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UCI Aerosol Photochemistry Group   
University of California at Irvine   Department of Chemistry   
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Aerosol Photochemistry Group Research

Introduction

Molecular Composition of Organic Aerosols

Photochemistry of Organic Aerosols

Chemistry of Brown Carbon

Water Uptake by Nanoparticles

Indoor Air Chemistry

Research Archives

Molecular Composition of Organic Aerosols

Atmospheric aerosols refer to the liquid or solid “clumps” of molecules floating through the ambient air. Typical sizes of aerosol particles range from several nanometers to several micrometers. They take a long time to settle to the ground because of the negligible gravitational pull relative to the Brownian motion forces exerted by random collisions with the gas-phase molecules and the forces originating from convective air currents. Aerosols play an important role in controlling the climate, driving atmospheric chemistry, and contributing to air pollution problems worldwide. For example, every single cloud or fog droplet requires a seed particle in order to grow. Atmospheric aerosols have received a lot of scientific attention in recent years because of the profound effects they have on the climate. Through multiple field observations, scientists have established that ambient particles contain a significant fraction of organic compounds. Particles that are dominated by the organic material are loosely defined as “organic aerosols” (OA), and further divided into primary and secondary by the mechanism of their generation. Primary Organic Aerosols (POA) are emitted in the atmosphere directly by various sources such as traffic, waves breaking, wind-blown soil, biomass burning, cooking, and so on. The molecular make-up of POA usually reflects the environment they came from. Secondary Organic Aerosols (SOA) are produced in the atmosphere as a result of complex chains of reactions that start with the oxidation of Volatile Organic Compounds (VOC) by ozone (O3), hydroxyl radical (OH) and nitrate radical (NO3) and end with the condensation and coagulation of low-volatility oxidation products into aerosols. The presence of nitrogen oxides (NOx), an important component of urban pollution affects the formation of the aerosols. One especially important group of VOC that efficiently form SOA is terpenes, a class of hydrocarbons emitted predominantly by tree foliage. Terpenes include isoprene (C5H8), monoterpenes (C10H16) and larger terpenes.

 

Imagine entering a garage in a house that has been occupied by a disorganized family for years (such as the Nizkorodov family). You will likely find dozens of dusty boxes filled with thousands of items that the family members used in the past but are now only vaguely aware of. Each particle in an organic aerosol is similar to such a garage in that it contains a bewildering number of products of atmospheric oxidation of various organic molecules, which were discarded by the air because they were not volatile enough to remain in the vapor state. Identifying each molecule in an organic aerosol is far more challenging then sorting through the mess of an old garage. However, it is worth doing because detailed knowledge of molecular composition of organic particles holds clues to their important properties. For example, if we knew what kinds of molecules particles contain, we could predict what types of effects they would have on our health when we inhale them.

Even SOA generated from a single VOC under controlled laboratory conditions may contain thousands of different organic compounds. The real-world SOA are even more complicated than that. Several years ago no one thought that figuring out the molecular composition of SOA would even be possible but recently this has all changed due to exciting developments in mass spectrometry. In collaboration with Prof. Alexander Laskin and Prof. Julia Laskin at Purdue University (formerly at EMSL, PNNL), we have been developing and applying methods of high resolution mass spectrometry (HRMS) to characterize the molecular structure of SOA [68]. This approach provides an unprecedented amount of detail about the composition of organic aerosols by supplying molecular formulas for thousands of aerosol species in a single measurement. Detailed analyses of the distribution of chemical formulas reveal useful mechanistic information about the chemistry leading to the initial formation and subsequent aging of biogenic and anthropogenic organic aerosols. The following figure is a highlight of our study of the composition of isoprene/ozone aerosol [64]; it displays a map of the O:C versus H:C ratios for about 1000 organic molecules that we were able to observe in this type of aerosol.

The collaboration between the UC Irvine and Purdue University research groups has been really productive and it has resulted in the observation of multifunctional monomeric and oligomeric aerosol compounds in SOA prepared by oxidation of limonene [51, 56, 61, 66, 67, 69, 84], isoprene [64, 70, 71, 75, 79, 80], alpha-pinene [99, 118], alpha-humulene [118], toluene [125], naphthalene [93], indole [119], diesel fuel [116], and other VOCs [100, 118].

In addition to examining lab-generated SOA, we have also analyzed ambient particulate matter samples collected in urban [96] and rural [85, 127] areas. For example, in collaboration with the group of Allen Goldstein from UCB, we analyzed aerosol samples from the 2010 CalNex field study in Bakersfield and Pasadena using positive mode nanospray-desorption electrospray ionization mass spectrometry [85].  That study represented the first systematic comparison between high-resolution mass spectra of field and chamber generated aerosols, and demonstrated that diesel was a major source of SOA in Bakersfield.

Recent work by our group along with our collaborators from Purdue University has focused on characterizing POA from biomass burning organic aerosol (BBOA) [67, 114, 123, 127]. For example, we collected BBOA from cookstoves used in villages in rural India. This resulted in an inventory of particle-phase species found in cookstove emissions [127]. We participated in the National Oceanic and Atmospheric Administration’s (NOAA) FIREX campaign. Forest fire fuels collected from around the country were burned during the 2016 fire lab intensive in Missoula, MT. We collected particles on filters and are characterizing the light-absorbing compounds using advanced chromatography and mass spectrometry techniques.

We have also worked on the development of new methods designed to make HRMS analysis more sensitive, quantitative, selective, and user-friendly. This method development work has been driven by our collaborators from Purdue University, Prof. Alexander Laskin and Prof. Julia Laskin. For example, we were the first to apply desorption electrospray ionization (DESI) [66], to SOA analysis, which made it possible to examine aerosol filter samples without prior extraction. This was followed by the development of nanospray desorption electrospray ionization (nano-DESI) by Profs. A. Laskin and J. Laskin, and first applications of nano-DESI to the analysis of laboratory [70] and field [85] samples. We were the first to apply reactive nano-DESI to SOA analysis [83], an approach that makes it possible to selectively and quantitatively observe carbonyl compounds in SOA. We suggested an original approach for an approximate quantification of concentrations of SOA extracts in HR ESI-MS without using standards [79], described a new method for doing HR ESI-MS analysis of organic aerosols using a particle-into-liquid-sampler (PILS) [67], demonstrated that HR ESI-MS is a useful method for quantitative measurements of the average O/C ratios in SOA [84], and studied solvent interference in the electrospray ionization (ESI) analysis of SOA [56]. More recently, we described applications of a powerful analytical HLPC-PDA-HRMS platform for separating molecules with HPLC, recording the absorption spectra of separated molecules with a photodiode array (PDA) detector, and determining mass-to-charge ratios for the eluted compounds with ESI-HRMS [109, 114].

Our Research Tools

aerosol chamber in the Nizkorodov groupAerosol Chamber. We use a 5 m3 Teflon aerosol smog chamber [64], which is housed inside a 20 m3 protective enclosure. The chamber is surrounded by 40 UV-B lamps for photochemical generation of OH from precursors like H2O2, HONO, and RONO. The OH then reacts with the VOC of interest, making SOA. SOA is collected through denuders onto filters or impacted onto other substrates for analysis. The reaction can be conducted at different VOC and NOx concentrations. The chamber is connected to a suite of state-of-the-art instruments that help control and monitor the reaction conditions: zero-air generator, NOy monitor, O3 monitor, RH/T probe, scanning mobility particle sizer (SMPS), chemical ionization mass spectrometer (CIMS), time-of-flight aerosol mass spectrometer (ToF-AMS), proton-transfer-reaction time-of-flight mass spectrometer (PTR-ToF-MS, see below). This chamber is our main “reactor” for making model SOA.

Aerosol Flow Reactor. In addition to static aerosol chambers, we use flow reactors to make aerosol samples. A VOC of interest is slowly injected with a syringe pump into a flow of air and carried a flow tube. Ozone is added to the flow through a separate port. If needed, OH is produced in the flow tube by photolysis of ozone in presence of water vapor.  The gases and particles exit the flow tube, and the remaining oxidants are stripped from the mixture with a denuder, while particles are collected with a filter or an impactor. The main advantages of flow tubes include the ability to keep the aerosol concentration constant over a significant period of time (hours) and the ability to collect large amounts of SOA material (mg quantities).

orbitrap corePTR-ToF-MS is a sophisticated mass spectrometer that is optimized for quantitative measurements of gas-phase alcohols, carbonyls, esters, amines, olefins, aromatic compounds, etc., with sensitivities approaching parts-per-trillion by volume. The PTR-ToF-MS instrument has sufficiently high resolving power (m/∆m = 6,000) to unambiguously identify small VOCs by their accurate molecular masses and sufficiently fast response time to monitor the reaction kinetics with 1 s time resolution. The ionization mechanism involves a charge-transfer from H3O+ onto VOCs. The VOC carbon skeleton remains intact upon the proton-transfer in most cases, which significantly simplifies the data analysis. This PTR-ToF-MS instrument is shared with other research groups in the AirUCI, an institute at UCI focusing on atmospheric science research.

HRMS.For our high resolution mass spectrometry research, we rely on an instrument with high resolving power (m/∆m = 100,000) and a soft-ionization ion source. This state-of-the-art instrument resides at Purdue University, in the labs of Prof. Alexander Laskin and Prof. Julia Laskin. In addition to the traditional ESI-MS approach, we often use nano-DESI developed by the Purdue team. In collaboration with Dr. Alexander Laskin and Dr. Julia Laskin, we have also been developing a method specifically designed for a detailed analysis of “brown” aerosol. This method relies on separation of the compounds by their polarity using high performance liquid chromatography (HPLC), followed by simultaneous measurement of the UV/Vis spectrum of the  eluting fractions with a photodiode array absorption detector (PDA) and the high resolution mass spectrometer.

The analysis of the mass spectra produced by this instrument takes advantage of specialized computer programs developed by our group and at Purdue University. The validity of the formula assignments is checked against information about isotopic patterns, chemical families, and known chemical mechanisms. The following figure schematically represents the steps we usually take in the data analysis (this image was created by Tran Nguyen as part of her PhD dissertation; click on the image to see a higher-resolution version).

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