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Lipid biomarker estimates of seasonal variations of aerosol organic carbon sources in coastal Qingdao, China
被引:9
|作者:
Chen, Qu
[1
,2
,3
]
Guo, Zhigang
[4
]
Yu, Meng
[1
,2
,3
]
Sachs, Julian P.
[1
,2
,5
]
Hou, Pengfei
[1
,2
,3
]
Li, Li
[1
,2
,3
]
Jin, Gui'e
[1
,2
,3
]
Liu, Yueying
[1
,2
,3
]
Zhao, Meixun
[1
,2
,3
]
机构:
[1] Ocean Univ China, Minist Educ, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Qingdao 266100, Peoples R China
[2] Ocean Univ China, Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao 266100, Peoples R China
[3] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China
[4] Fudan Univ, Dept Environm Sci & Engn, Shanghai Key Lab Atmospher Particle Pollut & Prev, Shanghai 200433, Peoples R China
[5] Univ Washington, Sch Oceanog, Box 355351, Seattle, WA 98195 USA
基金:
中国国家自然科学基金;
关键词:
Aerosol organic carbon;
Lipid biomarkers;
Fossil fuel OC;
Terrestrial plant OC;
Marine OC;
Air masses;
AIR-POLLUTION SOURCES;
N-ALKANES;
ATMOSPHERIC AEROSOLS;
FATTY-ACIDS;
MARINE ATMOSPHERE;
URBAN AREAS;
RURAL SITE;
NEW-DELHI;
MATTER;
PM2.5;
D O I:
10.1016/j.orggeochem.2020.104148
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
Aerosols represent a significant source of organic carbon (OC) to China's marginal seas, but their provenance and chemical composition remain understudied. At the boundary of the East Asian continent and China's marginal seas, the coastal city of Qingdao is well-situated to study the sources and seasonal variations of organic aerosols and their contribution to marginal seas. Twenty-nine aerosol samples collected in 2015-2016 were analyzed for total OC (TOC), n-alkanes (C-17-C-33), n-alkanols (C-20-C-32) and n-fatty acids (n-FAs, C-14-C-32). Concentrations of TOC (5.7-18 mu g/m(3)), n-alkanes (17.5-143 ng/m(3)), n-alkanols (18-41 ng/m(3)) and n-FAs (99.3-160 ng/m(3)) were highest in winter when total aerosol concentrations were highest. Organic carbon-normalized (OC-normalized) biomarker concentrations were used to apportion different sources of aerosol OC: short- and mid-chain n-alkanes (<C-26) for fossil fuel residues; long-chain n-alkanes (>= C-26), mid- and long-chain n-alkanols (>= C-20) and mid- and long-chain n-FAs (>= C-20) for terrestrial plant OC; short-chain n-FAs (<C-20) for marine OC. From these we inferred higher fossil fuel OC contributions during cold seasons when aerosols were mainly transported to Qingdao by continental air masses, higher terrestrial plant OC contributions during warm seasons when terrestrial plant productivity was at its peak, and higher marine OC contributions in warm seasons when marine air masses were transported to Qingdao. Comparing these results with those from other continental and marine locations demonstrates the utility of this biomarker approach in providing semi-quantitative estimates of temporal and spatial variations in the sources of organic aerosols at the land-sea interface of marginal seas, where carbon burial rates tend to be high. (C) 2020 Elsevier Ltd. All rights reserved.
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