53 citations as recorded by crossref.

1. Characterization of organic nitrate constituents of secondary organic aerosol (SOA) from nitrate-radical-initiated oxidation of limonene using high-resolution chemical ionization mass spectrometry C. Faxon et al. 10.5194/acp-18-5467-2018
2. The effect of sub-zero temperature on the formation and composition of secondary organic aerosol from ozonolysis of alpha-pinene K. Kristensen et al. 10.1039/C7EM00231A
3. Aerosol Volatility and Enthalpy of Sublimation of Carboxylic Acids K. Salo et al. 10.1021/jp910105h
4. Thresholds of secondary organic aerosol formation by ozonolysis of monoterpenes measured in a laminar flow aerosol reactor F. Bernard et al. 10.1016/j.jaerosci.2011.08.005
5. Predicting Thermal Behavior of Secondary Organic Aerosols J. Offenberg et al. 10.1021/acs.est.7b01968
6. Recent advances on SOA formation in indoor air, fate and strategies for SOA characterization in indoor air - A review K. Pytel et al. 10.1016/j.scitotenv.2022.156948
7. Investigation of RH effect on uncommon limonene ozonolysis products and SOA formation in indoor air with real time measurement techniques K. Pytel & B. Zabiegała 10.1016/j.chemosphere.2023.140854
8. Influence of Ozone and Radical Chemistry on Limonene Organic Aerosol Production and Thermal Characteristics R. Pathak et al. 10.1021/es301750r
9. The Aarhus Chamber Campaign on Highly Oxygenated Organic Molecules and Aerosols (ACCHA): particle formation, organic acids, and dimer esters from α-pinene ozonolysis at different temperatures K. Kristensen et al. 10.5194/acp-20-12549-2020
10. Characteristics of wintertime carbonaceous aerosols in two typical cities in Beijing-Tianjin-Hebei region, China: Insights from multiyear measurements R. Zhou et al. 10.1016/j.envres.2022.114469
11. Physical parameters effect on ozone-initiated formation of indoor secondary organic aerosols with emissions from cleaning products Y. Huang et al. 10.1016/j.jhazmat.2011.07.014
12. Contemporary sources dominate carbonaceous aerosol on the North Slope of Alaska C. Moffett et al. 10.1016/j.scitotenv.2022.154641
13. High molecular weight SOA formation during limonene ozonolysis: insights from ultrahigh-resolution FT-ICR mass spectrometry characterization S. Kundu et al. 10.5194/acp-12-5523-2012
14. Cold oceans enhance terrestrial new-particle formation in near-coastal forests T. Suni et al. 10.5194/acp-9-8639-2009
15. New Particle Formation Promoted by OH Reactions during α-Pinene Ozonolysis S. Inomata 10.1021/acsearthspacechem.1c00142
16. Volatility of secondary organic aerosol during OH radical induced ageing K. Salo et al. 10.5194/acp-11-11055-2011
17. A fibre-optic UV system for H2SO4 production in aerosol chambers causing minimal thermal effects A. Kupc et al. 10.1016/j.jaerosci.2011.05.001
18. Influence of relative humidity and temperature on the production of pinonaldehyde and OH radicals from the ozonolysis of α-pinene R. Tillmann et al. 10.5194/acp-10-7057-2010
19. Deposition of α-pinene oxidation products on plant surfaces affects plant VOC emission and herbivore feeding and oviposition A. Mofikoya et al. 10.1016/j.envpol.2020.114437
20. Studies of the Gas Phase Reactions of Linalool, 6-Methyl-5-hepten-2-ol and 3-Methyl-1-penten-3-ol with O3and OH Radicals F. Bernard et al. 10.1021/jp211355d
21. Temperature and humidity dependence of secondary organic aerosol yield from the ozonolysis of β-pinene C. von Hessberg et al. 10.5194/acp-9-3583-2009
22. Temperature response of the submicron organic aerosol from temperate forests W. Leaitch et al. 10.1016/j.atmosenv.2011.08.047
23. Carboxylic acids from limonene oxidation by ozone and hydroxyl radicals: insights into mechanisms derived using a FIGAERO-CIMS J. Hammes et al. 10.5194/acp-19-13037-2019
24. Effect of Relative Humidity on the Rate of New Particle Formation for Different VOCs A. Flueckiger & G. Petrucci 10.3390/atmos15040480
25. Updated aerosol module and its application to simulate secondary organic aerosols during IMPACT campaign May 2008 Y. Li et al. 10.5194/acp-13-6289-2013
26. Field measurements of biogenic volatile organic compounds in the atmosphere by dynamic solid-phase microextraction and portable gas chromatography-mass spectrometry L. Barreira et al. 10.1016/j.atmosenv.2015.05.064
27. Quantification of the role of stabilized Criegee intermediates in the formation of aerosols in limonene ozonolysis Y. Gong & Z. Chen 10.5194/acp-21-813-2021
28. Review of the influencing factors of secondary organic aerosol formation and aging mechanism based on photochemical smog chamber simulation methods Y. Zhang et al. 10.1016/j.jes.2022.10.033
29. Decreasing effect and mechanism of FeSO 4 seed particles on secondary organic aerosol in α -pinene photooxidation B. Chu et al. 10.1016/j.envpol.2014.06.018
30. Ozone-Driven Secondary Organic Aerosol Production Chain Y. Iinuma et al. 10.1021/es305156z
31. Large Discrepancy in the Formation of Secondary Organic Aerosols from Structurally Similar Monoterpenes D. Thomsen et al. 10.1021/acsearthspacechem.0c00332
32. The formation, properties and impact of secondary organic aerosol: current and emerging issues M. Hallquist et al. 10.5194/acp-9-5155-2009
33. Ozone and OH-induced oxidation of monoterpenes: Changes in the thermal properties of secondary organic aerosol (SOA) Å. Watne et al. 10.1016/j.jaerosci.2017.08.011
34. The effect of temperature and relative humidity on secondary organic aerosol formation from ozonolysis of Δ3-carene D. Thomsen et al. 10.1039/D3EA00128H
35. Secondary organic aerosol from biogenic volatile organic compound mixtures M. Hatfield & K. Huff Hartz 10.1016/j.atmosenv.2011.01.065
36. Assessing the Difference in the Effects of NOx on the Photooxidation Mechanisms of Isomeric Compounds of α-Pinene and Δ3-Carene Z. Zhang et al. 10.1021/acsearthspacechem.4c00159
37. Characteristics of carbonaceous aerosols in four northern Chinese cities during the 2022 Winter Olympics X. Li et al. 10.1016/j.atmosenv.2024.120699
38. Characterizing highly oxygenated organic molecules in limonene secondary organic aerosols: roles of temperature and relative humidity Y. Zhai et al. 10.1039/D4EA00153B
39. Impact of temperature on the role of Criegee intermediates and peroxy radicals in dimer formation from β-pinene ozonolysis Y. Gong et al. 10.5194/acp-24-167-2024
40. Relation Between Humidity and Size of Exhaled Particles H. Holmgren et al. 10.1089/jamp.2011.0880
41. Ultrafine Particle Production from the Ozonolysis of Personal Care Products M. Vannucci & W. Nazaroff 10.1021/acs.est.7b03596
42. The oxidation regime and SOA composition in limonene ozonolysis: roles of different double bonds, radicals, and water Y. Gong et al. 10.5194/acp-18-15105-2018
43. Vibrational Sum Frequency Generation Spectroscopy of Secondary Organic Material Produced by Condensational Growth from α-Pinene Ozonolysis M. Shrestha et al. 10.1021/jp405065d
44. Ozonolysis of α-Pinene and Δ3-Carene Mixtures: Formation of Dimers with Two Precursors D. Thomsen et al. 10.1021/acs.est.2c04786
45. Evidence and evolution of Criegee intermediates, hydroperoxides and secondary organic aerosols formedviaozonolysis of α-pinene A. Bagchi et al. 10.1039/C9CP06306D
46. Temperature dependence of yields of secondary organic aerosols from the ozonolysis of α-pinene and limonene H. Saathoff et al. 10.5194/acp-9-1551-2009
47. Investigation of RH Effect on Uncommon Limonene Ozonolysis Products and SOA Formation in Indoor Air with Real Time Measurement Techniques K. Pytel & B. Zabiegała 10.2139/ssrn.4160355
48. Morphological transformation of soot: investigation of microphysical processes during the condensation of sulfuric acid and limonene ozonolysis product vapors X. Pei et al. 10.5194/acp-18-9845-2018
49. Physico-chemical characterization of SOA derived from catechol and guaiacol – a model substance for the aromatic fraction of atmospheric HULIS J. Ofner et al. 10.5194/acp-11-1-2011
50. Influence of Humidity, Temperature, and Radicals on the Formation and Thermal Properties of Secondary Organic Aerosol (SOA) from Ozonolysis of β-Pinene E. Emanuelsson et al. 10.1021/jp4010218
51. Modelling non-equilibrium secondary organic aerosol formation and evaporation with the aerosol dynamics, gas- and particle-phase chemistry kinetic multilayer model ADCHAM P. Roldin et al. 10.5194/acp-14-7953-2014
52. Size distribution of exhaled particles in the range from 0.01 to 2.0μm H. Holmgren et al. 10.1016/j.jaerosci.2010.02.011
53. Temperature dependence of yields of secondary organic aerosols from the ozonolysis of α-pinene and limonene H. Saathoff et al. 10.5194/acpd-8-15595-2008