Decadal trends in atmospheric organic aerosol :

Organic aerosol (OA) makes up a substantial fraction of atmospheric particulate matter, yet its sources and controlling factors - and thus its impacts on climate and human health - are not well understood. Recently-developed analytical techniques have provided new insight into OA chemistry, but major uncertainty remains in how OA has changed over the past few decades. Characterizing long-term trends in OA would allow for better calibration of models that currently struggle to replicate ambient organic measurements as well as answer questions of how changes in OA relate to changes in emissions sources, anthropogenic-biogenic emissions interactions, altered chemistry, and more. This work represents a two-fold effort to better constrain our understanding of OA trends spatially, temporally, and chemically. First, trends in aerosol species concentrations over the past two decades are examined using existing data from the U.S. Interagency Monitoring of Protected Visual Environments (IMPROVE) network to provide insight into the long-term OA evolution across the rural U.S. Along with large decreases in total aerosol amounts (30-50%), OA is found to decrease at a fractional rate nearly equivalent to the decreases in three other major aerosol species: nitrate, sulfate, and elemental carbon. This suggests a link between the controlling factors of the different species, but explaining these observations is made challenging by the lack of chemical characterization of historic OA measurements that would help point to changing sources and chemistry. Thus, the second part of this work introduces a technique that enhances our ability to obtain important chemical information from small-volume environmental aerosol samples, such as filter extracts from remote regions like those monitored by the IMPROVE network, that were previously excluded from Aerodyne aerosol mass spectrometer (AMS) analysis due to the prohibitive volumes required for standard atomization. The Small Volume Nebulizer (SVN) nebulizes microlitersized liquid samples, allowing for highly time- and mass-resolved chemical analysis of dissolved organic species on the AMS and providing valuable insight into the factors that control observed OA trends. By examining historic trends in particulate matter loading and composition, and expanding AMS coverage to include small-volume environmental samples, we can begin to answer the question of how and why OA has changed over the past few decades - and what that means for OA chemistry, the climate, and regional and global air quality.

Department dc:contributor.department

Massachusetts Institute of Technology. Department of Civil and Environmental Engineering.

Grantor dc:publisher

Massachusetts Institute of Technology

Year dc:date.issued

2015

Author dc:creator

• Boulanger, Kelsey Jane

Advisor dc:contributor.advisor

• Jesse H. Kroll.

• Civil and Environmental Engineering.

Statement dc:rights

• M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.

Licence dc:rights.uri

• http://dspace.mit.edu/handle/1721.1/7582

Language dc:language.iso

eng

Handle dc:identifier.uri

http://hdl.handle.net/1721.1/101836

OAI identifier oai:identifier

oai:dspace.mit.edu:1721.1/101836