Chemistry of the Upper and Lower Atmosphere 2000
DOI: 10.1016/b978-012257060-5/50013-7
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Analytical Methods and Typical Atmospheric Concentrations for Gases and Particles

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Cited by 14 publications
(7 citation statements)
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“…Although the ATOFMS response is matrix-sensitive and may not directly reflect the quantitative composition of the measured aerosol (Gross et al, 2000;Fergenson et al, 2001;Bhave et al, 2002;Sullivan and Prather, 2005;Allen et al, 2006;Dall'Osto et al, 2006), relative peak intensities can be meaningful when particle constitution within a measured sample has not changed considerably during a given investigation (Gard et al, 1998;Finlayson-Pitts and Pitts, 2000). In this sense, the use of ATOFMS as a semi-quantifiable approach for the analysis of aged OL particles as a function of particle size is justifiable because individual laboratory based particles studied under experimentally controlled conditions are far less complex -and variable -than atmospheric aerosol (Allen, 2004).…”
Section: Aerosol Time-of-flight Mass Spectrometermentioning
confidence: 99%
“…Although the ATOFMS response is matrix-sensitive and may not directly reflect the quantitative composition of the measured aerosol (Gross et al, 2000;Fergenson et al, 2001;Bhave et al, 2002;Sullivan and Prather, 2005;Allen et al, 2006;Dall'Osto et al, 2006), relative peak intensities can be meaningful when particle constitution within a measured sample has not changed considerably during a given investigation (Gard et al, 1998;Finlayson-Pitts and Pitts, 2000). In this sense, the use of ATOFMS as a semi-quantifiable approach for the analysis of aged OL particles as a function of particle size is justifiable because individual laboratory based particles studied under experimentally controlled conditions are far less complex -and variable -than atmospheric aerosol (Allen, 2004).…”
Section: Aerosol Time-of-flight Mass Spectrometermentioning
confidence: 99%
“…Les valeurs obtenues 0,2 et 0,3 respectivement pour Fann et Faidherbe indiquent une déficience en chlore dans la formation du sel marin. Ceci pourrait se justifier par le fait que le Cl -est utilisé lors des réac-tions rapides du NaCl avec les acides sulfurique et nitrique lorsque l'humidité relative est comprise entre 50-100 %, contribuant ainsi à la production du HCl gazeux [24]. En effet, l'humidité relative moyenne de cette période est de 79 % [25].…”
Section: Discussionunclassified
“…The results using such systems provide insights about the properties of the inhaled aerosol, such as the sizes of the inhaled particles and the deposition fraction, which can be used for comparison with radionuclide imaging studies [ 19 ] or to validate in silico dosimetry models [ 20 , 21 , 22 ]. Cascade impactors consist of stages, each containing impaction plates which represent obstacles for an incoming airstream [ 23 ]. These plates create an abrupt bend in the airstream causing the particles, whose inertia exceeds a cutoff size, to deposit [ 24 ].…”
Section: Introductionmentioning
confidence: 99%