Publication


Featured researches published by Quentin Malloy.


Aerosol Science and Technology | 2009

Real-Time Aerosol Density Determination Utilizing a Modified Scanning Mobility Particle Sizer—Aerosol Particle Mass Analyzer System

Quentin Malloy; Shunsuke Nakao; Li Qi; Rebecca L. Austin; Clayton Stothers; Hiroyuki Hagino; David R. Cocker

Real time secondary organic aerosol (SOA) density evolution for m-xylene photo-oxidation and α-pinene ozonolysis was obtained using an Aerosol Particle Mass Analyzer (APM)/Scanning Mobility Particle Spectrometer (SMPS) setup, which has been modified to achieve higher transmission of particles and improved sampling frequency. The aerosol density of SOA generated from α-pinene ozonolysis was found to be 1.24 ± 0.03 g/cm3 while the aerosol generated from m-xylene photo-oxidation was determined to be 1.35 ± 0.03 g/cm3. These results confirm the measurement approach from a combined SMPS and Aerodyne Aerosol Mass Spectrometer (AMS) system and are found to be within good agreement with the effective density measurements.


Journal of Chromatography A | 2010

Determination of methylamines and trimethylamine-N-oxide in particulate matter by non-suppressed ion chromatography.

Mark Erupe; Allegra Liberman-Martin; Philip J. Silva; Quentin Malloy; Naomi Yonis; David R. Cocker; Kathleen L. Purvis-Roberts

An ion chromatography method with non-suppressed conductivity detection was developed for the simultaneous determination of methylamines (methylamine, dimethylamine, trimethylamine) and trimethylamine-N-oxide in particulate matter air samples. The analytes were well separated by means of cation-exchange chromatography using a 3 mM nitric acid/3.5% acetonitrile (v/v) eluent solution and a Metrosep C 2 250 (250 mm x 4 mm i.d.) separation column. The effects of the different chromatographic parameters on the separation were also investigated. Detection limits of methylamine, dimethylamine, trimethylamine, and trimethylamine-N-oxide were 43, 46, 76 and 72 microg/L, respectively. The relative standard deviations of the retention times were between 0.42% and 1.14% while the recoveries were between 78.8% and 88.3%. The method is suitable for determining if methylamines and trimethylamine-N-oxide are a significant component of organic nitrogen aerosol in areas with high concentration of these species.


Atmospheric Environment | 2008

In-use gaseous and particulate matter emissions from a modern ocean going container vessel

Harshit Agrawal; Quentin Malloy; William A. Welch; J. Wayne Miller; David R. Cocker


Environmental Science & Technology | 2008

Trimethylamine as precursor to secondary organic aerosol formation via nitrate radical reaction in the atmosphere.

Philip J. Silva; Mark Erupe; Derek J. Price; John Elias; Quentin Malloy; Qi Li; Bethany Warren; David R. Cocker


Atmospheric Chemistry and Physics | 2008

Secondary organic aerosol formation from primary aliphatic amines with NO 3 radical

Quentin Malloy; Li Qi; Bethany Warren; David R. Cocker; Mark E. Erupe; Philip J. Silva


Atmospheric Environment | 2010

Can secondary organic aerosol formed in an atmospheric simulation chamber continuously age

Li Qi; Shunsuke Nakao; Quentin Malloy; Bethany Warren; David R. Cocker


Environmental Science & Technology | 2007

Impact of propene on secondary organic aerosol formation from m-xylene.

Chen Song; Kwangsam Na; Bethany Warren; Quentin Malloy; David R. Cocker


Environmental Science & Technology | 2007

Secondary Organic Aerosol Formation from the Photooxidation of p- and o-Xylene

Chen Song; Kwangsam Na; Bethany Warren; Quentin Malloy; David R. Cocker


Environmental Science & Technology | 2007

Secondary Organic Aerosol Formation from m-Xylene in the Absence of NOx

Chen Song; Kwangsam Na; Bethany Warren; Quentin Malloy; David R. Cocker


Atmospheric Environment | 2009

Secondary organic aerosol formation from cyclohexene ozonolysis in the presence of water vapor and dissolved salts

Bethany Warren; Quentin Malloy; L. D. Yee; David R. Cocker

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