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Yang P, Yang H, Wang N, Du C, Pang S, Zhang Y. Hygroscopicity measurement of sodium carbonate, β-alanine and internally mixed β-alanine/Na 2CO 3 particles by ATR-FTIR. J Environ Sci (China) 2020; 87:250-259. [PMID: 31791498 DOI: 10.1016/j.jes.2019.07.002] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/09/2019] [Revised: 06/27/2019] [Accepted: 07/02/2019] [Indexed: 05/16/2023]
Abstract
Water-uptakes of pure sodium carbonate (Na2CO3), pure β-alanine and internally mixed β-alanine/Na2CO3 aerosol particles with different mole ratios are first monitored using attenuated total reflectance Fourier transform infrared spectroscopy (ATR-FTIR) technique. For pure Na2CO3 aerosol particles, combining the absorptions at 877 and 1422 cm-1 with abrupt water loss shows the efflorescence relative humidity (ERH) of 62.9%-51.9%. Upon humidifying, solid Na2CO3 firstly absorbs water to from Na2CO3·H2O crystal at 72.0% RH and then deliquesces at 84.5% RH (DRH). As for pure β-alanine particles, the crystallization takes place in the range of 42.4%-33.2% RH and becomes droplets at ~88.2% RH. When β-alanine is mixed with Na2CO3 at various mole ratios, it shows no efflorescence of Na2CO3 when β-alanine to Na2CO3 mole ratio (OIR) is 2:1. For 1:1 and 1:2 β-alanine/Na2CO3 aerosols, the ERHs of Na2CO3 are 51.8%-42.3% and 57.1%-42.3%, respectively. While β-alanine crystal appears from 62.7% RH for 2:1 and 59.4% RH for both 1:1 and 1:2 particles and lasts to driest state. On hydration, the DRH is 44.7%-75.2% for Na2CO3 with the OIR of 1:1 and 44.7%-69.0% for 1:2 mixture, and those of β-alanine are 74.8% for 2:1 mixture and 68.9% for two others. After the first dehumidification-humidification, all the water contents decrease despite of constituent fraction. And at ~92% RH, the remaining water contents are 92%, 89% and 82% at ~92% RH, corresponding to OIR of 2:1, 1:1 and 1:2 mixed system, respectively.
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Affiliation(s)
- Ping Yang
- School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, China
| | - Hui Yang
- School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, China
| | - Na Wang
- School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, China
| | - Chunyun Du
- School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, China
| | - Shufeng Pang
- School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, China.
| | - Yunhong Zhang
- School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, China
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Platt SM, El Haddad I, Pieber SM, Zardini AA, Suarez-Bertoa R, Clairotte M, Daellenbach KR, Huang RJ, Slowik JG, Hellebust S, Temime-Roussel B, Marchand N, de Gouw J, Jimenez JL, Hayes PL, Robinson AL, Baltensperger U, Astorga C, Prévôt ASH. Gasoline cars produce more carbonaceous particulate matter than modern filter-equipped diesel cars. Sci Rep 2017; 7:4926. [PMID: 28706240 PMCID: PMC5509693 DOI: 10.1038/s41598-017-03714-9] [Citation(s) in RCA: 101] [Impact Index Per Article: 14.4] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/05/2016] [Accepted: 05/10/2017] [Indexed: 11/17/2022] Open
Abstract
Carbonaceous particulate matter (PM), comprising black carbon (BC), primary organic aerosol (POA) and secondary organic aerosol (SOA, from atmospheric aging of precursors), is a highly toxic vehicle exhaust component. Therefore, understanding vehicle pollution requires knowledge of both primary emissions, and how these emissions age in the atmosphere. We provide a systematic examination of carbonaceous PM emissions and parameterisation of SOA formation from modern diesel and gasoline cars at different temperatures (22, -7 °C) during controlled laboratory experiments. Carbonaceous PM emission and SOA formation is markedly higher from gasoline than diesel particle filter (DPF) and catalyst-equipped diesel cars, more so at -7 °C, contrasting with nitrogen oxides (NOX). Higher SOA formation from gasoline cars and primary emission reductions for diesels implies gasoline cars will increasingly dominate vehicular total carbonaceous PM, though older non-DPF-equipped diesels will continue to dominate the primary fraction for some time. Supported by state-of-the-art source apportionment of ambient fossil fuel derived PM, our results show that whether gasoline or diesel cars are more polluting depends on the pollutant in question, i.e. that diesel cars are not necessarily worse polluters than gasoline cars.
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Affiliation(s)
- S M Platt
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland
- NILU-Norwegian Institute for Air Research, PO Box 100, 2027, Kjeller, Norway
| | - I El Haddad
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland.
| | - S M Pieber
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland
| | - A A Zardini
- European Commission Joint Research Centre, Directorate for Energy, Transport and Climate, Sustainable Transport Unit, 21027, Ispra, (VA), Italy
| | - R Suarez-Bertoa
- European Commission Joint Research Centre, Directorate for Energy, Transport and Climate, Sustainable Transport Unit, 21027, Ispra, (VA), Italy
| | - M Clairotte
- European Commission Joint Research Centre, Directorate for Energy, Transport and Climate, Sustainable Transport Unit, 21027, Ispra, (VA), Italy
| | - K R Daellenbach
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland
| | - R-J Huang
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland
- Key Laboratory of Aerosol Chemistry & Physics, State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061, China
| | - J G Slowik
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland
| | - S Hellebust
- Aix Marseille Univ, CNRS, LCE, Marseille, France
- Central Statistics Office, Cork, Ireland
| | | | - N Marchand
- Aix Marseille Univ, CNRS, LCE, Marseille, France
| | - J de Gouw
- NOAA Earth System Research Laboratory, Boulder, CO, USA
- CIRES, University of Colorado, Boulder, CO, USA
| | - J L Jimenez
- CIRES, University of Colorado, Boulder, CO, USA
- Department of Chemistry, University of Colorado, Boulder, CO, USA
| | - P L Hayes
- Département de Chimie, Université de Montréal, Montréal, Québec, Canada
| | - A L Robinson
- Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, 15213, USA
| | - U Baltensperger
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland
| | - C Astorga
- European Commission Joint Research Centre, Directorate for Energy, Transport and Climate, Sustainable Transport Unit, 21027, Ispra, (VA), Italy
| | - A S H Prévôt
- Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, CH-5232, Villigen, Switzerland.
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