SURFACE FREE-ENERGY COMPONENTS OF MONODISPERSE ZINC-SULFIDE

Citation
Jdg. Duran et al., SURFACE FREE-ENERGY COMPONENTS OF MONODISPERSE ZINC-SULFIDE, Materials chemistry and physics, 38(1), 1994, pp. 42-49
Citations number
23
Categorie Soggetti
Material Science
ISSN journal
02540584
Volume
38
Issue
1
Year of publication
1994
Pages
42 - 49
Database
ISI
SICI code
0254-0584(1994)38:1<42:SFCOMZ>2.0.ZU;2-6
Abstract
Apolar. Lifshitz-van der Waals (gamma(LW)) and polar, acid-base (Lewis ) (gamma(AB)) surface free energy components, of monosized, spherical ZnS colloidal particles were experimentally determined using the thin- layer wicking technique. The results were compared with those obtained on a pure, commercial sample of zinc sulfide. The fact that the synth etized sample showed a very high electron-donor (gamma(s)-) component suggested that some species, related in principle to surface oxidation of ZnS during the synthesis reaction, could be formed on the surface of the particles. To check for this possibility, the surface free ener gy components of pure and oxidized ZnS, and of zinc oxide and sulfate, were determined by both the contact angle and thin-layer wicking meth ods. The similarity between gamma(s) components obtained with both met hods for pure ZnS lead to the conclusion that both techniques give rel iable results. The high gamma(s)-value determined for synthetic ZnS pa rticles cannot be explained simply by surface oxidation of the colloid al particles, since partially oxidized ZnS, or even zinc oxide or sulf ate, gave very similar gamma(s)-, always lower than that found for syn thetic spherical ZnS. The fact that the Lifshitz-van der Waals (gamma( s)LW) component of the surface free energy is somewhat higher for the latter material is believed to be related to elemental sulfur present on the surface of the particles. The general compatibility of the resu lts obtained by both methods suggests that the thin-layer wicking tech nique is useful to further characterize these or other systems. partic ularly if the examined material is sufficiently monodisperse.