Abstract
Full Text
UDC 548.55+546.682′765
CRYSTALLOGRAPHY
L. Yu. KHARCHENKO, P. V. KLEVTSOV, T. M. POLYANSKAYA
SYNTHESIS AND CRYSTALLOGRAPHIC STUDY OF OXYTUNGSTATE CHLORIDES OF COMPOSITION
$\mathrm{Ln_3WO_6Cl_3}$ ($\mathrm{Ln}=\mathrm{Ce},\ \mathrm{Pr},\ \mathrm{Nd}$)
(Presented by Academician N. V. Belov, May 20, 1969)
A study of the conditions for the hydrothermal synthesis of crystals of alkali–rare-earth tungstates and rare-earth oxytungstates, carried out by us in aqueous solutions of alkali-metal and ammonium chlorides, as well as a detailed study of synthesis in certain chloride systems containing praseodymium and tungsten oxides ($^1$), led to the preparation of a new group of compounds, which, in addition to rare-earth elements and tungsten, contain chlorine anions. At present, two types of crystalline tungstate chlorides can already be distinguished in this group:
- $\mathrm{LnWO_4Cl}$ for La, Ce, Pr, and Nd.
- $\mathrm{Ln_3WO_6Cl}$ ($\mathrm{Ln_2WO_6\cdot LnCl_3}$) for Ce, Pr, and Nd.
The first type of these compounds was described by us in paper ($^2$). The present communication is devoted to compounds of composition $\mathrm{Ln_3WO_6Cl_3}$.
Experiments on hydrothermal crystallization were carried out in standard stainless-steel autoclaves with self-sealing closures. Titanium liners were used as reaction vessels. The charge was loaded in the form of mixtures $\mathrm{Ln_2O_3:WO_3}=1:1,\ 2:1,\ 3:1$ (molar ratios) or their sinters. The charge : solvent ratio was 1 : 5 and 1 : 10 (weight ratios).
Compounds $\mathrm{Ln_2WO_6Cl_3}$ for praseodymium and neodymium are formed in 5% ammonium chloride and in mixed solutions of 20% LiCl + 10% NH$_4$Cl and 20% KCl + 5% NH$_4$Cl over a wide temperature range: 500–600° in the first two cases and 450–600° in the last (the filling of the autoclaves, depending on temperature, varied from 70 to 40%). In addition, oxytungstate chlorides for cerium and neodymium were obtained in solutions of alkaline-earth-metal chlorides (20–35% MgCl$_2$ and 20% CaCl$_2$) at a temperature of 550° and an autoclave filling of 60%.
Experiments carried out on crystallization of these compounds from solution in a melt showed that oxytungstate chlorides can crystallize not only in closed aqueous systems at elevated temperatures and pressures, but also at atmospheric pressure and in the absence of water. Anhydrous lithium chloride was used as the solvent in this case,
Table 1
| Face | +x | +y | +u | +z | Number of faces | $hkil$ | Growth form |
|---|---|---|---|---|---|---|---|
| 1 | 30 | 90 | 150 | 90 | 6 | $10\bar{1}0$ | Hexagonal prism |
| 2 | 0 | 120 | 120 | 90 | 6 | $2\bar{1}\bar{1}0$ | » » |
| 3 | 61 | 90 | 119 | 33 | 12 | $10\bar{1}1$ | Hexagonal dipyramid |
The charge consisted of melts of medium tungstates of composition $\mathrm{Ln}_2(\mathrm{WO}_4)_3$, where $\mathrm{Ln}=\mathrm{Pr}, \mathrm{Nd}$. The maximum temperature, at which the experiment was held for about 10 h, was $800^\circ$; the cooling rate was $3^\circ$ per hour in the interval $800$–$600^\circ$ and below this $10^\circ$ per hour. The charge : solvent ratio in molar fractions was $\sim 1:50$.
Single crystals of $\mathrm{Ln}_3\mathrm{WO}_6\mathrm{Cl}_3$ have the form either of elongated hexagonal prisms or of thin hexagonal plates. The size of the single crystals is up to 1–2 mm. More often, the oxywolframate chlorides crystallize as intergrowths of needle-prismatic crystals or plates, the size of the intergrowths being 2–5 mm. Optical goniometric measurements of the single crystals showed that they belong to the class $L_6PC$. The growth forms of $\mathrm{Pr}_3\mathrm{WO}_6\mathrm{Cl}_3$ crystals are given in Table 1. The most strongly developed faces are those of the hexagonal prism $\{10\bar{1}0\}$. The ratio of the unit-cell parameters is $c/a=0.57$.
Fig. 1. Heating curves of differential thermal and thermogravimetric analysis of $\mathrm{Nd}_3\mathrm{WO}_6\mathrm{Cl}_3$ crystals
The chemical formula of the compound $\mathrm{Ln}_3\mathrm{WO}_6\mathrm{Cl}_3$ was established on the basis of chemical analysis and determination of its crystal structure (3). Tungsten, rare-earth element, and chlorine were found in the compound. Results of analysis of neodymium oxywolframate chloride: Nd 51.9% (calculated 52.7%), W 23.4% (calculated 22.5%), Cl 12.3% (calculated 13.0%). Quantitative analysis for alkali metals established that they do not enter the compound. According to IR spectroscopy data, the compound contains no water.
From the Debye patterns the isostructural character of the compounds $\mathrm{Ln}_3\mathrm{WO}_6\mathrm{Cl}_3$ for cerium, praseodymium, and neodymium was established. Table 2 gives the results of calculation of the powder X-ray pattern for $\mathrm{Pr}_3\mathrm{WO}_6\mathrm{Cl}_3$, recorded on a URS-50 diffractometer with Cu $K_\alpha$ radiation. The unit-cell parameters of this compound, obtained from oscillation and rotation X-ray patterns and refined on a computer from the powder diffractogram data according to program (4), are $a=9.314$, $c=5.369$ Å.
The character of the displacement of lines on the powder diffractograms of the investigated compounds $\mathrm{Ln}_3\mathrm{WO}_6\mathrm{Cl}_3$ indicates an increase in the unit-cell parameters—
Table 2
X-ray diffraction data for $\mathrm{Pr}_3\mathrm{WO}_6\mathrm{Cl}_3$
| $hkl$ | $d$, Å | $I/I_0$ | $hkl$ | $d$, Å | $I/I_0$ | $hkl$ | $d$, Å | $I/I_0$ |
|---|---|---|---|---|---|---|---|---|
| 100 | 8.10 | 25 | 400} | 2.015 | 40 | 213 | 1.542 | 15 |
| 110 | 4.61 | 4 | 212} | 2.015 | 40 | 420 | 1.522 | |
| 101 | 4.46 | 5 | 302} | 1.896 | 16 | 322 | 5 | |
| 200 | 4.05 | 10 | 401} | 1.896 | 16 | 303 | 1.488 | 4 |
| 111 | 3.524 | 40 | 230 | 1.848 | 11 | 412 | 1.468 | 12 |
| 201 | 3.230 | 43 | 410} | 1.758 | 27 | 421 | 1.465 | 13 |
| 210 | 3.050 | 39 | 222} | 1.758 | 27 | 510 | 1.446 | 7 |
| 300} | 2.683 | 38 | 231} | 1.758 | 27 | 511} | 1.393 | 11 |
| 002} | 2.683 | 38 | 103 | 1.743 | 33 | 313} | 1.393 | 11 |
| 211 | 2.645 | 100 | 312 | 1.713 | 7 | 004} | 1.339 | 4 |
| 301 | 2.403 | 4 | 113 | 1.669 | 8 | 403} | 1.339 | 4 |
| 310 | 2.232 | 20 | 203 | 1.635 | 8 | 422} | 1.322 | 4 |
| 221 | 2.136 | 4 | 500} | 1.604 | 7 | 104} | 1.322 | 4 |
| 311 | 2.059 | 5 | 402} | 1.604 | 7 |
of the unit cell in the series from Nd to Cl, in accordance with the increase in the ionic radius of $\mathrm{Ln}^{3+}$.
The behavior of the compounds $\mathrm{Ln}_3\mathrm{WO}_6\mathrm{Cl}_3$ upon heating in air was studied on a derivatograph. It was shown that they are rather stable substances, unlike $\mathrm{LnWO}_4\mathrm{Cl}$: their decomposition begins only at $1000^\circ$ (whereas $\mathrm{LnWO}_4\mathrm{Cl}$ begins at $570^\circ$) and proceeds rather slowly; moreover, on the thermal curve the effect is very weak and is detected mainly by analogy with the weight-loss curve (Fig. 1). Complete decomposition of the compound is achieved as a result of calcining it for 5 h at $1100^\circ$. The proposed decomposition scheme for the compounds
\[ \mathrm{Nd}_3\mathrm{WO}_6\mathrm{Cl}_3 + {}^3/_4\mathrm{O}_2 \rightarrow \mathrm{Nd}_2\mathrm{WO}_6 + {}^1/_2\mathrm{Nd}_2\mathrm{O}_3 + {}^3/_2\mathrm{Cl}_2 \uparrow \]
is confirmed by X-ray diffraction data for the substance after calcination at $1100^\circ$: all lines in the diffraction pattern belong to $\mathrm{Nd}_2\mathrm{WO}_6$ (the predominant phase) and $\mathrm{Nd}_2\mathrm{O}_3$. The weight loss calculated from the reaction upon calcination is 10.1%; experimentally, after 5 h of calcination, 9.9% was obtained.
Thus, it may be considered that the two rare-earth oxywolframate chlorides indicated above are derivatives of $1:2$ oxywolframate $\mathrm{Ln}_2\mathrm{W}_2\mathrm{O}_9$ ($\mathrm{Ln}, \mathrm{WO}_4\mathrm{Cl}$) and $1:1$ oxywolframate $\mathrm{Ln}_2\mathrm{WO}_6 \cdot (\mathrm{Ln}_3\mathrm{WO}_6\mathrm{Cl}_3)$.
Institute of Inorganic Chemistry
Siberian Branch of the Academy of Sciences of the USSR
Novosibirsk
Received
19 V 1969
CITED LITERATURE
- L. Yu. Kharchenko, P. V. Klevtsov, Kristallografiya, 14, No. 5 (1969).
- L. Yu. Kharchenko, P. V. Klevtsov, L. P. Solov’eva, DAN, 176, 826 (1967).
- T. M. Polyanskaya, S. V. Borisov, N. V. Belov, DAN, 187, No. 5 (1969).
- F. A. Brusen’ev, A. N. Rebenko, ZhSKh, 7, 136 (1966).