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Your search keyword '"Heinritzi, Martin"' showing total 207 results

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1. The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source

2. Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation

3. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range

4. Assessing the importance of nitric acid and ammonia for particle growth in the polluted boundary layer

5. The role of low-volatility organic compounds in initial particle growth in the atmosphere

6. Role of sesquiterpenes in biogenic new particle formation

7. An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles

8. Global atmospheric particle formation from CERN CLOUD measurements

10. Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere

11. Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation

12. Interactions of peroxy radicals from monoterpene and isoprene oxidation simulated in the radical volatility basis setElectronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ea00056k

13. The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source

14. High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures

15. Critical Role of Iodous Acid in Neutral Iodine Oxoacid Nucleation

17. An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles

18. Supplementary material to "An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles"

19. Cleaner Skies during the COVID-19 Lockdown

20. Neutral molecular cluster formation of sulfuric acid-dimethylamine observed in real time under atmospheric conditions

21. Ion-induced nucleation of pure biogenic particles

22. Survival of newly formed particles in haze conditions

23. Chemical composition of nanoparticles from <i>α</i>-pinene nucleation and the influence of isoprene and relative humidity at low temperature

24. Role of iodine oxoacids in atmospheric aerosol nucleation

25. An intercomparison study of four different techniques for measuring the chemical composition of nanoparticles.

26. Molecular understanding of sulphuric acid–amine particle nucleation in the atmosphere

27. Supplementary material to "Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature"

28. Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature

29. Chemical composition of nanoparticles from α-pinene nucleation and the influence of isoprene and relative humidity at low temperature

30. Role of iodine oxoacids in atmospheric aerosol nucleation

31. Molecular understanding of new-particle formation from α-pinene between −50 and +25 °C

32. Molecular understanding of new-particle formation from alpha-pinene between - 50 and + 25 degrees C

33. Determination of the collision rate coefficient between charged iodic acid clusters and iodic acid using the appearance time method

34. Molecular understanding of the suppression of new-particle formation by isoprene

35. Molecular understanding of new-particle formation from <i>α</i>-pinene between −50 and +25 °C

36. Enhanced growth rate of atmospheric particles from sulfuric acid

37. Measurement of ammonia, amines and iodine compounds using protonated water cluster chemical ionization mass spectrometry

38. Supplementary material to "Molecular understanding of the suppression of new-particle formation by isoprene"

39. Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C

40. Supplementary material to "Molecular understanding of new-particle formation from alpha-pinene between −50 °C and 25 °C"

41. Enhanced growth rate of atmospheric particles from sulfuric acid

42. Supplementary material to "Enhanced growth rate of atmospheric particles from sulfuric acid"

43. Synergistic HNO3–H2SO4–NH3upper tropospheric particle formation

44. Size-resolved online chemical analysis of nanoaerosol particles: a thermal desorption differential mobility analyzer coupled to a chemical ionization time-of-flight mass spectrometer

45. Multicomponent new particle formation from sulfuric acid, ammonia, and biogenic vapors

46. Measurement of ammonia, amines and iodine species using protonated water cluster chemical ionization mass spectrometry

47. Formation of Highly Oxygenated Organic Molecules from α-Pinene Ozonolysis: Chemical Characteristics, Mechanism, and Kinetic Model Development

48. Size resolved online chemical analysis of nano aerosol particles : a thermal desorption differential mobility analyzer coupled to a chemical ionization time of flight mass spectrometer

49. Size-resolved online chemical analysis of nanoaerosol particles : a thermal desorption differential mobility analyzer coupled to a chemical ionization time-of-flight mass spectrometer

50. Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range

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