Danielle C. Draper
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View article: NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere
NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere Open
View article: Observations of gas-phase products from the nitrate-radical-initiated oxidation of four monoterpenes
Observations of gas-phase products from the nitrate-radical-initiated oxidation of four monoterpenes Open
Chemical ionization mass spectrometry with the nitrate reagent ion (NO3- CIMS) was used to investigate the products of the nitrate radical (NO3) initiated oxidation of four monoterpenes in laboratory chamber experiments. α-Pinene, β-pinene…
View article: Comment on acp-2021-1020
Comment on acp-2021-1020 Open
Abstract. Chemical ionization mass spectrometry with nitrate reagent ion (NO3− CIMS) was used to investigate the products of nitrate radical (NO3) initiated oxidation of four monoterpenes i…
View article: Comment on acp-2021-1020
Comment on acp-2021-1020 Open
Abstract. Chemical ionization mass spectrometry with the nitrate reagent ion (NO3-Â CIMS) was used to investigate the products of the nitrate radical (NO3) initiated oxidat…
View article: Supplementary material to "Observations of gas-phase products from the nitrate radical-initiated oxidation of four monoterpenes"
Supplementary material to "Observations of gas-phase products from the nitrate radical-initiated oxidation of four monoterpenes" Open
KinSim model rate constants and resultsSummary of rate constants used for the model are shown in Table S1 and results for the a-pinene and b-pinene systems are shown in Figure S1.Most come from the JPL Kinetics Data Evaluation (JPL 2015) o…
View article: Observations of gas-phase products from the nitrate radical-initiated oxidation of four monoterpenes
Observations of gas-phase products from the nitrate radical-initiated oxidation of four monoterpenes Open
Chemical ionization mass spectrometry with nitrate reagent ion (NO3− CIMS) was used to investigate the products of nitrate radical (NO3) initiated oxidation of four monoterpenes in laboratory chamber experiments. α-Pinene, β-pinene, Δ-3-ca…
View article: Heterogeneous Nucleation Drives Particle Size Segregation in Sequential Ozone and Nitrate Radical Oxidation of Catechol
Heterogeneous Nucleation Drives Particle Size Segregation in Sequential Ozone and Nitrate Radical Oxidation of Catechol Open
Secondary organic aerosol formation via condensation of organic vapors onto existing aerosol transforms the chemical composition and size distribution of ambient aerosol, with implications for air quality and Earth's radiative balance. Gas…
View article: Atmospheric clusters to nanoparticles: Recent progress and challenges in closing the gap in chemical composition
Atmospheric clusters to nanoparticles: Recent progress and challenges in closing the gap in chemical composition Open
View article: Molecular understanding of new-particle formation from <i>α</i> -pinene between −50 and +25 °C
Molecular understanding of new-particle formation from <i>α</i> -pinene between −50 and +25 °C Open
Highly oxygenated organic molecules (HOMs) contribute substantially to the formation and growth of atmospheric aerosol particles, which affect air quality, human health and Earth's climate. HOMs are formed by rapid, gas-phase autoxidation …
View article: Size-dependent influence of NO <sub>x</sub> on the growth rates of organic aerosol particles
Size-dependent influence of NO <sub>x</sub> on the growth rates of organic aerosol particles Open
NO x is important for particle growth as it can participate in HOM formation and alter the HOM volatility distribution.
View article: Supplementary material to "Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C"
Supplementary material to "Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C" Open
View article: Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C
Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C Open
Highly-oxygenated organic molecules (HOMs) contribute substantially to the formation and growth of atmospheric aerosol particles, which affect air quality, human health and Earth's climate. HOMs are formed by rapid, gas-phase autoxidation …
View article: Atmospheric fungal nanoparticle bursts
Atmospheric fungal nanoparticle bursts Open
Bursts of fungal nanoparticle fragments were detected in ambient air.
View article: Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors
Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors Open
Atmospheric aerosol formation from biogenic vapors is strongly affected by air pollutants, like NO x , SO 2 , and NH 3 .
View article: Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range
Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range Open
Significance Aerosol particles can form and grow by gas-to-particle conversion and eventually act as seeds for cloud droplets, influencing global climate. Volatile organic compounds emitted from plants are oxidized in the atmosphere, and t…
View article: Water condensation-based nanoparticle charging system: Physical and chemical characterization
Water condensation-based nanoparticle charging system: Physical and chemical characterization Open
A water condensation-based ion charging system has been developed to enhance both the charging efficiency and the concentration of sub-20 nm particles. This NanoCharger consists of a bipolar ion source followed by a parallel plate water-ba…
View article: The role of ions in new particle formation in the CLOUD chamber
The role of ions in new particle formation in the CLOUD chamber Open
The formation of secondary particles in the atmosphere accounts for more than half of global cloud condensation nuclei. Experiments at the CERN CLOUD (Cosmics Leaving OUtdoor Droplets) chamber have underlined the importance of ions for new…
View article: The Role Of Ions In New-Particle Formation In The Cloud Chamber: Supporting Data
The Role Of Ions In New-Particle Formation In The Cloud Chamber: Supporting Data Open
Data that is presented in the publication "The role of ions in new-particle formation in the CLOUD chamber", ACP 2017.
View article: The Role Of Ions In New-Particle Formation In The Cloud Chamber: Supporting Data
The Role Of Ions In New-Particle Formation In The Cloud Chamber: Supporting Data Open
Data that is presented in the publication "The role of ions in new-particle formation in the CLOUD chamber", ACP 2017.
View article: The role of ions in new-particle formation in the CLOUD chamber
The role of ions in new-particle formation in the CLOUD chamber Open
The formation of secondary particles in the atmosphere accounts for more than half of global cloud condensation nuclei. Experiments at the CERN CLOUD (Cosmics Leaving OUtdoor Droplets) chamber have underlined the importance of ions for new…
View article: Secondary organic aerosol formation from in situ OH, O <sub>3</sub> , and NO <sub>3</sub> oxidation of ambient forest air in an oxidation flow reactor
Secondary organic aerosol formation from in situ OH, O <sub>3</sub> , and NO <sub>3</sub> oxidation of ambient forest air in an oxidation flow reactor Open
Ambient pine forest air was oxidized by OH, O3, or NO3 radicals using an oxidation flow reactor (OFR) during the BEACHON-RoMBAS (Bio–hydro–atmosphere interactions of Energy, Aerosols, Carbon, H2O, Organics and Nitrogen – Rocky Mountain Bio…
View article: Secondary organic aerosol formation from in situ OH, O <sub>3</sub> , and NO <sub>3</sub> oxidation of ambient forest air in an oxidation flow reactor
Secondary organic aerosol formation from in situ OH, O <sub>3</sub> , and NO <sub>3</sub> oxidation of ambient forest air in an oxidation flow reactor Open
Ambient pine forest air was oxidized by OH, O3, or NO3 radicals using an oxidation flow reactor (OFR) during the BEACHON-RoMBAS (Bio-hydro-atmosphere interactions of Energy, Aerosols, Carbon, H2O, Organics & Nitrogen–Rocky Mountain Bio…
View article: The lifetime of nitrogen oxides in an isoprene-dominated forest
The lifetime of nitrogen oxides in an isoprene-dominated forest Open
The lifetime of nitrogen oxides (NOx) affects the concentration and distribution of NOx and the spatial patterns of nitrogen deposition. Despite its importance, the lifetime of NOx is poorly constrained in rural and remote continental regi…
View article: The Lifetime of Nitrogen Oxides in an Isoprene Dominated Forest
The Lifetime of Nitrogen Oxides in an Isoprene Dominated Forest Open
The lifetime of NOx (NOx ≡ NO + NO2) affects the concentration and distribution of NOx and the spatial patterns of nitrogen deposition. Despite its importance, the lifetime of NOx is poorly constrained in rural and remote continental regio…
View article: Organic nitrate aerosol formation via NO&lt;sub&gt;3&lt;/sub&gt; + biogenic volatile organic compounds in the southeastern United States
Organic nitrate aerosol formation via NO<sub>3</sub> + biogenic volatile organic compounds in the southeastern United States Open
Abstract. Gas- and aerosol-phase measurements of oxidants, biogenic volatile organic compounds (BVOCs) and organic nitrates made during the Southern Oxidant and Aerosol Study (SOAS campaign, Summer 2013) in central Alabama…
View article: A qualitative comparison of secondary organic aerosol yields and composition from ozonolysis of monoterpenes at varying concentrations of NO <sub>2</sub>
A qualitative comparison of secondary organic aerosol yields and composition from ozonolysis of monoterpenes at varying concentrations of NO <sub>2</sub> Open
The effect of NO2 on secondary organic aerosol (SOA) formation from ozonolysis of α-pinene, β-pinene, Δ3-carene, and limonene was investigated using a dark flow-through reaction chamber. SOA mass yields were calculated for each monoterpene…
View article: Influence of crustal dust and sea spray supermicron particle concentrations and acidity on inorganic NO <sub>3</sub> <sup>−</sup> aerosol during the 2013 Southern Oxidant and Aerosol Study
Influence of crustal dust and sea spray supermicron particle concentrations and acidity on inorganic NO <sub>3</sub> <sup>−</sup> aerosol during the 2013 Southern Oxidant and Aerosol Study Open
Inorganic aerosol composition was measured in the southeastern United States, a region that exhibits high aerosol mass loading during the summer, as part of the 2013 Southern Oxidant and Aerosol Study (SOAS) campaign. Measurements using a …
View article: Organic nitrate aerosol formation via NO <sub>3</sub> + BVOC in the Southeastern US
Organic nitrate aerosol formation via NO <sub>3</sub> + BVOC in the Southeastern US Open
Gas- and aerosol-phase measurements of oxidants, biogenic volatile organic compounds (BVOC) and organic nitrates made during the Southern Oxidant and Aerosol Study (SOAS campaign, Summer 2013) in central Alabama show that nitrate radical (…
View article: A comparison of secondary organic aerosol (SOA) yields and composition from ozonolysis of monoterpenes at varying concentrations of NO <sub>2</sub>
A comparison of secondary organic aerosol (SOA) yields and composition from ozonolysis of monoterpenes at varying concentrations of NO <sub>2</sub> Open
The effect of NO2 on secondary organic aerosol (SOA) formation from ozonolysis of α-pinene, β-pinene, Δ3-carene, and limonene was investigated using a dark flow-through reaction chamber. SOA mass yields were calculated for each monoterpene…
View article: Influence of mineral dust and sea spray supermicron particle concentrations and acidity on inorganic NO <sub>3</sub> <sup>−</sup> aerosol during the 2013 Southern Oxidant and Aerosol Study
Influence of mineral dust and sea spray supermicron particle concentrations and acidity on inorganic NO <sub>3</sub> <sup>−</sup> aerosol during the 2013 Southern Oxidant and Aerosol Study Open
The inorganic aerosol composition was measured in the southeastern United States, a region that exhibits high aerosol mass loading during the summer, as part of the 1 June to 15 July 2013 Southern Oxidant and Aerosol Study (SOAS) campaign.…