Aerosol analysis using a Thermal-Desorption Proton-Transfer-Reaction Mass Spectrometer (TD-PTR-MS): a new approach to study processing of organic aerosols
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作者:
Holzinger, R.
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Inst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, NetherlandsInst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, Netherlands
Holzinger, R.
[1
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Williams, J.
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Max Planck Inst Chem, D-55128 Mainz, GermanyInst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, Netherlands
Williams, J.
[2
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Herrmann, F.
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Max Planck Inst Chem, D-55128 Mainz, GermanyInst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, Netherlands
Herrmann, F.
[2
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Lelieveld, J.
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Max Planck Inst Chem, D-55128 Mainz, GermanyInst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, Netherlands
Lelieveld, J.
[2
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Donahue, N. M.
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Carnegie Mellon Univ, Ctr Atmospher Particle Studies, Pittsburgh, PA 15213 USAInst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, Netherlands
Donahue, N. M.
[3
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Rockmann, T.
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Inst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, NetherlandsInst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, Netherlands
Rockmann, T.
[1
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机构:
[1] Inst Marine & Atmospher Res Utrecht, NL-3584 CC Utrecht, Netherlands
[2] Max Planck Inst Chem, D-55128 Mainz, Germany
[3] Carnegie Mellon Univ, Ctr Atmospher Particle Studies, Pittsburgh, PA 15213 USA
We present a novel analytical approach to measure the chemical composition of organic aerosol. The new instrument combines proton-transfer-reaction mass-spectrometry (PTR-MS) with a collection-thermal-desorption aerosol sampling technique. For secondary organic aerosol produced from the reaction of ozone with isoprenoids in a laboratory reactor, the TD-PTR-MS instrument detected typically 80% of the mass that was measured with a scanning mobility particle sizer (SMPS). The first field deployment of the instrument was the EUCAARI-IOP campaign at the CESAR tall tower site in the Netherlands. For masses with low background values (similar to 30% of all masses) the detection limit of aerosol compounds was below 0.2 ng/m(3) which corresponds to a sampled compound mass of 35 pg. Comparison of thermograms from ambient samples and from chamber-derived secondary organic aerosol shows that, in general, organic compounds from ambient aerosol samples desorb at much higher temperatures than chamber samples. This suggests that chamber aerosol is not a good surrogate for ambient aerosol and therefore caution is advised when extrapolating results from chamber experiments to ambient conditions.