Improved Inversion of Scanning DMA Data

By D. Collins, R. Flagan, John H. Seinfeld. 2002

158 citations recorded by the source corpus.

Subfields: Atmospheric Science, Physical and Theoretical Chemistry, Water Science and Technology

View Paper: https://www.semanticscholar.org/paper/15f235ec6483475133ec0f61fa575a27165cafd9

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. M. Petters
2. S. Kreidenweis
3. A. Prenni
4. Renyi Zhang
5. J. Medina
6. Richard H. Moore
7. P. DeMott
8. C. Carrico

In Physical and Theoretical Chemistry

1. J. Medina
2. Martin Gysel
3. Richard H. Moore
4. G. Mcfiggans
5. A. Nenes
6. H. Coe

In Water Science and Technology

1. J. Medina
2. Martin Gysel
3. Richard H. Moore
4. Hans Moosmüller
5. P. Mcmurry
6. G. Mcfiggans
7. A. Nenes
8. H. Coe

Citations in the corpus

• Inversion of tandem differential mobility analyser (TDMA) measurements (2009, methodology): “Otherwise an extra inversion step removing the CPC’s smearing effect from the recorded signal is required prior to further data analysis (e.g. Collins et al., 2002).”
• Scanning Mobility CCN Analysis—A Method for Fast Measurements of Size-Resolved CCN Distributions and Activation Kinetics (2010, methodology): “This issue could be addressed by increasing the voltage scan time at low supersaturations, or accounting for the integration time in the inversion (e.g., Russell et al. 1995; Collins et al. 2002).”
• Mobility particle size spectrometers: Calibration procedures and measurement uncertainties (2018, unknown): “The “ DMA transfer function ” (Birmili et al. 1997; Collins et al. 2002; Hagwood et al. 1999; Knutson and Whitby 1975; Russell et al. 1995; Stolzenburg 1988; Zhang and Flagan 1996) can be described as a triangle selecting a range of electrical mobilities with an averaged transfer probability of 50%.”
• Formation of highly hygroscopic soot aerosols upon internal mixing with sulfuric acid vapor (2009, methodology): “Particle size distributions were obtained from these data by taking into account particle charging probabilities and the instrument response, which included DMA transfer function, DMA diffusion broadening, diffusion losses in the connecting tubing, and CPC counting efficiency [Collins et al., 2002].”
• Cloud condensation nucleation activity of biomass burning aerosol (2009, background): “Many DMA inversion algorithms have been proposed in the literature, each valid for a certain experi- mental setup [e.g., Alofs and Balakumar, 1982; Collins et al., 2002; Gysel et al., 2009; Stratmann et al., 1997].”