Issue 6, 1991

Formation of Q8M10{[(CH3)3SiO]10Si8O11} from QM4{[(CH3)3SiO]4Si}, olivine and dioptase

Abstract

The preparation of three-dimensional silicate organosiloxane hybrids by the controlled polymerisation of monosilicic acids derived from silicate minerals such as olivine has been studied. A two-stage reaction process, for the formation of {[(CH3)3SiO]10Si8O11}[Q8M10; Q = SiO4/2, M =(CH3)3SiO1/2] has been outlined, which includes silicic acid polymerisation and polyorganosiloxane (QM polymer) redistributions. The structure of Q8M10 has been characterised and shown to be a major product of the partial trimethylsilylation of the minerals olivine or dioptase.

Article information

Article type
Paper

J. Mater. Chem., 1991,1, 943-946

Formation of Q8M10{[(CH3)3SiO]10Si8O11} from QM4{[(CH3)3SiO]4Si}, olivine and dioptase

G. J. Bratton, B. R. Currell, J. R. Parsonage and G. K. Wall, J. Mater. Chem., 1991, 1, 943 DOI: 10.1039/JM9910100943

To request permission to reproduce material from this article, please go to the Copyright Clearance Center request page.

If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given.

If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given. If you want to reproduce the whole article in a third-party publication (excluding your thesis/dissertation for which permission is not required) please go to the Copyright Clearance Center request page.

Read more about how to correctly acknowledge RSC content.

Spotlight

Advertisements