𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Zeta Potential Measurement in Catalyst Preparations

✍ Scribed by J. B. Stelzer; R. Nitzsche; J. Caro


Publisher
John Wiley and Sons
Year
2005
Tongue
English
Weight
219 KB
Volume
28
Category
Article
ISSN
0930-7516

No coin nor oath required. For personal study only.

✦ Synopsis


Oxide surfaces are covered with hydroxyl groups. In contact with water, positive or negative surface charges can be developed. The surface charge of oxide particles can be fine-tuned by changing the calcination temperature of the oxides before dispersion in water or by variation of the suspension pH. Strong negative or positive surface charges stabilize a suspension and avoid particle aggregation. Nano-structured catalysts suspended in water show surface charges different from those of compact TiO 2 . For spray drying, the cationic or anionic additives used have to be strongly attached via electrostatic forces to the surface of the suspended oxide particles. When noble metal complexes have to be brought to the support surface, the positively or negatively charged complexes must have an opposite charge relative to the surface charge. Zeta potential measurements can solve these problems.


πŸ“œ SIMILAR VOLUMES


Zeta Potential Measurements on Passive M
✍ Laurence BoulangΓ©-Petermann; A. Doren; B. Baroux; Marie-NΓΆelle Bellon-Fontaine πŸ“‚ Article πŸ“… 1995 πŸ› Elsevier Science 🌐 English βš– 362 KB
Progress in nanoparticles characterizati
✍ Renliang Xu πŸ“‚ Article πŸ“… 2008 πŸ› Elsevier 🌐 English βš– 194 KB

Characterization of various nanoparticles is on the center stage in nanotechnology development. The subjects for nanoparticles characterization are focused on particle size and particle surface charge determinations. This article summarizes the latest development in particle size analysis using dyna

Zeta potential and surface area measurem
✍ Suh-Shiang Chen; P.K. Mehta πŸ“‚ Article πŸ“… 1982 πŸ› Elsevier Science 🌐 English βš– 133 KB

It is well known that certain clay minerals can swell by adsorption of water. A combination of high surface area and unsatisfied surface charges is believed to be responsible for the attractive force between water and these clay minerals. On the basis of earlier work at the University of California