Junlin An

Junlin An


Research Focus & Metrics

Academic Career Length

24Years (2003-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 April 2016 in Chemosphere
Verified
Journal Article
Closed access
HWHonglei Wang
Honglei Wang
JAJunlin An
Junlin An
MCMengtian Cheng
Mengtian Cheng
LSLijuan Shen
Lijuan Shen
BZBin Zhu
Bin Zhu
LXLi Xia
Li Xia

27 February 2017 in Journal of Geophysical Research: Atmospheres
Verified
Journal Article
Closed access
PDF file
LDLiang Dai
Liang Dai
HWHonglei Wang
Honglei Wang
LZLuyu Zhou
Luyu Zhou
JAJunlin An
Junlin An
LTLili Tang
Lili Tang
Huan YuHuan Yu
Huan Yu

1 August 2014 in Science of The Total Environment
Verified
Journal Article
Closed access
HWHonglei Wang
Honglei Wang
JAJunlin An
Junlin An
LSLijuan Shen
Lijuan Shen
BZBin Zhu
Bin Zhu
CPChen Pan
Chen Pan
YWYuesi Wang
Yuesi Wang

15 August 2015 in Environmental Science and Pollution Research
Verified
Journal Article
Closed access
PDF file
JAJunlin An
Junlin An
JZJianan Zou
Jianan Zou
JWJunxiu Wang
Junxiu Wang
XLXu Lin
Xu Lin
BZBin Zhu
Bin Zhu

7 April 2017 in Atmosphere
Verified
Journal Article
Open access
PDF file
Honglei WangHonglei Wang
Honglei Wang
JAJunlin An
Junlin An
BZBin Zhu
Bin Zhu
LSLijuan Shen
Lijuan Shen
QDQing Duan
Qing Duan
YSYuanzhe Shi
Yuanzhe Shi
In order to investigate the size distributions and seasonal variations of carbonaceous aerosols (organic carbon (OC) and elemental carbon (EC)), the carbonaceous species were collected in Nanjing, a typical industrial city located in Yangtze River Delta, China, in the summer, autumn, and winter of 2013 and spring of 2014, and then analyzed by using a 9-stage Anderson-type aerosol sampler and DRI Model 2001A Thermal/Optical Carbon Analyzer. OC, EC, secondary organic carbon (SOC), and primary organic carbon (POC) exhibited obvious seasonal variations, with the highest levels in winter (39.1±14.0, 5.7 ± 2.1, 23.6 ± 11.7, and 14.1 ± 5.7 μg·m−3, respectively) and the lowest levels in summer (20.6 ± 6.7, 3.3 ± 2.0, 12.2 ± 3.8 and 8.4 ± 4.1 μg·m−3, respectively), and were mainly centralized in PM1.1 in four seasons. The concentrations of OC in PM1.1 varied in the order of winter > autumn > spring > summer, while EC ranked in the order of autumn > winter > summer > spring. In the PM1.1–2.1 and PM2.1–10, the concentrations of OC and EC decreased in the sequence of winter > spring > autumn > summer. The size spectra of OC, EC, and SOC had bimodal distributions in four seasons, except for EC with four peaks in summer. The size spectra of POC varied greatly with seasons, exhibiting bimodal distribution in winter, trimodal distribution in spring and summer, and four peaks in autumn. The OC/EC ratios were 7.0, 6.3, 7.6, and 6.9 in spring, summer, autumn and winter, respectively, which demonstrated the abundance of secondary organic aerosols in Nanjing. The sources of carbonaceous aerosol varied significantly with seasons, and were dominated by vehicle exhaust, and coal and biomass burning in PM2.1, and dominated by dust, and coal and biomass burning in PM2.1–10.

10 June 2021 in Advances in Atmospheric Sciences
Verified
Journal Article
Closed access
PDF file
JAJunlin An
Junlin An
HLHuan Lv
Huan Lv
MXMin Xue
Min Xue
ZZZefeng Zhang
Zefeng Zhang
BHBo Hu
Bo Hu
BZBin Zhu
Bin Zhu