Ns-Soot: A Material-Based Term for Strongly Light-Absorbing Carbonaceous Particles

被引:81
作者
Buseck, Peter R. [1 ,2 ]
Adachi, Kouji [1 ,2 ,3 ]
Andras Gelencser [4 ]
Tompa, Eva [4 ]
Mihaly Posfai [4 ]
机构
[1] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA
[2] Arizona State Univ, Dept Chem & Biochem, Tempe, AZ 85287 USA
[3] Meteorol Res Inst, Atmospher Environm & Appl Meteorol Res Dept, Tsukuba, Ibaraki 305, Japan
[4] Univ Pannonia, Dept Earth & Environm Sci, Veszprem, Hungary
基金
美国国家科学基金会;
关键词
TRANSMISSION ELECTRON-MICROSCOPY; INDIVIDUAL AEROSOL-PARTICLES; BLACK CARBON; SOUTHERN AFRICA; TAR BALLS; ABSORPTION MEASUREMENTS; RADIATIVE ABSORPTION; RAMAN-SPECTROSCOPY; MIXING STATE; REAL-TIME;
D O I
10.1080/02786826.2014.919374
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The climate-change and environmental literature, including that on aerosols, is replete with mention of black carbon (BC) and soot. The terms are used interchangeably in much of the literature, although BC and soot commonly have operational and source-based definitions, respectively, and reliable reference samples and aerosol standards do not exist for either one. The uncertainty about their exact chemical nature and properties can be decreased by materials-based measurement techniques and terminology. Here, we discuss ambiguities in common uses of BC and soot and propose the term ns-soot, where "ns" refers to carbon nanospheres, for a characteristic constituent of BC and soot. Based on its composition, morphology, and structure, we define ns-soot as particles that consist of nanospheres, typically with diameters <100 nm, that possess distinct structures of concentrically wrapped, graphene-like layers of carbon and with grape-like (aciniform) morphologies. We additionally propose that, because of their importance for climate modeling and health issues, distinctions are made among bare, coated, and embedded ns-soot particles.
引用
收藏
页码:777 / 788
页数:12
相关论文
共 74 条
[1]   Evolution of biomass burning aerosol properties from an agricultural fire in southern Africa [J].
Abel, SJ ;
Haywood, JM ;
Highwood, EJ ;
Li, J ;
Buseck, PR .
GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (15) :ASC1-1
[2]   Internally mixed soot, sulfates, and organic matter in aerosol particles from Mexico City [J].
Adachi, K. ;
Buseck, P. R. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2008, 8 (21) :6469-6481
[3]   Fractal parameters of individual soot particles determined using electron tomography: Implications for optical properties [J].
Adachi, Kouji ;
Chung, Serena H. ;
Friedrich, Heiner ;
Buseck, Peter R. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2007, 112 (D14)
[4]   Changes of ns-soot mixing states and shapes in an urban area during CalNex [J].
Adachi, Kouji ;
Buseck, Peter R. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2013, 118 (09) :3723-3730
[5]   Atmospheric tar balls from biomass burning in Mexico [J].
Adachi, Kouji ;
Buseck, Peter R. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2011, 116
[6]   Shapes of soot aerosol particles and implications for their effects on climate [J].
Adachi, Kouji ;
Chung, Serena H. ;
Buseck, Peter R. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2010, 115
[7]   Black carbon or brown carbon?: The nature of light-absorbing carbonaceous aerosols [J].
Andreae, M. O. ;
Gelencser, A. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :3131-3148
[8]   Consistency and Traceability of Black Carbon Measurements Made by Laser-Induced Incandescence, Thermal-Optical Transmittance, and Filter-Based Photo-Absorption Techniques [J].
不详 .
AEROSOL SCIENCE AND TECHNOLOGY, 2011, 45 (02) :295-312
[9]  
[Anonymous], 2006, ATMOS CHEM PHYS
[10]  
[Anonymous], 2012, ATMOS CHEM PHYS DISC