Synthesis and thermal stability of rare earth compounds REF3, REF3·nH2O and (H3O)RE3F10·nH2O (RE = Tb − Lu, Y), obtained from sulphide precursors

https://doi.org/10.1016/j.jfluchem.2017.12.001Get rights and content

Highlights

  • The REF3&903·nH2O and (H3O)RE3F10&903·nH2O compounds were synthesized from RE2S3 and HF.

  • The REF3&903·nH2O compounds have an amorphous phase.

  • After heat treatment the REF3&903·nH2O and (H3O)RE3F10&903·nH2O compounds moved into a REF3 compound of crystal structure as β-YF3.

Abstract

The nature of the interaction between sulphides of the rare-earth elements (RE) of the yttrium subgroup RE2S3 (Dy − Lu, Y) with hydrofluoric acid (concentration of 49%) was studied. Powders of RE2S3 compounds were obtained by the reaction between RE2O3 (Dy − Lu, Y) and Tb4O7 with a stream of H2S and CS2 in the 1000–1050 °C temperature range. The reaction between RE2S3 and HF was carried out in a glassy carbon crucible in the 21–25 °C temperature range in solution, and the precipitate was washed with H2O and dried at 90–100 °C. For the hydrates of RE fluorides with decreasing RE radius, the RE content increases the sorption of water for TbF3·0.5H2O; DyF3·0.5H2O; YF3·0.5H2O; HoF3·0.8H2O; and ErF3·0.9H2O. The powders of REF3·nH2O consisted of micro- and nano-sized particles containing the amorphous phase. Water loss occurs in the 50–180 °C temperature range and is accompanied by a natural increase in enthalpy: from 23.6 J/g for TbF3 · 0.5H2O to 97.8 J/g for ErF3·0.9H2O and from 51.1 J/g for (H3O)Tm3F10·1.7H2O to 64.5 J/g for (H3O)Lu3F10·0.9H2O. Exothermic effects of formation of polycrystalline phase REF3 were recorded in the 200–300 °C temperature range. The reaction of RE2S3 (Tm, Yb, Lu) powders with HF proceeds with the formation of the zeolite type compounds (H3O)Tm3F10·1.7H2O, (H3O)Yb3F10·1.0H2O and (H3O)Lu3F10·0.9H2O. Thermal dissociation occurs with gradual loss of water and HF to form RE fluorides with the β-YF3 structure as described by

Introduction

The unique electronic structure of rare earth elements (RE) leads to the appearance of compounds with different optical, electrical [[1], [2]] and magnetic [3] properties, which have attracted considerable interest from researchers in recent years. Fluorides of rare earth elements are widely used in many fields (optical telecommunications, lasers, new optoelectronic devices, diagnostics and biological markers) [[4], [5], [6], [7]]. In recent decades, a particularly extensive attention was devoted to rare earth fluorides (REF3) as luminescent materials [8]. Owing to the low energy of wave oscillations, the decrease in the radiating activity of doping substances in the electronic excitation state is minimal [[9], [10]]. As a consequence, a high-luminescence quantum yield can be achieved [5]. Currently, fluorides of rare earth elements are used or tested in optoelectronics, optical fibres and amplifiers, lasers, and medicine. In view of their chemical stability, materials based on REF3 could potentially be used as bioimaging fluorescent probes [[5], [8]].

Fluorides of rare earth elements La-Nd crystallize in the tysonite (LaF3) structure type (ST) (trigonal crystal system, space group P3¯c1). Morphotropics changed with decreasing ionic radius [[11], [12]]. For fluorides of Sm-Gd, dimorphism is typically observed with the low-temperature type β-YF3 (orthorhombic crystal system, space group Pnma) and high-temperature modifications of tysonite [[13], [14]]. The REF3 (Tb-Ho) retain the modification characteristic of β-YF3 up to their melting point, whereas for fluorides of Er-Lu, Y, in addition to the basic orthorhombic modification (β-YF3), the high-temperature structure with cubic α-YF3 cubic (space group P23) can be obtained [[15], [16]].

REF3 are obtained by chemical and physics-chemical methods. The most common and available is the method of precipitation from aqueous solutions, referred to as “soft chemistry” [[5], [17], [18]]. Methods of obtaining fluorides can be divided into hydrothermal [[19], [20], [21], [22]], micro-emulsion [23] and microwave [24] thermal decomposition [25] types. Synthesis of nanofluorides of RE is mainly realised by one of the following methods: pyrolysis of fluorine-containing precursors; hydrothermal synthesis; micro-emulsion method; solvo-thermal synthesis; and the sol-gel technique [[26], [27], [28]]. At elevated temperatures, RE fluorides participate in pyrohydrolysis reaction to form oxy-fluorides (REOF) [[29], [30]]. The preparation of REF3 of the cerium subgroup during the interaction of hydrofluoric acid with RE2S3 provides a yield of close to 100%, and does not contain rare-earth oxyfluoride impurities, because the formation of the H2S gas product shifts the equilibrium towards fluoride formation.

RE2S3 compounds exist in form of 4 basic modifications. RE2S3 compounds with RE = Ce-Dy have a low-temperature modification of the rhombic system of α-RE2S3 ST α-La2S3, sp.gr. Pnma and high-temperature cubic modification of γ-RE2S3 ST Th3P4, sp.gr. I43d. The δ-RE2S3 compounds (Re = Y, Ho, Er, Tm) have the monoclinic structure of ST δ-Ho2S3, sp.gr. P21/m. For ε-Yb2S3 and ε-Lu2S3, the hexagonal structure of ST α-Al2O3, sp.gr. R3c is found. In the literature, there is only one report on the extent of the RE2S3-xOx solid solutions, mainly for γ-RE2S3: γ-(Sm2S3 − Sm2S2.94O0.06) [31], γ-(Gd2S3 − Gd2S2.97O0.03) [32].

In the process of hydrothermal synthesis of fluorides of rare-earth elements (Er-Lu, Y), the interaction of lanthanide oxalates with hydrofluoric acid leads to the formation of compounds δ-(H3O)RE3F10·nH2O [33]. A compound with the (H3O+)Y3F10·nH2O structure was obtained as the second (secondary) phase by the interaction of a solution of yttrium nitrates and alkaline earth metal (strontium [34], barium [35]) with hydrofluoric acid (47%). The compound is crystallized in a cubic structure and consists of octahedral diamond [RE6F32]−14 blocks constructed from square REF8 anti-prisms [36]. The behaviour of water molecules and the cation-exchange properties are observed to be of the zeolite type [37]. Ionic radius of the atom RE is an important factor in the formation of stable fluoride compounds. The connection structure of diamond [38] is formed from rare earth elements rHo3+ (coordination number (CN) is 8) = 1.015 Å − rLu3+(CN8) = 0.977 Å, Y: ARE3F10·nH2O (A+ = K+, Rb+, NH4+, Cs+) [33], (C2N2H10)0.5RE3F10·nH2O [22], (C3N2H12)0.5RE3F10·nH2O [39].

In this paper, the nature of the interaction of sulphides of rare earth elements RE2S3 (Dy − Lu, Y) with hydrofluoric acid and the reaction products are studied, and their crystal chemical, physics-chemical characteristics, and thermal stability are considered.

Section snippets

Materials

We used 99.99 wt.% ultrapure RE2O3 and Tb4O7 (manufacturer Uralredmed, Verkhnyaya Pyshma, Russia), 99.9 wt.% pure HF and NH4SCN (manufactured by TEK Systems) and distilled water as our starting material without further purification.

Synthesis of RE2S3

Powders of RE sulphides were obtained by reacting powders of Tb4O7 and RE2O3 (Dy-Lu, Y) oxides with gaseous CS2 and H2S. The maximum mass of one batch does not exceed 7 g. The rate of supply of sulphiding gases is 20–25 ml/min [40]. The synthesis temperature is

Characteristics of the precursors RE2S3

The RE2S3 formation reaction proceeds through the dioxysulfide formation stage, in which the oxide is transformed into the sulphide according to: RE2O3 → RE2O2S → RE2S3. The structure of the RE2OS2 compositions (Sm-Yb, Y) is presented in previous works [[42], [43]]. The formation of the RE2OS2 compound as a co-product due to the interaction of oxides of RE with gaseous carbon disulphide and hydrogen sulphide was not detected. The impurity phase RE2O2S is identified by X-ray diffraction when its

Conclusions

The phase compositions of the products of the reactions of the RE2S3 (Tb-Lu, Y) compounds with an aqueous HF solution (49%) were established. The reactions were carried out at 21–25 °C, and the precipitate was decanted and dried at 90–100 °C. Rare earth element fluorides with the compositions TbF3·0·5H2O, DyF3·0·5H2O, YF3·0·5H2O, HoF3·0·8H2O, ErF3·0·9H2O were obtained. Upon heating, more than 2/3 of crystalline water passes into the gas phase in the 50–170 °C temperature range. This process is

Acknowledgements

The authors express their gratitude to Mrs. Sofia A. Basova for the preparation of this manuscript.

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