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

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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

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

Page 1: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

ISSAOS 2008

l‘Aquila, September 2008

Aerosol Mass Spectrometry:

General Principles and examples

Hugh CoeSchool of Earth, Atmospheric and Environmental Sciences

University of ManchesterReading:

• 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

Page 2: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

I. General Introduction – the advantages of Aerosol Mass Spectrometry

II. The component parts of an aerosol mass spectrometer

III. Examples of different mass spectrometric methods

IV. Advantages and disadvantages of different mass spectrometric methods

General Outline

Page 3: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

I. General Introduction – the advantages of Aerosol Mass Spectrometry

II. The component parts of an aerosol mass spectrometer

III. Examples of different mass spectrometric methods

IV. Advantages and disadvantages of different mass spectrometric methods

General Outline

Page 4: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
Page 5: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
Page 6: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
Page 7: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

I. General Introduction – the advantages of Aerosol Mass Spectrometry

II. The component parts of an aerosol mass spectrometer

III. Examples of different mass spectrometric methods

IV. Advantages and disadvantages of different mass spectrometric methods

General Outline

Page 8: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

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

Page 9: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

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

Page 10: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
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Page 13: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Effects on beam width

• non spherical particles may affect the ability of particle lens systems to focus the particle beam

Page 14: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
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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

Page 20: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

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

Page 21: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
Page 22: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

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

Page 23: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
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Ion Trap

• Can do MSn

• Can investigate ion-molecule reactions

Page 28: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

I. General Introduction – the advantages of Aerosol Mass Spectrometry

II. The component parts of an aerosol mass spectrometer

III. Examples of different mass spectrometric methods

IV. Advantages and disadvantages of different mass spectrometric methods

General Outline

Page 29: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
Page 30: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
Page 31: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.
Page 32: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

I. General Introduction – the advantages of Aerosol Mass Spectrometry

II. The component parts of an aerosol mass spectrometer

III. Examples of different mass spectrometric methods

IV. Advantages and disadvantages of different mass spectrometric methods

General Outline

Page 33: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

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

Page 34: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: PALMS (Murphy et al NOAA)

Page 35: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

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.

Page 36: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: Dall’Osto et al (Birmingham)

ATOFMS Identification of Hydroxymethanesulphonate during urban fog processing event

ART-2a analysis based on a neural network algorithm was used to identify a number of different particle classes

REPARTEE experiment in central London

Page 37: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: Dall’Osto et al (Birmingham)

ATOFMS Identification of Hydroxymethanesulphonate during urban fog processing event

Page 38: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: Jim Smith (NCAR)

Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

Page 39: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: Jim Smith (NCAR)

Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

Page 40: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: Jim Smith (NCAR)

Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

Page 41: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: Jim Smith (NCAR)

Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles

Page 42: ISSAOS 2008 l‘Aquila, September 2008 Aerosol Mass Spectrometry: General Principles and examples Hugh Coe School of Earth, Atmospheric and Environmental.

Example: Jim Smith (NCAR)

Thermal Desorption Ionisation Chemical-Ionisation MS (TDICIMS) chemical analysis of ultrafine particles