1977
DOI: 10.3891/acta.chem.scand.31b-0561
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Studies on the Degradation of Phenolic Lignin Units of the beta-Aryl Ether Type with Oxygen in Alkaline Media.

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Cited by 60 publications
(62 citation statements)
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“…The spiroepoxide moiety of 6 was established by the carbon chemical shifts of C-1 (68.2 ppm) and C-1Ј (59.2 ppm), showing that both were connected to oxygen, and the proton chemical shift of H1 at 3.28 ppm (33). The ring attached to the epoxide was oxidized to a quinone (C-4Ј as a carbonyl at 184.0 ppm), resulting in chemical shifts of H-2Ј, H-5Ј, and H-6Ј compatible with double bonds rather than an aromatic ring.…”
Section: Isolation and Characterization Of Curcumin Autoxidationmentioning
confidence: 99%
“…The spiroepoxide moiety of 6 was established by the carbon chemical shifts of C-1 (68.2 ppm) and C-1Ј (59.2 ppm), showing that both were connected to oxygen, and the proton chemical shift of H1 at 3.28 ppm (33). The ring attached to the epoxide was oxidized to a quinone (C-4Ј as a carbonyl at 184.0 ppm), resulting in chemical shifts of H-2Ј, H-5Ј, and H-6Ј compatible with double bonds rather than an aromatic ring.…”
Section: Isolation and Characterization Of Curcumin Autoxidationmentioning
confidence: 99%
“…The first phase of the oxidative ammonolysis is likely associated with the reactions of phenolic moieties of the original lignin, because their reactivity is much higher than etherified moieties. [16,17] About 60% of the maximum nitrogen uptake being incorporated in the first reaction phase correlates with amount of phenolic hydroxyl groups (70%) in Repap lignin reported by Faix et al [18] The second phase of the reaction is likely associated with original non-phenolic moieties. The original non-phenolic moieties could participate in the oxidative ammonolysis by their conversion to phenolic moieties via oxidative cleavage of side chains resulting in cleavage of alkyl-O-aryl bonds.…”
Section: The Reaction Mechanisms Of Oxidative Ammonolysis Of Ligninmentioning
confidence: 85%
“…Quinoide compounds seem to be important key intermediates in the natural formation of humic substances. They can be formed via both, homolytic (Kratzl et al 1967) and heterolytic processes (Gierer et al 1977) from any (substituted: guaiacyl, syringyl type) phenylpropane unit that bears a free phenolic group. Although these studies were based on lignin, lignite still contains phenylpropane units bearing free phenolic OH groups as lignin does (Wender 1976).…”
Section: Phenanthrene Sorptionmentioning
confidence: 99%