Dysprosium-EDTA complexed with sulfosalicylic acid (SSA) was synthesized, and the fluorescence properties and radiation process of the ternary complex have been studied. The Dy-EDTA-SSA ternary complex shows distinct fluorescence (Ex 325 nm, Em 576 nm, Φ
f 0.049, F.S.I. 2.2×10
-3 μm, τ
f 2.6 ms) which is attributed to radiative transition from
4F
9/2 level to
6H
13/2 level of centered Dy(III). This communication reported the optimum conditions for the fluorometric determination of Dy(III), and 2nd derivative fluorometric method was utilized for the analysis of trace amount of Dy(III) in xenotime and monazite minerals. The procedure for the determination of Dy(III) in minerals was established as follows: The rare earth mineral samples (xenotime and monazite) treated with hot conc. H
2SO
4 and twice precipitated with 0.5 mol dm
-3 oxalic acid (pH was adjusted to 2.02.2). Then the precipitates was filtered and ignited to give the rare earth oxide. Five hundred milligrams of the oxide was dissolved in conc. HCl and diluted with water in order to obtain the solution containing 50 μg cm
-3 rare earth oxide. In the case of monazite sample, an extraction procedure with di- (2-ethylhexyl) phosphine oxide/ cyclohexane solution is used for the separation of Dy(III) from light rare earth {La(III), Ce(III), Pr(III), Nd(III), and so on}. To aliquot of the solution (0.21.5 cm
3) containing less than 2.0μg as rare earth oxide, were added 1.0 cm
3 of 2.5×10
-3 mol dm
-3 EDTA solution, 1.0 cm
3 of 2.5×10
-2 mol dm
-3 SSA solution and 10 cm
3 of 1.0 mol dm
-3 diethylamine-hydrochloric acid buffer solution. The pH of the solution was adjusted to pH 11.9±0.1, and the solution was diluted to 25 cm
3 with water. The 2nd derivative fluorescence intensity [Ex: 325 nm, Em: 576 nm] was measured. Several rare earth mineral samples were analyzed. Xenotime contained 5.08% of Dy
2O
3 and monazite contained 1.83% of Dy
2O
3.
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