Field-deployable, high-resolution, time-of-flight aerosol mass spectrometer.
By P. DeCarlo, J. Kimmel, A. Trimborn, M. Northway, J. Jayne, A. Aiken, M. Gonin, K. Fuhrer, T. Horvath, K. Docherty and 2 more. Analytical Chemistry, 2006
2,055 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Engineering, Health, Toxicology and Mutagenesis
View Paper: https://www.semanticscholar.org/paper/683bdd7097df4caaccde3b63171ca73d14e7eadd
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Citations in the corpus
- Cloud condensation nuclei in pristine tropical rainforest air of Amazonia: size-resolved measurements and modeling of atmospheric aerosol composition and CCN activity (2009, positive): “An Aerodyne high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS, referred as " AMS " for brevity) was used to measure size-resolved chemical composition of non-refractory submicron aerosol particles (DeCarlo et al., 2006; Canagaratna et al., 2007; Chen et al., 2009).”
- A high-resolution mass spectrometer to measure atmospheric ion composition (2010, methodology): “…measurement methods of aerosol chemical composition (e.g., Jayne et al., 2000; Jimenez et al., 2002, 2009; Voisin et al., 2003; Smith et al., 2005; DeCarlo et al., 2006) has increased our capability to determine aerosol composition of smaller and smaller particles, down to 10 nm (Smith et al.,…”
- Particulate emissions from commercial shipping: Chemical, physical, and optical properties (2008, methodology): “…size-resolvedmass loadings of submicron particles weremeasured using a high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) developed at Aerodyne Research, Inc., (Billerica, Massachusetts, USA) [Allan et al., 2003; DeCarlo et al., 2006; Drewnick et al., 2005; Jayne et al., 2000].”
- Fine-particle pH for Beijing winter haze as inferred from different thermodynamic equilibrium models (2018, positive): “An Aerodyne high-resolution time-of-flight aerosol mass spectrometer (referred to as the AMS) was used to measure size-resolved non-refractory submicron aerosol (NR-PM 1 ) species (DeCarlo et al., 2006).”
- Optical properties and aging of light-absorbing secondary organic aerosol (2016, methodology): “The mass loading of the aerosol particles was measured using an Aerodyne highresolution time-of-flight mass spectrometer (HR-ToF-AMS) (DeCarlo et al., 2006), while the number and volume concentrations were measured with a TSI scanning mobility particle sizer (SMPS).”
- Methods for estimating uncertainty in PMF solutions: examples with ambient air and water quality data and guidance on reporting PMF results. (2015, background): “The HRAMSmeasures non-refractory PM1, includingdetailed spectra of organic aerosol (OA),which can then be decomposed by PMF (Allan et al., 2003; Jayne et al., 2000; Jimenez et al., 2003; DeCarlo et al., 2006; Ulbrich et al., 2009; Zhang et al., 2011; Lanz et al., 2010).”
- A simplified description of the evolution of organic aerosol composition in the atmosphere (2010, methodology): “This approach has recently been applied towards the mass spectrometric measurement of individual species within atmospheric OA [e.g., Bateman et al., 2009], but to our knowledge has not been used for bulk aerosol measurements.”