Published January 2021 | Version v1
Journal article

A 150-year record of black carbon (soot and char) and polycyclic aromatic compounds deposition in Lake Phayao, north Thailand

  • 1. Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences, Xi'an, 710061 (China)
  • 2. SKLLQG and KLACP, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061 (China)
  • 3. School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an, 710049 (China)
  • 4. Institute of Geography and Geoecology, Karlsruhe Institute of Technology (KIT), Reinhard-Baumeister Platz 1, 76131 Karlsruhe (Germany)
  • 5. Max Planck Institute for Chemistry, Multiphase Chemistry Department, Hahn-Meitner-Weg 1, 55128 Mainz (Germany)
  • 6. Institute of Geography and Oeschger Centre for Climate Change Research, University of Bern, Hallerstrasse 12, 3012 Bern (Switzerland)
  • 7. Department of Geosciences, Morrill Science Center, University of Massachusetts, 611 North Pleasant Street, Amherst, MA, 01003 (United States)
  • 8. School of Social & Environmental Development, National Institute of Development Administration (NIDA), 118 Sereethai Road, Klongchan, Bangkapi, Bangkok, 10240 (Thailand)
  • 9. Shanghai Carbon Data Research Center, CAS Key Laboratory of Low-Carbon Conversion Science and Engineering, Shanghai Advanced Research Institute, Chinese Academy of Sciences, Shanghai, 201210 (China)

Description

Highlights: • Deposition of black carbon, soot and PACs to a Thai sediment core sharply increased since ∼1980. • Variations in char and soot deposition in Thailand over the past 150 years were decoupled. • Decreasing biomass burning offset the recent increase in other soot emissions to the atmosphere. An improved understanding of the historical variation in the emissions and sources (biomass burning, BB vs. fossil fuel, FF combustion) of soot and char, the two components of black carbon (BC), and polycyclic aromatic compounds (PACs) may help in assessing the environmental effects of the Atmospheric Brown Cloud (ABC) in SE Asia. We therefore determined historical variations of the fluxes of soot, char, and PACs (24 polycyclic aromatic hydrocarbons (PAHs), 12 oxygenated PAHs (OPAHs), and 4 azaarenes) in a dated sediment core (covering the past ∼150 years) of Phayao Lake in Thailand. The soot fluxes have been increasing in recent times, but at a far lower rate than previously estimated based on BC emission inventories. This may be associated with a decreasing BB contribution as indicated by the decreasing char fluxes from old to young sediments. The fluxes of high- and low-molecular-weight (HMW and LMW) PAHs, OPAHs, and azaarenes all sharply increased after ∼1980, while the ΣLMW-/ΣHMW-PAHs ratios decreased, further supporting the reduction in BB contribution at the expense of increasing FF combustion emissions. We also suggest that the separate record of char and soot, which has up to now not been done in aerosol studies, is useful to assess the environmental effects of ABC because of the different light-absorbing properties of these two BC components. Our results suggest that besides the establishment of improved FF combustion technology, BB must be further reduced in the SE Asian region in order to weaken the ABC haze.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.envpol.2020.116148

Additional details

Identifiers

DOI
10.1016/j.envpol.2020.116148;
PII
S0269749120368378;

Publishing Information

Journal Title
Environmental Pollution (1987)
Journal Volume
269
Journal Page Range
vp.
ISSN
0269-7491
CODEN
ENPOEK

Optional Information

Copyright
Copyright (c) 2020 Elsevier Ltd. All rights reserved.