Individual particle morphology, coatings, and impurities of black carbon aerosols in Antarctic ice and tropical rainfall

A. Ellis, R. Edwards, Martin Saunders, R.K. Chakrabarty, R. Subramanian, N.E. Timms, A. Van Riessen, A.M. Smith, D. Lambrinidis, L.J. Nunes, P. Vallelonga, I.D. Goodwin, A.D. Moy, M.A.J. Curran, T.D. Van Ommen

Research output: Contribution to journalArticlepeer-review

6 Citations (Scopus)
260 Downloads (Pure)

Abstract

©2016. American Geophysical Union. All Rights Reserved.
Black carbon (BC) aerosols are a large source of climate warming, impact atmospheric chemistry, and are implicated in large-scale changes in atmospheric circulation. Inventories of BC emissions suggest significant changes in the global BC aerosol distribution due to human activity. However, little is known regarding BC's atmospheric distribution or aged particle characteristics before the twentieth century. Here we investigate the prevalence and structural properties of BC particles in Antarctic ice cores from 1759, 1838, and 1930 Common Era (C.E.) using transmission electron microscopy and energy-dispersive X-ray spectroscopy. The study revealed an unexpected diversity in particle morphology, insoluble coatings, and association with metals. In addition to conventionally occurring BC aggregates, we observed single BC monomers, complex aggregates with internally, and externally mixed metal and mineral impurities, tar balls, and organonitrogen coatings. The results of the study show BC particles in the remote Antarctic atmosphere exhibit complexity that is unaccounted for in atmospheric models of BC.
Original languageEnglish
Pages (from-to)11,875-11,883
JournalGeophysical Research Letters
Volume43
Issue number22
Early online date19 Nov 2016
DOIs
Publication statusPublished - 28 Nov 2016

Fingerprint

Dive into the research topics of 'Individual particle morphology, coatings, and impurities of black carbon aerosols in Antarctic ice and tropical rainfall'. Together they form a unique fingerprint.

Cite this