Fresh organic and soot particles from crop straw burning: Morphology, composition and size distribution

Author:

Li Yaowei12,Shao Longyi1ORCID,Wang Xinming3,Wang Wenhua4,Yang Cheng‐Xue5ORCID,Li Wenjun1,Fang Zheng3

Affiliation:

1. State Key Laboratory of Coal Resources and Safe Mining, School of Geoscience and Survey Engineering China University of Mining and Technology (Beijing) Beijing China

2. Hebei Center for Ecological and Environmental Geology Research Hebei GEO University Shijiazhuang China

3. State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environment Protection and Resources Utilization, Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

4. School of Resources and Materials Northeastern University at Qinhuangdao Qinhuangdao China

5. Institute of Earth Sciences China University of Geosciences Beijing Beijing China

Abstract

Particulate matter from biomass burning is considered to be one of the major sources of air pollution in China. To examine the characteristics of the particles emitted from the burning of crop straw, an open burning experiment is designed. Individual particles are collected in the flaming and smouldering stages, and analysed by individual particle analyses represented by high‐resolution transmission electron microscopy equipped with the energy‐dispersive X‐ray spectrometer. Five types of particles are identified, namely, pure organic particle, organic particle‐K (OP‐K), tar ball, K‐rich and soot particles. Of these, the OP‐K particles have the highest relative number percentage in all analysed particles in both the flaming and smouldering stages. Interestingly, the microscopic morphology of organic particles is completely different in the flaming and smouldering stages, being near‐spherical in the flaming stage and gel‐like in the smouldering stage. According to the elemental compositions, most of OP‐K particles contained potassium compounds in the form of KCl and K2SO4. High combustion efficiency and temperature promote the formation of crystal structure, resulting in the onion‐like microstructure of soot particles. Apparently, the soot microstructure is a fingerprint feature that helps identify combustion sources. In addition, the particles emitted in the flaming stage are smaller than those in the smouldering stage, implying that high temperature combustion tends to be associated with high combustion efficiency. The relationship between burning temperatures and particle sizes can help to understand the emission of particles from crop straw burning and find new ways to solve the problems caused by straw burning. The results of this study can provide more detailed ‘fingerprint’ characteristics of the particulate matter emitted from biomass‐burning sources, and an understanding of their potential impact on the atmospheric environment.

Funder

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

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