It has been found that an i.r. band observable at 1140 cm–1 on goethite, which undergoes several reversible splittings and shifts on dehydration of the sample, is the precursor of similar bands previously observed on haematite and assigned to adsorbed oxygen.
C. Morterra, C. Mirra and E. Borello, J. Chem. Soc., Chem. Commun., 1983, 767 DOI: 10.1039/C39830000767
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.
Please wait while we load your content...