map correspond to the large areas in the Mn map.
  • The small Fe containing particles (red points in the Fe map) do not correspond to Ca containing particles.
Foto: Mit PIXE gewonnene Elementkarten die einen Faserstruktur zeigen ©Copyright: Dr. Frans Munnik

Elemental maps obtained with PIXE showing a fibre structure

  • Three elements (Ba, K, Zn) show predominantely a fibre structure that is similar for each element.
  • The rightmost graph shows a RGB composite with each element assigned a basic colour. This graph shows a good correlation between all elements (white) but also fibres with only K (green) and fibres with Ba (L-lines) and Zn (pink).
Foto: Mit RBS gewonnene Elementkarten die einen Faserstruktur zeigen ©Copyright: Dr. Frans Munnik

Elemental maps obtained with RBS showing a fibre structure. Map r2d shows carbon near the surface, maps r2c and r2b show carbon below the surface and deeper in the sample, respectively.

  • These three maps show the teflon coated quartz fibres of the filter tape at different depths. These fibres are most clearly visible in the maps based on carbon because RBS with 3 MeV protons has a high sensitivity for carbon.
  • The rightmost graph shows a RGB composite with each RBS map assigned a basic colour.The graph clearly shows the fibre structure, even though they are at different depths.

Conclusion

  • PIXE provides good elemental identification and sensitivity but is not depth sensitive. It can be used to identify elements in aerosol particles.
  • RBS provides depth information and using a 3 MeV H-ion beam is especially useful for detecting light elements like C.
  • Elemental maps are a useful tool to assign elements to individual particles or fibres.

This work is part of the Helmholtz European Partnering Project CROSSING (PIE-0007)


Application 2: Analysis of wear processes in tribological ta-C coatings

Objective: Develop solid lubricants with the aim of eliminating liquid lubricants. This eliminates the consumption of lubricants, which results in
  • cost savings and
  • reduced environmental impact.

First tribological wear tests

  • ta-C (hydrogen-free, tetraedic, amorphous carbon) as a new and exciting solid lubricant coating on steel
  • Counter bodies of various materials, e.g. brass, steel, SiC
  • Apply tribological tests by rotating the counter body over the coating
Foto: SRV501_track v57 ©Copyright: Dr. Frans Munnik

Track on the ta-C coating produced by a SiC counter body


Analyse wear track and counter body for

  • Loss of coating
  • Transfer of material from counter body
=> Apply Ion Beam Analysis
Measurement conditions:
  • Use the ion microbeam because wear areas and tracks are small
    Focus: 5-10 µm
  • Different methods
    • PIXE
    • RBS
  • Different ions and energies
    • H+, 3 MeV
    • He2+, 2 MeV

Wear track on the ta-C coating made by the SiC counter body

  • PIXE and RBS with a 2 MeV He-ion beam
Foto: PIXE Spektrum für track V57 ©Copyright: Dr. Frans Munnik

PIXE spectrum showing three regions that are used for producing maps. The line for Si and the region for Ca are for information only.

Foto: RBS Spectrum für track V57 ©Copyright: Dr. Frans Munnik

RBS spectrum showing the three regions that are used for producing maps. The lines for Ca and Fe+Cr are for information only and show the energy of the ions scattered on the surface.


  • Maps of the wear track obtained from the regions in the PIXE and RBS spectra
Foto: PIXE and RBS maps of wear track V57 ©Copyright: Dr. Frans Munnik

PIXE (Cr, Fe, Cu) and RBS (O, Si, all) maps of the wear track made by the SiC counter body


Contact area on a steel counter body

  • PIXE and RBS with a 3 MeV H-ion beam
Foto: PIXE spectrum for counter body V57 (steel) ©Copyright: Dr. Frans Munnik

PIXE spectrum for the steel counter body showing the region for the main elements of steel (Cr, Mn, and Fe) and indicatiions for the Cu and pile-up peaks.

Foto: RBS spectrum for counterbody K59 (steel) ©Copyright: Dr. Frans Munnik

RBS spectrum for the steel counter body showing the regions for carbon (C) and for the main elements of steel near the surface (sur). The waves in the spectrum near this last region are caused by resonances in the non-Rutherford cross-sections.


  • Maps of the area on the counter body that was in contact with the ta-C coating
Foto: PIXE and RBS maps for counterbody K59 (steel) ©Copyright: Dr. Frans Munnik

PIXE map for Cr, Mn, and Fe (middle) and RBS maps for carbon (C, left) and for the main elements of steel near the surface (Surface, right). The black line in the maps is caused by a temporary loss of the ion beam.

  • RBS spectra are extracted from selected regions to do a detailed analysis
Foto: RBS spectra for rois for steel CB ©Copyright: Dr. Frans Munnik

RBS spectra for regions on a horizontal line across the carbon-rich area that show the increasing carbon content (channels 400 - 520). The positions of the regions are shown in the inset.

Conclusion

  • Optimising measurement conditions can provide information for both
    • a light matrix, the ta-C coating, using a 2 MeV He-ion beam and
    • a heavy matrix, the counter body, using a 3 MeV H-ion beam.
  • RBS provides depth information and is sensitive to the surface and
    • using a 3 MeV H-ion beam is especially useful for detecting light elements like C and O in a heavy matrix.
  • PIXE provides good elemental identification and sensitivity but is not depth sensitive,
    • using a 2 MeV He-ion beam increases the sensitivity for light elements.
  • Elemental maps are a useful tool to study transfer of material.

This work is part of the Deutsche Forschungsgemeinschaft (DFG) Projekt TRIGUS (415726702)