Hn. Erten et Z. Gokmenoglu, SORPTION BEHAVIOR OF CO2+, ZN2+ AND BA2+ IONS ON ALUMINA, KAOLINITE AND MAGNESITE, Journal of radioanalytical and nuclear chemistry, 182(2), 1994, pp. 375-384
The sorption behavior of Ba2+, Co2+ and Zn2+ ions on alumina, kaolinit
e and magnesite have been investigated using the batch method. Co-60,
Zn-65 and Ba-133 were used as radiotracers The mineral samples were se
parated into different particle size fractions using an Andreasen Pipe
tte. The particle sizes used in the sorption experiments were all less
than 38 mu m. Synthetic groundwaters were used which had compositions
similar to those from the regions where the minerals were recovered.
The samples were shaken with a lateral shaker at 190 rpm, the phases w
ere separated by centrifuging and radioactivity counted using a NaI(Tl
) detector. Kinetic studies indicated that sorption onto the minerals
took place in two stages with the slower process dominating. The highe
st sorption was observed on alumina. Both Freundlich and Dubinin-Radus
hkevich type isotherms were found to describe the sorption process wel
l. The distribution ratio, R(d), was found to be a function of the liq
uid volume to solid mass ratio. The R(d)'s for sorption on binary mixt
ures of minerals were experimentally determined and compared with thos
e predicted from R(d) values of each individual mineral.