University of Colorado, Boulder CU Scholar Chemistry & Biochemistry Graduate Theses & Chemistry & Biochemistry Dissertations Spring 1-1-2014 Optical Properties of Absorbing Organic Aerosol Particles Kyle J. Zarzana University of Colorado Boulder, [email protected] Follow this and additional works at:https://scholar.colorado.edu/chem_gradetds Part of theAtmospheric Sciences Commons, and theEnvironmental Chemistry Commons Recommended Citation Zarzana, Kyle J., "Optical Properties of Absorbing Organic Aerosol Particles" (2014).Chemistry & Biochemistry Graduate Theses & Dissertations. 131. https://scholar.colorado.edu/chem_gradetds/131 This Dissertation is brought to you for free and open access by Chemistry & Biochemistry at CU Scholar. It has been accepted for inclusion in Chemistry & Biochemistry Graduate Theses & Dissertations by an authorized administrator of CU Scholar. For more information, please contact [email protected]. Optical Properties of Absorbing Organic Aerosol Particles by Kyle J. Zarzana B.S., Harvey Mudd College, 2007 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Chemistry and Biochemistry 2014 This thesis entitled: Optical Properties of Absorbing Organic Aerosol Particles written by Kyle J. Zarzana has been approved for the Department of Chemistry and Biochemistry Margaret A. Tolbert Paul J. Ziemann Date The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. iii Zarzana, Kyle J. (Ph.D., Chemistry) Optical Properties of Absorbing Organic Aerosol Particles Thesis directed by Professor Margaret A. Tolbert Refractive indices can be used to quantify the amount of light scattered and absorbed by atmospheric aerosol particles. Accurate values for refractive indices are needed to determine the effect of aerosol particles on climate, but the refractive indices for many atmospheric species are poorly known, particularly for organic compounds. Determining refractive indices for organic aerosol is difficult because atmospheric aerosol contains numerous organic compounds, many of which are poorly characterized. While most organic aerosol is non-absorbing, a significant fraction is composed of a class of compounds termed brown carbon, which can absorb light at shorter wavelengths. Brown carbon is an important component of total radiative forcing, and can account for up to twenty percent of the total absorption at lower wavelengths. Even though brown carbon has been observed in many locations, the sources and properties are poorly known. One proposed source is aqueous phase reactions between carbonyls and species containing reduced nitrogen. Aqueous reactions are believed to be important sources of organic aerosol, and could also contribute to the formation of brown carbon. Thisthesisexaminestheopticalpropertiesofseveralbrowncarbonsurrogatesystems, aswell as ways of accurately determining those properties. First, the optical properties of the products formed by reactions between carbonyls and amines were examined at a wavelength of 532 nm using only extinction data. These reactions form brown products with optical properties significantly different than non-absorbing organics. Second, a theoretical study was performed to determine the mosteffectivewaytoaccuratelyandpreciselycalculatetheopticalpropertiesofbothabsorbingand non-absorbing aerosol. This study indicated the need for absorption data in addition to extinction data, andsoaphotoacousticspectrometerwasconstructedtodirectlymeasureabsorption. Finally, iv the optical properties of carbonyls reacted with ammonium were examined at a wavelength of 405 nm using the newly constructed instrumental setup, which is capable of simultaneous extinction and absorption measurements. These measurements represent some of the first refractive index values reported for these systems. Dedication To all the reactions and molecules that make our life complicated and interesting. vi Acknowledgements There are many people who have helped me during my graduate school career. Dan Lack, NickWagner, andDanLawofNOAAprovidedplans, hardwareandmuchtechnicalknowledgethat enabled me to build our photoacoustic spectrometers. Nick Wagner and Steve Brown provided me with plans and software that let me build the new CRD channel, and Steve also gave me the opportunity to participate in the 2011 BEACHON-RoMBAS campaign, which was my first exposure to field research. While on that campaign I had the opportunity to work with Prof. Juliane Fry of Reed College, which was a great experience. Prof. Chris Cappa of UC Davis was kindenoughtogivemehisCRD/PASsoftware, andwasinstrumentalinhelpingwiththerefractive index sensitivity study. I had an opportunity to work with Prof. David De Haan of the University of San Diego during his final months on sabbatical here, and he provided much useful advice as I started my research. Here at CU, Don David, Jim Kastegen, Ken Smith, and all the other members of the Inte- grated Instrument Development Facility did an amazing job fabricating the parts for all my instru- ments. Eleanor Waxman and Ryan Thalman of the Volkamer group have been great friends and research colleagues, and have provided much advice over the years. Ingrid Ulbrich of the Jimenez group has also been a great friend and I am indebted to her for all of the IGOR programming advice that she has provided over the years. In the Tolbert group, I have learned so much working with Prof. Miriam Freedman, Christa Hasenkopf, and Heidi Yoon. They have been great labmates and contributed to the great atmo- sphere in the group. The entire Tolbert group has been great to work with, and I am grateful for vii the time that I have spent in the group. My advisor, Maggie Tolbert, did an amazing job guiding my research and constantly providing me with advice and motivation. I finally would like to thank my brother, Chris Zarzana, for providing much technical assis- tance, and my parents for all their love and support. viii Contents Chapter 1 Introduction 1 1.1 Atmospheric aerosol . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 1.2 Effects of aerosol particles . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 1.3 Climate relevant aerosol properties . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 1.4 Brown carbon . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 1.5 Thesis focus . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 2 Optical properties of the products of α-dicarbonyl and amine reactions in simulated cloud droplets 8 2.1 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8 2.2 Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 10 2.3 Results and discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 14 2.3.1 AFM analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 14 2.3.2 CRD analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16 2.4 Implications and conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20 3 Sensitivity of aerosol refractive index retrievals using optical spectroscopy 25 3.1 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 3.2 Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 27 3.2.1 Sources and Magnitudes of Error . . . . . . . . . . . . . . . . . . . . . . . . . 27 ix 3.2.2 Calculations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 30 3.3 Results. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 3.3.1 Non and Weak Absorbers . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 3.3.2 Strong Absorbers . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 3.3.3 Discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 44 3.4 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 49 4 PASCaRD description 51 4.1 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 51 4.2 YAG CRD . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 51 4.2.1 Detailed description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 52 4.3 405 CRD . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 61 4.3.1 Detailed description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 62 4.4 405/532 PAS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 68 4.4.1 Detailed description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 69 4.5 Differential mobility analyzer . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 94 4.6 Condensation particle counter . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 95 4.7 Humidity and temperature probes . . . . . . . . . . . . . . . . . . . . . . . . . . . . 96 4.7.1 Detailed description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 96 4.8 Computer . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 99 4.8.1 Detailed description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 99 4.9 LabVIEW software . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 100 5 Optical properties of brown carbon surrogates formed by reactions between glyoxal and ammonium sulfate 110 5.1 Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 111 5.2 Results and discussion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 119 5.2.1 Extracted samples . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 119
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