
Journal of the American Chemical Society p. 5844 - 5849 (1985)
Update date:2022-08-05
Topics:
Aubry, J. M.
The possibility of singlet oxygen (1O2) occurrence in the decomposition of H2O2 by mineral compounds in aqueous basic solutions was examined.Tetrapotassium rubrene-2,3,8,9-tetrcarboxylate was used as a trap, giving an endoperoxide detected by HPLC.We found that four families of mineral compounds lead to the formation of the endoperoxide: the oxides of the alkaline earths Ca, Sr, and Ba; the derivatives of elements of groups 3A, 4A, 5A, and 6A in d0 configuration (expect niobium); the oxides of actinides and lanthanides; and finally the oxidizers ClO-, BrO-, Au3+, IO3-, and IO4-.One compound in each family was selected for further investigation in order to strengthen the 1O2 hypothesis.Thus, the yield of the endoperoxide of potassium 9,10-diphenylanthracene-2,3,6,7-tetracarboxylate was enhanced when the parent compound was introduced in a mixture of H2O2 + (ClO-, Nd2O3, MoO42-, Ca(OH)2 + deuterated water instead of light water.
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