Arid
DOI10.5194/acp-19-12175-2019
Laboratory study of the heterogeneous ice nucleation on black-carbon-containing aerosol
Nichman, Leonid1,2,7; Wolf, Martin3; Davidovits, Paul1; Onasch, Timothy B.1,2; Zhang, Yue1,2,4; Worsnop, Doug R.2; Bhandari, Janarjan5; Mazzoleni, Claudio5; Cziczo, Daniel J.3,6
通讯作者Nichman, Leonid
来源期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2019
卷号19期号:19页码:12175-12194
英文摘要Soot and black carbon (BC) particles are generated in the incomplete combustion of fossil fuels, biomass, and biofuels. These airborne particles affect air quality, human health, aerosol-cloud interactions, precipitation formation, and climate. At present, the climate effects of BC particles are not well understood. Their role in cloud formation is obscured by their chemical and physical variability and by the internal mixing states of these particles with other compounds. Ice nucleation in field studies is often difficult to interpret. Nonetheless, most field studies seem to suggest that BC particles are not efficient ice-nucleating particles (INPs). On the other hand, laboratory measurements show that in some cases, BC particles can be highly active INPs under certain conditions. By working with well-characterized BC particles, our aim is to systematically establish the factors that govern the ice nucleation activity of BC. The current study focuses on laboratory measurements of the effectiveness of BC-containing aerosol in the formation of ice crystals in temperature and ice supersaturation conditions relevant to cirrus clouds. We examine ice nucleation on BC particles under water-subsaturated cirrus cloud conditions, commonly understood as deposition-mode ice nucleation. We study a series of well-characterized commercial carbon black particles with vary- ing morphologies and surface chemistries as well as ethylene flame-generated combustion soot. The carbon black particles used in this study are proxies for atmospherically relevant BC aerosols. These samples were characterized by electron microscopy, mass spectrometry, and optical scattering measurements. Ice nucleation activity was systematically examined in temperature and saturation conditions in the ranges of 217 <= T <= 235 K and 1.0 <= S-ice <= 1.5 and 0.59 <= S-water <= 0.98, respectively, using a SPectrometer for Ice Nuclei (SPIN) instrument, which is a continuous-flow diffusion chamber coupled with instrumentation to measure light scattering and polarization. To study the effect of coatings on INPs, the BC-containing particles were coated with organic acids found in the atmosphere, namely stearic acid, cis-pinonic acid, and oxalic acid. The results show significant variations in ice nucleation activity as a function of size, morphology, and surface chemistry of the BC particles. The measured ice nucleation activity dependencies on temperature, supersaturation conditions, and the physicochemical properties of the BC particles are consistent with an ice nucleation mechanism of pore condensation followed by freezing. Coatings and surface oxidation modify the initial formation efficiency of pristine ice crystals on BC-containing aerosol. Depending on the BC mate- rial and the coating, both inhibition and enhancement in INP activity were observed. Our measurements at low temperatures complement published data and highlight the capability of some BC particles to nucleate ice under low ice supersaturation conditions. These results are expected to help refine theories relating to soot INP activation in the atmosphere.
类型Article
语种英语
国家USA ; Canada
开放获取类型Green Published, gold, Green Submitted
收录类别SCI-E
WOS记录号WOS:000488977600002
WOS关键词ORGANIC AEROSOL ; SOOT PARTICLES ; SIZE DISTRIBUTIONS ; MASS-SPECTROMETRY ; CIRRUS CLOUDS ; DESERT DUST ; PART 1 ; WATER ; ADSORPTION ; POLARIZATION
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/214484
作者单位1.Boston Coll, Dept Chem, Chestnut Hill, MA 02467 USA;
2.Aerodyne Res Inc, Billerica, MA 01821 USA;
3.MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA;
4.Univ North Carolina Chapel Hill, Dept Environm Sci & Engn, Gillings Sch Global Publ Hlth, Chapel Hill, NC 27599 USA;
5.Michigan Technol Univ, Dept Phys & Atmospher Sci, Houghton, MI 49931 USA;
6.MIT, Dept Civil & Environm Engn, 77 Massachusetts Ave, Cambridge, MA 02139 USA;
7.Natl Res Council Canada, Flight Res Lab, Ottawa, ON K1V 9B4, Canada
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Nichman, Leonid,Wolf, Martin,Davidovits, Paul,et al. Laboratory study of the heterogeneous ice nucleation on black-carbon-containing aerosol[J],2019,19(19):12175-12194.
APA Nichman, Leonid.,Wolf, Martin.,Davidovits, Paul.,Onasch, Timothy B..,Zhang, Yue.,...&Cziczo, Daniel J..(2019).Laboratory study of the heterogeneous ice nucleation on black-carbon-containing aerosol.ATMOSPHERIC CHEMISTRY AND PHYSICS,19(19),12175-12194.
MLA Nichman, Leonid,et al."Laboratory study of the heterogeneous ice nucleation on black-carbon-containing aerosol".ATMOSPHERIC CHEMISTRY AND PHYSICS 19.19(2019):12175-12194.
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