THE RHEOLOGICAL AND COLLOIDAL PROPERTIES OF BENTONITE DISPERSIONS IN THE PRESENCE OF ORGANIC-COMPOUNDS .2. FLOW BEHAVIOR OF WYOMING BENTONITE IN WATER-ALCOHOL
T. Permien et G. Lagaly, THE RHEOLOGICAL AND COLLOIDAL PROPERTIES OF BENTONITE DISPERSIONS IN THE PRESENCE OF ORGANIC-COMPOUNDS .2. FLOW BEHAVIOR OF WYOMING BENTONITE IN WATER-ALCOHOL, Clay Minerals, 29(5), 1994, pp. 761-766
The flow behaviour of Wyoming bentonite dispersions was studied in wat
er and water-alcohol mixtures (methanol, ethanol, n-propanol) with or
without the addition of NaCl. The yield value tau(o) and relative appa
rent viscosity tau(rel) (= tau* (dispersion/tau* (medium) at gamma =
94.5 s-1) increase to a maximum and then decrease with increasing alco
hol content. The increase of the flow values is caused by face-to-face
aggregation. Formation of band-type networks is a consequence of the
enhanced attraction between the silicate layers in water-alcohol mixtu
res. At higher alcohol contents the bands are contracted to discrete p
articles. Both effects are considerably strengthened by calcium ions w
hich are present in the crude bentonite.