Brown Carbon Formation from Nighttime Chemistry of Unsaturated

furan may not be a major contributor to SOA mass under a variety of common ... NO3 chemistry with these compounds may be an important SOA source, ...
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Environmental Processes

Brown Carbon Formation from Nighttime Chemistry of Unsaturated Heterocyclic Volatile Organic Compounds Huanhuan Jiang, Alexander L. Frie, Avi Lavi, Jin Chen, Haofei Zhang, Roya Bahreini, and Ying-Hsuan Lin Environ. Sci. Technol. Lett., Just Accepted Manuscript • DOI: 10.1021/acs.estlett.9b00017 • Publication Date (Web): 30 Jan 2019 Downloaded from http://pubs.acs.org on January 31, 2019

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Brown Carbon Formation from Nighttime Chemistry of Unsaturated Heterocyclic Volatile

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Organic Compounds

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Huanhuan Jiang†⊥, Alexander L. Frie†⊥, Avi Lavi‡, Jin Y. Chen§, Haofei Zhang‡§, Roya Bahreini†‡§, Ying-Hsuan Lin†§*

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Department of Environmental Sciences, University of California, Riverside, CA 92521, USA

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Department of Chemistry, University of California, Riverside, CA 92521, USA

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§

Environmental Toxicology Graduate Program, University of California, Riverside, CA 92521,

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USA

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These authors contributed equally to this work

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*

phone: +1-951-827-3785, email: [email protected]

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ABSTRACT:

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Nighttime atmospheric processing enhances the formation of brown carbon aerosol (BrC) in

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biomass burning plumes. Heterocyclic compounds, a group of volatile organic compounds

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(VOCs) abundant in biomass burning smoke, are possible BrC sources. Here, we investigated the

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nitrate radical (NO3)-initiated oxidation of three unsaturated heterocyclic compounds (pyrrole,

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furan, and thiophene) as a source of BrC. The imaginary component of the refractive index at

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375 nm (k375), the single scattering albedo at 375 nm (SSA375) and average mass absorption

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coefficients (290-700nm) of the resulting secondary organic aerosol (SOA) are reported.

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Compared to furan and thiophene, NO3 oxidation of pyrrole has the highest SOA yield. Pyrrole

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SOA (k375=0.015±0.003, SSA=0.86±0.01, 290-700nm=3400±700 cm2 g-1) is also more

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absorbing than furan SOA (290-700nm=1,100±200 cm2 g-1) and thiophene SOA

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(k375=0.003±0.002, SSA375=0.98±0.01, 290-700nm=3,000±500 cm2 g-1). Compared to other

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SOA systems, MACs reported in this study are higher than those from biogenic precursors, and

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similar to high-NOx anthropogenic SOA. Characterization of SOA molecular composition using

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high-resolution mass spectrometric measurements revealed unsaturated heterocyclic nitro

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products or organonitrates as possible chromophores in BrC from all three precursors. These

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findings reveal nighttime oxidation of fire-sourced heterocyclic compounds, particularly pyrrole,

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as a plausible source of BrC.

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TOC Art

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1. INTRODUCTION

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Aerosol’s radiative effects are the most uncertain components of current climate models.1

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One of the drivers of this uncertainty is the incomplete understanding of aerosol formation and

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aging processes that influence aerosols’ chemical composition and optical properties. Light-

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absorbing organic aerosols, known as brown carbon (BrC), are estimated to account for ~20% of

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aerosol-driven atmospheric heating.2 The chemical nature of BrC chromophores has been the

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focus of many recent studies, with field, laboratory, and modeling studies identifying aromatics,

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conjugated systems, and highly functionalized species, such as organic nitrates, as moieties

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responsible for absorption of tropospheric solar radiation.2-16 Specifically, nitroaromatic

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compounds have been recognized as significant components of BrC.13

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One previously unexplored pathway of BrC and nitroaromatic formation is the nitrate

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radical (NO3)-initiated oxidation of unsaturated heterocyclic compounds. Unsaturated

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heterocyclic compounds contain heteroatoms (N, O and S) within their ring structures and

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represent a unique family of reactive compounds. These compounds are emitted during biomass

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burning events, with estimated emission factors of 5–37% of total emitted carbon for furans.17

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High levels of NOx emissions in biomass burning plumes can readily react with O3 to form NO3

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radicals, the dominant atmospheric oxidant during nighttime.14,

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compounds and NO3 radicals are likely to co-occur in the nighttime atmosphere. Major

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unsaturated heterocyclic compounds are known to react quickly with NO3 radicals,20 forming

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condensable nitro- or nitrate-containing reaction products that are likely to absorb light in the

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UV-Visible range.7, 10, 21

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Thus, heterocyclic

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Here, the NO3 oxidation of unsaturated heterocyclic compounds is investigated as a

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probable and previously unrecognized source of BrC. Through a series of chamber experiments,

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we characterized chemical and optical properties of SOA from NO3-initiated oxidation of

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pyrrole, furan, and thiophene as model compounds for 5-membered unsaturated heterocyclic

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compounds. We used both online and offline techniques to evaluate single scattering albedo

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(SSA, λ=375 nm), refractive index (RI, λ=375 nm) and mass absorption coefficients (MAC, 290–

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700 nm) to provide a broad picture of the optical characteristics of SOA. Molecular composition

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of SOA was analyzed to identify potential chromophores.

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2. MATERIALS AND METHODS

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2.1. Controlled Chamber Experiments

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Experiments were performed under dry conditions (RH=2–16%) within a ~1.3 m3 FEP

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Teflon chamber located at University of California, Riverside. Before each experiment, the

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chamber was filled with zero air (Airgas). O3 was generated through corona discharge (Enaly,

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1000BT–12) and injected into the chamber until a concentration of ~1500 ppbv O3 was reached.

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Next, 2 L of NO (Praxair, 482 ppmv in air) was injected into the chamber. The chamber was

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equilibrated for an hour to allow reservoirs of NO3 and N2O5 to develop. As shown in Fig.

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S1, more than 9 ppbv NO3 can be generated after one hour as simulated using a kinetic box

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model.22-24 Then, pyrrole (TCI America, >99%), furan (TCI America, >99%,) or thiophene (Alfa

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Aesar, 99%) was added into a glass bulb and the vapors were introduced into the chamber by

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flowing ultra-zero air (Aadco Instruments Inc., 747-30) through the bulb to achieve an effective

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chamber concentration of ~200 ppbv. Under these conditions, the oxidation of all precursors is

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dominated by the NO3 pathway as shown in the supplemental information (SI, Section S1 and

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Table S1). Aerosol size distributions, NO2, NO and O3 were continuously monitored during

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experiments with a scanning electron mobility spectrometer (SEMS, Brechtel Manufacturing

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Inc.), NOx analyzer (Thermo 42i-LS) and an O3 analyzer (Thermo 49i), respectively. A summary

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of experimental conditions is provided in Table 1.

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2.2. Online Chemical and Optical Characterization

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Gas-phase reaction products were analyzed in real time by an iodide-adduct high-

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resolution time-of-flight chemical ionization mass spectrometer (HR-ToF-CIMS, Tofwerk AG,

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Aerodyne Research Inc.). Additional details are described in Section S2.

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Scattering and absorption coefficients at 375 nm (βscat,375 and βabs,375) were measured at 1

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Hz using a photoacoustic extinctiometer (PAX) (Droplet Measurement Technologies, Boulder,

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CO). PAX measurements were averaged to the SEMS scan time (140 s). PAX detection limits,

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defined as 3 times the standard deviation of scattering and absorption measurements of filtered

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air averaged to 140 s, were 1.29 Mm-1 and 1.08 Mm-1, respectively for βscat,375 and βabs,375. The

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single scattering albedo at 375 nm (SSA375) was calculated using Eq. 1.

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𝑆𝑆𝐴375 =

𝛽scat,375 𝛽scat,375 +𝛽abs,375

(1)

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The size parameter (x) is useful in understanding SSA dynamics due to SSA’s

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dependency on particle size and measurement wavelength. x relates the mode diameter of the

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size distribution (dmode) to the corresponding wavelength () of optical measurements, i.e.,

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=375 nm for PAX, as shown in Eq. 2. 𝑥𝜆 =

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𝜋𝑑𝑚𝑜𝑑𝑒 𝜆

(2)

2.3. Calculation of Refractive Index

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RI values are measures of the interactions of a material with radiation. The RI consists of

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two components, a real component that describes scattering (n) and an imaginary component that

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describes absorption (k). RI values were calculated using an optical closure procedure and

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applying Mie Theory (Section S3).25-29 Variabilities reported in Section 3.2 represent standard 6 ACS Paragon Plus Environment

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deviations of the measurements. Uncertainties were also estimated by forcing the RI calculation

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+0.007 +0.08 using instrumental uncertainties (Table S2);30 maximum uncertainties were 𝑘−0.005 and 𝑛−0.07

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+0.004 +0.09 for pyrrole and 𝑘−0.002 and 𝑛−0.06 for thiophene. For furan experiments, n375 and k375 values were

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not calculated because the majority of βabs,375 measurements were below or marginally higher

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than PAX detection limits.

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2.4. Offline Optical Characterization

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Aerosol samples were collected onto polytetrafluoroethylene membrane filters (Zefluor,

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Pall Laboratory, 47 mm, 1.0 µm pore size), after the particle volume concentration peaked.

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Filters were extracted in methanol and analyzed for UV-Vis absorbance (Beckman DU-640).

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This process is further detailed in Section S4.

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2.5. Calculation of Mass Absorption Coefficient and Absorption Angstrom Exponent Calculation of the solution-based MAC from UV-Vis spectra has been reported previously.31, 32 The effective MAC (cm2 g-1) is calculated using Eq 3.31, 32 MAC(𝜆) =

A(𝜆)×ln10

(3)

𝑏×𝐶m

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where A() is the absorbance at wavelength () of filter extracts, b is the path length (1 cm), and

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Cm (g cm-3) is the mass concentration of extracted SOA compounds in solution. Cm is determined

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by the filter sampling flow rate, average aerosol mass concentration during filter collection,

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sampling time, and extraction efficiency. The light-absorbing properties of aerosols are estimated

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by the average MAC () over the wavelengths range from 1=290 nm to n=700 nm).

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〈𝑀𝐴𝐶〉 =

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∑𝑛 𝑖=1 𝑀𝐴𝐶(𝜆𝑖 ) 𝑛

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To understand the wavelength dependence of light absorption, the absorption Ångstrӧm exponent (AAE) was calculated in the UV (290–400 nm) and visible (400–600 nm) ranges.32

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𝐴𝐴𝐸 =

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𝑀𝐴𝐶(𝜆1 ) ) 𝑀𝐴𝐶(𝜆2 ) 𝜆 𝑙𝑛( 1 ) 𝜆2

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−𝑙𝑛(

(5)

2.6. Offline Chemical Characterization

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The molecular composition of filter extracts was characterized using liquid

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chromatography (LC) coupled with a diode array detector (DAD) and a high-resolution time-of-

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flight mass spectrometer (HR-TOFMS, Agilent 6230 Series). The instrument was equipped with

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an electrospray ionization source (ESI), and the detector was operated under the negative (−) ion

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mode. Further details can be found in Section S5.

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3. RESULTS AND DISCUSSION

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3.1. NO3-Initiated SOA Formation from Heterocyclic Precursors

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By assuming all of the injected VOC reacted with NO3 radicals and propagating

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experimental uncertainties, the lower bound of SOA mass yields (Eq. S3) were estimated to be

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109±29% for pyrrole, 7±3% for furan, and 35±8% for thiophene, assuming a density of 1.3 g cm -

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comparing to more quantitative yield measures from other studies due to our small chamber size

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and potentially high particle wall-loss rates.

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. These values are estimates and are likely inter-comparable, but caution should be used when

The low SOA mass production from furan is consistent with the low SOA yields from

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OH oxidation of furan reported in other studies.34,

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furan may not be a major contributor to SOA mass under a variety of common oxidation

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conditions. Conversely, the larger SOA mass formed from thiophene and pyrrole indicates that

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NO3 chemistry with these compounds may be an important SOA source, particularly in biomass

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burning plumes where these compounds are readily found.17

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Together these observations reveal that

3.2. Optical Properties of SOA

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SSA375, n375, and k375 for pyrrole and thiophene experiments are displayed in Fig. 1A and

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1B. For the following discussion, SSA375 values are averaged for all measurements where x375>1

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because the size dependency of SSA is expected to be minimal within this region. 36 The n375

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values fell within the ranges previously observed for organic aerosols, with average values of

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1.41 ± 0.05, and 1.44 ± 0.02 for pyrrole and thiophene SOA, respectively.

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Pyrrole SOA was the most absorbing among the three tested precursors, with an average

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SSA375 of 0.86±0.01 and k375 of 0.015±0.003. These values are similar to those previously

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observed for peat biomass burning (SSA375: 0.93 and 0.85, and k375: 0.009–0.015 depending on

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fuel packing density) by Sumlin et al.37 Notably, the k375 values for pyrrole SOA decreased with

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exposure time and seem to be inversely related to SOA mass. This decrease in k375 could be

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driven by dilution of chromophores as more scattering components condense or by bleaching of

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existing chromophores. Bleaching might be driven by the oxidation of conjugated species by an

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oxidant (O3 or NO3) or particle phase processes such as hydrolysis of organonitrates.38

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Thiophene SOA was slightly absorbing, with an average SSA375 of 0.98±0.01 and k375 of

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0.003 ± 0.002. Thiophene k375 values are similar to those observed by Liu et al.21 for toluene

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SOA (k405=0.0041±0.0005) and m-xylene SOA (k405=0.0030 ±0.0003) formed from OH

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oxidation in the presence of NOx.21 These compounds are aromatic anthropogenic proxies,

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indicating that thiophene SOA products have similar absorption properties to SOA from

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anthropogenic precursors.

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The majority of βabs,375 measurements for furan SOA were below the PAX detection limit,

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which was likely caused by the low mass production of furan SOA in the chamber (Section 3.1)

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and its low light absorption at 375 nm (Section 3.3).

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3.3. The Absorption Spectra of BrC

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Similar to previously studied BrC SOA, samples collected from oxidation of unsaturated

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heterocyclic compounds absorb strongly in UV and near UV ranges, and the absorbance

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decreased as the wavelengths increased (Fig. 1C).15, 16 The absorbance spectra of pyrrole and

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thiophene SOA showed a shoulder at ~330 nm. The 290-700 values of pyrrole, thiophene

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and furan SOA were 3,400±700 cm2 g-1, 3,000±500 cm2 g-1, and 1,100±200 cm2 g-1, respectively

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(Table 1). Notably, the offline MAC of furan SOA over the whole spectra and at 375 nm was

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significantly lower than in the other systems, which explains its negligible βabs,375 values (Section

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3.2). These are much higher than those of SOA (200–500 cm2 g-1) derived from

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biogenic and anthropogenic VOCs under low or intermediate NOx conditions, but similar to the

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SOA from anthropogenic VOCs with high NOx (VOC/NOx