Insights into air pollution chemistry and sulphate formation from nitrous acid (HONO) measurements during haze events in Beijing-Reference-Cited by-同舟云学术

Insights into air pollution chemistry and sulphate formation from nitrous acid (HONO) measurements during haze events in Beijing

Published:2021 Issue: Volume:226 Page:223-238
ISSN:1359-6640
Container-title:Faraday Discussions
language:en
Short-container-title:Faraday Discuss.

Author:

Bloss William J.¹²³^ORCID,Kramer Louisa¹²³,Crilley Leigh R.¹²³,Vu Tuan¹²³,Harrison Roy M.¹²³^ORCID,Shi Zongbo¹²³^ORCID,Lee James D.⁴⁵⁶³^ORCID,Squires Freya A.⁴⁵⁶³^ORCID,Whalley Lisa K.⁷⁸³,Slater Eloise⁷⁸³,Woodward-Massey Robert⁷⁸³,Ye Chunxiang⁷⁸³,Heard Dwayne E.⁷⁸³^ORCID,Tong Shengrui⁹¹⁰¹¹¹²,Hou Siqi⁹¹⁰¹¹¹²,Sun Yele¹³¹⁴¹⁰¹¹¹²^ORCID,Xu Jingsha¹²³,Wei Lianfang¹³¹⁴¹⁰¹¹¹²,Fu Pingqing¹⁵¹⁶¹⁷¹²^ORCID

Affiliation:

1. School of Geography, Earth and Environmental Sciences

2. University of Birmingham

3. UK

4. Wolfson Atmospheric Chemistry Laboratories

5. Department of Chemistry

6. University of York

7. School of Chemistry

8. University of Leeds

9. Institute of Chemistry

10. Chinese Academy of Sciences

11. Beijing

12. China

13. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry

14. Institute of Atmospheric Physics

15. Institute of Surface-Earth System Science

16. Tianjin University

17. Tianjin 300072

Abstract

We integrate observations of gas phase species and time-resolved aerosol composition to explore observational constraints on the mechanisms responsible for sulphate growth during the onset of haze events in Beijing.

Funder

Natural Environment Research Council

Publisher

Royal Society of Chemistry (RSC)

Subject

Physical and Theoretical Chemistry

Link

http://pubs.rsc.org/en/content/articlepdf/2021/FD/D0FD00100G

Reference42 articles.

1. Heterogeneous chemistry: a mechanism missing in current models to explain secondary inorganic aerosol formation during the January 2013 haze episode in North China

2. Direct Kinetic Measurements of Criegee Intermediate (CH 2 OO) Formed by Reaction of CH 2 I with O 2

3. H2SO4 formation from the gas-phase reaction of stabilized Criegee Intermediates with SO2: Influence of water vapour content and temperature