Résumé:
A study was conducted on the interaction between Rhodamine B, a cationic dye, and the fine
fraction of a natural clay. Chemical analysis and X-ray diffraction revealed that this fraction
is mainly composed of beidellite. By examining the amounts of Rhodamine B adsorbed by
the beidellite under different experimental parameters (contact time, pH, sorbent mass, and
dye concentration), it was observed that: (1) the sorption kinetics are rapid and fit a pseudosecond-
order kinetic model, (2) pH significantly influences sorption efficiency, and (3) the
adsorption capacity of the clay, estimated using the Langmuir model, is approximately 0.54
mmol.g-1.