z-logo
open-access-imgOpen Access
Characterization of individual airborne particles by using aerosol time‐of‐flight mass spectrometry at Mace Head, Ireland
Author(s) -
Dall'Osto Manuel,
Beddows David C. S.,
Kinnersley Robert P.,
Harrison Roy M.,
Donovan Robert J.,
Heal Mathew R.
Publication year - 2004
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2004jd004747
Subject(s) - aerosol , sea salt , mass spectrometry , atmospheric sciences , chemical composition , environmental science , range (aeronautics) , air mass (solar energy) , sulfate , mineralogy , environmental chemistry , geology , chemistry , materials science , meteorology , physics , organic chemistry , boundary layer , chromatography , composite material , thermodynamics
An aerosol time‐of‐flight mass spectrometer was deployed at Mace Head (Ireland) during August 2002. The measurements provide qualitative chemical composition and size distribution (0.3–3 μm) information for single particles. Three broad categories of particles: sea salt, dust, and carbon‐containing particles were identified and apportioned, and their temporal evolution (1 hour resolution) is described. Aerosol sources were correlated with meteorological factors and with air mass trajectories, demonstrating long‐range transport of different continental air masses from Europe, Africa, and America. The major class of particles was derived from sea salt and was subdivided into pure, mixed, and aged sea salt according to the extent of displacement of chloride by nitrate. Two types of dust particles were found mainly in the coarse mode (>1 μm); the former, thought to originate from the Sahara, presented an aluminium/silicon signature, while the latter, of more local origin, had a calcium‐rich composition. Carbon‐containing particles were mainly distributed in the fine mode (<1 μm) and associated with different chemical species in different size modes, suggesting different mechanisms of formation.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom