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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

Photochemistry of Organic Aerosols

Chemical processes that convert volatile organic compounds (VOC) into secondary organic aerosols (SOA) are generally quite fast. For example, terpenes rarely last longer than an hour after they are released by vegetation on a hot sunny day. Once the condensable products of VOC oxidation partition into aerosols, the chemistry slows down considerably. However, it is incorrect to view SOA as a static collection of organic molecules which undergoes no chemistry after the initial particle condensation. A number of interesting “aging” processes leading to changes in the chemical composition and physical properties of aerosols occur on time scales ranging from minutes to days. Our group investigates mechanisms of chemical and photochemical aging in secondary organic aerosols using a combination of spectroscopic and mass spectrometric techniques.

SOA

Direct photochemical aging refers to processes initiated by absorption of solar radiation within the particle. This aging mechanism can be effective only if the following conditions are satisfied: (1) the organic aerosol material must have significant absorption in the tropospheric actinic window; (2) the yields for condensed-phase photochemical reactions, such as photodissociation, must be large compared to that for fluorescence, vibrational relaxation, geminate recombination, and various other non-reactive processes. We have found that SOA formed by ozonolysis and photooxidation of VOCs do indeed absorb light at atmospherically relevant wavelengths [107], leading to rich photochemistry within the particles such as direct photodissociation of peroxide [50] and carbonyl [57, 60] functional groups.

We have demonstrated the importance of condensed phase photochemistry in aging of organic aerosols. For example, we found that condensed-phase photochemical processes in alpha-pinene SOA result in a decrease in mass and diameter of particles occurring on atmospherically-relevant time scales [98]. Photodegradation of SOA produces a variety of small, oxygenated VOCs, which evaporate from the particles leading to the observed mass loss. This photodegradation process could produce upwards of a few Tg/year of formic acid in the atmosphere – comparable to its primary sources [111]. However, uptake of VOCs during irradiation is also possible in a so-called photosensitized process. We recently showed that photosensitized uptake of limonene occurs in competition with the photodegradation, but that the photodegradation occurs on a much faster time scale, and is therefore more important aerosol aging [122].

Another avenue of our research is photochemistry of SOA in aqueous environments, which is relevant for understanding cloud-processing of organic aerosols. In our first paper on this topic, we reported the effect of UV irradiation on the molecular composition of aqueous extracts of limonene ozonolysis SOA. We showed that photolysis had a significant effect on the composition of the dissolved organics: oligomeric compounds were destroyed, carbonyl compounds were photolyzed, carboxylic acids were generated during photolysis, and large organic peroxides were recycled into smaller peroxides. In a related study on high-NOx isoprene SOA [80] we discovered new photochemical reactions converting organic nitrates into unusual heterocyclic compounds containing nitrogen. In our follow up studies, we showed that aqueous photodegradation is common to a broad range of SOA [93, 100, 118]. We found that the SOA material became more volatile on average after the photolysis [118]. These results suggest that SOA dissolved in cloud/fog droplets should undergo significant photolytic processing on a time scale of hours to days, and may need to be considered by atmospheric models.

Our group also performs experiments on photochemistry of SOA material in a variety of matrices, where we control the viscosity of SOA (by adjusting temperature and humidity), and/or the embedded molecules. To investigate the role of the particle viscosity on photochemistry, we investigated photolysis of various molecules embedded in alpha-pinene SOA at high (liquid) and low (glassy) temperatures and showed that photochemistry is suppressed in the glassy state [91]. In a follow up study, we studied this effect in three types of SOA and found that the photochemistry is suppressed at lower temperature or lower relative humidity in all three model systems [110].

We also conduct fundamental studies of photodissociation of important atmospheric molecules in water and ice. For example, we found that photolysis of the simplest organic peroxide CH3OOH embedded in ice clusters results in rich photochemistry on a picosecond time scale [63]. This was followed by a combined experimental and theoretical investigation of photodissociation quantum yields and absorption cross sections of CH3OOH in water and in ice [78]. Another study involved the absorption spectra and aqueous photochemistry of alkyl nitrates. We determined that the aqueous photolysis of the alkyl nitrates was insignificant compared to the gas-phase photodegradation and aqueous OH reactions [104]. Finally, we have investigated the mechanisms of photochemistry of cyclohexanone, an atmospherically-relevant carbonyl compound [115].

MicelleAs opposed to SOA, which appear in the atmosphere as a result of VOC chemistry, primary organic aerosols (POA) are released directly into the atmosphere by their sources. POA include sea-salt aerosol particles generated by wave-breaking, soot particles produced by internal combustion engines, smoke particles produced by biomass burning, dust particles produced by re-suspension, and smelly particles emitted in the atmosphere by the cooking industry. Such particles are often decorated by an outer layer of fairly hydrophobic organic material such as phospholipids, fatty acids, and aromatics. This layer is slowly oxidized by OH, ozone, and nitrogen oxides in a process known as "chemical aging". We are interested in understanding the role of direct photochemical processes in processing fresh and aged POA particles. We have previously studied photodegradation of partially oxidized unsaturated fatty acids [47] and self-assembled monolayers (SAM) [43,46] as a model of photochemical aging occurring in POA particles. We discovered that reactions taking place during the oxidation of unsaturated films and SAM transform them into a photochemically active state capable of photolysis in the lower atmosphere. We think that photochemistry occurring in the oxidized aerosol contributes significantly to their aging. Our current efforts in this area focus on investigation of surface-specific photochemistry in SAM containing carbonyl and peroxide functional groups.

Aerosol Photodegradation Research Tools

Radiation sources. We use a variety of lamps and light emitting diodes (LEDs) in our laboratory. We use Xenon-arc lamps for broadband sources of radiation, and we utilize the LEDs for more narrowband experiments, where we can use a much narrower wavelength range to ascertain the dependence of some of these photochemical reactions on the incident wavelength of radiation

Flow Cells. We use flow cells and flow tubes to study aerosol photochemical processes. For example, we use a quartz flow tube surrounded by UV lamps to observe changes in SOA particle composition, concentration, and size. Before the particles are introduced to the flow tube, we can strip away the volatile species with a series of denuders. An example of this flow tube can be found in publication [98]. We also use custom-built flow cells for observing the gas-phase products from the photodegradation and photosensitized reactions of SOA. A CaF2 window with collected SOA material can be inserted into the flow cell, and a stream of zero air or zero air and a given VOC flows through it to investigate the photodegradation and photosensitized reactions, respectively. Examples of these flow cells can be found in publications [111] and [122].

CIMS and PTR-ToF-MS. To monitor the gaseous products from the photodegradation of SOA we have built a Chemical Ionization Mass Spectrometer (CIMS) instrument [60]. This apparatus uses a beta-source (63Ni) plus water vapor to generate H3O+, the ionizing agent. Because of the lower proton affinity of H3O+, protons are readily transferred from H3O+ to the organic molecules. After the proton transfer, the ions are sensitively detected with a quadrupole mass spectrometer (QMS). The advantage of this instrument compared to the IR-CRDS instrument is that it can detect more complicated volatile and semi-volatile, and monitor multiple products simultaneously.

SOA

More recently, we have upgraded this setup with help of a Proton Transfer Reaction Time-of-Flight Mass Spectrometer (PTR-ToF-MS). This instrument can quantitatively detect hundreds of gas-phase species in real time, and it samples gases at atmospheric pressures. This instrument is a specialized type of a CIMS instrument that uses the hydronium (H3O+) ion as its reagent ion. This instrument is ideal for real time observations of VOCs produced during photodegradation of SOA. Recent examples of using this instrument in SOA photochemical experiments can be found in Refs. [106, 111, 122].

CRDS setup. This figure shows an IR-CRDS (Infrared Cavity Ring-Down Spectroscopy) apparatus designed in our laboratory to study photodegradation processes in oxidized organic films and in SOA samples. CRDS is an ultrasensitive technique that quantifies optical absorption of molecules placed between two highly-reflective mirrors from the rate with which photons escape this cavity. The sample is excited with a wavelength-tunable radiation source, and the evolved products are observed with the IR-CRDS approach. This instrument is especially suitable for the detection of small molecular weight photolysis products such as CO, CO2, H2CO, and HCOOH via their highly-specific rotational-vibrational infrared absorptions.  Examples of using this instrument can be found in publications [46, 47, 50, 57].

SOA

SSSS setup. Another photochemical tool in our laboratory makes it possible to study photolysis of ice and organic films at low temperatures. We used it for the first time to measure absorption cross-sections and photodissociation quantum yields of CH3OOH in ice [76]. A small amount of sample and reference are placed in the form of liquid droplets on two identical slides, and covered with quartz cover slips. Slides are cooled by thermal contact with two Peltier coolers, which are in thermal contact with a water-cooled aluminum heat sink. To measure absorption spectra of the films, light from a deuterium light source is split and sent through the sample and reference and collected in two UV-Vis Ocean Optics spectrometers with optical fibers. Filtered photolysis radiation is delivered through a larger fiber from a Xenon arc lamp, and projected onto the sample slide under a small angle. An electronic shutter is used for blocking the photolyzing radiation without turning the lamp off. The compartment housing is continuously purged with dry, purified air to prevent water condensation on the microscope slides and cover slips.

QCM setup. (Quartz Crystal Microbalance) allows for very sensitive mass measurements for a thin film deposited on the surface of an oscillating AT-cut quartz crystal. According to a model developed by Dr. Günter Sauerbrey in 1959, such a film suppresses the oscillation frequency by an amount which is directly proportional to its mass. Our group uses QCM to study the SOA photodegradation processes.  Using this technique, it is possible to characterize processes leading to substantial reduction (or alternatively gain) in the SOA mass during UV irradiation.

 

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