X-ray diffraction and Raman spectroscopic studies of Zn-substituted carrboydite-like compounds
- 1. Inorganic Materials Research Program, School of Physical and Chemical Sciences, Queensland University of Technology, GPO Box 2434, Brisbane, Qld 4001 (Australia)
Description
Hydrotalcite-like compounds of the formula Ni xZn6-xAl2(OH)16(SO4).4H2O where x varies from 0 to 6, equivalent to a zinc-substituted carrboydite have been synthesised and characterised by X-ray diffraction, electron microscopy and vibrational spectroscopy. Both the d (0 0 3) spacing and the crystallite size are a function of the amount of zinc replacement for nickel in the carrboydite-like compounds. Transmission electron microscopy (TEM) shows the clay-like crystal structure for these hydrotalcite compounds. These compounds were characterised by vibrational spectroscopic techniques and a comparison made with the naturally occurring minerals. Additional bands in the sulphate antisymmetric stretching and bending region leads to the conclusion that the symmetry of the sulphate anion is reduced inferring the bonding of the sulphate anion to the hydrotalcite hydroxyl surface
Additional details
Identifiers
- DOI
- 10.1016/j.matchemphys.2005.12.028;
- PII
- S0254-0584(05)00871-0;
Publishing Information
- Journal Title
- Materials Chemistry and Physics
- Journal Volume
- 100
- Journal Issue
- 1
- Journal Page Range
- p. 174-186
- ISSN
- 0254-0584
- CODEN
- MCHPDR
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 38079137
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- ALUMINIUM COMPOUNDS; ANIONS; CLAYS; CRYSTAL STRUCTURE; NICKEL COMPOUNDS; SPECTROSCOPY; SULFATES; TRANSMISSION ELECTRON MICROSCOPY; X-RAY DIFFRACTION; ZINC COMPOUNDS
- Descriptors DEC
- CHARGED PARTICLES; COHERENT SCATTERING; DIFFRACTION; ELECTRON MICROSCOPY; IONS; MICROSCOPY; MINERALS; OXYGEN COMPOUNDS; SCATTERING; SILICATE MINERALS; SULFUR COMPOUNDS; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2005 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.