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Dive into the research topics where J. F. Hunter is active.

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Featured researches published by J. F. Hunter.


Atmospheric Chemistry and Physics | 2014

Laboratory studies of the aqueous-phase oxidation of polyols: submicron particles vs. bulk aqueous solution

Kelly E. Daumit; A. J. Carrasquillo; J. F. Hunter; Jesse H. Kroll

Abstract. Oxidation in the atmospheric aqueous phase (cloud droplets and deliquesced particles) has received recent attention as a potential pathway for the formation of highly oxidized organic aerosol. Most laboratory studies of aqueous-phase oxidation, however, are carried out in bulk solutions rather than aqueous droplets. Here we describe experiments in which aqueous oxidation of polyols (water-soluble species with chemical formula CnH2n+2On) is carried out within submicron particles in an environmental chamber, allowing for significant gas–particle partitioning of reactants, intermediates, and products. Dark Fenton chemistry is used as a source of hydroxyl radicals, and oxidation is monitored using a high-resolution aerosol mass spectrometer (AMS). Aqueous oxidation is rapid, and results in the formation of particulate oxalate; this is accompanied by substantial loss of carbon to the gas phase, indicating the formation of volatile products. Results are compared to those from analogous oxidation reactions carried out in bulk solution. The bulk-phase chemistry is similar to that in the particles, but with substantially less carbon loss. This is likely due to differences in partitioning of early-generation products, which evaporate out of the aqueous phase under chamber conditions (in which liquid water content is low), but remain in solution for further aqueous processing in the bulk phase. This work suggests that the product distributions from oxidation in aqueous aerosol may be substantially different from those in bulk oxidation experiments. This highlights the need for aqueous oxidation studies to be carried out under atmospherically relevant partitioning conditions, with liquid water contents mimicking those of cloud droplets or aqueous aerosol.


Environmental Science & Technology | 2014

Secondary Organic Aerosol Formation from Acyclic, Monocyclic, and Polycyclic Alkanes

J. F. Hunter; A. J. Carrasquillo; Kelly E. Daumit; Jesse H. Kroll

A large number of organic species emitted into the atmosphere contain cycloalkyl groups. While cyclic species are believed to be important secondary organic aerosol (SOA) precursors, the specific role of cyclic moieties (particularly for species with multiple or fused rings) remains uncertain. Here we examine the yields and composition of SOA formed from the reaction of OH with a series of C10 (cyclo)alkanes, with 0-3 rings, in order to better understand the role of multiple cyclic moieties on aerosol formation pathways. A chamber oxidation technique using high, sustained OH radical concentrations was used to simulate long reaction times in the atmosphere. This aging technique leads to higher yields than in previously reported chamber experiments. Yields were highest for cyclic and polycyclic precursors, though yield exhibited little dependence on number of rings. However, the oxygen-to-carbon ratio of the SOA was highest for the polycyclic precursors. These trends are consistent with aerosol formation requiring two generations of oxidation and 3-4 oxygen-containing functional groups in order to condense. Cyclic, unbranched structures are protected from fragmentation during the first oxidation step, with C-C bond scission instead leading to ring opening, efficient functionalization, and high SOA yields. Fragmentation may occur during subsequent oxidation steps, limiting yields by forming volatile products. Polycyclic structures can undergo multiple ring opening reactions, but do not have markedly higher yields, likely due to enhanced fragmentation in the second oxidation step. By contrast, C-C bond scission for the linear and branched structures leads to fragmentation prior to condensation, resulting in low SOA yields. The results highlight the key roles of multigenerational chemistry and susceptibility to fragmentation in the formation and evolution of SOA.


Journal of Physical Chemistry A | 2014

Secondary Organic Aerosol Formation via the Isolation of Individual Reactive Intermediates: Role of Alkoxy Radical Structure

A. J. Carrasquillo; J. F. Hunter; Kelly E. Daumit; Jesse H. Kroll

The study of the chemistry underlying secondary organic aerosol (SOA) formation is complicated by the large number of reaction pathways and oxidation generations available to a given precursor species. Here we simplify such complexity to that of a single alkoxy radical (RO), by forming SOA via the direct photolysis of alkyl nitrite (RONO) isomers. Chamber experiments were conducted with 11 C10 RONO isomers to determine how the position of the radical center and branching of the carbon skeleton influences SOA formation. SOA yields served as a probe of RO reactivity, with lower yields indicating that fragmentation reactions dominate and higher yields suggesting the predominance of RO isomerization. The largest yields were from straight-chain isomers, particularly those with radical centers located toward the terminus of the molecule. Trends in SOA yields can be explained in terms of two major effects: (1) the relative importance of isomerization and fragmentation reactions, which control the distribution of products, and (2) differences in volatility among the various isomeric products formed. Yields from branched isomers, which were low but variable, provide insight into the degree of fragmentation of the alkoxy radicals; in the case of the two β-substituted alkoxy radicals, fragmentation appears to occur to a greater extent than predicted by structure-activity relationships. Our results highlight how subtle differences in alkoxy radical structure can have major impacts on product yields and SOA formation.


ASME 2011 Internal Combustion Engine Division Fall Technical Conference | 2011

Real-Time Measurements of Engine-Out Trace Elements: Application of a Novel Soot Particle Aerosol Mass Spectrometer for Emissions Characterization

Eben S. Cross; Alexander Sappok; Edward Charles Fortner; J. F. Hunter; John T. Jayne; W. A. Brooks; Timothy B. Onasch; Victor W. Wong; A. Trimborn; D. R. Worsnop; Jesse H. Kroll

Lubricant-derived trace element emissions are the largest contributors to the accumulation of incombustible ash in diesel particulate filters (DPF), eventually leading to filter plugging and an increase in engine fuel consumption. Particulate trace element emissions also pose adverse health effects and are the focus of increasingly stringent air quality regulations. To date, the rates and physical and chemical properties of lubricant-derived additive emissions are not well characterized, largely due to the difficulties associated with conducting the measurements. This work investigated the potential for conducting real-time measurements of lubricant-derived particle emissions. The experiment used the Soot Particle Aerosol Mass Spectrometer (SP-AMS) developed by Aerodyne Research to measure the size, mass and composition of submicron particles in the exhaust. Results confirm the ability of the SP-AMS to measure engine-out emissions of calcium, zinc, magnesium, phosphorous, and sulfur. Further, emissions of previously difficult to detect elements, such as boron, and low-level engine wear metals, such as lead, were also measured. This paper provides an overview of the results obtained with the SP-AMS, and demonstrates the utility of applying real-time techniques to engine-out and tailpipe-out trace element emissions. The SP-AMS used in this study was developed for real-time characterization of refractory particles (i.e. black carbon or soot) in the ambient atmosphere. The instrument consists of an intra-cavity laser (1064 nm) for particle vaporization followed by electron impact ionization and ion detection via a time-of-flight mass spectrometer. Application of the SP-AMS for engine exhaust characterization followed a two-part approach: (1) measurement validation, and (2) measurement of engine-out exhaust. Measurement validation utilized a diesel burner with precise control of lubricant consumption. Results showed a good correlation between CJ-4 oil consumption and measured levels of lubricant-derived trace elements in the particle phase. Following measurement validation, the SP-AMS measured engine-out emissions from a medium-duty diesel engine, operated over a standard speed/load matrix. This work demonstrates the utility of state-of-the-art online techniques (such as the SP-AMS) to measure engine-out emissions, including trace species derived from lubricant additives. Results help optimize the combined engine-lubricant-aftertreatment system and provide a real-time characterization of emissions. As regulations become more stringent and emission controls more complex, advanced measurement techniques with high sensitivity and fast time response will become an increasingly important part of engine characterization studies.© 2011 ASME


Atmospheric Chemistry and Physics | 2015

Effect of oxidant concentration, exposure time, and seed particles on secondary organic aerosol chemical composition and yield

Andrew T. Lambe; P.S. Chhabra; Timothy B. Onasch; William H. Brune; J. F. Hunter; Jesse H. Kroll; Molly J. Cummings; James F. Brogan; Y. Parmar; D. R. Worsnop; Charles E. Kolb; P. Davidovits


Atmospheric Chemistry and Physics | 2016

In situ secondary organic aerosol formation from ambient pine forest air using an oxidation flow reactor

Brett B. Palm; Pedro Campuzano-Jost; Amber M. Ortega; Douglas A. Day; Lisa Kaser; Werner Jud; Thomas Karl; Armin Hansel; J. F. Hunter; Eben S. Cross; Jesse H. Kroll; Zhe Peng; William H. Brune; Jose L. Jimenez


Atmospheric Chemistry and Physics | 2015

Phase partitioning and volatility of secondary organic aerosol components formed from α-pinene ozonolysis and OH oxidation: the importance of accretion products and other low volatility compounds

Felipe D. Lopez-Hilfiker; Claudia Mohr; Mikael Ehn; F. Rubach; E. Kleist; J. Wildt; Th. F. Mentel; A. J. Carrasquillo; Kelly E. Daumit; J. F. Hunter; Jesse H. Kroll; D. R. Worsnop; Judith Thornton


Atmospheric Measurement Techniques | 2009

Elemental analysis of aerosol organic nitrates with electron ionization high-resolution mass spectrometry

A. W. Rollins; Juliane L. Fry; J. F. Hunter; Jesse H. Kroll; D. R. Worsnop; S. W. Singaram; R. C. Cohen


Environmental Science & Technology | 2012

Mass Spectral Analysis of Organic Aerosol Formed Downwind of the Deepwater Horizon Oil Spill: Field Studies and Laboratory Confirmations

R. Bahreini; Ann M. Middlebrook; C. A. Brock; J. A. de Gouw; S. A. McKeen; Leah R. Williams; Kelly E. Daumit; Andrew T. Lambe; Paola Massoli; Manjula R. Canagaratna; Ravan Ahmadov; A. J. Carrasquillo; Eben S. Cross; B. Ervens; John S. Holloway; J. F. Hunter; Timothy B. Onasch; I. B. Pollack; James M. Roberts; T. B. Ryerson; Carsten Warneke; P. Davidovits; D. R. Worsnop; Jesse H. Kroll


Atmospheric Chemistry and Physics | 2013

Online measurements of the emissions of intermediate-volatility and semi-volatile organic compounds from aircraft

Eben S. Cross; J. F. Hunter; A. J. Carrasquillo; Jonathan P. Franklin; Scott C. Herndon; John T. Jayne; D. R. Worsnop; Richard C. Miake-Lye; Jesse H. Kroll

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Jesse H. Kroll

Pacific Northwest National Laboratory

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A. J. Carrasquillo

Massachusetts Institute of Technology

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Kelly E. Daumit

Massachusetts Institute of Technology

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John T. Jayne

Massachusetts Institute of Technology

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Douglas R. Worsnop

Finnish Meteorological Institute

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Brett B. Palm

University of Colorado Boulder

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