Affiliations: Institute of Soil Science, Chinese Academy of
Sciences, Nanjing 210008, China
Note: [] Corresponding author
Abstract: It is observed that the adsorption of chromium are greater on
kaolinite minerals, red soil (R) and laterite (L) colloids than that on
montmorillonite, indicotic black (IB) and yellow brown (YB) soil colloids. The
adsorption process of Cr^IV on these media can be further described by Langmuir
or Freundlich equation quite well. The adsorption reaction of Cr^IV is fast,
and the adsorption equilibrium can be reached within the first two hours in
moderate temperature. The adsorption quantity of Cr^IV to kaolinite mineral
increased with the increasing pH in the range of 2.0 to 7.0, then decreased at
higher pH. But it showed some consistence among the four soil colloids. The
lower the pH, the stronger the adsorption. The possible mechanisms are further
discussed here. Meanwhile the influence of temperature on Cr^IV adsorption on
different soil colloid and clay minerals are also investigated.