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1 ions of unsaturated hydrocarbons with ozone (ozonolysis).
2 isoprene photo-oxidation and by alpha-pinene ozonolysis.
3 ultilayer model (KM-GAP) simulating triolein ozonolysis.
4 n of secondary organic aerosol formed during ozonolysis.
5 d allylic electrophiles, followed by a rapid ozonolysis.
6 In each case, SOA was produced by a-pinene ozonolysis.
7 ) that would form simultaneously in a-pinene ozonolysis.
8 ns of the Criegee intermediate formed during ozonolysis.
9 edox-catalyzed thiol-ene reaction and alkene ozonolysis.
10 ts in concentrations similar to alpha-pinene ozonolysis.
11 squalene-ozone (SqOz) reaction, or squalene ozonolysis.
12 urce of its production occurs through alkene ozonolysis.
13 organic compounds formed during alpha-pinene ozonolysis.
14 etween hydroxy-carbonyl products of squalene ozonolysis.
15 ethers 12, 15, 28, and 45 include controlled ozonolysis, 1,2-addition of the Normant reagent, and het
16 ne 1 was desymmetrized via a one-pot Criegee ozonolysis/acylation protocol to afford acetal-lactone 2
17 zylidene 2-C-methylerythritol silyl ether by ozonolysis afforded a 1,2,3-triol 3-monobenzoate interme
22 ular alkylidene C-H insertion to give, after ozonolysis and aldol condensation, (-)-mesembrine 1.
25 roperties of particulate HOMs generated from ozonolysis and OH oxidation of unsubstituted (C10H16) an
26 d NO3, consistent with previous studies that ozonolysis and oxidation by NO3 are sources of nighttime
31 SOA yield and composition from alpha-pinene ozonolysis and the photooxidation of toluene and acetyle
32 room-temperature oxidation process that used ozonolysis and ultraviolet irradiation effected both the
33 e ketone, saponification, iodolactonization, ozonolysis, and intramolecular aldol reaction) to a spir
35 iliary followed by chiral auxiliary removal, ozonolysis, and reductive amination/intramolecular nucle
36 ctional elaboration, by acetal substitution, ozonolysis, and sulfur ylide-mediated epoxidation, provi
37 3 yield is (7.9-0.2+0.4)% from HFO-1234ze(E) ozonolysis, and the PFC-14 yield is (1.04-0.05+0.07)% fr
38 alpha-pinene reacting with secondary OH from ozonolysis are key intermediates in the organic nitrate
41 ecause the reaction products from endocyclic ozonolysis are tethered, this system is ideal for consid
42 Criegee intermediates (CI), formed in alkene ozonolysis, are central for controlling the multiphase c
43 lly deuterated cyclohexene and cis-6-nonenal ozonolysis, as well as the influence of water addition t
44 ,6-tris(2-chloropropan)-2-yl-1,3,5-trioxane; ozonolysis at -80 degrees C of 2,4,6-tri(propan-2-yliden
45 SOA) can continue mediated by a mechanism of ozonolysis at interfaces, a better understanding about h
47 d in this synthetic route are regioselective ozonolysis, Au(I)-catalyzed cycloisomerization-induced c
48 the bicyclic myrtenal scaffold prior to the ozonolysis-based ring-opening step that furnishes the ta
49 time scales of SOA formed from alpha-pinene ozonolysis by measuring the dynamic response to a modest
50 ormed from other sources (e.g., alpha-pinene ozonolysis) by affecting gas-phase chemistry and gas-par
51 he primary ozonides initially generated upon ozonolysis can be reduced with Zn/AcOH to afford the car
55 ionally, we demonstrate that controlling the ozonolysis conditions used for the cleavage enables Clip
59 small diacids or products from alpha-pinene ozonolysis demonstrates that ions are ejected from the s
60 tified in the condensed phase which survived ozonolysis during new particle formation and growth.
61 egradation of unsaturated TGs due to ambient ozonolysis emerged with time and were detectable within
63 an those suggested from many previous alkene ozonolysis experiments and assumed in atmospheric modeli
65 nts of peroxy radicals (RO(2)) from flowtube ozonolysis experiments by an iodide-adduct chemical ioni
66 data allowed for the design of a homogeneous ozonolysis flow reactor capable of delivering precise qu
68 idence for mechanisms and products of olefin ozonolysis for reactions of ozone and ethene solely on t
69 e reagents which can mimic the reactivity of ozonolysis for the oxidative conversion of alkenyl bonds
70 ondensed-phase products of squalene particle ozonolysis found that an increase in water vapor concent
72 acid derived nitroalkenes 9, 10, and 11 and ozonolysis gave the alpha-hydroxy and alpha-amino thiol
74 ger, and the SOA mass yields for unscavenged ozonolysis generally fall within the range of mass yield
75 highly oxygenated products and cis-6-nonenal ozonolysis generated the same monomer product distributi
78 suite of oxidation products of alpha-pinene ozonolysis in an aerosol that is assumed to separate int
82 characterization of Criegee intermediates in ozonolysis in situ were proven difficult in decades of e
84 n to react with ozone are oxidized by direct ozonolysis in the hydrophobic interfacial environment, b
87 erically relevant AAHPs through liquid-phase ozonolysis, in which two types of monoterpene-derived SC
88 re significantly higher than SOA yields from ozonolysis including an OH scavenger, and the SOA mass y
90 ated ketone; (b) a domino sequence involving ozonolysis, intramolecular aldol reaction, and acetaliza
95 le component of SOM produced by alpha-pinene ozonolysis is quantified for 20- to 50-mum particles at
96 the importance of product quantification and ozonolysis kinetics in determining the overall environme
98 ocessing of alkenes, including isoprene, via ozonolysis leads to the formation of zwitterionic reacti
100 These highly oxidized products of squalene ozonolysis may accumulate on indoor dust and surfaces an
109 hydroxy-i-steroid 11 as a byproduct from the ozonolysis of 9 and an attempt to effect conversion of s
115 tion rate accelerations between 15-fold (for ozonolysis of alkenes in ionised lipids) and 90-fold (fo
119 ueous-phase ozonolysis, we herein report the ozonolysis of alkenes in water assisted by surfactants.
124 These oxidative reactions, together with the ozonolysis of alkenes, are also responsible for the nigh
125 mediates (CIs), mainly formed from gas-phase ozonolysis of alkenes, are considered as atmospheric oxi
130 nd radical concentrations, estimated for the ozonolysis of alpha-pinene (0.020 +/- 0.0050 nmol/mug),
131 18.9 +/- 3.2% of the mass of SOA formed from ozonolysis of alpha-pinene and beta-pinene, respectively
132 es of several major dimer esters in SOA from ozonolysis of alpha-pinene and beta-pinene-substantial g
134 ry organic aerosols (SOA) resulting from the ozonolysis of alpha-pinene and photooxidation of toluene
135 paction surface to study SOA formed from the ozonolysis of alpha-pinene at relative humidities (RHs)
137 ntration and particle mass concentration for ozonolysis of alpha-pinene exceed those from ozonolysis
142 morphologies of SOA particles formed during ozonolysis of alpha-pinene in the presence of dioctyl ph
143 nd incorporated into SOA particles formed by ozonolysis of alpha-pinene in the presence of PAH vapor.
153 easured product yields for the heterogeneous ozonolysis of alpha-terpineol adsorbed on glass, NaCl, a
156 This transformation proceeds by Criegee ozonolysis of an alkene, reductive cleavage of the resul
158 )H(9)CHOO, and C(5)H(11)CHOO), produced from ozonolysis of asymmetrical 1-alkenes (1-butene, 1-penten
159 ctrometry (DART-MS), kinetics studies of the ozonolysis of BaP in thin films exhibited fast initial l
162 formed in a variety of systems, ranging from ozonolysis of biogenic volatile organic compounds to aro
166 of highly oxidized organic compounds in the ozonolysis of cyclohexene (C6H10) was investigated by me
169 ozonolysis of alpha-pinene exceed those from ozonolysis of Delta(3)-carene alone, while their mixture
170 ary organic aerosol (SOA) formation from the ozonolysis of dominant GLVs, their mixtures and grass cl
171 pressure becomes important in the gas-phase ozonolysis of endocyclic alkenes for a carbon number bet
172 simplest Criegee intermediate, CH(2)OO, from ozonolysis of ethene by cavity ring-down spectroscopy in
176 the novel LC-OzID-IMS-MS configuration where ozonolysis of ionized lipids occurred rapidly (10 ms) wi
179 onomeric malonic anhydrides were prepared by ozonolysis of ketene dimers, a procedure validated by mo
180 xamine chemical aging of SOA produced by the ozonolysis of limonene (LSOA) in the presence of gaseous
182 condary organic aerosol (SOA) formation from ozonolysis of limonene at total aerosol mass loadings ra
187 phthalene into a water-methanol droplet, the ozonolysis of oleic acid, and localization of the carbon
189 Herein, we quantify "transient AMFs" from ozonolysis of pulse-emitted limonene in a ventilated cha
190 Previous studies have focused on surface ozonolysis of pure unsaturated compounds on impermeable
191 are robust reagents capable of withstanding ozonolysis of remote alkenes, thus providing a new route
201 anone derivatives in H(2)SO(4)/CH(3)CN or by ozonolysis of the corresponding cyclohexanone methyl oxi
202 lves alkylation of 1 with an allylic halide, ozonolysis of the double bond, and catalytic hydrogenati
203 highly substituted form and in high yield by ozonolysis of the enamine bond of 1,2,3,4-tetrahydro-9H-
208 ence of VOC-cross-product dimers in SOA from ozonolysis of the monoterpene mixture: a VOC-cross-produ
209 its hydroxyl function followed by reductive ozonolysis of the olefin and a subsequent one-pot three-
212 hydrides by methyl (S)-prolinate followed by ozonolysis of the resulting carboxylic acids is used to
213 entatively identified as products of aqueous ozonolysis of the two unsaturated terpenoic acids invest
216 functional organic compounds (HOMs) from the ozonolysis of three sesquiterpenes, alpha-cedrene, beta-
218 cept, we characterized HOM formed during the ozonolysis of two biogenic compounds (alpha-pinene and l
219 lar-level composition of SOA formed from the ozonolysis of two GLVs: cis-3-hexenol (HXL) and cis-3-he
220 condary organic aerosol (SOA) generated from ozonolysis of two structural monoterpene isomers: D-limo
222 hemical kinetics associated with the ambient ozonolysis of unsaturated triacylglycerols (TGs), a majo
223 ultaneously quantifies CIs produced from the ozonolysis of volatile organic compounds in the gas and
224 cles were produced in a flow tube reactor by ozonolysis of volatile organic compounds, including the
225 to the synthesis of 2 was a first-generation ozonolysis/olefination/aldol strategy to convert a [2.2.
226 position of SOA formed via dark alpha-pinene ozonolysis on either (NH(4))(2)SO(4) or Fe-containing (N
230 ne intermediate; (iii) development of a safe ozonolysis process conducted in an aqueous solvent mixtu
231 01+0.04)% from HFO-1234yf, while HCFO-1233xf ozonolysis produces CFC-13 in (0.034-0.006+0.009)% yield
232 exocyclic or the compound itself is acyclic, ozonolysis produces less ELVOC and the role of the OH ra
234 human occupancy on the dynamics of skin oil ozonolysis products (SOOPs) in an office in a LEED-certi
235 accurate mass and arrival time extraction of ozonolysis products facilitated correlation of precursor
238 n CSE-119 cells was strongly affected by the ozonolysis products of 6PPD but not by those of the othe
239 OCs were measured, including common skin oil ozonolysis products such as acetone, 6-MHO, and 4-OPA; h
240 locks with formulas corresponding to primary ozonolysis products such as pinic and pinonic acids, whe
242 SOA is primarily formed from low-volatility ozonolysis products, with a small contribution from high
244 involves the cleavage of olefinic groups via ozonolysis, providing the resulting two-merged net MOFs
246 s toward the gas phase exhibit heterogeneous ozonolysis rate constants that are 2 times faster than d
247 strating the rapid nature of this multiphase ozonolysis reaction at atmospherically relevant ozone le
248 rofiles benchmark the modeling of the ethene ozonolysis reaction network and mechanism, allowing for
249 pies along with GC-MS identified the aqueous ozonolysis reaction products as trans- and cis-lactols [
256 solvents on ozone solubility and the rate of ozonolysis reactions using rapid injection NMR spectrosc
259 an anionic oxy-Cope rearrangement, a one-pot ozonolysis-reductive amination, and a Lewis acid promote
263 - 2](+) product ions was probed by gas-phase ozonolysis revealing the presence of two new carbon-carb
264 s, which are highly abundant in alpha-pinene ozonolysis SOA (22 +/- 5% by weight), have an atmospheri
265 demonstrated by application to alpha-pinene ozonolysis SOA for which increased filter aerosol mass l
266 cular formulas matching those of monoterpene ozonolysis SOA were observed; they include organonitrate
267 latile compounds and ozone from alpha-pinene ozonolysis SOA with three 1-m-long denuders, and exposin
271 in terpenes capable of generating OH through ozonolysis, the much larger amount of ethanol solvent ac
272 h our previous studies on ethene and propene ozonolysis, the nascent sCI yields demonstrated an intri
273 however, are still limited, as they rely on ozonolysis to generate the key peroxide intermediates fr
274 oquinoline with formaldehyde produced in the ozonolysis to give a methyl (+/-)-1-methyl-2-alkyl-1,2,3
276 idation (IMP), we address the limitations of ozonolysis to rescue previously inaccessible alkene subs
277 s, as well as the first reported use of "dry ozonolysis" to reveal a masked carboxylic acid in the to
278 a presynthesized microporous UiO-type MOF to ozonolysis, to confer it with mesopores sufficiently lar
281 all the organic linkers (in this study, via ozonolysis under reductive conditions) liberates the SBU
283 be the partitioning of SOA from alpha-pinene ozonolysis using measurements from a dual-thermodenuder
288 ormed in a flow tube reactor by alpha-pinene ozonolysis, was studied by passing the fresh SOA into a
289 Inspired by the atmospheric aqueous-phase ozonolysis, we herein report the ozonolysis of alkenes i
290 ve organic species generated by alpha-pinene ozonolysis, we show that combining diethylammonium and n
291 rosol chamber investigations of alpha-pinene ozonolysis were conducted under near environmental precu
292 and LA that were produced following aqueous ozonolysis were identified as keto-BCA and keto-LA, resp
295 c double bond efficiently produce ELVOC from ozonolysis, whereas the yields from OH radical-initiated
296 micity is exhibited in the initial stages of ozonolysis, which has a powerful influence on the CHF(3)
297 tal piece of molecular insight into isoprene ozonolysis, which has broad tropospheric implications du
299 reaction rates for sCIs formed from isoprene ozonolysis with SO2 along with systematic discrepancies
300 produced with 21 to 23% yield from isoprene ozonolysis, yet its reactivity has not been directly stu