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A new method for analysis of trace mercury in water samples was developed, based on the combination of preconcentration/separation using dithizone-modified nanometer titanium dioxide (TiO2) as a solid phase extractant and determination by cold vapor atomic adsorption spectrometry (CVAAS). Dithizone was dissolved with alcohol and loaded on the surface of nano-sized TiO2 powders by stirring. The static adsorption behavior of Hg2+on the dithizone-modified nanoparticles was investigated in detail. It was found that excellent adsorption ratio for Hg2+ could be obtained in the pH range of 7-8 with an oscillation time of 15 min, and a 5 mL of 3.5 molL1 HCl solution could quantitatively elute Hg2+ from nanometer TiO2 powder. Common coexisting ions caused no obvious influence on the determination of mercury. The mechanisms for the adsorption and desorption were discussed. The detection limit (3σ) for Hg2+ was calculated to be 5 ngL1. The proposed method was applied to the determination of Hg2+ in a mineral water sample and a Zhujiang River water sample. By the standard addition method, the average recoveries were found to be 94.4%-108.3% with RSD (n = 5) of 2.9%-3.5%.
A new method for analysis of trace mercury in water samples was developed, based on the combination of preconcentration / separation using dithizone-modified nanometer titanium dioxide (TiO2) as a solid phase extractant and determination by cold vapor atomic adsorption spectrometry (CVAAS). Dithizone was dissolved with alcohol and loaded on the surface of nano-sized TiO2 powders by stirring. The static adsorption behavior of Hg2 + on the dithizone-modified nanoparticles was investigated in detail. It was found that excellent adsorption ratio for Hg2 + could be obtained in the The pH range of 7-8 with an oscillation time of 15 min and a 5 mL of 3.5 mol L1 HCl solution could quantitatively elute Hg2 + from nanometer TiO2 powder. Common coexisting ions caused no significant influence on the determination of mercury. The mechanisms for the adsorption The detection limit (3σ) for Hg2 + was calculated to be 5 ngL1. The proposed method was applied to the determination of Hg2 + By the standard addition method, the average recoveries were found to be 94.4% -108.3% with RSD (n = 5) of 2.9% -3.5%.