1 / 42

ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples

ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental Sciences University of Manchester. Reading:

callie
Télécharger la présentation

ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental Sciences University of Manchester Reading: • D Murphy, The design of single particle laser mass spectrometers, in: Mass Spectrometry Reviews, 2007, 26, 150-165. • M. R. Canagaratna et al., Chemical and microphysical characterisation of ambient aerosols with the Aerodyne Aerosol Mass Spectrometer in: Mass Spectrometry Reviews, 2007, 26, 185-222. • H. Coe and J. D. Allan, “Aerosol Mass Spectrometry” in “Atmospheric techniques” ed D. E. Heard, Blackwell Scientific Publishing, 2006 • http://cires.colorado.edu/jimenez/ams-papers.html • thanks to Jose Jimenez for the slides showing component parts of aerosol mass spectrometers

  2. General Outline • General Introduction – the advantages of Aerosol Mass Spectrometry • The component parts of an aerosol mass spectrometer • Examples of different mass spectrometric methods • Advantages and disadvantages of different mass spectrometric methods

  3. General Outline • General Introduction – the advantages of Aerosol Mass Spectrometry • The component parts of an aerosol mass spectrometer • Examples of different mass spectrometric methods • Advantages and disadvantages of different mass spectrometric methods

  4. General Outline • General Introduction – the advantages of Aerosol Mass Spectrometry • The component parts of an aerosol mass spectrometer • Examples of different mass spectrometric methods • Advantages and disadvantages of different mass spectrometric methods

  5. thanks to Jose Jimenez for the slides showing component parts of aerosol mass spectrometers

  6. Aerosol Inlets • Need to entrain aerosols from the atmosphere into a vacuum • Aerosol Inlets • Need to entrain aerosols from the atmosphere into a vacuum • Need to concentrate particles and remove the gas • 2.5 x 1019 molecules cm-3 in ambient air • 3.2 µg m-3 of particulate S = 10-7 moles m-3 of S • 6.2x1023x10-7x10-6=6.2x1010 molecules cm-3 • or around 2 ppb • Aerosol Inlets • Need to entrain aerosols from the atmosphere into a vacuum • Need to concentrate particles and remove the gas • 2.5 x 1019 molecules cm-3 in ambient air • 3.2 µg m-3 of particulate S = 10-7 moles m-3 of S • 6.2x1023x10-7x10-6=6.2x1010 molecules cm-3 • or around 2 ppb • May need to introduce a size dependent velocity onto the particles

  7. Effects on beam width • non spherical particles may affect the ability of particle lens systems to focus the particle beam

  8. Vaporization • Desorption/ionisation process can be coupled together • - This is certainly simpler but it is very difficult to quantify the mass of material detected • A two step process of desorption followed subsequently by ionisation provides a way of more easily quantifying mass • However, this comes at a price • - More volatile species may decompose • - Refractory material (NaCl, dust, soot) will not evapourate unless the temperature is very high • Vaporisation may be performed by • Thermal methods or • IR laser absorption

  9. Ionization Ideally should: • Produce ions from either solid or liquid particles or the desorbed gas • Need to produce a high number of ions per molecule (high efficiency) • Ideally the number of ions produced is proportional to the number of molecules • The ionisation is selective and universal • The molecular fragmentation is reproducible

  10. Laser Desorption/Ionisation: • The LDI process on particles is poorly understood • Laser wavelength is important • Sulphuric acid hard to ionise – due to transparency in UV • Dependent on laser beam cross sectional intensity • Laser pulse width dependence • In larger particles, not all particle may be ionized • Laser power density • -lower fluence reduces fragmentation • -higher fluence allows improved ionisation

  11. Ion Trap • Can do MSn • Can investigate ion-molecule reactions

  12. General Outline • General Introduction – the advantages of Aerosol Mass Spectrometry • The component parts of an aerosol mass spectrometer • Examples of different mass spectrometric methods • Advantages and disadvantages of different mass spectrometric methods

  13. General Outline • General Introduction – the advantages of Aerosol Mass Spectrometry • The component parts of an aerosol mass spectrometer • Examples of different mass spectrometric methods • Advantages and disadvantages of different mass spectrometric methods

  14. Advantages/Disadvantages of laser and thermal systems: • laser based systems: thermal systems: • can ionise a wide range of - Can be used to deliver • species quantitative mass information • -deliver single particle info - deliver information on the • and so enable estimates of particle ensemble • mixing state • -do not have consistent - Can be traced back to • ionisation and suffer shot to well characterised ionisation • shot variability libraries

  15. Example: PALMS (Murphy et al NOAA)

  16. Example: PALMS (Murphy et al NOAA) Murphy, D.M., Thomson, D.S. & Mahoney, T.M.J. (1998b) In situ measurements of organics, meteoritic material, mercury, and other elements in aerosols at 5 to 19 kilometers, Science, 282 (5394), 1664–1669.

  17. Example: Dall’Osto et al (Birmingham) ATOFMS Identification of Hydroxymethanesulphonate during urban fog processing event REPARTEE experiment in central London ART-2a analysis based on a neural network algorithm was used to identify a number of different particle classes

  18. Example: Dall’Osto et al (Birmingham) ATOFMS Identification of Hydroxymethanesulphonate during urban fog processing event

  19. Example: Jim Smith (NCAR) Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

  20. Example: Jim Smith (NCAR) Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

  21. Example: Jim Smith (NCAR) Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

  22. Example: Jim Smith (NCAR) Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

  23. Example: Jim Smith (NCAR) Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

More Related