Atmospheric Measurement Techniques (Nov 2020)
An interlaboratory comparison of aerosol inorganic ion measurements by ion chromatography: implications for aerosol pH estimate
- J. Xu,
- S. Song,
- R. M. Harrison,
- R. M. Harrison,
- C. Song,
- L. Wei,
- Q. Zhang,
- Y. Sun,
- L. Lei,
- C. Zhang,
- X. Yao,
- X. Yao,
- D. Chen,
- W. Li,
- M. Wu,
- H. Tian,
- L. Luo,
- S. Tong,
- W. Li,
- J. Wang,
- G. Shi,
- Y. Huangfu,
- Y. Tian,
- B. Ge,
- S. Su,
- C. Peng,
- Y. Chen,
- F. Yang,
- A. Mihajlidi-Zelić,
- D. Đorđević,
- S. J. Swift,
- I. Andrews,
- J. F. Hamilton,
- Y. Sun,
- A. Kramawijaya,
- J. Han,
- S. Saksakulkrai,
- C. Baldo,
- S. Hou,
- F. Zheng,
- K. R. Daellenbach,
- C. Yan,
- Y. Liu,
- M. Kulmala,
- P. Fu,
- Z. Shi
Affiliations
- J. Xu
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- S. Song
- School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138, USA
- R. M. Harrison
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- R. M. Harrison
- Department of Environmental Sciences/Center of Excellence in Environmental Studies, King Abdulaziz University, P.O. Box 80203, Jeddah, 21589, Saudi Arabia
- C. Song
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- L. Wei
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China
- Q. Zhang
- Institute of Surface-Earth System Science, Tianjin University, Tianjin, 300072, China
- Y. Sun
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China
- L. Lei
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China
- C. Zhang
- Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, and Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266100, China
- X. Yao
- Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, and Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266100, China
- X. Yao
- Laboratory for Marine Ecology and Environmental Sciences, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266071, China
- D. Chen
- Key Laboratory of Marine Environment and Ecology, Ministry of Education of China, and Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266100, China
- W. Li
- Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, 310027, China
- M. Wu
- Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, 310027, China
- H. Tian
- State Key Laboratory of Environmental Simulation and Pollution Control & Center for Atmospheric Environmental Studies, School of Environment, Beijing Normal University, Beijing 100875, China
- L. Luo
- State Key Laboratory of Environmental Simulation and Pollution Control & Center for Atmospheric Environmental Studies, School of Environment, Beijing Normal University, Beijing 100875, China
- S. Tong
- State Key Laboratory for Structural Chemistry of Unstable and Stable Species, Institute of Chemistry, Chinese Academy of Sciences, Beijing, 100190, China
- W. Li
- State Key Laboratory for Structural Chemistry of Unstable and Stable Species, Institute of Chemistry, Chinese Academy of Sciences, Beijing, 100190, China
- J. Wang
- School of Environment, Tsinghua University, Beijing, 100084, China
- G. Shi
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Centre of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin, 300350, China
- Y. Huangfu
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Centre of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin, 300350, China
- Y. Tian
- State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, Centre of Urban Transport Emission Research, College of Environmental Science and Engineering, Nankai University, Tianjin, 300350, China
- B. Ge
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China
- S. Su
- Research Center for Atmospheric Environment, Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing, 400714, China
- C. Peng
- Research Center for Atmospheric Environment, Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing, 400714, China
- Y. Chen
- Research Center for Atmospheric Environment, Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing, 400714, China
- F. Yang
- Department of Environmental Science and Engineering, Sichuan University, Chengdu, 610065, China
- A. Mihajlidi-Zelić
- Centre of Excellence in Environmental Chemistry and Engineering – ICTM, University of Belgrade, Njegoševa 12 (Studentski trg 14–16), Belgrade, Serbia
- D. Đorđević
- Centre of Excellence in Environmental Chemistry and Engineering – ICTM, University of Belgrade, Njegoševa 12 (Studentski trg 14–16), Belgrade, Serbia
- S. J. Swift
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, YO10 5DD, UK
- I. Andrews
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, YO10 5DD, UK
- J. F. Hamilton
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, YO10 5DD, UK
- Y. Sun
- School of Space and Environment, Beihang University, Beijing, 100191, China
- A. Kramawijaya
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- J. Han
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- S. Saksakulkrai
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- C. Baldo
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- S. Hou
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- F. Zheng
- Aerosol and Haze Laboratory, Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, 100029, China
- K. R. Daellenbach
- Aerosol and Haze Laboratory, Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, 100029, China
- C. Yan
- Aerosol and Haze Laboratory, Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, 100029, China
- Y. Liu
- Aerosol and Haze Laboratory, Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, 100029, China
- M. Kulmala
- Aerosol and Haze Laboratory, Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, 100029, China
- P. Fu
- Institute of Surface-Earth System Science, Tianjin University, Tianjin, 300072, China
- Z. Shi
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK
- DOI
- https://doi.org/10.5194/amt-13-6325-2020
- Journal volume & issue
-
Vol. 13
pp. 6325 – 6341
Abstract
Water-soluble inorganic ions such as ammonium, nitrate and sulfate are major components of fine aerosols in the atmosphere and are widely used in the estimation of aerosol acidity. However, different experimental practices and instrumentation may lead to uncertainties in ion concentrations. Here, an intercomparison experiment was conducted in 10 different laboratories (labs) to investigate the consistency of inorganic ion concentrations and resultant aerosol acidity estimates using the same set of aerosol filter samples. The results mostly exhibited good agreement for major ions Cl−, SO42-, NO3-, NH4+ and K+. However, F−, Mg2+ and Ca2+ were observed with more variations across the different labs. The Aerosol Chemical Speciation Monitor (ACSM) data of nonrefractory SO42-, NO3- and NH4+ generally correlated very well with the filter-analysis-based data in our study, but the absolute concentrations differ by up to 42 %. Cl− from the two methods are correlated, but the concentration differ by more than a factor of 3. The analyses of certified reference materials (CRMs) generally showed a good detection accuracy (DA) of all ions in all the labs, the majority of which ranged between 90 % and 110 %. The DA was also used to correct the ion concentrations to showcase the importance of using CRMs for calibration check and quality control. Better agreements were found for Cl−, SO42-, NO3-, NH4+ and K+ across the labs after their concentrations were corrected with DA; the coefficient of variation (CV) of Cl−, SO42-, NO3-, NH4+ and K+ decreased by 1.7 %, 3.4 %, 3.4 %, 1.2 % and 2.6 %, respectively, after DA correction. We found that the ratio of anion to cation equivalent concentrations (AE / CE) and ion balance (anions–cations) are not good indicators for aerosol acidity estimates, as the results in different labs did not agree well with each other. In situ aerosol pH calculated from the ISORROPIA II thermodynamic equilibrium model with measured ion and ammonia concentrations showed a similar trend and good agreement across the 10 labs. Our results indicate that although there are important uncertainties in aerosol ion concentration measurements, the estimated aerosol pH from the ISORROPIA II model is more consistent.