GSTDTAP  > 地球科学
DOI10.1016/j.atmosres.2019.01.004
Levoglucosan as a tracer of biomass burning: Recent progress and perspectives
Bhattarai, Hemraj1,8; Saikawa, Eri3; Wan, Xin1,8; Zhu, Hongxia5; Ram, Kirpa1,4; Gao, Shaopeng1; Kang, Shichang2,7; Zhang, Qianggong1,7; Zhang, Yulan2; Wu, Guangming1,8; Wang, Xiaoping1,7; Kawamura, Kimitaka6; Fu, Pingqing9; Cong, Zhiyuan1,7
2019-05-15
发表期刊ATMOSPHERIC RESEARCH
ISSN0169-8095
EISSN1873-2895
出版年2019
卷号220页码:20-33
文章类型Review
语种英语
国家Peoples R China; USA; India; Japan
英文摘要

Biomass burning (BB) is a major source of air pollution from local to global scale, having variable effects on air quality, human health, and climate system. Therefore, the source identification and characterization of BB derived aerosols and tracer gases in the ambient environment is crucial. This review provides recent updates on the applicability of levoglucosan as a BB tracer in different environmental matrices such as aerosols, marine, snow and ice-cores etc. Among several tracer of BB emissions, levoglucosan has recently received widespread attention due to its unique origin solely from the pyrolysis of cellulose and hemicellulose, making it as a robust marker for characterization and quantification of BB throughout the world. This review first summarizes the established and emerging analytical methods, and their advantages and disadvantages for measurement of levoglucosan. Second, we discuss the formation mechanism, lifetime and its stability in different environmental conditions. In addition, we also try to deliberate on the application of ratios of levoglucosan with different organic components such as mannosan (M) and organic carbon (OC) for better identification of emission sources. Spatial distributions of levoglucosan in different locations (e.g., urban, rural, forest, marine, poles and higher altitude) are discussed scrupulously and meticulously on a global scale. We also reviewed the distributions of levoglucosan in snow, ice core and sediments to understand its applicability to construct paleofire records. Finally, we propose some key recommendations for future work in different ambient environmental conditions by utilizing the ratios of levoglucosan with other compounds (not limited only to M and OC) and the use of levoglucosan to reconstruct the paleo-historical records of fire-activity.


英文关键词Levoglucosan Biomass burning Organic tracer Aerosol
领域地球科学
收录类别SCI-E
WOS记录号WOS:000459364100003
WOS关键词ANION-EXCHANGE CHROMATOGRAPHY ; PERFORMANCE LIQUID-CHROMATOGRAPHY ; WESTERN NORTH PACIFIC ; SECONDARY ORGANIC AEROSOL ; FINE-PARTICLE EMISSIONS ; LONG-RANGE TRANSPORT ; ICE-CORE RECORDS ; ATMOSPHERIC AEROSOLS ; MASS-SPECTROMETRY ; BLACK-CARBON
WOS类目Meteorology & Atmospheric Sciences
WOS研究方向Meteorology & Atmospheric Sciences
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/183200
专题地球科学
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;
2.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou 730000, Gansu, Peoples R China;
3.Emory Univ, Atlanta, GA 30322 USA;
4.Banaras Hindu Univ, Inst Environm & Sustainable Dev, Varanasi 221005, Uttar Pradesh, India;
5.China Natl Environm Monitoring Ctr, Beijing 100012, Peoples R China;
6.Chubu Univ, Chubu Inst Adv Studies, Kasugai, Aichi 4878501, Japan;
7.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;
8.Univ Chinese Acad Sci, Beijing 100049, Peoples R China;
9.Tianjin Univ, Inst Surface Earth Syst, Tianjin 300072, Peoples R China
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GB/T 7714
Bhattarai, Hemraj,Saikawa, Eri,Wan, Xin,et al. Levoglucosan as a tracer of biomass burning: Recent progress and perspectives[J]. ATMOSPHERIC RESEARCH,2019,220:20-33.
APA Bhattarai, Hemraj.,Saikawa, Eri.,Wan, Xin.,Zhu, Hongxia.,Ram, Kirpa.,...&Cong, Zhiyuan.(2019).Levoglucosan as a tracer of biomass burning: Recent progress and perspectives.ATMOSPHERIC RESEARCH,220,20-33.
MLA Bhattarai, Hemraj,et al."Levoglucosan as a tracer of biomass burning: Recent progress and perspectives".ATMOSPHERIC RESEARCH 220(2019):20-33.
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