2019
DOI: 10.1073/pnas.1911136116
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Impact of a hydrophobic ion on the early stage of atmospheric aerosol formation

Abstract: SignificanceGas-to-particle conversion, also known as atmospheric aerosol nucleation, is responsible for about half of the global cloud condensation nuclei. It has been further argued that homogenous ternary nucleation including water is the major pathway for atmospheric aerosol formation. In contrast to earlier results on pure protonated water clusters, the shape of the measured velocity distributions of water molecules evaporated from excited water clusters doped with pyridinium, an abundant anthropogenic io… Show more

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Cited by 10 publications
(7 citation statements)
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“…[1][2][3][4][5][6] Atmospheric new particle formation (NPF) through gas-to-particle conversion constitutes over half of the global aerosol budget. [1][2][3][4][5][6][7][8][9][10][11][12] It is widely accepted that gaseous sulfuric acid (SA) formed from SO2 oxidation plays a key role in atmospheric NPF, 3,5,6,[13][14][15][16][17][18][19][20][21][22] and a broad variety of atmospheric compounds such as ammonia, amines, and organic acids efficiently enhance SA-driven NPF by stabilizing the newly formed molecular clusters. 3,13,14,20,[23][24][25][26][27][28] However, significant gaps remain between the observed particle formation rates in the field and laboratories and the rates predicted by simulations.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…[1][2][3][4][5][6] Atmospheric new particle formation (NPF) through gas-to-particle conversion constitutes over half of the global aerosol budget. [1][2][3][4][5][6][7][8][9][10][11][12] It is widely accepted that gaseous sulfuric acid (SA) formed from SO2 oxidation plays a key role in atmospheric NPF, 3,5,6,[13][14][15][16][17][18][19][20][21][22] and a broad variety of atmospheric compounds such as ammonia, amines, and organic acids efficiently enhance SA-driven NPF by stabilizing the newly formed molecular clusters. 3,13,14,20,[23][24][25][26][27][28] However, significant gaps remain between the observed particle formation rates in the field and laboratories and the rates predicted by simulations.…”
Section: Introductionmentioning
confidence: 99%
“…Aerosols have significant effects on the global climate, visibility, and human health. Atmospheric new particle formation (NPF) through gas-to-particle conversion constitutes over half of the global aerosol budget. It is widely accepted that gaseous sulfuric acid (SA) formed from SO 2 oxidation plays a key role in atmospheric NPF, ,,, and a broad variety of atmospheric compounds such as ammonia, amines, and organic acids efficiently enhance SA-driven NPF by stabilizing the newly formed molecular clusters. ,,,, However, significant gaps remain between the observed particle formation rates in the field and laboratories and the rates predicted by simulations. ,,, Therefore, there is a need to consider the involvement of other gaseous precursors in NPF to reduce the gaps between experiments and simulations.…”
Section: Introductionmentioning
confidence: 99%
“…Figure 5 shows the time correlation function ⟨ K ( t ) K (0)⟩/⟨ K 2 (0)⟩ averaged from 1000 independent trajectories and compares the results obtained for differently sized pyridinium–water cluster ions, together with earlier results obtained for the protonated water tetramer cluster ion. 29 Typical average relaxation times for the neat water clusters are on the order of some picoseconds, and times for the pyridinium–water clusters are found to lie at least one order of magnitude higher. Moreover, it is interesting to see that for these pyridinium–water cluster ions studied, the relaxation is faster for clusters containing more water molecules.…”
Section: Resultsmentioning
confidence: 96%
“…Additional molecular dynamics simulations were performed to characterize the redistribution kinetics, by evaluating the time variations K ( t ) of the kinetic energy in the ionic impurity after its excitation at time t = 0. Figure shows the time correlation function ⟨ K ( t ) K (0)⟩/⟨ K 2 (0)⟩ averaged from 1000 independent trajectories and compares the results obtained for differently sized pyridinium–water cluster ions, together with earlier results obtained for the protonated water tetramer cluster ion . Typical average relaxation times for the neat water clusters are on the order of some picoseconds, and times for the pyridinium–water clusters are found to lie at least one order of magnitude higher.…”
Section: Resultsmentioning
confidence: 96%
“…Neutral molecular clusters are produced by adiabatic expansion of a molecular vapor of either glycine and water or a dry (anhydrous) vapor of glycine 23 (see the Experimental Section in the Supporting Information). The ions formed by electron impact ionization of the neutral cluster beam are analyzed by mass spectrometry.…”
Section: ■ Methodsmentioning
confidence: 99%