Articles | Volume 26, issue 15
https://doi.org/10.5194/acp-26-11153-2026
https://doi.org/10.5194/acp-26-11153-2026
Research article
 | 
10 Aug 2026
Research article |  | 10 Aug 2026

Exploring the hydrogen abstraction pathway in HOM formation from α-pinene photooxidation systems under varying NO conditions

Hui Wang, Hongru Shen, Defeng Zhao, Sungah Kang, Rongrong Wu, Yarê Baker, Quanfu He, Annika Zanders, Mathias Bachner, Douglas R. Worsnop, Thorsten Hohaus, Thomas F. Mentel, and Sören R. Zorn
Abstract

Highly oxygenated organic molecules (HOM) are formed via autoxidation during OH-initiated oxidation of α-pinene. We investigated the relative contributions of OH-addition and hydrogen (H)-abstraction to HOM formation from α-pinene photooxidation under varying nitrogen oxide (NO) conditions. HOM molecules were detected by a nitrate chemical ionization mass spectrometer (CIMS). In the absence of NO, C10H17Ox peroxy radicals and related termination products (e.g. C10H18Ox) dominated the HOM spectrum, accounting for > 70 % of total HOM. The presence of NO substantially altered HOM products, particularly by rapid formation of C10H15Ox-related HOM, like C10H15NO8. The ratio of C10H15NOx to C10H17NOx increased from 0.34 to 0.84 as the RO2 loss rate via reaction with NO increased from 0.18 to 1.06 s−1. Under high-NO conditions, C10H15Ox-related HOM contributed up to 34 % to total HOM from α-pinene oxidation systems. The H-abstraction channel proved to be the source of C10H15Ox-related HOM. Fuzzy c-means clustering indicated that C10H15Ox-related HOM exhibited the fastest formation rate among the identified HOM groups, consistent with first-generation products. Comparison with pinonaldehyde oxidation, obtained by normalizing HOM yields to pinonaldehyde turnover, suggests that pinonaldehyde contributed  5 % of HOM in α-pinene systems, excluding secondary oxidation as the dominant source. Detection of C10H15NO4 under high-NO conditions by propylamine-CIMS indicates the formation of C10H15O3 peroxy radicals, formed by alkoxy radical decomposition and six-membered ring opening in the H-abstraction channel. This study highlights the role of the H-abstraction pathway in OH-initiated α-pinene oxidation under NO-influenced conditions and provides new constraints on detailed HOM formation mechanisms.

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1 Introduction

Secondary organic aerosols (SOA) in the atmosphere contribute significantly to particulate matter in the PM1 size range and can affect regional air quality, human health and global radiative forcing (Jimenez et al., 2009; Peng et al., 2016). The oxidation of biogenic volatile compounds (BVOC) contributes significantly to the total formed SOA. Highly oxygenated organic compounds (HOM) are produced via autoxidation of peroxy radicals (RO2). They typically contain at least six oxygen atoms and consequently show a low to extremely low volatility. This enables them to nucleate or to condense onto existing particles and thus to significantly contribute to SOA formation (Bianchi et al., 2019; Mentel et al., 2015; Ehn et al., 2014).

α-pinene is globally the most abundant monoterpene and has been shown to form significant amounts of HOM when it is oxidized by O3 or by hydroxyl radicals (OH) (Ehn et al., 2014; Berndt et al., 2016). OH initiated oxidation of α-pinene occurs via the OH-addition pathway ( 90 %) and the hydrogen (H)-abstraction pathway ( 10 %), leading to the formation of peroxy radicals (RO2) with the formulas C10H17O3 and C10H15O2, respectively (Vereecken et al., 2007).

The OH-addition pathway is known to effectively form HOM with fast rates when the four-membered ring is broken (Berndt, 2021; Xu et al., 2019). However, the potential role of the H-abstraction pathway for HOM formation has received far less attention and was thought to be negligible until Shen and coworkers suggested its significant contribution to HOM (Shen et al., 2022). In addition, Luo et al. (2023) also highlighted the significance of H-abstraction to HOM formation from limonene photooxidation in the presence of NO. Therefore, the H-abstraction pathway can be a potential explanation for the observations in Hyytiälä where C10H15Ox-related HOM species (e.g. C10H15NO8) are dominant and have been identified as fingerprints of daytime oxidation (Yan et al., 2016). However, confirmation and clarification of the contribution of the H-abstraction pathway to HOM formation are still required. In the study by Shen et al. (2022) the potential role of the conversion of pinonaldehyde to C10H15Ox species was only estimated and not directly measured. The extent to which pinonaldehyde oxidation contributes to C10H15Ox-related HOM in α-pinene systems remains uncertain.

The detection of C10H15Ox related products with fewer than five oxygen atoms suggests contributions from H-abstraction pathways. However, Shen et al. (2022) reported only HOM with oxygen numbers greater than six, and NO was present in all experiments performed (Shen et al., 2022). The presence or absence of NO can have a significant impact, as it strongly influences the rearrangement of alkoxy radicals, which is crucial to facilitate HOM formation via the H-abstraction pathway (Shen et al., 2022). Therefore, systematic experiments under varying NO conditions, especially including NO-free conditions, are essential for confirming the occurrence of the H-abstraction pathway, to elucidate its product distribution, and to clarify its role in HOM and subsequent SOA formation in α-pinene photooxidation systems.

Competition between termination pathways of C10H17Ox and C10H15Ox peroxy radicals determines the product distributions (Mentel et al., 2015). All products are separated into various families based on the numbers of carbon atoms, hydrogen atoms and oxygen atoms. The C10H18Ox family, which includes compounds containing ten carbon atoms, eighteen hydrogen atoms, and a varying number of oxygen atoms with hydroperoxide or alcohol functions, can only be attributed to C10H17Ox via termination either by HO2 radicals (Reaction R1) or by other peroxy radicals (RO2) via Reaction (R3) (Baker et al., 2024). Similarly, the organic nitrate C10H17NOx family is formed via the reaction of C10H17Ox with NO (Reaction R6) (Berndt, 2021). The C10H14Ox family, comprising carbonyl containing compounds, is generated either via reactions of C10H15Ox with RO2 or via self-termination (Reaction R8) (Rissanen et al., 2014). In the atmosphere, alkoxy radicals with the formula C10H15Ox−1 are mainly products of the reaction between C10H15Ox and NO (Reaction R2) (Berndt, 2021). The C10H15NOx family is uniquely attributed to the reaction of C10H15Ox peroxy radicals with NO (Reaction R6). Thus, the appearance of HOM with formulas C10H18Ox and C10H17NOx can clearly be traced to C10H17Ox, while C10H14Ox and C10H15NOx are clearly related to C10H15Ox. The formation of the C10H16Ox family can occur via multiple pathways including termination reactions of C10H15Ox with HO2 or RO2, termination of C10H17Ox with RO2, or self-termination of C10H17Ox. The important initiation of reactions is shown in Fig. S1 in the Supplement, and termination pathways of RO2 and corresponding products are shown below in Fig. 1.

(R1)RO2+HO2ROOH +O2(R2)RO2+HO2RO+OH+O2(R3)RO2+RO2R=O+ROH+O2(R4)RO2+RO2RO+RO+O2(R5)RO2+RO2ROOR+O2(R6)RO2+NORONO2(R7)RO2+NORO+NO2(R8)RO2R=O+OH
https://acp.copernicus.org/articles/26/11153/2026/acp-26-11153-2026-f01

Figure 1A schematic diagram illustrating OH initiated α-pinene photooxidation through either the OH-addition pathway or the H-abstraction pathway. The unique peroxy radicals and their subsequent termination reactions are also depicted. The potential closure products are categorized into different families based on their formation pathways and the number of hydrogen atoms in molecules.

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In our study we conducted systematic experiments of α-pinene photooxidation under varying NO concentrations to investigate the role of the H-abstraction pathway in HOM formation. We focused on early reaction stages, which means the first minutes after OH generation by photolysis of H2O2, to capture primary generation product distributions, during which only autoxidation and reaction with NO were the two dominant reaction pathways for RO2. Fuzzy c-means clustering was applied to distinguish C10H15Ox-related HOM from other products based on their formation pathways. To elucidate the role of secondary oxidation, pinonaldehyde was investigated under identical conditions, and the results were compared with the α-pinene system. Both less oxygenated and highly oxygenated products were detected by employing propylamine and nitrate reagents in chemical ionization mass spectrometry (CIMS).

Combination of the results provides complementary and consistent insights into product distributions and formation pathways, highlighting the importance of the H-abstraction pathway to produce HOM and subsequently contribute to SOA formation. The results demonstrate that the H-abstraction pathway is an important process generating product distributions highlighting its potential contribution to HOM and SOA formation.

2 Experiments and Methods

2.1 Simulation experiments in SAPHIR STAR

The experiments were conducted in SAPHIR-STAR, a 2 m3 continuously stirred tank reactor (SAPHIR: Simulation of Atmospheric PHotochemistry In a large Reaction chamber; STAR: – STirred Atmospheric flow Reactor). The details about its basic concept of operation have been described previously (Mentel et al., 2009; Baker et al., 2024). For this study the system was operated with a total flow rate of 60 L min−1, of which 32 L min−1 were injected into the reactor, resulting in a residence time of approximately 60 min. Experimental conditions were maintained at 20 °C and at 20 % relative humidity. OH radicals were produced by photolyzing hydrogen peroxide (H2O2) using two 254 nm UV-C lamps (TUV 16W 4P SE, Philips). The photolysis rate was controlled by reducing the photon flux by covering part of the lamps with adjustable bellows. H2O2 vapor was introduced into SAPHIR-STAR by bubbling a 0.2 L min−1 nitrogen (N2) flow through a 30 % w/w H2O2 solution (Sigma-Aldrich).

In the α-pinene photooxidation experiments a continuous flow of 0.012 L min−1 from an α-pinene cylinder (with a concentration of  48.8 ppm) was injected into SAPHIR-STAR resulting in an initial concentration of  10 ppbv. For pinonaldehyde photooxidation, liquid pinonaldehyde (Orgentis chemicals, 99.7 %) was introduced by use of a syringe pump (Fusion 4000, Chemyx Inc.) at a flow rate of 0.145 µL h−1 resulting in a concentration of 5 ppbv of pinonaldehyde in the reactor. NO was injected into the chamber from a gas cylinder (20.09 ppm NO in N2 5.0) via a mass flow controller for initial concentrations before reaction ranging between 0 and 7.5 ppbv.

To investigate the role of the H-abstraction pathway in α-pinene photooxidation we focused on the early stages of the reaction systems before secondary-generation products become important. All precursors were injected into the dark chamber. Once all precursors were well mixed and showed stable concentrations, the UV-C lamps were switched on for OH production by photolysis. The UV-C lamps were then kept on at a constant setting for one hour to initialize the photooxidation of α-pinene, followed by three hours without irradiation to allow for products to be flushed out and for precursors to recover initial concentrations. This cycle was repeated three times for every system investigated.

Since the first hour of photooxidation is crucial for investigating the relative role of the H-abstraction channel compared to the OH-addition channel, a cycle of one hour of photolysis followed by three hours without irradiation was repeated three times for each experimental condition listed in Table 1, as mentioned before. The time series of α-pinene, H2O2, and C10H17O7 peroxy radicals over a total run of the experiments (14 h) are shown in Fig. S2, together with an example of the experimental procedure. During the final cycle the lamps were kept on continuously for 6 h to allow the system to reach steady state.

2.2 Methods and instrumentation

2.2.1 Instrumentation

The α-pinene concentration was measured by a proton-transfer-reaction mass spectrometry (PTR-TOF-MS, Ionicon Analytik GmbH). Gas concentrations of NO and NOx were detected by a NO monitor (nCLD899, Eco Physics GmbH) coupled to a self-built photolytic NO2 converter, with a detection limit of 0.05 ppb for NO measurement. O3 was measured by O3 monitor (O342e, Envea GmbH), with a detection limit of 0.2 ppb. H2O was monitored by a Picarro CRDS analyzer (G2401, Picarro Inc.).

An Eisele type inlet (Eisele and Tanner, 1993) was coupled to an atmospheric-pressure-interference time-of-flight mass spectrometer (Api-TOF-MS, Tofwerk AG) using a positive reagent ion (C3H7NH3+) produced from propylamine (C3H7NH2,  99 %, Sigma Aldrich) to ionize less oxygenated organic products in gas phase (Berndt et al., 2018). The resolution of this instrument was  3500 m/Δ m FWHM for m/z larger than 150. C3H7NH3+ has the advantage that it does cluster with pinonaldehyde very efficiently, which is vital for investigating α-pinene related systems since pinonaldehyde is a major oxidation product and a representative for the OH-addition pathway. The sensitivity of pinonaldehyde (Fig. S3) was calibrated in propylamine CIMS (amine-CIMS) by using a Liquid Calibration Unit (LCU, Ionicon Analytik GmbH). The long TOF-MS (LTOF, Tofwerk AG), with a resolution  8500 m/Δ m FWHM for masses larger than 200 Th, was coupled with a multi-scheme ionization inlet (MION, Karsa Oy) (Rissanen et al., 2019). The MION inlet allows switching between bromide and nitrate modes, utilizing Br and NO3- as reagent ions, respectively. The Br was mainly used to detect HO2 radicals and their relative change (Albrecht et al., 2019). NO3- CIMS has been shown to efficiently detect HOM (Ehn et al., 2014). Wang et al. have also shown that HOM(NO3-) clusters with four or more oxygen atoms in the HOM have a higher bonding strength than the H2SO4(NO3-) cluster (Wang et al., 2024), possibly due to the multiple hydroperoxyl and hydroxy functional groups present in HOM molecules (Bianchi et al., 2019). This indicates a relative sensitivity at the collision limit for these highly functionalized HOM. Since the study by Wang and coworkers (Wang et al., 2024) used the same setup regarding instrument and inlet we assumed that the MION-CIMS used in this study detects HOM compound with same sensitivity. All CIMS data were processed using the IGOR Pro (WaveMetrics) based Tofware v3.3.0.

2.2.2OH concentration, VOC turnover, and HO2 concentration during steady stages

The concentration of OH radicals was calculated based on the reacted fraction of α-pinene or pinonaldehyde under steady-state conditions (Eq. 1) (Kiendler-Scharr et al., 2009). When the system is in steady-state, all parameters are stable and injection rates equal loss rates. In Eq. (1), F represents the total flow through the chamber, and V is the volume of chamber. [VOC]0 and [VOC]SS represent the VOC concentration in the dark and in steady state (SS), respectively. kOH denotes the rate constants for the reaction of α-pinene or pinonaldehyde with OH radicals, which are 5.4×10-11 cm3 s−1 and 4.0×10-11 cm3 s−1 at 20 °C, respectively (Atkinson and Arey, 2003; Rolletter et al., 2020). The estimated OH concentrations are listed in Table 1. The turnover of VOC by OH can be calculated using Eq. (2), which represents the amount of VOC consumed by the reaction with OH (Baker et al., 2024).

(1)OHSS=FV×VOC0-VOCssVOCsskOH(2)turnovervoc=kOH×VOCSS×[OH]SS

To determine the concentrations of HO2 in the chamber, a series of isoprene photooxidation experiments was conducted, and a corresponding box model based on the MCM v3.3.1 chemistry, which used the same boundary conditions, was applied. More details about the box model can be found in Baker et al. (2024).

In these experiments, a continuous flow of 0.050 L min−1 of isoprene from a gas cylinder (11.8 ± 0.24 ppmv, Linde GmbH) was introduced into the chamber to achieve a target concentration of 10 ppbv before reactions. The UV-C lamps were then adjusted in five different steps by varying the lamp bellows to vary [OH]SS. The box model reproduced both [isoprene]SS and [OH]SS for each step within the measurement uncertainties (Fig. S4). A linear fit was applied to normalized HO2/ [Br-+(H2O)Br] (in normalized counts per second, ncps) and modelled [HO2]SS (Fig. S5), and the slope was used as calibration factor for calculating HO2 levels in subsequent experiments (Table 1).

2.2.3 Fuzzy c-means clustering (FCM)

Hierarchical clustering has been shown to be an effective dimensionality-reduction technique to identify major ion groups and patterns of chemical behaviour in mass spectrometry previously (Koss et al., 2020). Wu et al. demonstrated the application of the soft clustering method FCM for simplifying complex mass spectrometric data to reveal chemical and kinetic characteristics of chemical reaction systems (Wu et al., 2024). Here, FCM was applied to mass spectrometric data to explore the formation rates of a variety of products along competing reaction channels. The time series of 156 ions in the early reaction stage (up to 3000 s after start of the photooxidation processes) were selected for clustering. Herein, the major ions from both nitrate-CIMS and amine-CIMS were combined. Normalization was applied to all ions used since their typical time behaviour was more important for clustering than their absolute abundance. Initially, all ion signals were normalized relative to their corresponding reagent ions. Subsequently, Frobenius normalization was applied to each ion across the entire time range.

Three parameters were calculated to help to constrain the optimal number of clusters: sum of squared errors (SSE), distortions, and silhouette coefficient (Wu et al., 2024; Campello and Hruschka, 2006). The FCM algorithm was run 50 times for each cluster number in a range between 2 to 13. The results of the three parameters as function of cluster numbers are shown in Fig. S6. The four-cluster solution was then selected for the subsequent analysis.

2.2.4 Model simulations to determine early reaction stages

To clarify the role of the H-abstraction channel under various NO conditions, the early reaction stages are particularly relevant. In this study, we define early reaction stages using three criteria: (i) α-pinene turnover exceeds that of pinonaldehyde by a factor of ten, (ii) under conditions with NO, biomolecular reactions of RO2 are dominated by RO2 + NO and contribute more than 90 % to the biomolecular loss of RO2, and (iii) α-pinene oxidation is primarily driven by OH rather than O3. Therefore, model simulations for α-pinene photooxidation systems were conducted to quantitively identify early reaction stages.

As shown in Fig. 2a-1 to c-1, the model captures the evolution of the system quite well but generally underestimates NO and O3 concentrations. These discrepancies may arise from differences in the temporal resolution of measurements and simulations, physical effects introduced by the activation of the UV-C lamps (e.g., changing emissions due to temperature adjustment of the UV-C lamp), and uncertainties in the chemical mechanism including reactions currently not represented in the model framework. The HO2 and RO2 concentrations obtained from the simulations are shown in Fig. 2a-2 to c-2 together with the relative contributions of RO2 + NO, RO2 + HO2 and RO2 + NO to the total biomolecular RO2 loss. Here, the reaction rates were calculated with k[RO2][HO2] = 1.85 × 10−11 cm3 s−1, k[RO2][NO]=1× 10−11 cm3 s−1 and k[RO2][RO2]=5× 10−12 cm3 s−1 (Baker et al., 2024; Berndt et al., 2016; Jenkin et al., 1997).

Based on these results, reactions occurring within the first 100, 100, and 320 s after initiation of reactions by starting the photooxidation were defined as early stages for the NO-free, low-NO, and high-NO conditions, respectively. The average bimolecular reaction rates for RO2 + NO were negligible for cases without NO and increased to 0.179 and 1.06 s−1 for the low-NO and high-NO conditions, respectively. For RO2 + HO2 reactions, the rates were 0.0055, 0.011, and 0.0075 s−1, while those for RO2 + RO2 reactions were 0.0075, 0.0029, and 0.0014 s−1 for NO-free, low-NO, and high-NO conditions, respectively. The contribution of RO2 + NO was higher than 90 % under both low-NO and high-NO conditions.

For pinonaldehyde photooxidation under high-NO conditions, the reactions within the early reaction stages were also investigated to facilitate comparison with the corresponding α-pinene system under high NO conditions. Besides H-abstraction channel, reactions of α-pinene with O3, and pinonaldehyde with OH may also contribute to the formation of C10H15Ox radicals. Therefore, the loss of α-pinene due to oxidation by O3 formed as a byproduct of other reactions, and the loss of pinonaldehyde via OH oxidation, were evaluated. The results are shown in detail in Fig. S7. In both cases, losses are smaller than 1 % of the reaction rate of α-pinene with OH, which further supports our definition of early reaction stage being reasonable and representative.

https://acp.copernicus.org/articles/26/11153/2026/acp-26-11153-2026-f02

Figure 2Results of model simulations for α-pinene photooxidation under NO-free (a-1, a-2), low-NO (b-1, b-2), and high-NO conditions (c-1, c-2). The upper panels show modelled and measured concentrations of α-pinene, NO, and O3 across the three conditions, while the lower panels show the corresponding radical concentrations of RO2 and HO2. In addition, the lower panels illustrate the relative contributions of RO2 + HO2, RO2 + RO2 and RO2 + NO reactions to the total bimolecular reaction rate of RO2 (shown as RO2 fate on the right y-axis).

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3 Results and Discussion

3.1 C10H15Ox-related HOM form rapidly from α-pinene photooxidation in the presence of NO

All major products from α-pinene photooxidation that were detected by NO3- CIMS, in the absence or presence of NO, were categorized into the following groups: C10 monomers, C20 dimers, and C<10 fragments. The time series for contributions of each group varies for the three different NO conditions, as shown in Fig. 3a-1, a-2, a-3. A comparison under varying NO conditions is critical to elucidate the role of NO, since the presence of NO, ring opening and isomerization of alkoxy radicals, can be crucial in facilitating HOM formation from H-abstraction channel (Shen et al., 2022). The analysis was focused on the early reaction stages to explore the importance of the H-abstraction channel for HOM formation. The average product distributions of C10 monomers from early stage α-pinene photooxidation without and with NO are illustrated by Kendrik Mass Defect (KMD) plots as a function of oxygen number (Kendrick Mass = oxygen, Fig. 3b-1, b-2, b-3). Each plot features seven distinct families, with compounds in each family sharing the same carbon and hydrogen numbers but differing in oxygen content.

Table 1Overview of experimental conditions: pinonaldehyde photooxidation without NO (NO-free) and with high NO (high-NO), α-pinene photooxidation without NO (NO-free), with low NO (low-NO), and with high NO (high-NO). The precursor concentrations in the dark and in photooxidation steady-state conditions are shown at t0 and tS, respectively. The measurement uncertainty is less than 5 %. Details about how to estimate OH and HO2 radicals are given in Sect. 2.2.

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Under α-pinene NO-free conditions the relative contributions of C10H18Ox, C10H16Ox, and C20H34Ox are 56.1 %, 11.1 %, and 8.8 %, respectively, and they are all closed-shell products related to C10H17Ox. The first generation peroxy radicals with four-membered ring-opening, C10H17O3, can undergo fast unimolecular reactions with rates of 4 ± 2 s−1 (Xu et al., 2019). As shown in Fig. 3b-1, species with the formula C10H17O7 are identified as predominantly HOM peroxy radicals and are detected in the nitrate mass spectra as C10H17O7(NO3-). This agrees with previous observations by Berndt (2021), which were obtained using four different reagent ions, and calculations by Piletic and Kleindienst (2022). Additional HO2 radicals were produced in our experiments via the reaction of the OH radical with H2O2. The increasing contribution of C10H18Ox (Fig. 3(1-a)) indicates a significant termination reaction of RO2 by HO2. Among the C10H18Ox family, C10H18O7 shows the highest intensity and is likely produced via termination reactions of C10H17O7 with HO2, which aligns with the dominance of C10H17O7 in the C10H17Ox family. Compounds with six oxygen atoms but one hydrogen less or one more hydrogen than C10H17O7 (i.e., C10H16O6 and C10H18O6) are significant contributors to the total product signal of the C10H17Ox family. Compounds with the formula C10H16O6 likely have carbonyl functionalities and are formed either directly from Reaction (R3) or from self-termination reactions of C10H17O7 (Reaction R8) (Iyer et al., 2018; Jenkin et al., 2019). In contrast, C10H18O6 species are possibly alcohols formed from C10H17O7 via Reaction (R3), or more likely hydroperoxides derived from C10H17O6 via Reaction (R1) (Iyer et al., 2018; Jenkin et al., 2019).

In addition to C10 HOM monomers, C20 accretion products also significantly contribute to HOM, particularly species containing 8, 10, or 12 oxygen atoms (Fig. S8). These have been identified as the most abundant dimers from OH initiated α-pinene photooxidation system by Berndt et al. (2016). C20H34O(8,10,12) can be mechanistically explained by recombination of C10H17O7 with C10H17O3, C10H17O5, or another C10H17O7 via Reaction (4). C10H17O(3,5,7) have previously been reported to dominate the product spectrum (Lee et al., 2023; Berndt, 2021). In summary, the obtained HOM distributions in the base case without NO addition are consistent with previous studies and show mechanistically reasonable results.

When reactions are initiated in the presence of NO, the product distribution in the early reaction stage (when the RO2 + NO regime is dominant) differs significantly from the NO-free case. The C10H17NOx product family, identified as organic nitrates, accounts for 29.9 % and 29.4 % of the total signal under low-NO and high-NO conditions, respectively, and dominates C10H17Ox-related HOM families. The most abundant species with formulas C10H17NO(6,7,8) most likely represent organic nitrates formed via reactions of C10H17O(5,6,7) with NO. As the initial NO concentration increases, contribution from C10H17O6-derived HOM, such as C10H17NO7 and C10H18O6, also rises (Figure S9). When the initial NO increased from 0.91 ± 0.05 to 7.4 ± 0.05 ppbv, the ratios of C10H17NO7 to C10H17NO8 and C10H18O6 to C10H18O7 are enhanced from 0.32 to 0.43 and from 0.63 to 0.78, respectively. At least one alkoxy step (Reaction R7) is necessary to produce peroxy radicals with even number, e.g. C10H17O6. Therefore, the presence NO promotes the occurrence of alkoxy steps in HOM formation. Compared to the NO-free condition, the contributions of accretion products with C20H34O(9,11) are also promoted. For forming C20H34O(9,11) via Reaction (R5) an C10H17Ox peroxy radical with an even oxygen number must be involved, e.g. C10H17O4 and C10H17O6, further highlighting the role of alkoxy steps in HOM formation.

The C10H17O7 peroxy radicals exhibit a rapid formation rate and a high molar yield in α-pinene photooxidation systems, but their formation shows only a weak dependence on the NO concentration. Although OH addition to α-pinene yields three structural first-generation isomers (C10H17O3), only the isomer that undergoes an opening of the four-membered ring is capable of subsequent autoxidation (Lee et al., 2023; Piletic and Kleindienst, 2022; Berndt et al., 2016). The ring-opened C10H17O3 can then undergo two rapid unimolecular autoxidation steps, with a rate constant of approximately 4 s−1 for the first step which will lead to the formation of C10H17O5, and a rate constant around 10 s−1 for the subsequent step and formation of C10H17O7 species (Piletic and Kleindienst, 2022; Xu et al., 2019). The fast autoxidation steps of the resulting peroxy radicals imply that the characteristic timescales of their formation are significantly shorter than those of competing bimolecular reactions with NO, RO2, and HO2, whose maximum effective rates in our experiments range from 0.02 to 1.88 s−1 under NO-free, low-NO, and high-NO conditions, respectively. Therefore, biomolecular reactions, particularly involving NO, cannot effectively compete with the rapid autoxidation reactions, which can explain the observed weak NO dependence of the formation of C10H17O7-related HOM.

In addition to the change of C10H17Ox-related HOM, C10H15Ox-related HOM families emerge once NO is introduced into the system (Fig. 3a-2, a-3, b-2, b-3). Under the NO-free condition, neither the C10H15NOx nor the C10H14Ox family contributes more than 2 %. However, under low-NO conditions their contribution rises to 10.3 % and 4.7 %, respectively, and further increases to 24.9 % and 6.0 % under high-NO conditions. The most abundant peroxy radical in C10H15Ox family is C10H15O7, as shown in Fig. S9, followed by C10H15O9, which is consistent with the closed shell organic nitrate distribution, where C10H15NO8 is most prevalent, followed by C10H15NO10. The C10H14Ox family contains products with carbonyl groups and is formed via self-termination reactions of peroxy radicals. In addition to C10 monomers, accretion products with the formula C20H30Ox and C20H32Ox, derived from Reaction (R5), also increase with elevated NO concentrations. Here at least one peroxy radical containing 15 hydrogen atoms must be involved (Berndt et al., 2018). Compared to monomers, formation of accretion products is reduced since in early stages of the reactions the RO2 + RO2 pathway is less important compared to the NO + RO2 pathway or the RO2 autoxidation. The intensity of C10H16O7 increases gradually until it surpasses that of C10H16O6, which in the absence of NO is the most abundant peak. C10H16O7 is likely a carbonyl compound (or family), formed either through Reaction (R3), or from self-termination. Both need C10H17O8 as precursors. However, analysis of the closed-shell families C10H18Ox and C10H17NOx indicates the absence of significant formation of C10H17O8 in presence of NO, which also aligns with Berndt (2021) and Piletic and Kleindienst (2022). C10H16O7 may also be a hydroperoxide produced via Reaction (R2), or an alcohol produced via Reaction (R3), with C10H15O7 peroxy radicals or C10H15O8 peroxy radicals serving as precursors. Products formed via RO2 + RO2 reactions were produced at significantly slower rates than other species, as will be discussed in Sect. 3.2. Additionally, when C10H15O7 reacts with another RO2 radical, it forms C10H16O6 or C10H14O6 rather than C10H16O7. Thus, Reaction (R3) was considered to not contribute significantly, and the reaction of C10H15O7 with HO2 most likely accounts for the significant increase of C10H16O7. Similarly, species in the C10H16Ox family that have more than seven oxygen atoms can be attributed to reactions of C10H15Ox peroxy radicals with HO2.

Contributions from peroxy radicals containing more than seven oxygen atoms to the C10H17Ox family are negligible, which is consistent with the number of oxygen atoms in the observed closed-shell products. This phenomenon is in accordance with previous measurement studies and calculations (Berndt, 2021; Lee et al., 2023). In the NO-free condition, compounds with more than seven oxygen atoms account for only 0.1 % of the C10H18Ox family, whereas for the low-NO and high-NO cases, compounds with more than eight oxygen atoms contribute 5 % and 6 %, respectively, to the C10H17NOx family. Although the fate of the C10H17O7 family remains unclear, the product distributions indicate that it is unlikely for them to undergo further steps of autoxidation. However, the C10H15Ox-related HOM are more oxidized than C10H17Ox-related HOM. For example, species containing more than eight oxygen atoms in C10H15NOx account for 43.6 % and 46.7 % in low-NO and high-NO cases, respectively, of the entire C10H15NOx family. Obviously C10H15Ox isomers with x≥7 are formed, which exhibit faster unimolecular reaction rates than the accessible isomers of the C10H17Ox peroxy radicals.

The distribution of the less oxygenated compounds was investigated based on the mass spectra detected by amine-CIMS, which are shown in Fig. S10. Consistent with nitrate-CIMS, C10H15Ox-related less oxygenated compounds also emerge with elevated NO concentrations, particularly those in the C10H14Ox and C10H15NOx families. The dominant compounds in the C10H15NOx family are C10H15NO4, C10H15NO6, and C10H15NO8, which should be derived from Reaction (R6) involving peroxy radicals with the formula C10H15O3, C10H15O5, and C10H15O7, respectively. Among the major compounds in the C10H15NOx family detected by amine-CIMS only highly oxidized species with the formular C10H15NO8 can also be detected in significant amounts by nitrate-CIMS. The same phenomenon can also be seen for C10H17Ox-related compounds. In amine-CIMS, the first-generation peroxy radical, C10H17O3, and its associated closed-shell products play a dominant role in the combined C10H17Ox, C10H18Ox, and C10H17NOx families, although the C10H17O7 related products are dominant in the mass spectrum obtained by nitrate-CIMS. For example, C10H17NO4 and C10H18O3 are major peaks, which are produced mechanistically through termination reactions of C10H17O3 by NO and by HO2 radicals, respectively. C10H17NO4 contributes 56.6 % and 57.5 % to the C10H17NOx family in low-NOand high-NO conditions, respectively. C10H18O3accounts for 70.6 %, 77.6 %, and 69.3 % in NO-free, low-NO, and high-NO cases, respectively.

Only ring-opened C10H17O3 can undergo fast autoxidation reactions to produce HOM, and they account only for approximately 25 % of the sum of C10H17O3 peroxy radicals derived from the OH addition pathway (Xu et al., 2019, Vereecken et al., 2007). However, the nitrate-CIMS technique ionizes specifically highly oxygenated organics (Ehn et al., 2014), resulting in the detection of only a narrow range of highly oxidized compounds derived from four-membered ring-opened C10H17O3. The amine-CIMS is efficient in detecting a large range of products including less oxygenated compounds (O < 7) (Berndt, 2021). C10H16O2(C3H7NH3+) is found to be the strongest peak among the entire mass spectrum in amine-CIMS, indicating the production of pinonaldehyde. Pinonaldehyde can be formed from the formation of alkoxy radicals via reactions of four-membered ring-retained C10H17O3 peroxy radicals and NO, which then undergo a fast opening of the six-membered ring, shown in Fig. S1 (Rolletter et al., 2019). The inclusion of amine-CIMS extends the detection of products, especially less oxygenated ones, which could indicate the fate of four-membered ring-retained C10H17O3 peroxy radicals.

Alkoxy radicals derived from reactions involving C10H17Ox peroxy radicals and NO can undergo an H-shift, β-scissions, or a HO2 loss step; however, none of these reactions are expected to form C10H15Ox peroxy radicals directly. For example, neither H-migration nor β-scission will lead to the loss of a hydrogen atom without a carbon-carbon bond cleavage, and the resulting alkyl radicals will react efficiently with O2 to regenerate C10H17Ox radicals and thus continue the autooxidation cycle. The HO2 loss channel is expected to be a minor pathway for the considered alkoxy radicals, because intramolecular H-migration and β-scission are more favorable, as previously shown by Vereecken and Peeters (2009, 2010). If the HO2 loss channel would happen, it would lead to the formation of carbonyl and HO2, losing one hydrogen atom forming C10H16Ox products. While the C10H16Ox products could, in principle, react with OH radical again to produce C10H15Ox intermediates, this process would occur on the timescale of secondary chemistry and is therefore unlikely to contribute significantly during the early reaction stages. Pinonaldehyde was dominant among C10H16Ox compounds, but its oxidation cannot become a significant source of C10H15Ox-related HOM, which will be discussed in Sect. 3.2.

In conclusion, the product distributions from α-pinene photooxidation during early reaction stages were investigated. Compared to NO-free conditions, the presence of NO enhanced the formation of organic nitrates and promoted alkoxy formation steps, which lead to significant formation of C10H15Ox-related compounds. These were detected by both nitrate-CIMS and amine-CIMS. The initial peroxy radicals leading to C10H15Ox related products were identified as C10H15O3, which cannot arise from ozonolysis of α-pinene since α-pinene was dominantly oxidized by OH radicals rather than O3, as shown in Fig. S7. Also, C10H15O4 peroxy radicals are mechanistically expected to be first generation peroxy radicals in ozonolysis. Potential mechanisms that could be responsible for the emergence of C10H15Ox-related HOM will be discussed in the following section.

https://acp.copernicus.org/articles/26/11153/2026/acp-26-11153-2026-f03

Figure 3Panels (a-1), (a-2), (a-3) show stacked figures with the contributions of each product family from α-pinene photooxidation as a function of reaction time. The families representing major monomers (C = 10), fragments (C < 10), and accretion products (C = 20) are included in panels (a-1, a-2, a-3). Time series of concentrations for α-pinene, NO, and O3 are also presented. The corresponding panels (b-1), (b-2), (b-3) located below each stack plot show the Kendrik Mass Defect (KMD, based on oxygen weight) of monomer compounds as a function of oxygen number, with marker sizes indicating the relative abundance of each compound in the early reaction stages (0–100, 0–100, and 0–320 s after reaction starts for (b-1), (b-2), and (b-3), respectively. This is also indicated by the vertical white lines in (a-1), (a-2), and (a-3)). Compounds aligned along the same horizontal dashed lines are in same family, with the same carbon and hydrogen number but differing in oxygen number. Family names are shown on the right. The texts in panels (b-1), (b-2), (b-3) highlight major compounds with high abundance and their possible formation pathways. NO conditions increase in the panels from left to right, from NO-free and low-NO to high-NO, respectively. The products here are detected by nitrate-CIMS.

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3.2 C10H15Ox-related HOM attributed to H-abstraction pathway

In α-pinene oxidation systems three possible pathways can lead to monomers with 15 hydrogen atoms: either the H-abstraction channel by OH radicals (Shen et al., 2022) , ozonolysis (Berndt, 2022), or oxidation of pinonaldehyde (Rolletter et al., 2020). However, as mentioned in Sects. 2.2 and 3.1, ozone was not present at the beginning of each transient cycle and accounted for less than 1 % of α-pinene reaction loss. Thus ozonolysis cannot explain the significant formation of C10H15Ox-related products, in particular OH-initiation yields more HOM than ozonolysis (Berndt, 2022). To explore potential formation pathways of C10H15Ox-related compounds, FCM clustering was applied to the time series of 156 ions detected by nitrate-CIMS and amine-CIMS. Selection criteria for the ions were contributions of more than 0.1 % to the total ion signal in nitrate-CIMS or more than 1 % to the total ion signal in amine-CIMS.

A four-cluster solution was identified as the optimal solution. Corresponding results are presented in Fig. 4. Figure 4a shows the time series of the four cluster centers and the contributing ions. Compounds in cluster 1 form immediately after reactions are initiated by switching on the UV-C lamps, followed by cluster 2 and cluster 3, while compounds in cluster 4 show the longest formation time. The cluster centers peak at approximately 160, 210, 290, and 850 s, respectively. As shown in Fig. 4b, the major monomers in the C10H18Ox family and the major dimers (C20H30Ox, C20H32H12, C20H34O8) are all found in cluster 4, which exhibits the slowest formation rate among four clusters. These compounds originate from biomolecular termination reactions (Reactions R1 and R5), with their production rates largely controlled by the concentration of HO2 and RO2 radicals. NO is already in a steady state in the dark chamber, while HO2 and RO2 only begin to accumulate after the UV-C lamps are switched on. Therefore, the RO2 fate is immediately affected by NO. Consequently, under high-NO conditions, RO2 + NO reactions as well as autoxidation play a dominant role for the RO2 in early reactions, and only these two reactions are discussed in following sections.

Compounds in cluster 1 and cluster 2 initially increase dramatically before decreasing again, and cluster 1 exhibits a steeper decline than cluster 2. The bulk chemical properties and the average carbon oxidation state (OSc) of each cluster are calculated (Kroll et al., 2011; Wu et al., 2021) and plotted as a function of average carbon (nC) or nitrogen atoms (nN) (Fig. S11). The early-generation cluster 1 exhibits the highest OSc and nN but the lowest nC, indicating that it mainly consists of highly oxidized nitrogen-containing compounds and fragments (C < 10). This characteristic distinguishes cluster 1 from the other clusters. It is determined by the emerging of OH radicals at elevated NO concentration in the early stage.

The formation rate of each cluster can be interpreted kinetically as “typical” chemical formation rate (Wu et al., 2024). The compounds C10H15NO7(NO3-) and C10H15NO8(NO3-) are assigned to cluster 1 with the fastest formation rate; thus, they are likely first-generation products. Pinonaldehyde (C10H16O2(C3H7NH3+)), a possible precursor, can only be found in cluster 3, which has a much slower formation rate. This clearly shows that pinonaldehyde oxidation cannot explain the production of C10H15NO7(NO3-) or C10H15NO8(NO3-). C7H9NO8(NO3-), which is detected in high amount in nitrate-CIMS and also attributed to cluster 1, goes through a fragmentation step and is possibly formed via decomposition of C10H15Ox, followed by further autoxidation and termination reactions by NO (Shen et al., 2022). Therefore, H-abstraction is probably the reason for the significant formation of C10H15Ox-related HOM, and not the oxidation of pinonaldehyde. The fragment C7H11NO8(NO3-) is formed faster than the organic nitrate monomer C10H17NO8(NO3-), even though both are initialized by the OH-addition channel. This relation differs from that of C7H9NO8(NO3-) and C10H15NO8(NO3-).

As shown in Fig. S12, the summed abundance of C7 families (C7H(10,12)Ox, C7H(9,11)NOx) increases accordingly with the increase of the NO injection, accounting for 0.01 %, 0.3 % and 2.4 % of HOM compounds under NO-free, low-NO and high-NO conditions, respectively. It indicates increasing alkoxy radical decomposition with increasing NO. C7 fragments are formed via dissociation of C10 alkoxy radicals derived from bimolecular reactions of C10 peroxy radicals with NO. Thus, the presence of NO promotes C7 fragments by enhancing the production of alkoxy radicals (Vereecken and Peeters, 2000; Berndt, 2021). The most abundant families, C7H9NOx and C7H11NOx, likely originate from decomposition of C10H15Ox−1 and C10H17Ox−1, respectively. Under high-NO conditions, the ratio of C7H9NOx to C10H15NOx reaches 0.22, substantially higher than the ratio of C7H11NOx to C10H17NOx (0.05). This observation suggests that either alkoxy radical formation or subsequent decomposition is more efficient in the H-abstraction pathway than in the OH-addition pathway.

Evidence for alkoxy radical H-migration is provided by the enhanced formation of C10H17NO7 and C20H34O11 under high-NO conditions (Fig. S9). According to the oxygen-parity framework, C10H17Ox radicals formed solely through autoxidation are expected to contain an odd number of oxygen atoms, whereas an alkoxy H-migration step changes the oxygen parity from odd to even (Kang et al., 2025). Thus, the observed increase in C10H17NO7 and C20H34O11 suggests the formation of C10H17O6 peroxy radicals through at least one alkoxy radical isomerization step.

To initialize the HOM chain via OH-addition pathway, four-membered rings must open from chemically activated tertiary radicals, which is independent of NO (Xu et al., 2019). In contrast, HOM formation through the H-abstraction pathway requires NO. The initially formed peroxy radicals (C10H15O2) are unlikely to undergo autoxidation directly; therefore, their reaction with NO to form alkoxy radicals (C10H15O), followed by the ring-opening step producing C10H15O3 radicals, is necessary to initiate the HOM formation chain.

As autoxidation proceeds, higher oxygenated peroxy radicals, such as C10H17Ox and C10H15Ox, are formed from C10H17O3 and C10H15O4, respectively. These peroxy radicals can further react with NO, yielding either the corresponding alkoxy radicals (C10H17Ox−1 and C10H15Ox−1) or organic nitrates (C10H17NOx+1 and C10H15NOx+1). However, the branching ratio between these two channels remains poorly constrained, contributing substantial uncertainty to the role of NO in HOM formation. Once formed, the fate of alkoxy radicals strongly depends on alkoxy radical structure (Vereecken and Peeters, 2010, 2009). Regardless of whether the precursor RO2 radicals originate from the OH-addition or H-abstraction pathway, their subsequent chemistry can proceed through alkoxy radical intermediates. Therefore, the fate of these alkoxy radicals ultimately determines the impact of NO on HOM formation.

Overall, NO does influence HOM formation through alkoxy-radical chemistry. By promoting the conversion of RO2 radicals to RO radicals, NO initializes pathways for H-migration and decomposition that would otherwise be less important. The extent to which these processes enhance or suppress HOM formation depends strongly on the structures of both the peroxy and alkoxy radicals, introducing substantial uncertainty into the overall role of NO.

To assess the robustness of the clustering results, additional cluster analysis was performed using a three- and five-cluster solution, as shown in Figs. S13 and S14, respectively. Consistent conclusions are obtained regardless of the number of clusters specified. In particular, the key compounds derived from the H-abstraction channel, such as C10H15NO8(NO3-) and C7H9NO8(NO3-), were consistently assigned to the first cluster with the fastest formation rate. The stability of the clustering results was further evaluated by performing 50 clustering runs with random initializations and using the four-cluster solution. The distributions of the cluster assignments were then analysed, as shown in Fig. S15, with particular attention given to the key compounds discussed above, including C10H15NO8(NO3-), C7H9NO8(NO3-), and C10H16O2(C3H7NH3+). The results demonstrate the high stability of the cluster solution, as these compounds were consistently assigned to the same cluster across all runs. For example, C10H15NO8(NO3-) was assigned to the first cluster in all runs. Therefore, the clustering results and insights derived from them are highly robust and reliable.

https://acp.copernicus.org/articles/26/11153/2026/acp-26-11153-2026-f04

Figure 4Results of fuzzy c-means clustering for the dominant peaks (156 in total) during early reaction stages of α-pinene photooxidation under high NO condition are shown in panel (a). The four-cluster solution is shown here. The time series of the cluster centers are displayed as colored solid lines, while individual species are shown in gray lines. Panel (b) illustrates the cluster apportionment of selected major products detected in both nitrated-CIMS (N) and amine-CIMS (A).

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https://acp.copernicus.org/articles/26/11153/2026/acp-26-11153-2026-f05

Figure 5Panel (a-1) displays concentrations and turnover of α-pinene and pinonaldehyde (Pinal) during α-pinene photooxidation under high-NO conditions, while panel (a-2) represents concentrations and turnover of pinonaldehyde during pinonaldehyde photooxidation under high-NO conditions. Major product distributions are shown in panels (b-1) to (b-4). Signals detected in the pinonaldehyde experiment are normalized by the ratio of the pinonaldehyde turnover during the pinonaldehyde experiment to the respective turnover during the α-pinene experiment. The products are separated into four groups: (A)C10H14Ox, (A)C10H15NOx, (N)C10H14Ox, (N)C10H15NOx, of which (A) and (N) represent signals derived from amine-CIMS and nitrate-CIMS, respectively. Data from α-pinene oxidation and pinonaldehyde oxidation are colored in pink and blue, respectively.

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To assess the potential contribution of pinonaldehyde oxidation to the formation of C10H15Ox-related HOM, pinonaldehyde photooxidation experiments were conducted under NO-free and high-NO conditions, analogous to conditions applied in the α-pinene systems (Table 1). Time series of α-pinene and its oxidation product pinonaldehyde during the first 30 min of the α-pinene (high-NO) experiment are shown in Fig. 5a-1. The corresponding turnovers of α-pinene and pinonaldehyde are presented in Fig. 5a-1. Similarly, the concentration of pinonaldehyde and its turnover during the pinonaldehyde (high-NO) experiment are shown in Fig. 5a-2. OH concentrations were estimated using model simulations.

During the early stage, the average pinonaldehyde turnover was 8.9 × 106 molecules cm−3 s−1 under pinonaldehyde (high-NO) condition, approximately 6 times higher than the turnover (1.5 × 106 molecules cm−3 s−1) under α-pinene (high-NO) condition. To facilitate comparison between the two experiments, we calculated the pinonaldehyde turnover for both experiments and compared it to obtain the ratio between the α-pinene (high-NO) and pinonaldehyde (high-NO) experiments (hereafter referred to as the pinonaldehyde turnover ratio). Signals measured in the pinonaldehyde experiment were subsequently normalized by this ratio to account for differences in the pinonaldehyde turnover between the two systems. The distributions of major C10H15Ox-related products observed during α-pinene and pinonaldehyde experiments are presented in Fig. 5b. Major products belonging to the C10H14Ox and C10H15NOxfamily detected by both nitrate-CIMS (N) and amine-CIMS (A) are included. The data shown in Fig. 5b represents averages over the first 320 s following the initiation of oxidation, corresponding to the early reaction stage, during which RO2 + NO accounts for more than 90 % of the total bimolecular RO2 loss rate. In addition, all product signals here as well as all data used for comparison in the following paragraphs have been normalized by the pinonaldehyde turnover.

The pinonaldehyde turnover ratio during the first 320 s exceeded 5 and was substantially higher during the first 100 s. This large difference arose because pinonaldehyde was present at the start of the pinonaldehyde system and was therefore immediately available for reaction with OH. In contrast, under the α-pinene system, pinonaldehyde had to be formed through α-pinene oxidation before it could undergo further reactions, resulting in a much lower pinonaldehyde turnover during the early stages of the experiment. For C10H15Ox-related HOM detected by nitrate-CIMS the summed signals of the C10H14Ox and C10H15NOx families under the α-pinene system exceed those of pinonaldehyde system by factors of approximately 20 and 10, respectively. Although pinonaldehyde oxidation contributes to the formation of C10H15Ox-related HOM under high-NO conditions, this contribution is minor and can explain approximately 5 % of the HOM yield observed from α-pinene oxidation. Similarly, for less oxygenated products measured by amine-CIMS, the summed concentrations of the C10H14Ox and C10H15NOx families were 98 times higher in the α-pinene system, and 6.7 times higher in the pinonaldehyde system.

For highly oxygenated compounds detected by nitrate-CIMS, species containing more than 10 oxygen atoms account for 11 % of the C10H14Ox family and for 13 % of the C10H15NOx family under α-pinene high-NO condition, whereas their contributions are much lower for pinonaldehyde high-NO conditions (3 % and 5 %, respectively). The initial NO concentrations (Table 1) for two conditions are comparable, and consequently autoxidation rates can be the reason responsible for the differences in HOM distributions. Therefore, for peroxy radicals with more than 9 oxygen atoms the autoxidation chain of C10H15Ox peroxy radicals in pinonaldehyde photooxidation experiments are more easily terminated by NO than for peroxy radicals resulting from α-pinene photooxidation systems. The difference in the product distributions is significant between the two systems. In the pinonaldehyde system, the intensity of the C10H14Ox family is lower than that of the C10H15NOx family, indicating that the branching towards Reaction (R8) undergoing self-termination is lower than the branching towards Reaction (R6).

For less oxygenated compounds detected by amine-CIMS, the most abundant species in C10H15NOx family, C10H15NO4,derived from the reaction of C10H15O3 peroxy radicals with NO in the α-pinene system, does not appear in the pinonaldehyde system. Primary peroxy radicals with a formula of C10H15O4 are formed when OH abstracts a hydrogen atom, mainly from the aldehyde group in pinonaldehyde (Rolletter et al., 2020; Fantechi et al., 2002), as a prerequisite for autoxidation. C10H15O3 form when OH radicals abstract a hydrogen atom from α-pinene molecules, followed an alkoxy step (Reaction R7), a 6-membered ring opening, and an O2 molecule addition (Shen et al., 2022). Here, the appearance of C10H15NO4 could be explained by termination reactions between C10H15O3 and NO in the α-pinene system, when the H-abstraction pathway indeed exists. The species detected in amine-CIMS with the formula C10H15NO6 are significantly higher than other compounds in the C10H15NOx family in the pinonaldehyde system. These species are less important than C10H15NO4 in the α-pinene system. If an alkoxy radical is formed by the reaction of C10H15O4 with NO, followed by H-shift and an O2 addition, C10H15O5 peroxy radicals will be produced and can be terminated by NO to produce C10H15NO6 species. This is a potential pathway which could be responsible for the significant formation of C10H15NO6 in the pinonaldehyde system.

In summary, clustering analysis shows that C10H15NOx HOM species exhibit the fastest formation rate among all HOM compounds. They are also faster than first-generation product generation (e.g., pinonaldehyde) in the OH-addition channel under α-pinene high-NO conditions. The intensity of C10H15Ox related HOM (C10H14Ox and C10H15NOx) in the α-pinene photooxidation system is still 11 times higher than those under the pinonaldehyde system although the pinonaldehyde turnover is corrected. In addition, product distributions observed in the α-pinene system differ substantially from those in the pinonaldehyde system, regardless of whether they are detected by nitrate-CIMS or amine-CIMS. Therefore, these findings demonstrate that the H-abstraction pathway, rather than the oxidation of pinonaldehyde, accounts for the formation of C10H15Ox related HOM in the α-pinene system.

4 Conclusions and Atmospheric Implications

In this study a series of photooxidation experiments was conducted under varying NO levels to investigate the effect of NO on the C10H15Ox-related HOM formation in the α-pinene photooxidation system, and to unravel potential formation pathways of these products. The chemical system was brought to a steady state in the dark. Afterwards, reactions were initiated by photolyzing H2O2. We focused on early reaction stages (the first hundreds of seconds), during which RO2 + NO reactions and RO2 autoxidation reactions dominate the fate of the RO2. C10H17Ox-related HOM were dominantly formed via the OH-addition pathway. Product distributions, potential formation pathways, and rates of C10H17Ox-related HOM have been widely and extensively studied (Berndt, 2021; Xu et al., 2019), and our findings on C10H17Ox-related HOM formation are consistent with previous studies. However, potential formation pathways, distributions, and NO dependence of C10H15Ox-related compounds derived from the H-abstraction channel were missing systematic exploration so far.

To constrain the potential contribution of H-abstraction to HOM formation, regimes with and without NO were directly compared, and a separate experiment of pinonaldehyde oxidation under similar conditions was performed. Additionally, measurements by amine-CIMS were used to detect less oxygenated products. Since the photolysis of H2O2 was utilized to produce OH radicals, O3 did not accumulate during the early reaction stages; therefore, ozonolysis did not interfere with the OH pathways. FCM analysis proves that the dominant species in the C10H15NOx family, C10H15NO8 and C7H9NO8, can be distinguished from other species by their fast formation rates in the presence of NO. Pinonaldehyde oxidation can only contribute  5 % to HOM formation in α-pinene oxidation systems. Therefore, neither ozonolysis nor secondary oxidation can explain the significant formation of C10H15Ox-related HOM, which points to H-abstraction from α-pinene by OH being the most likely formation pathway.

As illustrated in Figs. S12 and S16, the contribution of the H-abstraction pathway to HOM formation increases with elevated NO levels compared to the OH-addition pathway. The ratios between major C10H15Ox-related HOM and C10H17Ox-related HOM rise with increasing NO concentrations. The ratios of C10H15Ox peroxy radicals to C10H17Ox peroxy radicals are 0.06, 0.83, and 1.42 under NO-free, low-NO, and high-NO conditions, respectively. Similarly, the ratio of C10H15NOx to C10H17NOx increases from 0.34 to 0.84 when NO levels increase from low to high. The sum of the major C10H15Ox-related closed-shell HOM (C10H14Ox and C10H15NOx) contributes 24 % and 34 % under low-NO and high-NO conditions, while being negligible under NO-free conditions.

The contribution of H-abstraction related products observed in this study was lower than that reported by Shen and coworkers, who reported a contribution of more than 70 % (Shen et al., 2022). The experiments of the two studies were conducted in different chambers, under different conditions, and with different instrumentations applied. The two chambers could introduce different wall losses of HOM, which can further differ between less oxygenated HOM and highly oxygenated HOM.

In this study the OH radicals were generated via photolysis of H2O2, whereas HONO photolysis was the main source of OH in Shen et al. (2022). The consecutive reaction between OH and H2O2 in our experiments led to an enhanced production of HO2 radicals, resulting in an HO2 concentration of  4 × 108 molecule cm−3, which was approximately one order of magnitude higher than that reported by Shen et al. (2022). Also, the NO concentration in Shen et al. was constantly around  20 ppb, while it was only  7 ppb before reaction in our study, resulting in a concentration of  1 ppb during the early-reaction stage. Despite these differences, the contributions of RO2 + NO reactions were dominant in both studies, accounting for more than 95 % of RO2 biomolecular losses under high-NO conditions. In addition, we did only consider early reaction stages, during which secondary oxidation was negligible and RO2 chemistry was dominated by autoxidation and RO2 + NO reactions. Therefore, the chemical system can be expected to be similar for both studies, at least under high-NO conditions. However, the constantly higher level of NO in the study by Shen et al. (2022) may continuously promote the H-abstraction channel.

The discrepancy may also arise from differences in measurement techniques: Shen et al. (2022) used an Eisele type inlet (Mauldin et al., 1999), while in this study a MION inlet was used (Rissanen et al., 2019). To compare both inlet systems, we conducted an experiment where both types of inlets were simultaneously used to measure the same oxidation systems. The reference system was α-pinene oxidation by OH, with the addition of NO (Fig. S17). The results indicate that the MION inlets detects a larger fraction of lesser oxygenated HOM (less than eight oxygen atoms) than the Eisele inlet, and that these HOM dominate the C10H17Ox-related HOM family, while the relative contribution of higher oxygenated HOM (more than eight oxygen atoms) was larger in the study by Shen et al. (2022). When only the highly oxygenated HOM compounds are considered, which were analysed by Shen and coworkers, the relative contribution of C10H15Ox-related HOM to the total HOM does increase to 64 %. Therefore, a deeper comparison of the two inlet types may be of interest in the future but is outside the scope of this study.

These findings indicate that the HOM yield attributed to the H-abstraction pathway compared to the OH-addition pathway can be significant and should not be overlooked when assessing the importance of HOM in SOA formation, especially in the presence of NO. Comprehensive product distributions formed through the H-abstraction pathway in α-pinene oxidation are illustrated in this study. HOM species with the formula C10H15NO8, recognized as characteristic indicators of OH initiated monoterpene oxidation in the presence of NO under daytime atmospheric conditions (Yan et al., 2016; Kulmala et al., 2013), may potentially be attributed to the H-abstraction pathway. However, even the NO concentrations in the low-NO case of this study were higher than those typically observed at Hyytiälä. Therefore, the significance of the H-abstraction pathway under typical low-NO boreal forest conditions remains uncertain and requires further investigation. In contrast, the contribution of the H-abstraction channel to HOM formation is expected to be more pronounced in megacities supposed to be under high NO conditions. The presence of NO not only terminates peroxy radicals and suppresses HOM formation, but also propagates the oxidative radical chain through the formation of alkoxy radicals and their subsequent isomerization, a process that under high NO levels can even compete with autoxidation (Kang et al., 2025). These reactions lead to effective NO-NO2 conversion and can then become a crucial step to promote O3 formation. The occurrence of alkoxy steps can also directly be related to O3 formation in addition to O3 sensitivity via the ratio of organic nitrate and non-nitrate HOM (Zhang et al., 2024). However, branching ratios towards alkoxy radical formation remain uncertain, when RO2 reacts with NO. Further investigation is needed to clarify the role of alkoxy processes in both SOA and O3 formation.

Data availability

The measurement data, the data used for clustering, and the data used as model input in this study are available at: https://doi.org/10.26165/JUELICH-DATA/ZZPLMZ (Wang et al., 2026).

Supplement

The supplement related to this article is available online at https://doi.org/10.5194/acp-26-11153-2026-supplement.

Author contributions

HW and HS prepared the manuscript with contributions by SK, TFM, DRW, DZ, and SRZ. HW, AZ, MB, YB, RW, SK, QH, TH, and SRZ conducted the experiments and performed the measurements. HW, HS, and SK analyzed the data. HW performed the model calculations. The compiled data set was interpreted by HW, HS, DZ, and SRZ. All co-authors discussed the results and commented on the manuscript.

Competing interests

At least one of the (co-)authors is a member of the editorial board of Atmospheric Chemistry and Physics. The peer-review process was guided by an independent editor, and the authors also have no other competing interests to declare.

Disclaimer

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. The authors bear the ultimate responsibility for providing appropriate place names. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.

Acknowledgements

The authors would like to thank the editor, the two anonymous reviewers, and Shunyu Yao for their constructive comments that helped to improve the manuscript.

Financial support

This research was supported by the Federal Ministry of Education and Research (BMBF, Germany) under the FONA strategy “Research for Sustainability” through the ACTRIS-D project (funding code: 01LK200010). Hongru Shen and Defeng Zhao would like to thank for funding support from the Shanghai Pilot Program for Basic Research-Fudan University 21TQ1400100 (22TQ010).

The article processing charges for this open-access publication were covered by the Forschungszentrum Jülich.

Review statement

This paper was edited by Jason Surratt and reviewed by two anonymous referees.

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Chamber simulations were conducted to investigate formation of highly oxygenated organic molecules (HOM) from OH-initiated α-pinene oxidation under varying NO levels, with emphasis on the hydrogen-abstraction pathway. Without NO, C10H17Oₓ· species dominated. With NO, C10H15Oₓ· products became more abundant, accounting for ~34 % at high NO levels. Clustering results and comparison with α-pinene and pinonaldehyde systems show that hydrogen-abstraction is likely the source of C10H15Oₓ·-related HOM.
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