Literature DB >> 25406110

Insight into acid-base nucleation experiments by comparison of the chemical composition of positive, negative, and neutral clusters.

Federico Bianchi1, Arnaud P Praplan, Nina Sarnela, Josef Dommen, Andreas Kürten, Ismael K Ortega, Siegfried Schobesberger, Heikki Junninen, Mario Simon, Jasmin Tröstl, Tuija Jokinen, Mikko Sipilä, Alexey Adamov, Antonio Amorim, Joao Almeida, Martin Breitenlechner, Jonathan Duplissy, Sebastian Ehrhart, Richard C Flagan, Alessandro Franchin, Jani Hakala, Armin Hansel, Martin Heinritzi, Juha Kangasluoma, Helmi Keskinen, Jaeseok Kim, Jasper Kirkby, Ari Laaksonen, Michael J Lawler, Katrianne Lehtipalo, Markus Leiminger, Vladimir Makhmutov, Serge Mathot, Antti Onnela, Tuukka Petäjä, Francesco Riccobono, Matti P Rissanen, Linda Rondo, António Tomé, Annele Virtanen, Yrjö Viisanen, Christina Williamson, Daniela Wimmer, Paul M Winkler, Penglin Ye, Joachim Curtius, Markku Kulmala, Douglas R Worsnop, Neil M Donahue, Urs Baltensperger.   

Abstract

We investigated the nucleation of sulfuric acid together with two bases (ammonia and dimethylamine), at the CLOUD chamber at CERN. The chemical composition of positive, negative, and neutral clusters was studied using three Atmospheric Pressure interface-Time Of Flight (APi-TOF) mass spectrometers: two were operated in positive and negative mode to detect the chamber ions, while the third was equipped with a nitrate ion chemical ionization source allowing detection of neutral clusters. Taking into account the possible fragmentation that can happen during the charging of the ions or within the first stage of the mass spectrometer, the cluster formation proceeded via essentially one-to-one acid-base addition for all of the clusters, independent of the type of the base. For the positive clusters, the charge is carried by one excess protonated base, while for the negative clusters it is carried by a deprotonated acid; the same is true for the neutral clusters after these have been ionized. During the experiments involving sulfuric acid and dimethylamine, it was possible to study the appearance time for all the clusters (positive, negative, and neutral). It appeared that, after the formation of the clusters containing three molecules of sulfuric acid, the clusters grow at a similar speed, independent of their charge. The growth rate is then probably limited by the arrival rate of sulfuric acid or cluster-cluster collision.

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Year:  2014        PMID: 25406110     DOI: 10.1021/es502380b

Source DB:  PubMed          Journal:  Environ Sci Technol        ISSN: 0013-936X            Impact factor:   9.028


  6 in total

1.  The missing base molecules in atmospheric acid-base nucleation.

Authors:  Runlong Cai; Rujing Yin; Chao Yan; Dongsen Yang; Chenjuan Deng; Lubna Dada; Juha Kangasluoma; Jenni Kontkanen; Roope Halonen; Yan Ma; Xiuhui Zhang; Pauli Paasonen; Tuukka Petäjä; Veli-Matti Kerminen; Yongchun Liu; Federico Bianchi; Jun Zheng; Lin Wang; Jiming Hao; James N Smith; Neil M Donahue; Markku Kulmala; Douglas R Worsnop; Jingkun Jiang
Journal:  Natl Sci Rev       Date:  2022-07-25       Impact factor: 23.178

2.  Atmospheric Sulfuric Acid Dimer Formation in a Polluted Environment.

Authors:  Ke Yin; Shixin Mai; Jun Zhao
Journal:  Int J Environ Res Public Health       Date:  2022-06-03       Impact factor: 4.614

3.  Electrospray Ionization-Based Synthesis and Validation of Amine-Sulfuric Acid Clusters of Relevance to Atmospheric New Particle Formation.

Authors:  Sarah E Waller; Yi Yang; Eleanor Castracane; John J Kreinbihl; Kathleen A Nickson; Christopher J Johnson
Journal:  J Am Soc Mass Spectrom       Date:  2019-09-10       Impact factor: 3.109

4.  Ion-induced sulfuric acid-ammonia nucleation drives particle formation in coastal Antarctica.

Authors:  T Jokinen; M Sipilä; J Kontkanen; V Vakkari; P Tisler; E-M Duplissy; H Junninen; J Kangasluoma; H E Manninen; T Petäjä; M Kulmala; D R Worsnop; J Kirkby; A Virkkula; V-M Kerminen
Journal:  Sci Adv       Date:  2018-11-28       Impact factor: 14.136

5.  Impact of a hydrophobic ion on the early stage of atmospheric aerosol formation.

Authors:  Linda Feketeová; Paul Bertier; Thibaud Salbaing; Toshiyuki Azuma; Florent Calvo; Bernadette Farizon; Michel Farizon; Tilmann D Märk
Journal:  Proc Natl Acad Sci U S A       Date:  2019-10-21       Impact factor: 11.205

6.  Effect of dimethylamine on the gas phase sulfuric acid concentration measured by Chemical Ionization Mass Spectrometry.

Authors:  L Rondo; S Ehrhart; A Kürten; A Adamov; F Bianchi; M Breitenlechner; J Duplissy; A Franchin; J Dommen; N M Donahue; E M Dunne; R C Flagan; J Hakala; A Hansel; H Keskinen; J Kim; T Jokinen; K Lehtipalo; M Leiminger; A Praplan; F Riccobono; M P Rissanen; N Sarnela; S Schobesberger; M Simon; M Sipilä; J N Smith; A Tomé; J Tröstl; G Tsagkogeorgas; P Vaattovaara; P M Winkler; C Williamson; D Wimmer; U Baltensperger; J Kirkby; M Kulmala; T Petäjä; D R Worsnop; J Curtius
Journal:  J Geophys Res Atmos       Date:  2016-03-24       Impact factor: 4.261

  6 in total

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