Lijuan Shen

Lijuan Shen


Research Focus & Metrics

Academic Career Length

15Years (2012-Present)

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

Representative Publications

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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.

29 January 2024 in Science of The Total Environment
Verified
Journal Article
Closed access
LSLijuan Shen
Lijuan Shen
YDYiwei Diao
Yiwei Diao
TZTianliang Zhao
Tianliang Zhao
XGXuesong Gu
Xuesong Gu
SSShuang Shuang Shi
Shuang Shuang Shi

1 March 2017 in Preprints.org
Verified
Preprint
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 (OC and EC), the carbonaceous species were collected and then analyzed by using a 9-stage Anderson-type aerosol sampler and DRI Model 2001A Thermal/Optical Carbon Analyzer on the typical industrial city Nanjing in Yangtze River Delta, China in the summer, autumn and winter of 2013 and spring of 2014. OC, EC, SOC and POC exhibited obvious seasonal variations, with the highest level in winter (39.1±14.0, 5.7±2.1, 23.6±11.7 and 14.1±5.7 μg•m-3) and the lowest level in summer (20.6±6.7, 3.3±2.0, 12.2±3.8 and 8.4±4.1 μg•m-3), 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, coal and biomass burning in PM2.1, and dominant by dust, coal and biomass burning in PM2.1-10.

1 September 2014
Verified
Journal Article
Closed access
HWHong-Lei Wang
Hong-Lei Wang
BZBin Zhu
Bin Zhu
JAJunlin An
Junlin An
QDQing Duan
Qing Duan
JZJia-Nan Zou
Jia-Nan Zou
LSLijuan Shen
Lijuan Shen

1 May 2014
Verified
Journal Article
Closed access
LSLijuan Shen
Lijuan Shen
LLLi Li
Li Li
SLSheng Lü
Sheng Lü
XZXiao-Han Zhang
Xiao-Han Zhang
BWBo Wu
Bo Wu
FWFei Wang
Fei Wang

1 March 2012
Verified
Journal Article
Closed access
HWHong-Lei Wang
Hong-Lei Wang
BZBin Zhu
Bin Zhu
LSLijuan Shen
Lijuan Shen
HKHan-Qing Kang
Han-Qing Kang
YDYi-Wei Diao
Yi-Wei Diao