Abstract: Lead adsorption behavior was investigated using four Zeolite minerals (clinoptilolite, analcime, phillipsite and chabazite). The used Pb2+ concentrations were 0, 0.1, 0.5, 1.0, 2.0, 3.0 and 5 μol mL-1. Results indicated that Pb2+ sorption followed the Langmuir adsorption isotherm, but over limited concentration ranges for clinoptilolite and analcime. The bindg energy (Kd) reached, 2.400 and 0.875 g L-1 for phillipsite and chabazite, respectively. The maximum adsorption capacity for such minerals reached 208.33 and 204.08 mg g-1 with correlation coefficient (R2) reached, 0.997 and 0.995, respectively. Meanwhile, two stages for Pb2+adsorption were observed with clinoptilolite and analcime in the low and high concentrations of the applied Pb2+. Data also was applicable to the Freundlich adsorption isotherm over the used entire Pb2+ concentration ranges. The binding energy (n) reached, 1.014, 1.005, 1.001 and 1.001 g L-1 for clinoptilolite, analcime, phillipsite and chabazite, respectively. However, the b values (maximum adsorption capacity) reached 202.582, 201.651, 207.062 and 206.871 mg g-1 with correlation coefficient (R2) nearly one for all studying minerals, respectively. Desorption data indicated that most of the sorbed Pb2+ was extracted in the 1st extraction following the adsorption experiment. The ability of the used zeolite minerals to retain Pb2+ was high and there were differences between the studied minerals in sorption of Pb2+. In conclusion, data eliminated that, zeolite minerals especially, philipsite and chabazite, could be successfully used as packing material in subsurface reactive barriers intercepting ground water plumes and for fixed bed reactors designed to remove Pb2+ from industrial wastewater.