Lekhendra Tripathee

Dr. Lekhendra Tripathee


Research Focus & Metrics

Academic Career Length

14Years (2013-Present)

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

Representative Publications

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12 October 2016 in Bulletin of Environmental Contamination and Toxicology
Verified
Journal Article
Closed access
PDF file
LTLekhendra Tripathee
Lekhendra Tripathee
SKShichang Kang
Shichang Kang
CSChhatra Mani Sharma
Chhatra Mani Sharma
DRDipesh Rupakheti
Dipesh Rupakheti
RPRukumesh Paudyal
Rukumesh Paudyal
Mika E. T. SillanpääMika E. T. Sillanpää
Mika E. T. Sillanpää

1 June 2017 in Science of The Total Environment
Verified
Journal Article
Closed access
XLXiaofei Li
Xiaofei Li
SKShichang Kang
Shichang Kang
XHXiaobo He
Xiaobo He
BQBin Qu
Bin Qu
LTLekhendra Tripathee
Lekhendra Tripathee
CLChaoliu Li
Chaoliu Li

21 July 2017 in Atmospheric Chemistry and Physics
Verified
Journal Article
Open access
PDF file
XWXin Wan
Xin Wan
SKShichang Kang
Shichang Kang
QLQuanlian Li
Quanlian Li
DRDipesh Rupakheti
Dipesh Rupakheti
QZQianggong Zhang
Qianggong Zhang
ZCZhiyuan Cong
Zhiyuan Cong
To better understand the characteristics of biomass burning in the northern Indo-Gangetic Plain (IGP), total suspended particles were collected in a rural site, Lumbini, Nepal, during April 2013 to March 2014 and analyzed for the biomass burning tracers (i.e., levoglucosan, mannosan, vanillic acid). The annual average concentration of levoglucosan was 734 ± 1043 ng m−3 with the maximum seasonal mean concentration during post-monsoon season (2206 ± 1753 ng m−3), followed by winter (1161 ± 1347 ng m−3), pre-monsoon (771 ± 524 ng m−3) and minimum concentration during monsoon season (212 ± 279 ng m−3). The other biomass burning tracers (mannosan, galactosan, p-hydroxybenzoic acid, vanillic acid, syringic acid and dehydroabietic acid) also showed the similar seasonal variations. There were good correlations among levoglucosan, organic carbon (OC) and elemental carbon (EC), indicating significant impact of biomass burning activities on carbonaceous aerosol loading throughout the year in Lumbini area. According to the characteristic ratios, levoglucosan ∕ mannosan (lev ∕ man) and syringic acid ∕ vanillic acid (syr ∕ van), we deduced that the high abundances of biomass burning products during non-monsoon seasons were mainly caused by the burning of crop residues and hardwood while the softwood had less contribution. Based on the diagnostic tracer ratio (i.e., lev ∕ OC), the OC derived from biomass burning constituted large fraction of total OC, especially during post-monsoon season. By analyzing the MODIS fire spot product and 5-day air-mass back trajectories, we further demonstrated that organic aerosol composition was not only related to the local agricultural activities and residential biomass usage but also impacted by the regional emissions. During the post-monsoon season, the emissions from rice residue burning in western India and eastern Pakistan could impact particulate air pollution in Lumbini and surrounding regions in southern Nepal. Therefore, our finding is meaningful and has a great importance for adopting the appropriate mitigation measures, not only at the local level but also by involving different regions and nations, to reduce the biomass burning emissions in the broader IGP region nations.

1 October 2014 in Atmospheric Environment
Verified
Journal Article
Closed access
LTLekhendra Tripathee
Lekhendra Tripathee
SKShichang Kang
Shichang Kang
JHJie Huang
Jie Huang
CSChhatra Mani Sharma
Chhatra Mani Sharma
Mika E. T. SillanpääMika E. T. Sillanpää
Mika E. T. Sillanpää
RPRukumesh Paudyal
Rukumesh Paudyal

1 October 2019 in Environmental Pollution
Verified
Journal Article
Closed access
PCPengfei Chen
Pengfei Chen
SKShichang Kang
Shichang Kang
CLChaoliu Li
Chaoliu Li
QZQianggong Zhang
Qianggong Zhang
JGJunming Guo
Junming Guo
ZJZhenming Ji
Zhenming Ji

19 December 2015 in Environmental Earth Sciences
Verified
Journal Article
Closed access
PDF file
RPRukumesh Paudyal
Rukumesh Paudyal
SKShichang Kang
Shichang Kang
CSChhatra Mani Sharma
Chhatra Mani Sharma
LTLekhendra Tripathee
Lekhendra Tripathee
JHJie Huang
Jie Huang
Mika E. T. SillanpääMika E. T. Sillanpää
Mika E. T. Sillanpää