The electrokinetic behavior and stability of aqueous suspensions containing
serpentine minerals of different deposits have been studied. Crystallochem
ical analyses carried out by X-ray diffraction, IR spectroscopy, TEM, DTA/T
G, and XRF revealed that all samples are lizardite-type serpentines with a
similar chemical composition. It has been determined that the electrokineti
c behavior of lizardite aqueous suspensions is mainly a function of the Mg/
Si atomic ratio on surface. So, the low isoelectric point observed in some
samples has been linked to values of this ratio lower than that of the idea
l lizardite (Mg/Si = 1.5). Dissolution studies have shown that the removal
of Mg cations from the solid at speeds faster than that theoretically expec
ted (Mg/Si = 1.5), i.e., incongruent dissolution, is responsible for the en
richment of Si cations on surface. Therefore, it has been clearly establish
ed that the surface charge value developed in the lizardite/aqueous electri
cal interface is a function of the lizardite surface alteration grade. (C)
2000 Academic Press.