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1.2.3- Trioxolanes primary ozonides

The most commonly employed transformations for the construction of five-membered rings containing three sulfur or oxygen atoms in the 1,2,4-positions are shown in Table 11. These have attracted more interest than the syntheses from acyclic components. The rearrangement of a 1,2,3-trioxolane (primary ozonide) to a 1,2,4-trioxolane (secondary ozonide) is the most generally applicable method for preparation of this ring system and will be discussed further in Sections... [Pg.609]

The IR spectroscopy of the extremely unstable 1,2,3-trioxolanes (primary ozonides) has been possible only in the recent past when special low-temperature IR cells became available. These cells enabled the preparation of primary ozonides from alkenes and ozone in the spectrometer itself. As shown in Table 4, most of the primary ozonides studied by this... [Pg.858]

Experimental studies have shown that ozone-alkene reactions in the gas phase likewise proceed via intermediate formation of 1,2,3-trioxolanes (primary ozonides) whose spontaneous decomposition then as a rule leads to a variety of subsequent products, including 1,2,4-trioxolanes (81JA3807). Because ozone is present in the atmosphere (from 0.02p.p.m. at sea level up to 0.2 p.p.m. and more in industrial and urbanized areas), reactions of... [Pg.894]

Unsaturated compounds undergo ozonization to initially produce highly unstable primary ozonides (15), ie, 1,2,3-trioxolanes, also known as molozonides, which rapidly spHt into carbonyl compounds (aldehydes and ketones) and 1,3-zwitterion (16) intermediates. The carbonyl compound-zwitterion pair then recombines to produce a thermally stable secondary ozonide (17), also known as a 1,2,4-trioxolane (44,64,125,161,162). [Pg.117]

Ozone (332) generally combines with alkenes in a 1,3-dipolar fashion giving the so-called primary ozonides which recombine to 1,2,4-trioxolanes (ozonides). Its reaction with the parent MCP (1) is not known, whereas it reacts readily at... [Pg.57]

Significant advances in the chemistry of these ring systems over the past 10 years include the first unambiguous detection, and characterization by microwave spectroscopy as 1,2,3-trioxolane, of the primary ozonide from ethene and ozone (cf. Section 4.15.3.2), and the introduction of 1,3,2-dioxathiolane 2,2-dioxides as epoxide equivalents in organic synthesis (cf. Section 4.15.5.3). Advances have also been made in the synthesis and characterization of the chemistry of 1,2,3-trithiolanes and 1,2,3-trithioles. [Pg.547]

Acid-catalyzed dimerization and oligomerization of 1,2,4-trioxolanes will be covered in Section 4.16.5.2.1. In general, ozonides are not prone to spontaneous polymerization. Polymeric products can be obtained from the ozonolysis of alkenes but most likely arise from reaction of the primary ozonide. Bicyclic 1,2,4-trioxolanes such as 2,5-dimethylfuran endoperoxide can dimerize on warming in CCI4 (Section 4.16.5.1.1). 1,2,4-Trithiolane tends to polymerize at room temperature especially if left open to air, whilst more highly substituted ring systems are stable. [Pg.599]

Ozonolysis of alkenes in participating solvents such as alcohols often leads to trapping of intermediates. Most commonly, an alcohol will react with the carbonyl oxide zwitterion, generated from cycloreversion of the primary ozonide (Section 4.16.8.2), to give an alkoxy hydroperoxide. The secondary ozonide (1,2,4-trioxolane) is usually more stable to nucleophilic attack from alcohols. [Pg.601]

Trioxolane (1) has only been prepared by the ozonolysis of ethylene. The rearrangement of the primary ozonide occurs above — 100°C to give 1,2,4-trioxolane as a colorless, explosive liquid <42LA(553)187>. 1,2,4-Trithiolane (2) is still best prepared by a classical reaction of Na2S2.5 with excess dichloromethane. Some 1,2,4,5-tetrathiolane is also produced, but (2) can be isolated as a pale-yellow distillable liquid. It is best kept stored under inert atmosphere below 0°C to avoid polymerization <67CPB988>. Parent compounds (3)-(6) are not known and the 1- and 4-5-oxides for 1,2,4-trithiolane have been mentioned previously (see Section 4.16.5.2.3). [Pg.610]

One of the most important features of the ozonolysis reaction of alkenes is one in which ozone adds to the C=C bond to form a primary ozonide (1,2,3-trioxolane). The Criegee mechanism suggests that this unstable intermediate decomposes into a carbonyl compound and a carbonyl oxide that recombine to form a final isomeric ozonide (1,2,4-trioxolane). Direct spectroscopic evidence for a substituted carbonyl oxide has only recently been reported by Sander and coworkers for the NMR characterization of dimesityl carbonyl oxide. Kraka and coworkers have theoretically modeled dimesityl carbonyl oxide and confirmed the structural aspects reported by Sander and coworkers on the basis of NMR data. [Pg.29]

Although a large amount of work has been done on the mechanism of ozonization (formation of 11), not all the details are known. The basic mechanism was formulated by Criegee.I7 l The first step of the Criegee mechanism is a 1,3 dipolar addition (5-46) of ozone to the substrate to give the initial or primary ozonide, the structure of which has been shown to be the 1,2,3-trioxolane 12 by microwave and other spectral methods.174 However,... [Pg.1178]

Unsaturated compounds undergo ozonization to initially produce highly unstable primary ozonides (11), i.e., 1.2,3-trioxolanes, also known as molozonides, which rapidly split into carbonyl compounds (aldehydes and... [Pg.1235]

Despite the complexities of alkene ozonolysis47, the reaction between alkenes and ozone may be summarized by Scheme 7. The reaction involves several steps48 with the formation of a variety of intermediates, such as a primary ozonide (1,2,3-trioxolane) (12), its isomer of rearrangement 13 and a carbonyl oxide (14). [Pg.374]

First step is a 1,3-dipoIar cycloaddition of ozone to the alkene leading to the primary ozonide (molozonide, 1,2,3-trioxolane, or Criegee intermediate) which decomposes to give a carbonyl oxide and a carbonyl compound ... [Pg.88]

There are six possible five-membered monocycles 1-6 containing three oxygen or sulfur atoms in the 1,2,3-positions <1996CHEC-II(4)545>. 1,2,3-Trioxolane 1 is the parent compound of the so-called primary ozonides, the primary reaction products in the reaction of alkenes with ozone. They are extremely unstable and rearrange to the more stable ozonides (1,2,4-trioxolanes). This rearrangement represents a key step in the reaction of ozonolysis. However, the parent compound 1 and a few derivatives have been characterized at low temperatures (see Section 6.05.10.1). 1,2,3-Trithiolanes have been synthesized (Section 6.05.10.3) some of them undergo slow decomposition at room temperature. Derivatives of 1,2,3-dioxathiolane 3 are unknown, and the other heterocycles of the mixed types 4-6 are known only in the oxidized forms, mostly as -oxides and J -dioxides, and also A-imino and A-thiono derivatives <1996CHEC-II(4)545>. The A-oxides and AA -dioxides of... [Pg.146]

A comparison of various calculations revealed <1997PCA9421> that an accurate description of the ozonolysis of ethene is obtained at the CCSD(T) level with a TZ+2P basis set, while other methods, which cover less correlation effects, fail to provide a consistent description of all reaction steps. It was shown that the primary ozonides (1,2,3-trioxolanes) are not collisionally stabilized under atmosphere conditions <1997PCA9421>. [Pg.147]

The formation of 1,2,3-trioxolane 1 (the primary ozonide) and of 1,2,4-trioxolane (the secondary ozonide) in the reaction of ozone with ethene in a cryogenic matrix was observed by IR spectroscopy at much lower temperatures than previously reported as low as 25 K in the amorphous CO2 matrix < 1996JA3687>. There was no indication of Criegee intermediates -carbonyl oxide and formaldehyde. No reaction was found in an argon matrix at temperatures up to 35 K. The identification of the ozonides was supported by ab initio calculation of the IR spectmm <1996JA3687, 1996SAA1479>. [Pg.149]

Fragmentation, even at low temperatures, of highly unstable 1,2,3-trioxolanes (the primary ozonides) to carbonyl oxides and carbonyl compound (Criegee intermediates) with a subsequent recombination to more stable 1,2,4-trioxolanes... [Pg.151]

Since there have been some confusions in the nomenclature <1990AGE344, 1991CRV335>, it must be emphasized that (1) 1,2,3-trioxolanes are primary ozonides or moloxides (2) 1,2,4-trioxolanes are secondary or final ozonides and (3) Criegee s carbonyl oxide intermediate 1, 2 has been found theoretically to have a pronounced diradical character 3, not only in the gas phase, but also in solution in nonpolar solvents only its reaction with carbonyl compounds in solution has a polar character. Nevertheless, the name carbonyl oxide is so well entrenched that it will continue to be used for intermediates 1-3. [Pg.193]

Since the publication of CHEC-II(1996), in the field of 1,2,4-trioxolane chemistry (also commonly known as ozonide chemistry), two research directions have been pursued. First, mechanistic investigations on how the primary ozonide is fragmenting have led to predictive rules that show that both steric and electronic factors need to be considered. Second, and more importantly, a relatively large number of chemical transformations have been performed on ozonides, remote from the heterocyclic moiety. This is of interest as the ozonide has proved to be stable in a number of chemical transformations and can thus function as a masked or protected aldehyde. [Pg.212]

The mechanism proposed by Criegee for the ozonolysis of alkenes <1975AGE745> considers an initial it-complex between the alkene and ozone which decays via a 1,3-dipolar cycloaddition into a 1,2,3-trioxolane or primary ozonide, known also as the molozonide . These compounds are unstable, even at low temperatures, and due to cycloreversion decompose into a carbonyl fragment and a CO, which may recombine by another 1,3-dipolar cycloaddition step to form the more stable 1,2,4-trioxolane ( secondary ozonide or final ozonide (see also Section 6.06.2). [Pg.212]

Treatment of 2-butyne with ozone leads to unstable primary ozonides that cleave to cr-oxo-carbonyl oxides these could be trapped in the presence of aldehydes or ketones affording cross- -oxo-l, 2,4-trioxolanes. Subsequent cycloadditions between such cr-oxo-ozonides and cyclohexanone oxide, generated in situ from O-methylcyclohex-anone oxime (which affords methyl nitrite as a side-product), yield cr-diozonides 101 (Scheme 30) <1997J(P1)1601>. [Pg.218]

Density functional theoretical calculations were applied to the formation of internal primary ozonides from three PAHs (pyrene, coronene, and circum-pyrene O Hm) to simulate the atmospheric interaction between ozone and soot. No 1,2,4-trioxolane intermediate was considered in the conversion of the 1,2,3-trioxolane into aromatic epoxides via ring-opened trioxyl diradicals <2005PCA10929>. [Pg.223]

The reaction of ozone with a C=C double bond begins with a 1,3-dipolar cycloaddition. It results in a 1,2,3-trioxolane, the so-called primary ozonide ... [Pg.683]

In contrast to the carbonyl oxide of Figure 15.47, they do not undergo a cycloaddition with each other. Instead, they undergo a 1,3-dipolar cycloaddition to the C=0 double bond of the concomitantly formed aldehyde(s). The orientation selectivity is such that the trioxolane formed differs from the primary ozonide the 1,2,4-trioxolane products are the so-called secondary ozonides. [Pg.685]


See other pages where 1.2.3- Trioxolanes primary ozonides is mentioned: [Pg.192]    [Pg.192]    [Pg.611]    [Pg.1523]    [Pg.173]    [Pg.546]    [Pg.610]    [Pg.612]    [Pg.612]    [Pg.247]    [Pg.721]    [Pg.247]    [Pg.721]    [Pg.477]    [Pg.147]    [Pg.217]    [Pg.227]    [Pg.233]    [Pg.852]    [Pg.852]   
See also in sourсe #XX -- [ Pg.721 ]




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