Determination of the Effects of a Bipolar Polypyridylosmium(II) Complex on the Stability of Montmorillonite Colloids
β Scribed by Elena S. Franklin; Nicholas C. Kallan; Joseph M. Mahoney; David N. Blauch
- Publisher
- Elsevier Science
- Year
- 1998
- Tongue
- English
- Weight
- 213 KB
- Volume
- 204
- Category
- Article
- ISSN
- 0021-9797
No coin nor oath required. For personal study only.
β¦ Synopsis
Adsorption of a large cationic complex on the surface of a montmorillonite colloid results in flocculation of the colloid. This destabilization of the colloid does not occur when the cationic complex has been modified to contain a side-chain terminating in an anionic group (i.e., the complex is bipolar). The influence of such a bipolar complex on the particle sizes in montmorillonite colloids was examined using a polypyridylosmium(II) complex. Laser Doppler velocimetry was employed to determine the particle-size distributions in montmorillonite colloids containing various concentrations of the osmium complex and 1.00 g L-1 of clay. At loadings below the cation-exchange capacity of the clay, the particle-size distribution was independent of the total concentration of the bipolar osmium(II) complex. Under these conditions, at least 98% of the complex was adsorbed on the clay. Copyright 1998 Academic Press.
π SIMILAR VOLUMES
Colloidal particles stabilize emulsions both by providing steric hindrance to drop-drop coalescence and by modifying the rheological properties of the interfacial region. The effectiveness of colloidal particles in stabilizing emulsions depends in part on the ability of these particles to reside at
We use dynamic light scattering to measure the time-dependent increase of the average hydrodynamic radius of colloidal silica particles in the presence of salt. This increase appears to be linear in time up to twice the radius of unaggregated particles. The method is a very useful tool in monitoring
Adsorption behavior of polyvinylpyrrolidone (PVP) on sodium montmorillonite, a swelling clay mineral, was investigated in diluted solutions at an ionic strength of 0.01 M, representative of environmental soil solution conditions. Physicochemical methods such as microcalorimetry, light scattering abs