Real-time analysis of insoluble particles in glacial ice using single-particle mass spectrometry

dc.contributor.author Osman, Matthew B.
dc.contributor.author Zawadowicz, Maria
dc.contributor.author Das, Sarah B.
dc.contributor.author Cziczo, Daniel J.
dc.date.accessioned 2017-12-11T18:49:52Z
dc.date.available 2017-12-11T18:49:52Z
dc.date.issued 2017-11-21
dc.description © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Atmospheric Measurement Techniques 10 (2017): 4459-4477, doi:10.5194/amt-10-4459-2017. en_US
dc.description.abstract Insoluble aerosol particles trapped in glacial ice provide insight into past climates, but analysis requires information on climatically relevant particle properties, such as size, abundance, and internal mixing. We present a new analytical method using a time-of-flight single-particle mass spectrometer (SPMS) to determine the composition and size of insoluble particles in glacial ice over an aerodynamic size range of  ∼  0.2–3.0 µm diameter. Using samples from two Greenland ice cores, we developed a procedure to nebulize insoluble particles suspended in melted ice, evaporate condensed liquid from those particles, and transport them to the SPMS for analysis. We further determined size-dependent extraction and instrument transmission efficiencies to investigate the feasibility of determining particle-class-specific mass concentrations. We find SPMS can be used to provide constraints on the aerodynamic size, composition, and relative abundance of most insoluble particulate classes in ice core samples. We describe the importance of post-aqueous processing to particles, a process which occurs due to nebulization of aerosols from an aqueous suspension of originally soluble and insoluble aerosol components. This study represents an initial attempt to use SPMS as an emerging technique for the study of insoluble particulates in ice cores. en_US
dc.description.sponsorship This work was supported by an internal Reed Grant from MIT and National Science Foundation award PLR-1205196 to Sarah B. Das. Matthew Osman acknowledges government support awarded by DoD, Air Force Office of Scientific Research, National Defense Science and Engineering Graduate (NDSEG) Fellowship, 32 CFR 168a. Maria A. Zawadowicz acknowledges the support of NASA Earth and Space Science Fellowship. Daniel J. Cziczo acknowledges the support of the Victor P. Starr Career Development Chair at MIT. en_US
dc.identifier.citation Atmospheric Measurement Techniques 10 (2017): 4459-4477 en_US
dc.identifier.doi 10.5194/amt-10-4459-2017
dc.identifier.uri https://hdl.handle.net/1912/9415
dc.language.iso en_US en_US
dc.publisher Copernicus Publications on behalf of the European Geosciences Union en_US
dc.relation.uri https://doi.org/10.5194/amt-10-4459-2017
dc.rights Attribution 3.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/3.0/
dc.title Real-time analysis of insoluble particles in glacial ice using single-particle mass spectrometry en_US
dc.type Article en_US
dspace.entity.type Publication
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relation.isAuthorOfPublication.latestForDiscovery 3f6e95de-6b1f-4f09-929f-a3c26b255d94
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