4.7 Article

Natural organic matter in urban aerosols: Comparison between water and alkaline soluble components using excitation-emission matrix fluorescence spectroscopy and multiway data analysis

期刊

ATMOSPHERIC ENVIRONMENT
卷 102, 期 -, 页码 1-10

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2014.11.042

关键词

Water-soluble organic matter; Alkaline-soluble organic matter; Atmospheric aerosols; Fluorescence spectroscopy; Emission-excitation matrix; PARAFAC-ALS

资金

  1. Centre for Environmental and Marine Studies (University of Aveiro, Portugal) [PEsT-c/MAR/LA0017/2013]
  2. Portuguese Science and Technology Foundation (FCT) through European Social Fund (ESF)
  3. Programa Operacional Potencial Humano - POPH
  4. FCT [SFRH/BD/84247/2012]
  5. Portuguese Institute for Development (IPAD)
  6. FEDER under Operational Program for Competitiveness Factors - COMPETE
  7. National funds via FCT [PTDC/CTE-ATM/118551/2010, PTDC/AAG-MAA/2584/2012]
  8. Fundação para a Ciência e a Tecnologia [SFRH/BD/84247/2012, PTDC/AAG-MAA/2584/2012, PTDC/CTE-ATM/118551/2010] Funding Source: FCT

向作者/读者索取更多资源

Understanding the complexity of Natural Organic Matter (NOM) in atmospheric aerosols has remained an important goal for the atmospheric research community. This work employs a Parallel Factor Model (PARAFAC) with Alternating Least Squares (ALS) algorithm to decompose and further compare sets of excitation-emission matrices fluorescence spectra of Water-soluble and Alkaline-soluble Organic Matter (WSOM and ASOM, respectively), sequentially extracted from urban aerosols collected during different seasons. The PARAFAC-ALS modelling identified three components in both WSOM and ASOM, whose maximum intensities follow a clear seasonal trend and which are likely to represent the dominant fluorescent moieties in NOM from urban aerosols. The PARAFAC-ALS modelling also indicated differences between the colder and warmer seasons in the fluorescence map of one WSOM component, which contrast with the results obtained for the ASOM, where the fluorescence signatures were found to be constant along the seasons, suggesting that the ASOM may have an in situ origin. (C) 2014 Elsevier Ltd. All rights reserved.

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