<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing with OASIS Tables v3.0 20080202//EN" "journalpub-oasis3.dtd">
<article xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:oasis="http://docs.oasis-open.org/ns/oasis-exchange/table" xml:lang="en" dtd-version="3.0"><?xmltex \makeatother\@nolinetrue\makeatletter?>
  <front>
    <journal-meta><journal-id journal-id-type="publisher">AMT</journal-id><journal-title-group>
    <journal-title>Atmospheric Measurement Techniques</journal-title>
    <abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">1867-8548</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/amt-11-3081-2018</article-id><title-group><article-title>Identification of organic hydroperoxides and peroxy acids<?xmltex \hack{\break}?> using atmospheric pressure chemical
ionization–tandem<?xmltex \hack{\break}?> mass spectrometry (APCI-MS/MS): application to<?xmltex \hack{\break}?> secondary organic aerosol</article-title><alt-title>Identification of organic hydroperoxides and peroxy acids using APCI-MS/MS</alt-title>
      </title-group><?xmltex \runningtitle{Identification of organic hydroperoxides and peroxy acids using APCI-MS/MS}?><?xmltex \runningauthor{S.~Zhou et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Zhou</surname><given-names>Shouming</given-names></name>
          <email>szhou@chem.utoronto.ca</email>
        <ext-link>https://orcid.org/0000-0003-1725-531X</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2 aff3">
          <name><surname>Rivera-Rios</surname><given-names>Jean C.</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2 aff3">
          <name><surname>Keutsch</surname><given-names>Frank N.</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Abbatt</surname><given-names>Jonathan P. D.</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-3372-334X</ext-link></contrib>
        <aff id="aff1"><label>1</label><institution>Department of Chemistry, University of Toronto, Toronto, Canada</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Department of Chemistry and Chemical Biology, Harvard University, Cambridge, MA, USA</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Shouming Zhou (szhou@chem.utoronto.ca)</corresp></author-notes><pub-date><day>30</day><month>May</month><year>2018</year></pub-date>
      
      <volume>11</volume>
      <issue>5</issue>
      <fpage>3081</fpage><lpage>3089</lpage>
      <history>
        <date date-type="received"><day>3</day><month>November</month><year>2017</year></date>
           <date date-type="accepted"><day>10</day><month>May</month><year>2018</year></date>
           <date date-type="rev-recd"><day>17</day><month>April</month><year>2018</year></date>
           <date date-type="rev-request"><day>4</day><month>January</month><year>2018</year></date>
      </history>
      <permissions>
        
        
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018.html">This article is available from https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018.html</self-uri><self-uri xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018.pdf</self-uri>
      <abstract>
    <p id="d1e127">Molecules with hydroperoxide functional groups are of extreme
importance to both the atmospheric and biological chemistry fields. In
this work, an analytical method is presented for the identification of organic hydroperoxides and peroxy acids (ROOH) by direct
infusion of liquid samples into a positive-ion atmospheric pressure chemical ionization–tandem mass spectrometer
((<inline-formula><mml:math id="M1" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>)-APCI-MS/MS). Under collisional dissociation conditions, a characteristic neutral loss of 51 <inline-formula><mml:math id="M2" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> (arising from loss of
<inline-formula><mml:math id="M3" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow></mml:math></inline-formula><inline-formula><mml:math id="M4" display="inline"><mml:mrow><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>+</mml:mo></mml:mrow></mml:math></inline-formula><inline-formula><mml:math id="M5" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) from ammonium adducts of the molecular ions (<inline-formula><mml:math id="M6" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) is observed for ROOH standards
(i.e. cumene hydroperoxide, isoprene-4-hydroxy-3-hydroperoxide (ISOPOOH), <italic>tert</italic>-butyl hydroperoxide, 2-butanone peroxide and peracetic
acid), as well as the ROOH formed from the reactions of <inline-formula><mml:math id="M7" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> with aldehydes (i.e.  acetaldehyde, hexanal, glyoxal and
methylglyoxal). This new ROOH detection method was applied to methanol extracts of secondary organic aerosol (SOA) material generated
from ozonolysis of <inline-formula><mml:math id="M8" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene, indicating a number of ROOH molecules in the SOA material. While the full-scan mass spectrum of
SOA demonstrates the presence of monomers (<inline-formula><mml:math id="M9" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M10" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 80–250), dimers (<inline-formula><mml:math id="M11" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M12" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 250–450) and trimers (<inline-formula><mml:math id="M13" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M14" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 450–600), the neutral loss
scan shows that the ROOH products all have masses less than 300 Da, indicating that ROOH molecules may not contribute significantly
to the SOA oligomeric content. We anticipate this method could also be applied to biological systems with considerable value.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <title>Introduction</title>
      <p id="d1e292">Organic hydroperoxides and peroxy acids (ROOH) are produced by the gas-phase oxidation of volatile organic compounds (VOCs) (Jackson
et al., 1999; Lee et al., 2000; Atkinson and Arey, 2003), as well as in cloud and wet aerosols (Zhao et al., 2013; Lim and Turpin,
2015). Atmospheric oxidation of VOCs leads to secondary organic aerosol (SOA), an important fraction of the atmospheric aerosol
burden. Both modeling and experimental studies indicate that organic peroxides (i.e. organic peroxides (ROOR) and ROOH species) are major components of SOA
(Jenkin, 2004; Bonn et al., 2004; Docherty et al., 2005). In recent years, ROOH in particular have been proposed to be involved in
high-molecular-weight products leading to SOA formation (Krapf et al., 2016; Kristensen et al., 2016; Sakamoto et al., 2017). Organic
peroxides are also widely used industrially as radical initiators; bleaching and disinfecting agents; and reactive intermediates in the
polymer, food and pharmaceutical industries (Odian, 2004; Moll et al., 1979; Reile et al., 2011). In biological systems, ROOH are
formed from the reactions of radicals and singlet oxygen with amino acids, peptides and proteins (Gebicki and Gebicki, 1993; Wright
et al., 2002; Agon et al., 2006; Morgan et al., 2008).  Classified as one component of reactive oxygen species (ROS), ROOH are
hazardous, irritating to skin, eyes and mucous membranes. They also cause progressive oxidative damage, cell death and even cancer
(Liou and Storz, 2010).</p>
      <?pagebreak page3082?><p id="d1e295"><?xmltex \hack{\newpage}?>Despite their importance in both atmospheric and biological chemistry, the
identification of specific ROOH molecules in a complex mixture remains
analytically challenging. There are two reasons for this: (i) unavailability
of the ROOH standards because of their thermally unstable nature (Bach
et al., 1996) and (ii) the lack of appropriate analytical techniques. So far,
the analysis of ROOH in the condensed phase has mainly been done by means of
chemical assays, such as the iodometric (Docherty et al., 2005; Banerjee and
Budke, 1964), triphenylphosphine (Nakamura and Maeda, 1991), ferrous
oxidation–xylenol orange (Wasylaschuk et al., 2007), and horseradish
peroxidase approaches (Walker et al., 2006; Hong et al., 2008). These
techniques react ROOH with reducing agents followed by analysis of the
reaction products. ROOH have also been analyzed by high-performance liquid chromatography (HPLC) analysis followed by
the post-column chemical derivatization method (Valverde-Canossa et al.,
2005; Francois et al., 2005; Hasson et al., 2001).</p>
      <p id="d1e299">The disadvantage of the assay techniques is that they measure total peroxide
content (some combination of organic peroxides, organic hydroperoxides, and
hydrogen peroxide) and are not able to identify specific molecules. There are
limited studies on direct analysis of ROOH in the literature. Using
electrospray ionization–mass spectrometry (ESI-MS), Hui et al. (2012a, b)
identified ROOH formed from the oxidation of cholesteryl ester, reporting
ammonium and sodium adducts of the ROOH molecular ions under positive ion
mode and acetate adducts of ROOH molecular ions under negative ion mode (Hui
et al., 2012a, b). Reinnig et al. (2009) identified ROOH using online ion
trap mass spectrometry, proposing that neutral loss (NL) of 34 <inline-formula><mml:math id="M15" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>
(loss of <inline-formula><mml:math id="M16" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) from the protonated molecular ions is
a characteristic fragmentation route for ROOH. Using this technique, the
authors identified three ROOH molecules from SOA generated from reaction of
<inline-formula><mml:math id="M17" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene and ozone (Reinnig et al., 2009).</p>
      <p id="d1e332">Recently, using high-resolution mass spectrometry, a number of studies have proposed ROOH detection arising from atmospheric oxidation of
biogenic organics (Zhang et al., 2017; Riva et al., 2017). However, due to the fact that the high-resolution mass spectrometry can only
provide elemental composition of the molecules, the identification of ROOH in the reaction systems remains speculative.</p>
      <p id="d1e336">In the present work, a positive-ion atmospheric pressure chemical ionization–tandem mass spectrometer ((<inline-formula><mml:math id="M18" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>)-APCI-MS/MS) is applied to
identify specific ROOH molecules. The analytical method is developed by using ROOH commercial standards and ROOH molecules that are
generated from the reactions of aldehydes with <inline-formula><mml:math id="M19" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>. The method is applied to SOA formed from ozonolysis of
<inline-formula><mml:math id="M20" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene, and a number of ROOH molecules are identified. The goal of this work is to provide an analytical technique that can widely be applied
in not only the atmospheric chemistry field but also other settings.</p>
</sec>
<sec id="Ch1.S2">
  <title>Experimental section</title>
<sec id="Ch1.S2.SS1">
  <title>Chemicals and reagents</title>
      <p id="d1e380">Cumene hydroperoxide (80 %), <italic>tert</italic>-butyl hydroperoxide
(35 %), 2-butanone peroxide (35 %), peracetic acid (32 %),
di-<italic>tert</italic>-butyl peroxide (98 %), benzoyl peroxide (<inline-formula><mml:math id="M21" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">98</mml:mn></mml:mrow></mml:math></inline-formula> %), di(dodecanoyl) peroxide (97 %), 2-nonenal (97 %),
<italic>meso</italic>-erythritol (<inline-formula><mml:math id="M22" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">99</mml:mn></mml:mrow></mml:math></inline-formula> %), <italic>cis</italic>-pinonic acid
(98 %), formaldehyde (37 %), acetaldehyde (<inline-formula><mml:math id="M23" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">99</mml:mn></mml:mrow></mml:math></inline-formula> %), hexanal
(98 %), methyl glyoxal (40 %), glyoxal (40 %), hydrogen peroxide
(<inline-formula><mml:math id="M24" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, 30 %), <inline-formula><mml:math id="M25" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene (<inline-formula><mml:math id="M26" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">99</mml:mn></mml:mrow></mml:math></inline-formula> %) and ammonium
acetate (<inline-formula><mml:math id="M27" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">99.99</mml:mn></mml:mrow></mml:math></inline-formula> %) are all purchased from Sigma-Aldrich (Canada).
Isoprene-4-hydrox-3-hydroperoxide (ISOPOOH) is synthesized according to the
literature (Rivera-Rios et al., 2014). Methanol (MeOH, LC-MS grade) is
purchased from VWR, Canada. All the chemicals and reagents are used as
received.</p>
</sec>
<sec id="Ch1.S2.SS2">
  <?xmltex \opttitle{Sample preparation and reactions of aldehydes with {$\chem{H_{2}O_{2}}$}}?><title>Sample preparation and reactions of aldehydes with <inline-formula><mml:math id="M28" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula></title>
      <p id="d1e491">Stock solutions for ROOH standards (i.e. cumene hydroperoxide, ISOPOOH,
<italic>tert</italic>-butyl hydroperoxide, 2-butanone peroxide and peracetic acid),
other peroxides (di-<italic>tert</italic>-butyl peroxide, benzoyl peroxide and
di(dodecanoyl) peroxide), 2-nonenal, <italic>meso</italic>-erythritol and
<italic>cis</italic>-pinonic acid are prepared by dissolution of the substances in
MeOH (2.0–10 <inline-formula><mml:math id="M29" display="inline"><mml:mi mathvariant="normal">mM</mml:mi></mml:math></inline-formula>). One hundred microliters of stock solutions are
further diluted in MeOH to a final volume of 1 <inline-formula><mml:math id="M30" display="inline"><mml:mi mathvariant="normal">mL</mml:mi></mml:math></inline-formula> for mass
spectrometry analysis. In some cases, ammonium acetate (AA) is added (<inline-formula><mml:math id="M31" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">5</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M32" display="inline"><mml:mi mathvariant="normal">mM</mml:mi></mml:math></inline-formula>) to enhance the signal for the ammonium adducts of the
molecular ions in the mass spectra.</p>
      <p id="d1e538">Reactions of the selected aldehydes (i.e. formaldehyde, acetaldehyde, hexanal, glyoxal and methyl glyoxal) with <inline-formula><mml:math id="M33" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> are
performed by mixing the reactants in MeOH (<inline-formula><mml:math id="M34" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M35" display="inline"><mml:mi mathvariant="normal">mM</mml:mi></mml:math></inline-formula> and <inline-formula><mml:math id="M36" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">13</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M37" display="inline"><mml:mi mathvariant="normal">mM</mml:mi></mml:math></inline-formula> for aldehydes and <inline-formula><mml:math id="M38" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, respectively)
at room temperature (<inline-formula><mml:math id="M39" display="inline"><mml:mrow><mml:mn mathvariant="normal">295</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M40" display="inline"><mml:mi mathvariant="normal">K</mml:mi></mml:math></inline-formula>) for <inline-formula><mml:math id="M41" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> min. AA is added (<inline-formula><mml:math id="M42" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">5</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M43" display="inline"><mml:mi mathvariant="normal">mM</mml:mi></mml:math></inline-formula>) before the samples are
analyzed. Sample blanks (i.e. aldehydes <inline-formula><mml:math id="M44" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> AA and <inline-formula><mml:math id="M45" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M46" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> AA) are prepared and analyzed in the same manner as the
reaction mixtures.</p>
</sec>
<sec id="Ch1.S2.SS3">
  <title>Secondary organic aerosol (SOA) generation and collection</title>
      <p id="d1e691">SOA is generated in a steady-state manner in a 1 <inline-formula><mml:math id="M47" display="inline"><mml:mrow><mml:msup><mml:mi mathvariant="normal">m</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> Teflon (FEP) chamber from gas-phase reaction of <inline-formula><mml:math id="M48" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene with
ozone (Aljawhary et al., 2013). <inline-formula><mml:math id="M49" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-Pinene is introduced into the chamber by passing a <inline-formula><mml:math id="M50" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M51" display="inline"><mml:mrow><mml:mi mathvariant="normal">mL</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> nitrogen
through a bubbler containing <inline-formula><mml:math id="M52" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene that is chilled to <inline-formula><mml:math id="M53" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>20 <inline-formula><mml:math id="M54" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C and mixed with 5 <inline-formula><mml:math id="M55" display="inline"><mml:mrow><mml:mi mathvariant="normal">L</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> purified
air. Ozone is generated by passing <inline-formula><mml:math id="M56" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M57" display="inline"><mml:mrow><mml:mi mathvariant="normal">L</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> purified air through a mercury lamp. The final concentration of ozone
is monitored to be <inline-formula><mml:math id="M58" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">7.4</mml:mn><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<inline-formula><mml:math id="M59" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">12</mml:mn></mml:msup></mml:math></inline-formula> <inline-formula><mml:math id="M60" display="inline"><mml:mrow><mml:mi mathvariant="normal">molecules</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> by a UV photometric ozone analyzer (Thermo Model 49i), and the
<inline-formula><mml:math id="M61" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene concentration is estimated to be <inline-formula><mml:math id="M62" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">3.7</mml:mn><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<inline-formula><mml:math id="M63" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">12</mml:mn></mml:msup></mml:math></inline-formula> <inline-formula><mml:math id="M64" display="inline"><mml:mrow><mml:mi mathvariant="normal">molecules</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>.</p>
      <?pagebreak page3083?><p id="d1e899"><?xmltex \hack{\newpage}?>SOA generation is confirmed by a Scanning Mobility Particle Sizer (SMPS, Model 3034) and collected on quartz fiber filters
(47 <inline-formula><mml:math id="M65" display="inline"><mml:mi mathvariant="normal">mm</mml:mi></mml:math></inline-formula> diameter) for 72 h at a flow rate of <inline-formula><mml:math id="M66" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">15</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M67" display="inline"><mml:mrow><mml:mi mathvariant="normal">L</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The filters are preheated at 500 <inline-formula><mml:math id="M68" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C for 24 h
to remove organic impurities before SOA collection. After SOA collection, the filter is extracted with 10 <inline-formula><mml:math id="M69" display="inline"><mml:mi mathvariant="normal">mL</mml:mi></mml:math></inline-formula> MeOH, and the
extract is immediately analyzed by the mass spectrometer.</p>
</sec>
<sec id="Ch1.S2.SS4">
  <title>Atmospheric pressure chemical ionization–tandem mass spectrometer (APCI-MS/MS)</title>
      <p id="d1e959">A unit resolution APCI-MS/MS instrument (Thermo TSQ Endura) is operated in positive ion mode with direct infusion of the samples into
the mass spectrometer. The sample is injected at a flow rate of 10 <inline-formula><mml:math id="M70" display="inline"><mml:mrow><mml:mi mathvariant="normal">µ</mml:mi><mml:mi mathvariant="normal">L</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> using a syringe pump (Chemyx, Inc.,
USA; model: Fusion 101) to the APCI source through polyether ether ketone (PEEK) tubing. The spray voltage is set at <inline-formula><mml:math id="M71" display="inline"><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M72" display="inline"><mml:mi mathvariant="normal">V</mml:mi></mml:math></inline-formula>;
vaporizer temperature and ion transfer tubing temperature are set at 200 <inline-formula><mml:math id="M73" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C. Sheath gas, auxiliary gas and sweep gas flows are
set (arbitrary units) at 5, 2 and 0, respectively. The mass spectrometer is a triple quadrupole that is calibrated with
polytyrosine. Mass spectra are obtained under either full-scan mode or selected ion monitoring (SIM) mode.</p>
      <p id="d1e1007">In full-scan mode, RF lens voltages are the default from the optimization in the mass calibration. The SIM scan is achieved by
isolating and monitoring a range of masses with maximum mass range of 50 <inline-formula><mml:math id="M74" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>. The RF lens voltages in SIM mode can be manually
varied and are optimized to maximize the intensities of the ammonium adducts of the molecular ions.</p>
      <p id="d1e1017">Ion fragmentation in the <inline-formula><mml:math id="M75" display="inline"><mml:mrow><mml:mtext>MS</mml:mtext><mml:mo>/</mml:mo><mml:mtext>MS</mml:mtext></mml:mrow></mml:math></inline-formula> is accomplished by application of electrical potentials (2–10 <inline-formula><mml:math id="M76" display="inline"><mml:mi mathvariant="normal">V</mml:mi></mml:math></inline-formula>) and collision
gas (Argon, 0.5 <inline-formula><mml:math id="M77" display="inline"><mml:mi mathvariant="normal">mTorr</mml:mi></mml:math></inline-formula>) in the collision-induced dissociation (CID) cell. Mass spectra from product scans are obtained by
transmitting ions of a specific <inline-formula><mml:math id="M78" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> through the first quadrupole (precursor ions), fragmenting in the CID cell, and monitoring the
resulting fragment ions (product ions) by the third quadrupole.</p>
      <p id="d1e1058">In the NL scan mode, the first and third quadrupoles are scanned at the same
rate over mass ranges of the same width; i.e. the third quadrupole transmits
ions at a fixed mass-to-charge ratio lower than the first quadrupole. In the
NL scan, the CID voltage and argon pressure are set at 2–10 <inline-formula><mml:math id="M79" display="inline"><mml:mi mathvariant="normal">V</mml:mi></mml:math></inline-formula> and
0.5 <inline-formula><mml:math id="M80" display="inline"><mml:mi mathvariant="normal">mTorr</mml:mi></mml:math></inline-formula>, respectively. The limit of detection (LOD) of the
analytical method is established by direct injection of the ROOH standard
solution in MeOH with 2–10 <inline-formula><mml:math id="M81" display="inline"><mml:mi mathvariant="normal">mM</mml:mi></mml:math></inline-formula> ammonium acetate into the APCI source
with the tandem mass spectrometer being operated under NL scan mode. Three
ROOH standards – namely 2-butanone peroxide, <italic>tert</italic>-butyl
hydroperoxide and cumene hydroperoxide – are analyzed. Since a neutral loss
of 51 <inline-formula><mml:math id="M82" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> from the ammoniated molecular ion (<inline-formula><mml:math id="M83" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) of
the ROOH is characteristic for ROOH molecules, as will be seen in the next
section, the calibration is performed by operating with a loss of
51 <inline-formula><mml:math id="M84" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> in NL scan. The ROOH concentrations are selected when the
<inline-formula><mml:math id="M85" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> ions are well above the noise and clearly seen in the
average mass spectra. The LOD is reported as 3 times the <inline-formula><mml:math id="M86" display="inline"><mml:mrow><mml:mi>S</mml:mi><mml:mo>/</mml:mo><mml:mi>N</mml:mi></mml:mrow></mml:math></inline-formula> where noise is
estimated at mass-to-charge ratios different from the mass-to-charge ratio
for <inline-formula><mml:math id="M87" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>.</p>
</sec>
</sec>
<sec id="Ch1.S3">
  <title>Results and discussion</title>
<sec id="Ch1.S3.SS1">
  <title>APCI mass spectra of ROOH standards</title>
      <p id="d1e1190">Figure 1 presents examples of the direct infusion (<inline-formula><mml:math id="M88" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>)-APCI mass spectra
for (a) cumene hydroperoxide (cumene HP) and (b) 4,3-ISOPOOH, with and
without addition of AA. The chemical structures and molecular weights (MWs) of
the ROOH analyzed are given in Fig. S1 in the Supplement. Note that we do not
attempt to interpret the mass spectra of ROOH and other standards obtained
under full-scan and SIM modes due to the presence of stabilizers and other
impurities in the standard samples that make the mass spectra complex.
Instead, we focus on the protonated and ammoniated molecular ions of the ROOH
molecules.</p>
      <p id="d1e1200">It can be seen from Fig. 1 that, although cumene HP demonstrates the proton adduct of the molecular ion at <inline-formula><mml:math id="M89" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">153</mml:mn></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M90" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:mi mathvariant="normal">H</mml:mi><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>
(top panel of Fig. 1a), addition of AA results in the ammonium adduct at <inline-formula><mml:math id="M91" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">170</mml:mn></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M92" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) (bottom panel of
Fig. 1a). For ISOPOOH, the molecular ion is not seen in the full-scan mass spectrum (top panel of Fig. 1b), and the dehydrated molecular
ion at <inline-formula><mml:math id="M93" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">101</mml:mn></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M94" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:mi mathvariant="normal">H</mml:mi><mml:mtext>-</mml:mtext><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) is clearly observed instead (top panel of Fig. 1b). This is consistent with previous studies
claiming that hydroperoxy group (-OOH) is not a favorable protonation or deprotonation site with ESI or APCI (Reinnig et al., 2008;
Rondeau et al., 2003; Nilsson et al., 2008).  The addition of AA again leads to significant production of the ammonium adduct of the
molecular ion at <inline-formula><mml:math id="M95" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> 136 (bottom panel of Fig. 1b). Similar effects of AA on the APCI mass spectra are observed for other ROOH
species.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1"><caption><p id="d1e1335">(<inline-formula><mml:math id="M96" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>)-APCI mass spectra of ROOH with and without addition of
ammonium acetate (AA) for <bold>(a)</bold> cumene HP and <bold>(b)</bold> ISOPOOH.</p></caption>
          <?xmltex \igopts{width=199.169291pt}?><graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-f01.png"/>

        </fig>

      <p id="d1e1357">In comparison, a number of other common molecules in atmospheric samples –
e.g. ROOR, carbonyls, alcohols and carboxylic acids – were
also analyzed. The chemical structures of the other oxygenated organics are
given in Fig. S2. Similar to the ROOH samples, the ammonium adducts of the
molecular ions (<inline-formula><mml:math id="M97" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) are obtained for all the substances.
The only difference is that in some cases, e.g. benzoyl peroxide, the
ammonium adduct of the molecular ions can be clearly seen without addition of
AA, via trace levels of ammonia present in the water or air.</p>
</sec>
<sec id="Ch1.S3.SS2">
  <?xmltex \opttitle{Product spectra of {$\chem{{[}M+NH_{{4}}{]}^{{+}}}$} for ROOH and other organics}?><title>Product spectra of <inline-formula><mml:math id="M98" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> for ROOH and other organics</title>
      <p id="d1e1411">Figure 2 gives the CID fragment patterns (i.e. product spectra) for ammonium
adducts of the molecular ions (<inline-formula><mml:math id="M99" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) of (a) cumene HP and
(b) ISOPOOH. Two types of fragmentation, i.e. loss of 35 and 51 <inline-formula><mml:math id="M100" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>
from the respective <inline-formula><mml:math id="M101" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> ions, are observed in both cumene
HP and ISOPOOH. The loss of 35 <inline-formula><mml:math id="M102" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>, corresponding to
[-<inline-formula><mml:math id="M103" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow></mml:math></inline-formula>-<inline-formula><mml:math id="M104" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>]<?pagebreak page3084?> (Fig. S3), is also observed in
<italic>meso</italic>-erythritol and pinonic acid (Fig. S4). Neutral loss of
51 <inline-formula><mml:math id="M105" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>, corresponding to [-<inline-formula><mml:math id="M106" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>-<inline-formula><mml:math id="M107" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>] (Fig. S3), is
only observed from fragmentation of the <inline-formula><mml:math id="M108" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> ions of ROOH
(Figs. 2 and S4). It is known that the loss of the <inline-formula><mml:math id="M109" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow></mml:math></inline-formula> molecule from
protonated molecular ions (<inline-formula><mml:math id="M110" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:mi mathvariant="normal">H</mml:mi><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) is typical for epoxides,
alcohols and carboxylic acids (Holcapek et al., 2010). But the loss of
35 <inline-formula><mml:math id="M111" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> from <inline-formula><mml:math id="M112" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> is not characteristic for ROOH.
Instead, the loss of 51 <inline-formula><mml:math id="M113" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> from <inline-formula><mml:math id="M114" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> is only
observed in ROOH standards, including peracetic acid (Fig. S5). Hence we
propose that the neutral loss of 51 <inline-formula><mml:math id="M115" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> from <inline-formula><mml:math id="M116" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> is
characteristic for ROOH molecules. This is consistent with previous work that
suggested that neutral loss of <inline-formula><mml:math id="M117" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> from <inline-formula><mml:math id="M118" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:mi mathvariant="normal">H</mml:mi><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> is also
characteristic for ROOH species (Reinnig et al., 2009).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2"><caption><p id="d1e1714">Product spectra of <inline-formula><mml:math id="M119" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msubsup><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn><mml:mo>+</mml:mo></mml:msubsup><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> for <bold>(a)</bold> cumene HP
and <bold>(b)</bold> ISOPOOH.</p></caption>
          <?xmltex \igopts{width=199.169291pt}?><graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-f02.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3" specific-use="star"><caption><p id="d1e1755">ROOH formation from reactions of <inline-formula><mml:math id="M120" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> with
<bold>(a)</bold> methylglyoxal and <bold>(b)</bold> glyoxal.</p></caption>
          <?xmltex \igopts{width=312.980315pt}?><graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-f03.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4"><caption><p id="d1e1789"><bold>(a)</bold> Mass spectrum of reaction of methylglyoxal with
<inline-formula><mml:math id="M121" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> in the presence of AA; <bold>(b)</bold> product mass spectrum of
<inline-formula><mml:math id="M122" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> 124 from panel <bold>(a)</bold>.</p></caption>
          <?xmltex \igopts{width=199.169291pt}?><graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-f04.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5"><caption><p id="d1e1836">Mass spectra of SOA from ozone reaction with <inline-formula><mml:math id="M123" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene under
dry conditions (RH <inline-formula><mml:math id="M124" display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 5 %) obtained with <bold>(a)</bold> full scan and
<bold>(b)</bold> neutral loss scan of 51 <inline-formula><mml:math id="M125" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>.</p></caption>
          <?xmltex \igopts{width=199.169291pt}?><graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-f05.png"/>

        </fig>

</sec>
<sec id="Ch1.S3.SS3">
  <?xmltex \opttitle{ROOH formation from the reactions of aldehydes and {$\chem{H_{2}O_{2}}$}}?><title>ROOH formation from the reactions of aldehydes and <inline-formula><mml:math id="M126" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula></title>
      <p id="d1e1894">Using <inline-formula><mml:math id="M127" display="inline"><mml:mrow class="chem"><mml:msup><mml:mi/><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">H</mml:mi></mml:mrow></mml:math></inline-formula> NMR spectroscopy, it has been shown that ROOH species form
from the reactions of aldehydes with <inline-formula><mml:math id="M128" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> (Zhao et al., 2013). As
shown in Fig. 3, the reaction proceeds via reversible nucleophilic addition
of <inline-formula><mml:math id="M129" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> to the carbonyl group in aldehydes, leading to
<inline-formula><mml:math id="M130" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-hydroxyhydroperoxides (HHP). The addition of <inline-formula><mml:math id="M131" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
to methylglyoxal (MGL; MW <inline-formula><mml:math id="M132" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">72</mml:mn></mml:mrow></mml:math></inline-formula>) gives rise to MGL HHP (MW <inline-formula><mml:math id="M133" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">106</mml:mn></mml:mrow></mml:math></inline-formula>)
(Fig. 3a), whose ammonium adduct is seen at <inline-formula><mml:math id="M134" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> 124 in Fig. 4a. The mass
spectrum of the reaction mixture of glyoxal and <inline-formula><mml:math id="M135" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> suggests that,
rather than a direct addition to glyoxal, <inline-formula><mml:math id="M136" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> is instead added to
the glyoxal geminal diol formed by the hydrolysis of glyoxal (Fig. 3b),
producing <inline-formula><mml:math id="M137" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> at <inline-formula><mml:math id="M138" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> 128 (Fig. S6a). The
<inline-formula><mml:math id="M139" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> ROOH peaks are also observed in the reactions of other
aldehydes with <inline-formula><mml:math id="M140" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> (data not shown).</p>
      <p id="d1e2102">The fragmentation spectra of the <inline-formula><mml:math id="M141" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> of the ROOH from
methylglyoxal and glyoxal are given in Figs. 4b and S6b, respectively. It is
clear that the neutral loss of 51 <inline-formula><mml:math id="M142" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> is again observed in the
fragments of the ROOH molecules. The ROOH products from all the other
aldehyde reactions with <inline-formula><mml:math id="M143" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> also show loss of 51 <inline-formula><mml:math id="M144" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> in
<inline-formula><mml:math id="M145" display="inline"><mml:mrow><mml:mtext>MS</mml:mtext><mml:mo>/</mml:mo><mml:mtext>MS</mml:mtext></mml:mrow></mml:math></inline-formula> mode. Overall, we conclude that the neutral loss of
51 <inline-formula><mml:math id="M146" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> from <inline-formula><mml:math id="M147" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> fragmentation can be used to
identify ROOH molecules.</p>
</sec>
<sec id="Ch1.S3.SS4">
  <title>Identification of ROOH in SOA material</title>
      <p id="d1e2205">Figure 5 presents mass spectra of the methanol extract of SOA generated from
ozonolysis of <inline-formula><mml:math id="M148" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene under dry conditions (relative humidity
(RH) <inline-formula><mml:math id="M149" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">5</mml:mn></mml:mrow></mml:math></inline-formula> %). There are three features of note. First, the
well-characterized products from this reaction – such as nopinone aldehyde
(MW <inline-formula><mml:math id="M150" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">154</mml:mn></mml:mrow></mml:math></inline-formula>), terpenylic acid (MW <inline-formula><mml:math id="M151" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">172</mml:mn></mml:mrow></mml:math></inline-formula>) and <italic>cis</italic>-pinic acid
(MW <inline-formula><mml:math id="M152" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">186</mml:mn></mml:mrow></mml:math></inline-formula>) (Jenkin et al., 2000; Larsen et al., 2001; Claeys et al., 2009)
– are present as protonated molecular ions (<inline-formula><mml:math id="M153" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:mi mathvariant="normal">H</mml:mi><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) in the
full-scan mode (Fig. 5a). Second, the full-scan mass spectrum (Fig. 5a) shows
the presence of monomer (<inline-formula><mml:math id="M154" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">80</mml:mn></mml:mrow></mml:math></inline-formula>–250), dimer (<inline-formula><mml:math id="M155" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">250</mml:mn></mml:mrow></mml:math></inline-formula>–450) and trimer
(<inline-formula><mml:math id="M156" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">450</mml:mn></mml:mrow></mml:math></inline-formula>–600)<?pagebreak page3085?> species, as has been reported in previous work (Venkatachari
and Hopke, 2008). Third, and perhaps most importantly, the 51 <inline-formula><mml:math id="M157" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>
neutral loss scan (Fig. 5b) indicates that all the ROOH species have masses
<inline-formula><mml:math id="M158" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">300</mml:mn></mml:mrow></mml:math></inline-formula> Da (Fig. 5b).</p>
      <p id="d1e2344">To confirm the observation of ROOH obtained with the neutral loss scan, CID
fragmentation spectra of a few intense peaks at <inline-formula><mml:math id="M159" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> 190, 202, 206, 218 and
220 in Fig. 5b are analyzed. All the fragments of these products show loss of
51 <inline-formula><mml:math id="M160" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula>. An example of the fragment pattern for <inline-formula><mml:math id="M161" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula> 206 is given in
Fig. S7.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1"><caption><p id="d1e2381">Possible identities of the ROOH in <inline-formula><mml:math id="M162" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene SOA.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="3">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="center"/>
     <oasis:thead>
       <oasis:row>  
         <oasis:entry colname="col1"><inline-formula><mml:math id="M163" display="inline"><mml:mrow><mml:mi>m</mml:mi><mml:mo>/</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col2">Molecular</oasis:entry>  
         <oasis:entry colname="col3">Chemical</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">(<inline-formula><mml:math id="M164" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">M</mml:mi><mml:mo>+</mml:mo><mml:msup><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub><mml:mo>+</mml:mo></mml:msup><mml:msup><mml:mo>]</mml:mo><mml:mo>+</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col2">weight (MW)</oasis:entry>  
         <oasis:entry colname="col3">structure</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">174</oasis:entry>  
         <oasis:entry colname="col2">156</oasis:entry>  
         <oasis:entry colname="col3"/>
       <?xmltex \interline{[-11.381102pt]}?></oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"><?xmltex \igopts{width=46.2528pt}?><inline-graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-g01.pdf"/></oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">190</oasis:entry>  
         <oasis:entry colname="col2">172</oasis:entry>  
         <oasis:entry colname="col3"/>
       <?xmltex \interline{[-11.381102pt]}?></oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"><?xmltex \igopts{width=46.2528pt}?><inline-graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-g02.pdf"/></oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">202</oasis:entry>  
         <oasis:entry colname="col2">184</oasis:entry>  
         <oasis:entry colname="col3"/>
       <?xmltex \interline{[-11.381102pt]}?></oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"><?xmltex \igopts{width=47.6982pt}?><inline-graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-g03.pdf"/></oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">206</oasis:entry>  
         <oasis:entry colname="col2">188</oasis:entry>  
         <oasis:entry colname="col3"/>
       <?xmltex \interline{[-11.381102pt]}?></oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"><?xmltex \igopts{width=47.6982pt}?><inline-graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-g04.pdf"/></oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">218</oasis:entry>  
         <oasis:entry colname="col2">200</oasis:entry>  
         <oasis:entry colname="col3"/>
       <?xmltex \interline{[-11.381102pt]}?></oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"><?xmltex \igopts{width=50.589pt}?><inline-graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-g05.pdf"/></oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">220</oasis:entry>  
         <oasis:entry colname="col2">202</oasis:entry>  
         <oasis:entry colname="col3"/>
       <?xmltex \interline{[-11.381102pt]}?></oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"><?xmltex \igopts{width=60.7068pt}?><inline-graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-g06.pdf"/></oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">232</oasis:entry>  
         <oasis:entry colname="col2">214</oasis:entry>  
         <oasis:entry colname="col3"/>
       <?xmltex \interline{[-11.381102pt]}?></oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"><?xmltex \igopts{width=48.4209pt}?><inline-graphic xlink:href="https://amt.copernicus.org/articles/11/3081/2018/amt-11-3081-2018-g07.pdf"/></oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <p id="d1e2637"><?xmltex \hack{\newpage}?>The ROOH products in SOA are tentatively identified and listed in Table 1.  It should be noted that the chemical structures of these
products are only obtained from their molecular ions and, therefore, remain speculative.</p>
      <?pagebreak page3086?><p id="d1e2642">Several mechanisms for oligomer product formation in SOA arising from VOC
oxidation have been proposed: (i) self- and cross-reactions of the peroxy
radicals (<inline-formula><mml:math id="M165" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">RO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) (Zhang et al., 2015); (ii) reaction of ozonolysis
products in the condensed-phase, such as aldol condensation, esterification,
hemiacetal and peroxyhemiacetal formation (Ziemann, 2003; Tolocka et al.,
2004; Kristensen et al., 2014; Docherty et al., 2005; Muller et al., 2009;
Yasmeen et al., 2010; Hall and Johnston, 2012; Witkowski and Gierczak, 2014;
DePalma et al., 2013; Lim and Turpin, 2015); (iii) dimer cluster formation
from carboxylic acids (Hoffmann et al., 1998; Tobias and Ziemann, 2000;
Claeys et al., 2009; Camredon et al., 2010; DePalma et al., 2013);
(iv) reactions of Criegee intermediates (CIs) with VOCs oxidation products
(Bonn et al., 2002; Lee and Kamens, 2005; Tolocka et al., 2006; Heaton
et al., 2007; Witkowski and Gierczak, 2012; Kristensen et al., 2016; Wang
et al., 2016); and (v) reactions of R<inline-formula><mml:math id="M166" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> radicals with Cis (Sadezky
et al., 2008; Zhao et al., 2015). Among them, the reactions of CIs with
protic substances (water, alcohols, acids and hydroperoxides) can form ROOH.
However, the nature of the ROOH products observed in SOA material suggests
that these reactions do not take place to a significant extent given that
ROOH do not contribute significantly to the dimer and trimer SOA signals
(Fig. 5b). The similar mass patterns for the SOA and ROOH obtained under dry
(RH <inline-formula><mml:math id="M167" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">5</mml:mn></mml:mrow></mml:math></inline-formula> %) and humid (RH <inline-formula><mml:math id="M168" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">50</mml:mn></mml:mrow></mml:math></inline-formula> %) conditions support this
conclusion (Fig. S9). Of course, we can not rule out that the oligomeric ROOH
may not be sensitive with the analytical method used. Additionally, while the
ROOH formation mechanisms are proposed via gas-phase ozonolysis of
<inline-formula><mml:math id="M169" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene (Fig. S8), the ROOH observed in the SOA could also
potentially be arising from the decomposition of peroxyhemiacetals during
methanol extraction.</p>
      <p id="d1e2694">In the neutral loss scan mode, the LOD were measured to be 0.2, 0.3 and
20 <inline-formula><mml:math id="M170" display="inline"><mml:mi mathvariant="normal">mM</mml:mi></mml:math></inline-formula> for 2-butanone peroxide, cumene hydroperoxide and
<italic>tert</italic>-butyl hydroperoxide, respectively. The LODs obtained by this
method are a rough estimation and will vary dependent on a number of
parameters: ionization voltage, sample injection flow, gas flow, CID gas
pressure, CID voltages etc. More importantly, if a specific ROOH is to be
analyzed, then multiple reaction monitoring mode would be applied and the LOD
of the ROOH would be substantially reduced.</p>
</sec>
</sec>
<sec id="Ch1.S4" sec-type="conclusions">
  <title>Conclusions</title>
      <p id="d1e2714">Organic hydroperoxides are molecules of crucial importance to atmospheric chemistry, arising under VOC oxidation schemes that proceed
under low-NO<inline-formula><mml:math id="M171" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> conditions. Indeed, as NO<inline-formula><mml:math id="M172" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> levels continue to drop throughout many parts of the atmosphere through emission control
measures, it is expected that these species will become even more prevalent. Furthermore, many of these ROOH molecules are known to
constitute an important component of secondary organic aerosol material. Once in atmospheric particles, ROOH can participate in
condensed-phase reactions, including nucleophilic processes and photolysis, and they are likely harmful when deposited into lung fluid.</p>
      <p id="d1e2735">A major complication in the study of ROOH chemistry has been the lack of detection techniques that are able to identify different ROOH
species. In this work we present an offline method for the identification of aqueous-phase ROOH molecules which involves first
ionization by adduct formation with ammonium ions and then collision-induced dissociation by a unique fragmentation pathway involving
the simultaneous loss of both <inline-formula><mml:math id="M173" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M174" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>. Although only a fraction of the total ion fragmentation pathway involves
51 <inline-formula><mml:math id="M175" display="inline"><mml:mi mathvariant="normal">Da</mml:mi></mml:math></inline-formula> neutral loss, the specificity of the tandem mass spectrometry approach will yield low detection limits.</p>
      <p id="d1e2772">We illustrate the utility of this analytical method by demonstrating that
a set of ROOH molecules is present in <inline-formula><mml:math id="M176" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene ozonolysis SOA, all
arising from known oxidation mechanisms. Perhaps most interestingly, ROOH
species were not observed to be present in the oligomeric fraction of
<inline-formula><mml:math id="M177" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene ozonolysis SOA, indicating that reactions such as Criegee
radicals reacting with protic substances are not a source of such dimeric and
trimeric molecules (Lim and Turpin, 2015). In this manner, we believe that
this new analytical approach could be used widely to decipher the prevalence
of ROOH molecules in different forms of SOA. Given the specificity of the
method, it could also be used to monitor the kinetics of condensed-phase
reactions of individual ROOH molecules.</p>
      <p id="d1e2789">Although this work focused on the use of this new analytical method to analyze for atmospheric ROOH molecules,<?pagebreak page3087?> it could equally well be
applied to the detection of ROOH molecules in other systems, especially biological ones.</p>
</sec>

      
      </body>
    <back><notes notes-type="dataavailability">

      <p id="d1e2797">Data are available upon request from Jonathan P. D. Abbatt
(jabbatt@chem.utoronto.ca).</p>
  </notes><app-group>
        <supplementary-material position="anchor"><p id="d1e2800"><bold>The Supplement related to this article is available online at <inline-supplementary-material xlink:href="https://doi.org/10.5194/amt-11-3081-2018-supplement" xlink:title="pdf">https://doi.org/10.5194/amt-11-3081-2018-supplement</inline-supplementary-material>.</bold></p></supplementary-material>
        </app-group><notes notes-type="competinginterests">

      <p id="d1e2806">The authors declare that they have no conflict of
interest.</p>
  </notes><ack><title>Acknowledgements</title><p id="d1e2812">This work was supported by the Alfred P. Sloan Foundation and NSERC.
Frank N. Keutsch and Jean C. Rivera-Rios would also like to acknowledge the
support of the National Science Foundation (AGS 1628491, 1628530, 1247421
and 1321987).<?xmltex \hack{\newline}?><?xmltex \hack{\newline}?>
Edited by: Pierre Herckes<?xmltex \hack{\newline}?>
Reviewed by: three anonymous referees</p></ack><ref-list>
    <title>References</title>

      <ref id="bib1.bib1"><label>1</label><mixed-citation> Agon, V. V., Bubb, W. A., Wright, A., Hawkins, C. L., and Davies, M. J.: Sensitizer-mediated photooxidation of histidine
residues: evidence for the formation of reactive side-chain peroxides, Free Radical Bio. Med., 46, 698–710, 2006.</mixed-citation></ref>
      <ref id="bib1.bib2"><label>2</label><mixed-citation>Aljawhary, D., Lee, A. K. Y., and Abbatt, J. P. D.: High-resolution chemical ionization mass spectrometry (ToF-CIMS):
application to study SOA composition and processing, Atmos. Meas. Tech., 6, 3211–3224, <ext-link xlink:href="https://doi.org/10.5194/amt-6-3211-2013" ext-link-type="DOI">10.5194/amt-6-3211-2013</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib3"><label>3</label><mixed-citation> Atkinson, R. and Arey, J.: Atmospheric degradation of volatile organic compounds, Chem. Rev., 103, 4605–4638, 2003.</mixed-citation></ref>
      <ref id="bib1.bib4"><label>4</label><mixed-citation>Bach, R. D., Ayala, P. Y., and Schlegel, H. B.: A reassessment of the bond dissociation energies of peroxides. An
<italic>ab Initio</italic> study, J. Am. Chem. Soc., 118, 12857–12765, 1996.</mixed-citation></ref>
      <ref id="bib1.bib5"><label>5</label><mixed-citation> Banerjee, D. K. and Budke, C. C.: Spectrophotometric determination of traces of peroxides in organic solvents, Anal. Chem.,
36, 792–796, 1964.</mixed-citation></ref>
      <ref id="bib1.bib6"><label>6</label><mixed-citation> Bonn, B., Schuster, G., and Moortgat, G. K.: Influence of water vapor on the process of new particle formation during
monoterpene ozonolysis, J. Phys. Chem. A, 106, 2869–2881, 2002.</mixed-citation></ref>
      <ref id="bib1.bib7"><label>7</label><mixed-citation>Bonn, B., von Kuhlmann, R., and Lawrence, M. G.: High contribution of biogenic hydroperoxides to secondary organic aerosol
formation, Geophys. Res. Lett., 31, L10108, <ext-link xlink:href="https://doi.org/10.1029/2003GL019172" ext-link-type="DOI">10.1029/2003GL019172</ext-link>, 2004.</mixed-citation></ref>
      <ref id="bib1.bib8"><label>8</label><mixed-citation>Camredon, M., Hamilton, J. F., Alam, M. S., Wyche, K. P., Carr, T., White, I. R., Monks, P. S., Rickard, A. R., and Bloss,
W. J.: Distribution of gaseous and particulate organic composition during dark <inline-formula><mml:math id="M178" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene ozonolysis, Atmos. Chem. Phys., 10,
2893–2917, <ext-link xlink:href="https://doi.org/10.5194/acp-10-2893-2010" ext-link-type="DOI">10.5194/acp-10-2893-2010</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib9"><label>9</label><mixed-citation>Claeys, M., Iinuma, Y., Szmigielski, R., Surratt, J. D., Blockhuys, F., Van Alsenoy, C., Böge, O., Sierau, B.,
Gomez-Gonzalez, Y., Vermeylen, R., Van Der Veken, P., Shahgholi, M., Chan, A. W. H., Herrmann, H., Seinfeld, J. H., and Maenhaut, W.:
Terpenylic acid and related compounds from the oxidation of <inline-formula><mml:math id="M179" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene: Implications for new particle formation and growth above
forests, Environ. Sci. Technol., 43, 6976–6982, 2009.</mixed-citation></ref>
      <ref id="bib1.bib10"><label>10</label><mixed-citation> DePalma, J. W., Horan, A. J., Hall, W. A., and Johnston, M. V.: Thermodynamics of oligomer formation: implications for
secondary organic aerosol formation and reactivity, Phys. Chem. Chem. Phys., 15, 6935–6944, 2013.</mixed-citation></ref>
      <ref id="bib1.bib11"><label>11</label><mixed-citation>Docherty, K. S., Wu, W., Lim, Y. B., and Ziemann, P. J.: Contributions of organic peroxides to secondary aerosol formed
from reactions of monoterpenes with <inline-formula><mml:math id="M180" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, Environ. Sci. Technol., 39, 4049–4059, 2005.</mixed-citation></ref>
      <ref id="bib1.bib12"><label>12</label><mixed-citation>Francois, S., Sowka, I., Monod, A., Temime-Roussel, B., Laugier, J. M., and Wortham, H.: Development of an online analyzer
of atmospheric <inline-formula><mml:math id="M181" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and several organic hydroperoxides for field campaigns, Atmos. Res., 74, 525–545, 2005.</mixed-citation></ref>
      <ref id="bib1.bib13"><label>13</label><mixed-citation> Gebicki, S. and Gebicki, J. M.: Formation of peroxides in amino acids and proteins exposed to oxygen free radicals,
Biochem. J., 289, 743–749, 1993.</mixed-citation></ref>
      <ref id="bib1.bib14"><label>14</label><mixed-citation>Hall, W. A. and Johnston, M. V.: Oligomer formation pathways in secondary organic aerosol from MS and
<inline-formula><mml:math id="M182" display="inline"><mml:mrow><mml:mtext>MS</mml:mtext><mml:mo>/</mml:mo><mml:mtext>MS</mml:mtext></mml:mrow></mml:math></inline-formula> measurements with high mass accuracy and resolving power, J. Am. Soc. Mass Spectr., 23, 1097–1108, 2012.</mixed-citation></ref>
      <ref id="bib1.bib15"><label>15</label><mixed-citation> Hasson, A. S., Ho, A. W., Kuwata, K. T., and Paulson, S. E.: Production of stabilized Criegee intermediates and peroxides
in the gas phase ozonolysis of alkenes. 2. Asymmetric and biogenic alkenes, J. Geophys. Res., 106, 34143–34153, 2001.</mixed-citation></ref>
      <ref id="bib1.bib16"><label>16</label><mixed-citation> Heaton, K. J., Dreyfus, M. A., Wang, S., and Johnston, M. V.: Oligomer in the early stage of biogenic secondary organic
aerosol formation and growth, Environ. Sci. Technol., 41, 6129–6136, 2007.</mixed-citation></ref>
      <ref id="bib1.bib17"><label>17</label><mixed-citation>Hoffmann, T., Bandur, R., Marggraf, U., and Linscheid, M.: Molecular composition of organic aerosols formed in the
<inline-formula><mml:math id="M183" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene<inline-formula><mml:math id="M184" display="inline"><mml:mo>/</mml:mo></mml:math></inline-formula><inline-formula><mml:math id="M185" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> reaction: implication for new particle formation processes, J. Geophys. Res., 103, 25569–25578, 1998.</mixed-citation></ref>
      <ref id="bib1.bib18"><label>18</label><mixed-citation> Holcapek, M., Jirasko, R., and Lisa, M.: Basic rules for the interpretation of atmospheric pressure ionization mass
spectra of small molecules, J. Chromatogr. A, 1217, 3908–3921, 2010.</mixed-citation></ref>
      <ref id="bib1.bib19"><label>19</label><mixed-citation> Hong, S. B., Kim, G. S., Kang, C. H., and Lee, J. H.: Measurement of ambient hydroperoxides using an automated HPLC system
and various factors which affect variations of their concentrations in Korea, Environ. Monit. Assess., 147, 23–34, 2008.</mixed-citation></ref>
      <ref id="bib1.bib20"><label>20</label><mixed-citation> Hui, S.-P., Sakurai, T., Ohkawa, F., Furumaki, H., Jin, S., Fuda, H., Takeda, S., Kurosawa, T., and Chiba, H.: Detection and
characterization of cholesteryl ester hydroperoxides in oxidized LDL and oxidized HDL by use of an Orbitrap mass spectrometer,
Anal. Bioanal. Chem., 404, 101–112, 2012a.</mixed-citation></ref>
      <ref id="bib1.bib21"><label>21</label><mixed-citation> Hui, S.-P., Taguchi, Y., Takeda, S., Ohkawa, F., Sakurai, T., Yamaki, S., Jin, S., and Fuda, H.: Quantitative
determination of phosphatidylcholine hydroperoxides during copper oxidation of LDL and HDL by liquid chromatography/mass
spectrometry, Anal. Bioanal. Chem., 403, 1831–1840, 2012b.</mixed-citation></ref>
      <ref id="bib1.bib22"><label>22</label><mixed-citation> Jackson, A. V. and Hewitt, C. N.: Atmospheric hydrogen peroxide and organic hydroperoxides: A review,
Environ. Sci. Technol., 29, 175–228, 1999.</mixed-citation></ref>
      <?pagebreak page3088?><ref id="bib1.bib23"><label>23</label><mixed-citation>Jenkin, M. E.: Modelling the formation and composition of secondary organic aerosol from <inline-formula><mml:math id="M186" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>- and <inline-formula><mml:math id="M187" display="inline"><mml:mi mathvariant="italic">β</mml:mi></mml:math></inline-formula>-pinene
ozonolysis using MCM v3, Atmos. Chem. Phys., 4, 1741–1757, <ext-link xlink:href="https://doi.org/10.5194/acp-4-1741-2004" ext-link-type="DOI">10.5194/acp-4-1741-2004</ext-link>, 2004.</mixed-citation></ref>
      <ref id="bib1.bib24"><label>24</label><mixed-citation>Jenkin, M. E., Shallcross, D. E., and Harvey, J. N.: Development and application of a possible mechanism for the
generation of cis-pinic acid from the ozonolysis of <inline-formula><mml:math id="M188" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>- and <inline-formula><mml:math id="M189" display="inline"><mml:mi mathvariant="italic">β</mml:mi></mml:math></inline-formula>-pinene, Atmos. Environ., 34, 2837–2850, 2000.</mixed-citation></ref>
      <ref id="bib1.bib25"><label>25</label><mixed-citation> Krapf, M., Haddad, I. E., Bruns, E. A., Molteni, U., Daellenbach, K. R., Prevot, A. S. H., Baltensperger, U., and
Dommen, J.: Labile peroxides in secondary organic aerosol, Chemistry, 1, 603–616, 2016.</mixed-citation></ref>
      <ref id="bib1.bib26"><label>26</label><mixed-citation>Kristensen, K., Cui, T., Zhang, H., Gold, A., Glasius, M., and Surratt, J. D.: Dimers in <inline-formula><mml:math id="M190" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene secondary organic
aerosol: effect of hydroxyl radical, ozone, relative humidity and aerosol acidity, Atmos. Chem. Phys., 14, 4201–4218,
<ext-link xlink:href="https://doi.org/10.5194/acp-14-4201-2014" ext-link-type="DOI">10.5194/acp-14-4201-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib27"><label>27</label><mixed-citation>Kristensen, K., Watne, Å. K., Hammes, J., Lutz, A., Petäjä, T., Hallquist, M., Bilde, M., and Glasius, M.:
High-molecular weight dimer esters are major products in aerosols from <inline-formula><mml:math id="M191" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene ozonolysis and the boreal forest,
Environ. Sci. Tech. Let., 3, 280–285, 2016.</mixed-citation></ref>
      <ref id="bib1.bib28"><label>28</label><mixed-citation> Larsen, B. R., Di Bella, D., Glasius, M., Winterhalter, R., Jensen, N. S., and Hjorth, J.: Gas-phase OH oxidation of
monoterpenes: gaseous and particulate products, J. Atmos. Chem., 38, 231–276, 2001.</mixed-citation></ref>
      <ref id="bib1.bib29"><label>29</label><mixed-citation> Lee, M., Heikes, B. G., and O'Sullivan, D. W.: Hydrogen peroxide and organic hydroperoxide in the troposphere: A review,
Atmos. Environ., 34, 3475–3494, 2000.</mixed-citation></ref>
      <ref id="bib1.bib30"><label>30</label><mixed-citation>Lee, S. and Kamens, R. M.: Particle nucleation from the reaction of <inline-formula><mml:math id="M192" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene and <inline-formula><mml:math id="M193" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, Atmos. Environ., 39,
6822–6832, 2005.</mixed-citation></ref>
      <ref id="bib1.bib31"><label>31</label><mixed-citation>Lim, Y. B. and Turpin, B. J.: Laboratory evidence of organic peroxide and peroxyhemiacetal formation in the aqueous phase
and implications for aqueous OH, Atmos. Chem. Phys., 15, 12867–12877, <ext-link xlink:href="https://doi.org/10.5194/acp-15-12867-2015" ext-link-type="DOI">10.5194/acp-15-12867-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib32"><label>32</label><mixed-citation>Liou, G.-Y. and Storz, P.: Reactive oxygen species in cancer, Free Radical Res., 44, 479–496,
<ext-link xlink:href="https://doi.org/10.3109/10715761003667554" ext-link-type="DOI">10.3109/10715761003667554</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib33"><label>33</label><mixed-citation> Moll, C., Biermann, U., and Grosch, W.: Occurrence and formation of bitter-tasting trihydroxy fatty acids in
soybeans, J. Agr. Food Chem., 27, 239–243, 1979.</mixed-citation></ref>
      <ref id="bib1.bib34"><label>34</label><mixed-citation> Morgan, P. M., Pattison, D. I., Hawkins, C. L., and Davies, M. J.: Separation, detection, and quantification of
hydroperoxides formed at side-chain and backbone sites on amino acids, peptides, and proteins, Free Radical Bio. Med., 45,
1279–1289, 2008.</mixed-citation></ref>
      <ref id="bib1.bib35"><label>35</label><mixed-citation> Muller, L., Reinnig, M. C., Hayen, H., and Hoffmann, T.: Characterization of oligomeric compounds in secondary organic
aerosol using liquid chromatography coupled to electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry,
Rapid Commun. Mass Sp., 23, 971–979, 2009.</mixed-citation></ref>
      <ref id="bib1.bib36"><label>36</label><mixed-citation> Nakamura, T. and Maeda, H.: A simple assay for lipid hydroperoxides based on triphenylphosphine oxidation and
high-performance liquid chromatography, Lipids, 26, 765–768, 1991.</mixed-citation></ref>
      <ref id="bib1.bib37"><label>37</label><mixed-citation> Nilsson, J., Carlberg, J., Abrahamsson, P., Hulthe, G., Persson, B. A., and Karlberg, A. T.: Evaluation of ionization
techniques for mass spectrometric detection of contact allergenic hydroperoxides formed by autoxidation of fragrance terpenes, Rapid
Commun. Mass Sp., 22, 3593–3598, 2008.</mixed-citation></ref>
      <ref id="bib1.bib38"><label>38</label><mixed-citation> Odian, G.: Principles of Polymerization, 4th ed., Wiley-Interscience, New York, USA, 2004.</mixed-citation></ref>
      <ref id="bib1.bib39"><label>39</label><mixed-citation>Reile, I., Paju, A., Müürisepp, A.-M., Pehk, T., and Lopp, M.: Oxidation of cyclopentane-1,2-dione: a study with
<inline-formula><mml:math id="M194" display="inline"><mml:mrow class="chem"><mml:msup><mml:mi/><mml:mn mathvariant="normal">18</mml:mn></mml:msup><mml:mi mathvariant="normal">O</mml:mi></mml:mrow></mml:math></inline-formula> labeled reagents, Tetrahedron, 67, 5942–5948, 2011.</mixed-citation></ref>
      <ref id="bib1.bib40"><label>40</label><mixed-citation> Reinnig, M. C., Mueller, L., Warnke, J., and Hoffmann, T.: Characterization of selected organic compound classes in
secondary organic aerosol from biogenic VOCs by HPLC/MSn, Anal. Bioanal. Chem., 391, 171–182, 2008.</mixed-citation></ref>
      <ref id="bib1.bib41"><label>41</label><mixed-citation> Reinnig, M. C., Warnke, J., and Hoffmann, T.: Identification of organic hydroperoxides and hydroperoxy acids in secondary
organic aerosol formed during the ozonolysis of different monoterpenes and sesquiterpenes by on-line analysis using atmospheric
pressure chemical ionization ion trap mass spectrometry, Rapid Commun. Mass Sp., 23, 1735–1741, 2009.</mixed-citation></ref>
      <ref id="bib1.bib42"><label>42</label><mixed-citation> Riva, M., Budisulistiorini, S. H., Zhang, Z., Gold, A., Thornton, J. A., Turpin, B. J., and Surratt, J. D.: Multiphase
reactivity of gaseous hydroperoxide oligomers produced from isoprene ozonolysis in the presence of acidified aerosols,
Atmos. Environ., 152, 314–322, 2017.</mixed-citation></ref>
      <ref id="bib1.bib43"><label>43</label><mixed-citation> Rivera-Rios, J. C., Nguyen, T. B., Crounse, J. D., Jud, W., St. Clair, J. M., Mikoviny, T., Gilman, J. B., Lerner, B. M.,
Kaiser, J. B., de Gouw, J., Wisthaler, A., Hansel, A., Wennberg, P. O., Seinfeld, J. H., and Keutsch, F. N.: Conversion of
hydroperoxides to carbonyls in field and laboratory instrumentation: Observational bias in diagnosing pristine versus
anthropogenically controlled atmospheric chemistry, Geophys. Res. Lett., 41, 8645–8651, 2014.</mixed-citation></ref>
      <ref id="bib1.bib44"><label>44</label><mixed-citation> Rondeau, D., Vogel, R., and Tabet, J. C.: Unusual atmospheric pressure chemical ionization conditions for detection of
organic peroxides, J. Mass Spectrom., 38, 931–940, 2003.</mixed-citation></ref>
      <ref id="bib1.bib45"><label>45</label><mixed-citation>Sadezky, A., Winterhalter, R., Kanawati, B., Römpp, A., Spengler, B., Mellouki, A., Le Bras, G., Chaimbault, P., and
Moortgat, G. K.: Oligomer formation during gas-phase ozonolysis of small alkenes and enol ethers: new evidence for the central role
of the Criegee Intermediate as oligomer chain unit, Atmos. Chem. Phys., 8, 2667–2699, <ext-link xlink:href="https://doi.org/10.5194/acp-8-2667-2008" ext-link-type="DOI">10.5194/acp-8-2667-2008</ext-link>, 2008.</mixed-citation></ref>
      <ref id="bib1.bib46"><label>46</label><mixed-citation> Sakamoto, Y., Yajima, R., Inomata, S., and Hirokawa, J.: Water vapour effects on secondary organic aerosol formation in
isoprene ozonolysis, Phys. Chem. Chem. Phys., 19, 3165–3175, 2017.</mixed-citation></ref>
      <ref id="bib1.bib47"><label>47</label><mixed-citation>Tobias, H. J. and Ziemann, P. J.: Thermal desorption mass spectrometric analysis of organic aerosol formed from reactions
of 1-tetradecene and <inline-formula><mml:math id="M195" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> in the presence of alcohols and carboxylic acids, Environ. Sci. Technol., 34, 2105–2115, 2000.</mixed-citation></ref>
      <ref id="bib1.bib48"><label>48</label><mixed-citation> Tolocka, M. P., Jang, M., Ginter, J. M., Cox, F. J., Kamens, R. M., and Johnston, M. V.: Formation of oligomers in
secondary organic aerosol, Environ. Sci. Technol., 38, 1428–1434, 2004.</mixed-citation></ref>
      <ref id="bib1.bib49"><label>49</label><mixed-citation>Tolocka, M. P., Heaton, K. J., Dreyfus, M. A., Wang, S. Y., Zordan, C. A., Saul, T. D., and Johnston, M. V.: Chemistry of
particle inception and growth during <inline-formula><mml:math id="M196" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene ozonolysis, Environ. Sci. Technol., 40, 1843–1848, 2006.</mixed-citation></ref>
      <ref id="bib1.bib50"><label>50</label><mixed-citation>Valverde-Canossa, J., Wieprecht, W., Acker, K., and Moortgat, G. K.: <inline-formula><mml:math id="M197" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and organic peroxide measurements in an
orographic cloud: The FEBUKO experiment, Atmos. Environ., 39, 4279–4290, 2005.</mixed-citation></ref>
      <?pagebreak page3089?><ref id="bib1.bib51"><label>51</label><mixed-citation>Venkatachari, P. and Hopke, P. K.: Characterization of products formed in the reaction of ozone with <inline-formula><mml:math id="M198" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene: Case
for organic peroxides, J. Environ. Monitor., 10, 966–974, 2008.</mixed-citation></ref>
      <ref id="bib1.bib52"><label>52</label><mixed-citation>Walker, S. J., Evans, M. J., Jackson, A. V., Steinbacher, M., Zellweger, C., and McQuaid, J. B.: Processes controlling the
concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland, Atmos. Chem. Phys., 6, 5525–5536,
<ext-link xlink:href="https://doi.org/10.5194/acp-6-5525-2006" ext-link-type="DOI">10.5194/acp-6-5525-2006</ext-link>, 2006.</mixed-citation></ref>
      <ref id="bib1.bib53"><label>53</label><mixed-citation> Wang, M., Yao, L., Zheng, J., Wang, X., Chen, J., Yang, X., Worsnop, D. R., Donahue, N. M., and Wang, L.: Reactions of
atmospheric particulate stabilized Criegee intermediates lead to high-molecular-weight aerosol components, Environ. Sci. Technol.,
50, 5702–5710, 2016.</mixed-citation></ref>
      <ref id="bib1.bib54"><label>54</label><mixed-citation> Wasylaschuk, W. R., Harmon, P. A., Wagner, G., Harman, A. B., Templeton, A. C., Xu, H., and Reed, R. A.: Evaluation of
hydroperoxides in common pharmaceutical excipients, J. Pharm. Sci., 96, 106–116, 2007.</mixed-citation></ref>
      <ref id="bib1.bib55"><label>55</label><mixed-citation>Witkowski, B. and Gierczak, T.: Early stage composition of SOA produced by <inline-formula><mml:math id="M199" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene<inline-formula><mml:math id="M200" display="inline"><mml:mo>/</mml:mo></mml:math></inline-formula>ozone reaction:
<inline-formula><mml:math id="M201" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-Acyloxyhydroperoxy aldehydes and acidic dimers, Atmos. Environ., 95, 59–70, 2014.</mixed-citation></ref>
      <ref id="bib1.bib56"><label>56</label><mixed-citation> Wright, A., Bubb, W. A., Haekins, C. L., and Davis, M. J.: Singlet oxygen-mediated protein oxidation: Evidence for the
formation of reactive side chain peroxides on tyrosine residues, Photochem. Photobiol., 76, 35–46, 2002.</mixed-citation></ref>
      <ref id="bib1.bib57"><label>57</label><mixed-citation>Yasmeen, F., Vermeylen, R., Szmigielski, R., Iinuma, Y., Böge, O., Herrmann, H., Maenhaut, W., and Claeys, M.:
Terpenylic acid and related compounds: precursors for dimers in secondary organic aerosol from the ozonolysis of <inline-formula><mml:math id="M202" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>- and
<inline-formula><mml:math id="M203" display="inline"><mml:mi mathvariant="italic">β</mml:mi></mml:math></inline-formula>-pinene, Atmos. Chem. Phys., 10, 9383–9392, <ext-link xlink:href="https://doi.org/10.5194/acp-10-9383-2010" ext-link-type="DOI">10.5194/acp-10-9383-2010</ext-link>, 2010.
</mixed-citation></ref><?xmltex \hack{\newpage}?>
      <ref id="bib1.bib58"><label>58</label><mixed-citation>Zhang, X., McVay, R. C., Huang, D. D., Dalleska, N. K., Aumont, B., Flagan, R. C., and Seinfeld, J. H.: Formation and
evolution of molecular products in <inline-formula><mml:math id="M204" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene secondary organic aerosol, P. Natl. Acad. Sci. USA, 112, 14168–14173,
2015.</mixed-citation></ref>
      <ref id="bib1.bib59"><label>59</label><mixed-citation>Zhang, X., Lambe, A. T., Upshur, M. A., Brooks, W. A., Be, A. G., Thomson, R. J., and Geiger, F. M.: Hihgly oxygenated
multifunctional compounds in <inline-formula><mml:math id="M205" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene secondary organic aerosol, Environ. Sci. Technol., 51, 5932–5940, 2017.</mixed-citation></ref>
      <ref id="bib1.bib60"><label>60</label><mixed-citation>Zhao, R., Lee, A. K. Y., Soong, R., Simpson, A. J., and Abbatt, J. P. D.: Formation of aqueous-phase
<inline-formula><mml:math id="M206" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-hydroxyhydroperoxides (<inline-formula><mml:math id="M207" display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-HHP): potential atmospheric impacts, Atmos. Chem. Phys., 13, 5857–5872,
<ext-link xlink:href="https://doi.org/10.5194/acp-13-5857-2013" ext-link-type="DOI">10.5194/acp-13-5857-2013</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib61"><label>61</label><mixed-citation> Zhao, Y., Wingen, L. M., Perraud, V., Greaves, J., and Finlayson-Pitts, B. J.: Role of the reaction of stabilized Criegee
intermediates with peroxy radicals in particle formation and growth in air, Phys. Chem. Chem. Phys., 17, 12500–12514, 2015.</mixed-citation></ref>
      <ref id="bib1.bib62"><label>62</label><mixed-citation>Ziemann, P. J.: Formation of alkoxyhydroperoxy aldehydes and cyclic peroxyhemiacetals from reactions of cyclic alkenes
with <inline-formula><mml:math id="M208" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> in the presence of alcohols, J. Phys. Chem. A, 107, 2048–2060, 2003.</mixed-citation></ref>

  </ref-list></back>
    <!--<article-title-html>Identification of organic hydroperoxides and peroxy acids using atmospheric pressure chemical ionization–tandem mass spectrometry (APCI-MS/MS): application to secondary organic aerosol</article-title-html>
<abstract-html><p>Molecules with hydroperoxide functional groups are of extreme
importance to both the atmospheric and biological chemistry fields. In
this work, an analytical method is presented for the identification of organic hydroperoxides and peroxy acids (ROOH) by direct
infusion of liquid samples into a positive-ion atmospheric pressure chemical ionization–tandem mass spectrometer
((+)-APCI-MS/MS). Under collisional dissociation conditions, a characteristic neutral loss of 51 Da (arising from loss of
H<sub>2</sub>O<sub>2</sub>+NH<sub>3</sub>) from ammonium adducts of the molecular ions ([M + NH<sub>4</sub>]<sup>+</sup>) is observed for ROOH standards
(i.e. cumene hydroperoxide, isoprene-4-hydroxy-3-hydroperoxide (ISOPOOH), <i>tert</i>-butyl hydroperoxide, 2-butanone peroxide and peracetic
acid), as well as the ROOH formed from the reactions of H<sub>2</sub>O<sub>2</sub> with aldehydes (i.e.  acetaldehyde, hexanal, glyoxal and
methylglyoxal). This new ROOH detection method was applied to methanol extracts of secondary organic aerosol (SOA) material generated
from ozonolysis of <i>α</i>-pinene, indicating a number of ROOH molecules in the SOA material. While the full-scan mass spectrum of
SOA demonstrates the presence of monomers (<i>m</i>∕<i>z</i>  =  80–250), dimers (<i>m</i>∕<i>z</i>  =  250–450) and trimers (<i>m</i>∕<i>z</i>  =  450–600), the neutral loss
scan shows that the ROOH products all have masses less than 300 Da, indicating that ROOH molecules may not contribute significantly
to the SOA oligomeric content. We anticipate this method could also be applied to biological systems with considerable value.</p></abstract-html>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation> Agon, V. V., Bubb, W. A., Wright, A., Hawkins, C. L., and Davies, M. J.: Sensitizer-mediated photooxidation of histidine
residues: evidence for the formation of reactive side-chain peroxides, Free Radical Bio. Med., 46, 698–710, 2006.
</mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation> Aljawhary, D., Lee, A. K. Y., and Abbatt, J. P. D.: High-resolution chemical ionization mass spectrometry (ToF-CIMS):
application to study SOA composition and processing, Atmos. Meas. Tech., 6, 3211–3224, <a href="https://doi.org/10.5194/amt-6-3211-2013" target="_blank">https://doi.org/10.5194/amt-6-3211-2013</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib3"><label>3</label><mixed-citation> Atkinson, R. and Arey, J.: Atmospheric degradation of volatile organic compounds, Chem. Rev., 103, 4605–4638, 2003.
</mixed-citation></ref-html>
<ref-html id="bib1.bib4"><label>4</label><mixed-citation> Bach, R. D., Ayala, P. Y., and Schlegel, H. B.: A reassessment of the bond dissociation energies of peroxides. An
<i>ab Initio</i> study, J. Am. Chem. Soc., 118, 12857–12765, 1996.
</mixed-citation></ref-html>
<ref-html id="bib1.bib5"><label>5</label><mixed-citation> Banerjee, D. K. and Budke, C. C.: Spectrophotometric determination of traces of peroxides in organic solvents, Anal. Chem.,
36, 792–796, 1964.
</mixed-citation></ref-html>
<ref-html id="bib1.bib6"><label>6</label><mixed-citation> Bonn, B., Schuster, G., and Moortgat, G. K.: Influence of water vapor on the process of new particle formation during
monoterpene ozonolysis, J. Phys. Chem. A, 106, 2869–2881, 2002.
</mixed-citation></ref-html>
<ref-html id="bib1.bib7"><label>7</label><mixed-citation> Bonn, B., von Kuhlmann, R., and Lawrence, M. G.: High contribution of biogenic hydroperoxides to secondary organic aerosol
formation, Geophys. Res. Lett., 31, L10108, <a href="https://doi.org/10.1029/2003GL019172" target="_blank">https://doi.org/10.1029/2003GL019172</a>, 2004.
</mixed-citation></ref-html>
<ref-html id="bib1.bib8"><label>8</label><mixed-citation> Camredon, M., Hamilton, J. F., Alam, M. S., Wyche, K. P., Carr, T., White, I. R., Monks, P. S., Rickard, A. R., and Bloss,
W. J.: Distribution of gaseous and particulate organic composition during dark <i>α</i>-pinene ozonolysis, Atmos. Chem. Phys., 10,
2893–2917, <a href="https://doi.org/10.5194/acp-10-2893-2010" target="_blank">https://doi.org/10.5194/acp-10-2893-2010</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib9"><label>9</label><mixed-citation> Claeys, M., Iinuma, Y., Szmigielski, R., Surratt, J. D., Blockhuys, F., Van Alsenoy, C., Böge, O., Sierau, B.,
Gomez-Gonzalez, Y., Vermeylen, R., Van Der Veken, P., Shahgholi, M., Chan, A. W. H., Herrmann, H., Seinfeld, J. H., and Maenhaut, W.:
Terpenylic acid and related compounds from the oxidation of <i>α</i>-pinene: Implications for new particle formation and growth above
forests, Environ. Sci. Technol., 43, 6976–6982, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib10"><label>10</label><mixed-citation> DePalma, J. W., Horan, A. J., Hall, W. A., and Johnston, M. V.: Thermodynamics of oligomer formation: implications for
secondary organic aerosol formation and reactivity, Phys. Chem. Chem. Phys., 15, 6935–6944, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib11"><label>11</label><mixed-citation> Docherty, K. S., Wu, W., Lim, Y. B., and Ziemann, P. J.: Contributions of organic peroxides to secondary aerosol formed
from reactions of monoterpenes with O<sub>3</sub>, Environ. Sci. Technol., 39, 4049–4059, 2005.
</mixed-citation></ref-html>
<ref-html id="bib1.bib12"><label>12</label><mixed-citation> Francois, S., Sowka, I., Monod, A., Temime-Roussel, B., Laugier, J. M., and Wortham, H.: Development of an online analyzer
of atmospheric H<sub>2</sub>O<sub>2</sub> and several organic hydroperoxides for field campaigns, Atmos. Res., 74, 525–545, 2005.
</mixed-citation></ref-html>
<ref-html id="bib1.bib13"><label>13</label><mixed-citation> Gebicki, S. and Gebicki, J. M.: Formation of peroxides in amino acids and proteins exposed to oxygen free radicals,
Biochem. J., 289, 743–749, 1993.
</mixed-citation></ref-html>
<ref-html id="bib1.bib14"><label>14</label><mixed-citation> Hall, W. A. and Johnston, M. V.: Oligomer formation pathways in secondary organic aerosol from MS and
MS∕MS measurements with high mass accuracy and resolving power, J. Am. Soc. Mass Spectr., 23, 1097–1108, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib15"><label>15</label><mixed-citation> Hasson, A. S., Ho, A. W., Kuwata, K. T., and Paulson, S. E.: Production of stabilized Criegee intermediates and peroxides
in the gas phase ozonolysis of alkenes. 2. Asymmetric and biogenic alkenes, J. Geophys. Res., 106, 34143–34153, 2001.
</mixed-citation></ref-html>
<ref-html id="bib1.bib16"><label>16</label><mixed-citation> Heaton, K. J., Dreyfus, M. A., Wang, S., and Johnston, M. V.: Oligomer in the early stage of biogenic secondary organic
aerosol formation and growth, Environ. Sci. Technol., 41, 6129–6136, 2007.
</mixed-citation></ref-html>
<ref-html id="bib1.bib17"><label>17</label><mixed-citation> Hoffmann, T., Bandur, R., Marggraf, U., and Linscheid, M.: Molecular composition of organic aerosols formed in the
<i>α</i>-pinene∕O<sub>3</sub> reaction: implication for new particle formation processes, J. Geophys. Res., 103, 25569–25578, 1998.
</mixed-citation></ref-html>
<ref-html id="bib1.bib18"><label>18</label><mixed-citation> Holcapek, M., Jirasko, R., and Lisa, M.: Basic rules for the interpretation of atmospheric pressure ionization mass
spectra of small molecules, J. Chromatogr. A, 1217, 3908–3921, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib19"><label>19</label><mixed-citation> Hong, S. B., Kim, G. S., Kang, C. H., and Lee, J. H.: Measurement of ambient hydroperoxides using an automated HPLC system
and various factors which affect variations of their concentrations in Korea, Environ. Monit. Assess., 147, 23–34, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib20"><label>20</label><mixed-citation> Hui, S.-P., Sakurai, T., Ohkawa, F., Furumaki, H., Jin, S., Fuda, H., Takeda, S., Kurosawa, T., and Chiba, H.: Detection and
characterization of cholesteryl ester hydroperoxides in oxidized LDL and oxidized HDL by use of an Orbitrap mass spectrometer,
Anal. Bioanal. Chem., 404, 101–112, 2012a.
</mixed-citation></ref-html>
<ref-html id="bib1.bib21"><label>21</label><mixed-citation> Hui, S.-P., Taguchi, Y., Takeda, S., Ohkawa, F., Sakurai, T., Yamaki, S., Jin, S., and Fuda, H.: Quantitative
determination of phosphatidylcholine hydroperoxides during copper oxidation of LDL and HDL by liquid chromatography/mass
spectrometry, Anal. Bioanal. Chem., 403, 1831–1840, 2012b.
</mixed-citation></ref-html>
<ref-html id="bib1.bib22"><label>22</label><mixed-citation> Jackson, A. V. and Hewitt, C. N.: Atmospheric hydrogen peroxide and organic hydroperoxides: A review,
Environ. Sci. Technol., 29, 175–228, 1999.
</mixed-citation></ref-html>
<ref-html id="bib1.bib23"><label>23</label><mixed-citation> Jenkin, M. E.: Modelling the formation and composition of secondary organic aerosol from <i>α</i>- and <i>β</i>-pinene
ozonolysis using MCM v3, Atmos. Chem. Phys., 4, 1741–1757, <a href="https://doi.org/10.5194/acp-4-1741-2004" target="_blank">https://doi.org/10.5194/acp-4-1741-2004</a>, 2004.
</mixed-citation></ref-html>
<ref-html id="bib1.bib24"><label>24</label><mixed-citation> Jenkin, M. E., Shallcross, D. E., and Harvey, J. N.: Development and application of a possible mechanism for the
generation of cis-pinic acid from the ozonolysis of <i>α</i>- and <i>β</i>-pinene, Atmos. Environ., 34, 2837–2850, 2000.
</mixed-citation></ref-html>
<ref-html id="bib1.bib25"><label>25</label><mixed-citation> Krapf, M., Haddad, I. E., Bruns, E. A., Molteni, U., Daellenbach, K. R., Prevot, A. S. H., Baltensperger, U., and
Dommen, J.: Labile peroxides in secondary organic aerosol, Chemistry, 1, 603–616, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib26"><label>26</label><mixed-citation> Kristensen, K., Cui, T., Zhang, H., Gold, A., Glasius, M., and Surratt, J. D.: Dimers in <i>α</i>-pinene secondary organic
aerosol: effect of hydroxyl radical, ozone, relative humidity and aerosol acidity, Atmos. Chem. Phys., 14, 4201–4218,
<a href="https://doi.org/10.5194/acp-14-4201-2014" target="_blank">https://doi.org/10.5194/acp-14-4201-2014</a>, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib27"><label>27</label><mixed-citation> Kristensen, K., Watne, Å. K., Hammes, J., Lutz, A., Petäjä, T., Hallquist, M., Bilde, M., and Glasius, M.:
High-molecular weight dimer esters are major products in aerosols from <i>α</i>-pinene ozonolysis and the boreal forest,
Environ. Sci. Tech. Let., 3, 280–285, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib28"><label>28</label><mixed-citation> Larsen, B. R., Di Bella, D., Glasius, M., Winterhalter, R., Jensen, N. S., and Hjorth, J.: Gas-phase OH oxidation of
monoterpenes: gaseous and particulate products, J. Atmos. Chem., 38, 231–276, 2001.
</mixed-citation></ref-html>
<ref-html id="bib1.bib29"><label>29</label><mixed-citation> Lee, M., Heikes, B. G., and O'Sullivan, D. W.: Hydrogen peroxide and organic hydroperoxide in the troposphere: A review,
Atmos. Environ., 34, 3475–3494, 2000.
</mixed-citation></ref-html>
<ref-html id="bib1.bib30"><label>30</label><mixed-citation> Lee, S. and Kamens, R. M.: Particle nucleation from the reaction of <i>α</i>-pinene and O<sub>3</sub>, Atmos. Environ., 39,
6822–6832, 2005.
</mixed-citation></ref-html>
<ref-html id="bib1.bib31"><label>31</label><mixed-citation> Lim, Y. B. and Turpin, B. J.: Laboratory evidence of organic peroxide and peroxyhemiacetal formation in the aqueous phase
and implications for aqueous OH, Atmos. Chem. Phys., 15, 12867–12877, <a href="https://doi.org/10.5194/acp-15-12867-2015" target="_blank">https://doi.org/10.5194/acp-15-12867-2015</a>, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib32"><label>32</label><mixed-citation> Liou, G.-Y. and Storz, P.: Reactive oxygen species in cancer, Free Radical Res., 44, 479–496,
<a href="https://doi.org/10.3109/10715761003667554" target="_blank">https://doi.org/10.3109/10715761003667554</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib33"><label>33</label><mixed-citation> Moll, C., Biermann, U., and Grosch, W.: Occurrence and formation of bitter-tasting trihydroxy fatty acids in
soybeans, J. Agr. Food Chem., 27, 239–243, 1979.
</mixed-citation></ref-html>
<ref-html id="bib1.bib34"><label>34</label><mixed-citation> Morgan, P. M., Pattison, D. I., Hawkins, C. L., and Davies, M. J.: Separation, detection, and quantification of
hydroperoxides formed at side-chain and backbone sites on amino acids, peptides, and proteins, Free Radical Bio. Med., 45,
1279–1289, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib35"><label>35</label><mixed-citation> Muller, L., Reinnig, M. C., Hayen, H., and Hoffmann, T.: Characterization of oligomeric compounds in secondary organic
aerosol using liquid chromatography coupled to electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry,
Rapid Commun. Mass Sp., 23, 971–979, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib36"><label>36</label><mixed-citation> Nakamura, T. and Maeda, H.: A simple assay for lipid hydroperoxides based on triphenylphosphine oxidation and
high-performance liquid chromatography, Lipids, 26, 765–768, 1991.
</mixed-citation></ref-html>
<ref-html id="bib1.bib37"><label>37</label><mixed-citation> Nilsson, J., Carlberg, J., Abrahamsson, P., Hulthe, G., Persson, B. A., and Karlberg, A. T.: Evaluation of ionization
techniques for mass spectrometric detection of contact allergenic hydroperoxides formed by autoxidation of fragrance terpenes, Rapid
Commun. Mass Sp., 22, 3593–3598, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib38"><label>38</label><mixed-citation> Odian, G.: Principles of Polymerization, 4th ed., Wiley-Interscience, New York, USA, 2004.
</mixed-citation></ref-html>
<ref-html id="bib1.bib39"><label>39</label><mixed-citation> Reile, I., Paju, A., Müürisepp, A.-M., Pehk, T., and Lopp, M.: Oxidation of cyclopentane-1,2-dione: a study with
<sup>18</sup>O labeled reagents, Tetrahedron, 67, 5942–5948, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib40"><label>40</label><mixed-citation> Reinnig, M. C., Mueller, L., Warnke, J., and Hoffmann, T.: Characterization of selected organic compound classes in
secondary organic aerosol from biogenic VOCs by HPLC/MSn, Anal. Bioanal. Chem., 391, 171–182, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib41"><label>41</label><mixed-citation> Reinnig, M. C., Warnke, J., and Hoffmann, T.: Identification of organic hydroperoxides and hydroperoxy acids in secondary
organic aerosol formed during the ozonolysis of different monoterpenes and sesquiterpenes by on-line analysis using atmospheric
pressure chemical ionization ion trap mass spectrometry, Rapid Commun. Mass Sp., 23, 1735–1741, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib42"><label>42</label><mixed-citation> Riva, M., Budisulistiorini, S. H., Zhang, Z., Gold, A., Thornton, J. A., Turpin, B. J., and Surratt, J. D.: Multiphase
reactivity of gaseous hydroperoxide oligomers produced from isoprene ozonolysis in the presence of acidified aerosols,
Atmos. Environ., 152, 314–322, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib43"><label>43</label><mixed-citation> Rivera-Rios, J. C., Nguyen, T. B., Crounse, J. D., Jud, W., St. Clair, J. M., Mikoviny, T., Gilman, J. B., Lerner, B. M.,
Kaiser, J. B., de Gouw, J., Wisthaler, A., Hansel, A., Wennberg, P. O., Seinfeld, J. H., and Keutsch, F. N.: Conversion of
hydroperoxides to carbonyls in field and laboratory instrumentation: Observational bias in diagnosing pristine versus
anthropogenically controlled atmospheric chemistry, Geophys. Res. Lett., 41, 8645–8651, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib44"><label>44</label><mixed-citation> Rondeau, D., Vogel, R., and Tabet, J. C.: Unusual atmospheric pressure chemical ionization conditions for detection of
organic peroxides, J. Mass Spectrom., 38, 931–940, 2003.
</mixed-citation></ref-html>
<ref-html id="bib1.bib45"><label>45</label><mixed-citation> Sadezky, A., Winterhalter, R., Kanawati, B., Römpp, A., Spengler, B., Mellouki, A., Le Bras, G., Chaimbault, P., and
Moortgat, G. K.: Oligomer formation during gas-phase ozonolysis of small alkenes and enol ethers: new evidence for the central role
of the Criegee Intermediate as oligomer chain unit, Atmos. Chem. Phys., 8, 2667–2699, <a href="https://doi.org/10.5194/acp-8-2667-2008" target="_blank">https://doi.org/10.5194/acp-8-2667-2008</a>, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib46"><label>46</label><mixed-citation> Sakamoto, Y., Yajima, R., Inomata, S., and Hirokawa, J.: Water vapour effects on secondary organic aerosol formation in
isoprene ozonolysis, Phys. Chem. Chem. Phys., 19, 3165–3175, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib47"><label>47</label><mixed-citation> Tobias, H. J. and Ziemann, P. J.: Thermal desorption mass spectrometric analysis of organic aerosol formed from reactions
of 1-tetradecene and O<sub>3</sub> in the presence of alcohols and carboxylic acids, Environ. Sci. Technol., 34, 2105–2115, 2000.
</mixed-citation></ref-html>
<ref-html id="bib1.bib48"><label>48</label><mixed-citation> Tolocka, M. P., Jang, M., Ginter, J. M., Cox, F. J., Kamens, R. M., and Johnston, M. V.: Formation of oligomers in
secondary organic aerosol, Environ. Sci. Technol., 38, 1428–1434, 2004.
</mixed-citation></ref-html>
<ref-html id="bib1.bib49"><label>49</label><mixed-citation> Tolocka, M. P., Heaton, K. J., Dreyfus, M. A., Wang, S. Y., Zordan, C. A., Saul, T. D., and Johnston, M. V.: Chemistry of
particle inception and growth during <i>α</i>-pinene ozonolysis, Environ. Sci. Technol., 40, 1843–1848, 2006.
</mixed-citation></ref-html>
<ref-html id="bib1.bib50"><label>50</label><mixed-citation> Valverde-Canossa, J., Wieprecht, W., Acker, K., and Moortgat, G. K.: H<sub>2</sub>O<sub>2</sub> and organic peroxide measurements in an
orographic cloud: The FEBUKO experiment, Atmos. Environ., 39, 4279–4290, 2005.
</mixed-citation></ref-html>
<ref-html id="bib1.bib51"><label>51</label><mixed-citation> Venkatachari, P. and Hopke, P. K.: Characterization of products formed in the reaction of ozone with <i>α</i>-pinene: Case
for organic peroxides, J. Environ. Monitor., 10, 966–974, 2008.
</mixed-citation></ref-html>
<ref-html id="bib1.bib52"><label>52</label><mixed-citation> Walker, S. J., Evans, M. J., Jackson, A. V., Steinbacher, M., Zellweger, C., and McQuaid, J. B.: Processes controlling the
concentration of hydroperoxides at Jungfraujoch Observatory, Switzerland, Atmos. Chem. Phys., 6, 5525–5536,
<a href="https://doi.org/10.5194/acp-6-5525-2006" target="_blank">https://doi.org/10.5194/acp-6-5525-2006</a>, 2006.
</mixed-citation></ref-html>
<ref-html id="bib1.bib53"><label>53</label><mixed-citation> Wang, M., Yao, L., Zheng, J., Wang, X., Chen, J., Yang, X., Worsnop, D. R., Donahue, N. M., and Wang, L.: Reactions of
atmospheric particulate stabilized Criegee intermediates lead to high-molecular-weight aerosol components, Environ. Sci. Technol.,
50, 5702–5710, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib54"><label>54</label><mixed-citation> Wasylaschuk, W. R., Harmon, P. A., Wagner, G., Harman, A. B., Templeton, A. C., Xu, H., and Reed, R. A.: Evaluation of
hydroperoxides in common pharmaceutical excipients, J. Pharm. Sci., 96, 106–116, 2007.
</mixed-citation></ref-html>
<ref-html id="bib1.bib55"><label>55</label><mixed-citation> Witkowski, B. and Gierczak, T.: Early stage composition of SOA produced by <i>α</i>-pinene∕ozone reaction:
<i>α</i>-Acyloxyhydroperoxy aldehydes and acidic dimers, Atmos. Environ., 95, 59–70, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib56"><label>56</label><mixed-citation> Wright, A., Bubb, W. A., Haekins, C. L., and Davis, M. J.: Singlet oxygen-mediated protein oxidation: Evidence for the
formation of reactive side chain peroxides on tyrosine residues, Photochem. Photobiol., 76, 35–46, 2002.
</mixed-citation></ref-html>
<ref-html id="bib1.bib57"><label>57</label><mixed-citation> Yasmeen, F., Vermeylen, R., Szmigielski, R., Iinuma, Y., Böge, O., Herrmann, H., Maenhaut, W., and Claeys, M.:
Terpenylic acid and related compounds: precursors for dimers in secondary organic aerosol from the ozonolysis of <i>α</i>- and
<i>β</i>-pinene, Atmos. Chem. Phys., 10, 9383–9392, <a href="https://doi.org/10.5194/acp-10-9383-2010" target="_blank">https://doi.org/10.5194/acp-10-9383-2010</a>, 2010.

</mixed-citation></ref-html>
<ref-html id="bib1.bib58"><label>58</label><mixed-citation> Zhang, X., McVay, R. C., Huang, D. D., Dalleska, N. K., Aumont, B., Flagan, R. C., and Seinfeld, J. H.: Formation and
evolution of molecular products in <i>α</i>-pinene secondary organic aerosol, P. Natl. Acad. Sci. USA, 112, 14168–14173,
2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib59"><label>59</label><mixed-citation> Zhang, X., Lambe, A. T., Upshur, M. A., Brooks, W. A., Be, A. G., Thomson, R. J., and Geiger, F. M.: Hihgly oxygenated
multifunctional compounds in <i>α</i>-pinene secondary organic aerosol, Environ. Sci. Technol., 51, 5932–5940, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib60"><label>60</label><mixed-citation> Zhao, R., Lee, A. K. Y., Soong, R., Simpson, A. J., and Abbatt, J. P. D.: Formation of aqueous-phase
<i>α</i>-hydroxyhydroperoxides (<i>α</i>-HHP): potential atmospheric impacts, Atmos. Chem. Phys., 13, 5857–5872,
<a href="https://doi.org/10.5194/acp-13-5857-2013" target="_blank">https://doi.org/10.5194/acp-13-5857-2013</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib61"><label>61</label><mixed-citation> Zhao, Y., Wingen, L. M., Perraud, V., Greaves, J., and Finlayson-Pitts, B. J.: Role of the reaction of stabilized Criegee
intermediates with peroxy radicals in particle formation and growth in air, Phys. Chem. Chem. Phys., 17, 12500–12514, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib62"><label>62</label><mixed-citation> Ziemann, P. J.: Formation of alkoxyhydroperoxy aldehydes and cyclic peroxyhemiacetals from reactions of cyclic alkenes
with O<sub>3</sub> in the presence of alcohols, J. Phys. Chem. A, 107, 2048–2060, 2003.
</mixed-citation></ref-html>--></article>
