• No results found

University of Groningen Characterization and source apportionment of carbonaceous aerosols in China Ni, Haiyan

N/A
N/A
Protected

Academic year: 2021

Share "University of Groningen Characterization and source apportionment of carbonaceous aerosols in China Ni, Haiyan"

Copied!
2
0
0

Bezig met laden.... (Bekijk nu de volledige tekst)

Hele tekst

(1)

University of Groningen

Characterization and source apportionment of carbonaceous aerosols in China

Ni, Haiyan

DOI:

10.33612/diss.79450942

IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from

it. Please check the document version below.

Document Version

Publisher's PDF, also known as Version of record

Publication date:

2019

Link to publication in University of Groningen/UMCG research database

Citation for published version (APA):

Ni, H. (2019). Characterization and source apportionment of carbonaceous aerosols in China. University of

Groningen. https://doi.org/10.33612/diss.79450942

Copyright

Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons).

Take-down policy

If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim.

Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. For technical reasons the number of authors shown on this cover page is limited to 10 maximum.

(2)

Propositions belonging to the PhD thesis

Characterization and Source Apportionment of Carbonaceous

Aerosols in China

Haiyan Ni

1. Chinese air pollution is a global problem.

2. China’s commitment to improve air quality should be based on the knowledge and understanding the sources and nature of carbonaceous aerosols (organic and elemental carbon), a major contributor to air pollution.

(This thesis)

3. Radiocarbon (14C) analysis shows that a sizeable fraction of carbonaceous aerosols

is from non-fossil origins (e.g., biomass burning, biogenic emissions), even for aerosols collected in urban areas.

(Chapter 2 &3 of this thesis)

4. In addition to primary carbonaceous aerosols that are directly emitted from a large variety of anthropogenic and biogenic sources, there is a considerable amount of secondary organic carbon (OC) formed in the atmosphere from gaseous precursors. (Chapter 2 & 3 of this thesis)

5. The relative contribution of fossil sources to the more volatile fraction of OC is significantly larger than to total OC and secondary OC. This is mainly related to the influence of fossil primary emissions.

(Chapter 3 of this thesis)

6. Coal combustion is an important contributor to carbonaceous aerosols. However, as the most abundant and relatively cheap fossil fuel, coal will inevitably remain an important indigenous energy resource for the foreseeable future.

7. Coal combustion is an important source of brown carbon, and should be considered in further modelling of OC radiative forcing.

(Chapter 4 of this thesis)

8. Studies like the one conducted in this thesis fulfil the desire as formulated by James H. Vincent in 2007: “Aerosol sampling is a central aspect of the study, characterization and surveillance of atmospheric environments and it needed to be addressed scientifically in an integrated way in order that the results of aerosol sampling in the real world would have any meaning”.

Referenties

GERELATEERDE DOCUMENTEN

The research presented in this thesis was performed at the Centre for Isotope Research (CIO), which is part of the Energy and Sustainability Research Institute

Unlike EC that exclusively emitted as primary aerosols, OC includes both primary and secondary OC (SOC), where SOC is formed in the atmosphere by chemical reaction and

MCMC4-derived posterior probability density functions (PDF) of the relative source contributions of liquid fossil fuel combustion (vehicle), coal and biomass burning (C3

The photochemical processing of OA can lead to accumulation of carbon in the more refractory organic fraction and also larger organic compounds (Masalaite et al., 2017). The

organic aerosols from primary and aged emissions. The tested coals were burned in the stove, and the emissions were sampled from the chimney, diluted by the dilutor, and then

Because the observed total OC also includes secondary OC from fossil fuel combustion (i.e., coal combustion and vehicle emissions) and non-fossil sources (e.g.,

SOC is formed in the atmosphere via atmospheric oxidation of organic gases from both fossil and non-fossil sources (e.g., biomass burning, biogenic emissions, and

SOC wordt in de atmosfeer gevormd via atmosferische oxidatie van organische gassen van zowel fossiele als niet-fossiele bronnen (bijvoorbeeld verbranding van biomassa,