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Groundwater is contaminated with phenol and Zn
2+
in eastern Thailand, requiring study of the adsorption behavior of these co-contaminants on the aquifer for remediation design. The aquifer characteristics, the effect of temperature on kinetics, and the equilibrium of sorption on the aquifer were investigated. X-ray fluorescence (XRF) analysis of the flood plain aquifer revealed that the aquifer was a dispersive aluminosilicate mineral with a SiO
2
composition of 58.24%. In the endothermic reaction, an increase in the temperature resulted in an increasing adsorption rate. The adsorption kinetics was well described using a pseudo-second-order kinetic model. The intraparticle diffusion model indicated that this was not the only rate-limiting step. The adsorption isotherm data were well described by Freundlich equations. The maximum adsorption capacity of the aquifer for phenol was 24.8 mg g
−1
and for Zn
2+
was 18.7 mg g
−1
at 25 °C. The adsorption capacities of both phenol and Zn
2+
decreased in a binary system. The overall adsorption process was endothermic and spontaneous. After equilibrium, FTIR analysis indicated the adsorption properties of phenol and Zn
2+
onto the surface of the aquifer. These results showed that the flood plain deposit aquifer had differing adsorption properties of phenol and Zn
2+
at different temperatures in the contaminated groundwater.