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1 ions of unsaturated hydrocarbons with ozone (ozonolysis).
2 urce of its production occurs through alkene ozonolysis.
3 organic compounds formed during alpha-pinene ozonolysis.
4 etween hydroxy-carbonyl products of squalene ozonolysis.
5 isoprene photo-oxidation and by alpha-pinene ozonolysis.
6 ethers 12, 15, 28, and 45 include controlled ozonolysis, 1,2-addition of the Normant reagent, and het
7 ne 1 was desymmetrized via a one-pot Criegee ozonolysis/acylation protocol to afford acetal-lactone 2
8 zylidene 2-C-methylerythritol silyl ether by ozonolysis afforded a 1,2,3-triol 3-monobenzoate interme
12 ular alkylidene C-H insertion to give, after ozonolysis and aldol condensation, (-)-mesembrine 1.
14 roperties of particulate HOMs generated from ozonolysis and OH oxidation of unsubstituted (C10H16) an
15 d NO3, consistent with previous studies that ozonolysis and oxidation by NO3 are sources of nighttime
18 SOA yield and composition from alpha-pinene ozonolysis and the photooxidation of toluene and acetyle
19 room-temperature oxidation process that used ozonolysis and ultraviolet irradiation effected both the
20 e ketone, saponification, iodolactonization, ozonolysis, and intramolecular aldol reaction) to a spir
22 iliary followed by chiral auxiliary removal, ozonolysis, and reductive amination/intramolecular nucle
23 ctional elaboration, by acetal substitution, ozonolysis, and sulfur ylide-mediated epoxidation, provi
24 alpha-pinene reacting with secondary OH from ozonolysis are key intermediates in the organic nitrate
27 ecause the reaction products from endocyclic ozonolysis are tethered, this system is ideal for consid
28 Criegee intermediates (CI), formed in alkene ozonolysis, are central for controlling the multiphase c
29 lly deuterated cyclohexene and cis-6-nonenal ozonolysis, as well as the influence of water addition t
30 ,6-tris(2-chloropropan)-2-yl-1,3,5-trioxane; ozonolysis at -80 degrees C of 2,4,6-tri(propan-2-yliden
31 SOA) can continue mediated by a mechanism of ozonolysis at interfaces, a better understanding about h
33 time scales of SOA formed from alpha-pinene ozonolysis by measuring the dynamic response to a modest
34 he primary ozonides initially generated upon ozonolysis can be reduced with Zn/AcOH to afford the car
39 tified in the condensed phase which survived ozonolysis during new particle formation and growth.
40 an those suggested from many previous alkene ozonolysis experiments and assumed in atmospheric modeli
44 acid derived nitroalkenes 9, 10, and 11 and ozonolysis gave the alpha-hydroxy and alpha-amino thiol
46 ger, and the SOA mass yields for unscavenged ozonolysis generally fall within the range of mass yield
47 highly oxygenated products and cis-6-nonenal ozonolysis generated the same monomer product distributi
48 suite of oxidation products of alpha-pinene ozonolysis in an aerosol that is assumed to separate int
51 n to react with ozone are oxidized by direct ozonolysis in the hydrophobic interfacial environment, b
52 re significantly higher than SOA yields from ozonolysis including an OH scavenger, and the SOA mass y
56 le component of SOM produced by alpha-pinene ozonolysis is quantified for 20- to 50-mum particles at
58 These highly oxidized products of squalene ozonolysis may accumulate on indoor dust and surfaces an
65 hydroxy-i-steroid 11 as a byproduct from the ozonolysis of 9 and an attempt to effect conversion of s
73 These oxidative reactions, together with the ozonolysis of alkenes, are also responsible for the nigh
74 mediates (CIs), mainly formed from gas-phase ozonolysis of alkenes, are considered as atmospheric oxi
80 ry organic aerosols (SOA) resulting from the ozonolysis of alpha-pinene and photooxidation of toluene
81 paction surface to study SOA formed from the ozonolysis of alpha-pinene at relative humidities (RHs)
86 morphologies of SOA particles formed during ozonolysis of alpha-pinene in the presence of dioctyl ph
90 easured product yields for the heterogeneous ozonolysis of alpha-terpineol adsorbed on glass, NaCl, a
95 formed in a variety of systems, ranging from ozonolysis of biogenic volatile organic compounds to aro
97 of highly oxidized organic compounds in the ozonolysis of cyclohexene (C6H10) was investigated by me
100 ary organic aerosol (SOA) formation from the ozonolysis of dominant GLVs, their mixtures and grass cl
101 pressure becomes important in the gas-phase ozonolysis of endocyclic alkenes for a carbon number bet
104 the novel LC-OzID-IMS-MS configuration where ozonolysis of ionized lipids occurred rapidly (10 ms) wi
105 xamine chemical aging of SOA produced by the ozonolysis of limonene (LSOA) in the presence of gaseous
107 condary organic aerosol (SOA) formation from ozonolysis of limonene at total aerosol mass loadings ra
111 phthalene into a water-methanol droplet, the ozonolysis of oleic acid, and localization of the carbon
113 Herein, we quantify "transient AMFs" from ozonolysis of pulse-emitted limonene in a ventilated cha
114 are robust reagents capable of withstanding ozonolysis of remote alkenes, thus providing a new route
121 anone derivatives in H(2)SO(4)/CH(3)CN or by ozonolysis of the corresponding cyclohexanone methyl oxi
122 lves alkylation of 1 with an allylic halide, ozonolysis of the double bond, and catalytic hydrogenati
123 highly substituted form and in high yield by ozonolysis of the enamine bond of 1,2,3,4-tetrahydro-9H-
127 its hydroxyl function followed by reductive ozonolysis of the olefin and a subsequent one-pot three-
130 hydrides by methyl (S)-prolinate followed by ozonolysis of the resulting carboxylic acids is used to
132 functional organic compounds (HOMs) from the ozonolysis of three sesquiterpenes, alpha-cedrene, beta-
134 lar-level composition of SOA formed from the ozonolysis of two GLVs: cis-3-hexenol (HXL) and cis-3-he
135 condary organic aerosol (SOA) generated from ozonolysis of two structural monoterpene isomers: D-limo
136 cles were produced in a flow tube reactor by ozonolysis of volatile organic compounds, including the
137 to the synthesis of 2 was a first-generation ozonolysis/olefination/aldol strategy to convert a [2.2.
140 exocyclic or the compound itself is acyclic, ozonolysis produces less ELVOC and the role of the OH ra
142 accurate mass and arrival time extraction of ozonolysis products facilitated correlation of precursor
145 locks with formulas corresponding to primary ozonolysis products such as pinic and pinonic acids, whe
146 SOA is primarily formed from low-volatility ozonolysis products, with a small contribution from high
148 s toward the gas phase exhibit heterogeneous ozonolysis rate constants that are 2 times faster than d
149 pies along with GC-MS identified the aqueous ozonolysis reaction products as trans- and cis-lactols [
155 an anionic oxy-Cope rearrangement, a one-pot ozonolysis-reductive amination, and a Lewis acid promote
157 s, which are highly abundant in alpha-pinene ozonolysis SOA (22 +/- 5% by weight), have an atmospheri
158 cular formulas matching those of monoterpene ozonolysis SOA were observed; they include organonitrate
159 latile compounds and ozone from alpha-pinene ozonolysis SOA with three 1-m-long denuders, and exposin
162 oquinoline with formaldehyde produced in the ozonolysis to give a methyl (+/-)-1-methyl-2-alkyl-1,2,3
165 be the partitioning of SOA from alpha-pinene ozonolysis using measurements from a dual-thermodenuder
168 ormed in a flow tube reactor by alpha-pinene ozonolysis, was studied by passing the fresh SOA into a
169 rosol chamber investigations of alpha-pinene ozonolysis were conducted under near environmental precu
171 c double bond efficiently produce ELVOC from ozonolysis, whereas the yields from OH radical-initiated
173 reaction rates for sCIs formed from isoprene ozonolysis with SO2 along with systematic discrepancies
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