The Iron Sulfides Crystal Growth from the Halide Melts

Abstract

A new approach to a single crystals growth of the iron sulfide phases of definite structure and nonstoichiometry is developed and applied. This approach is based on the method of crystal growing from solution melts. This approach is based on the crystallization or recrystallization of iron sulfides from iron sulfide solutions in iron dihalide melts under fixed sulfur vapor pressure in the closed system in non-isothermal (two-temperature) conditions. It allows to regulate the composition and structure of the resulting iron sulphide. In particular, at a relatively low pressure (<0.4 atm), pyrrhotite with a trigonal 3T structure is synthesized. At higher pressure pyrite β-FeS₂ is grown. Reaction scheme for the formation of iron sulphides based on the reversible oxidation of sulfur by iron dihalide is proposed and substantiated. On the base of the {pyrite + marcasite} - mixture annealing under the melts of the deepest eutectic compositions of KCl - FeCl₂ and NaCl - KCl - FeCl₂ systems, the instability of the marcasite phase regarding the pyrite one (at least, for T ≥ 340°C) was shown.

Keywords:
iron sulfides; pyrite; pyrrhotite; iron halide; recrystallization

1. Introduction

The intermediate phases of Fe - S system are potentially promising materials in different areas of high-tech. Although the phases with stoichiometry similar to FeS composition (γ-pyrrhotite, α-pyrrhotite, troilite) are unattractive for Material Science, their nonstoichiometry-sensitive properties (magnetic and optical) may be used as indication markers for detection of valuable associated minerals in ores^1,2.

High hopes for practical use are associated with iron disulfide FeS₂ in pyrite phase, which is regarded as a promising material for solar energetics (E_g = 0.95 eV, absorption in the near-IR region)^3-6. In^5,6 it is noted that the regulation of pyrite composition within the homogeneity region can open great possibilities for optimizing its properties.

The lack of knowledge about the phase diagram of the Fe - S system is one of the reasons for poor reproducibility of the properties of pyrite-based materials. Whereas the high-temperature region (T > 680 °C) is studied well enough⁷, (Fig. 1), the relatively low-temperature (T < 680°C) regions of the phase diagram of the Fe - S system are debatable^8-10. It is not still clear whether marcasite and FeS₂ "hybrid" structures of pyrite and marcasite (pararammelsbergite type¹¹) are always metastable relative to pyrite with any values of T, p, x. There is another unclear question concerning the number of phases and structures that are present at relatively low temperatures near FeS compound at 0.46 ≤ x_S ≤ 0.56 (Fig. 1 and Fig.2). The reason for these problems is primarily related to the difficulty of achieving equilibrium states and the tendency of iron sulfides to retain their metastable states at relatively low temperatures. For this reason, many researchers prefer mineralogical findings of iron sulfides for which the relaxation time in nature may exceed by many orders the time of annealing in laboratory experiments^11,12. However, this approach does not guarantee obtaining reliable information on the phase diagram because the sample "annealing" pressure and temperature are not sufficiently known and the concentration of impurities in these minerals can be high.

Figure 1
Phase diagram of the Fe–S system (according to ref.⁷).

Figure 2
Low-temperature part of the Fe–S phase diagram (according to ref.¹⁰)

In view of the above, the purpose of our study was to investigate phase relations in the system Fe - S at moderate temperatures (330 - 680°C). The priority task necessary for achieving this purpose was to find a method of controlled synthesis of iron sulfide single crystals. Our approach to dealing with this particular problem is described in detail in the current work which opens a series of papers. The structural analysis and the analysis of phase transformations in the Fe - S system will be covered in the next study of this series.

2. Experimental

Crystallization from iron halide melts. In order to achieve our main goal, we elaborated a new way of synthesizing iron sulfide single crystals. Our way is a variation of widely used method of crystal growing from solution-melts. It is based on recrystallization of iron sulfides from the melts of iron (II) halides (FeX₂, X = Cl, Br, I) under controlled vapor pressure of sulfur. This is an important distinctive feature of the suggested approach as it allows controlling the composition and non-stoichiometry of the resultant products.

Let us note that the method of synthesis of metal sulfides from molten salts (FeCl₂, FeBr₂^13,14 or PbCl₂¹⁵) is described in the literature. However, the impossibility of controlling the vapor pressure of a volatile component (sulfur), when using the afore-mentioned method, led to crystallization of polycrystalline ingots that could often contain not only pyrite β-FeS₂ but also pyrrhotite Fe_1-xS¹³. In attempts to solve the main problem of this work, the synthesis of iron sulfides from melts was performed at lower temperatures, comparing to^13-15.

For crystallization from molten salts at temperatures lower than 670-680°C we also used the eutectic melts of KCl - FeCl₂ and NaCl - KCl - FeCl₂ systems as solvents. According to our assumption, the low rate of iron sulfides crystallization allows one to approach the close-to-equilibrium state. The lower limit of the selected temperature range (330°C) corresponded to the crystallization of NaCl - KCl - FeCl₂ eutectic melt. The upper one (690°C) matched the temperature of crystallization of iron sulfides from the FeBr₂ melt (iron (II) bromide has the highest melting point among the halide compounds under discussion).

Crystallization or recrystallization of the iron sulfides was carried out in a two-temperature closed system according to the following scheme. The reactor for synthesis is a cylindrical silica ampoule having the internal diameter of 16 - 18 mm and the length of 300 - 400 mm. The weights of pure sulfur (5 - 10 g) and anhydrous iron (II) halide (4 - 7 g) are introduced into a quartz boat. In the majority of the experiments the charge of pre-synthesized powdered mixture of Fe_1-xS and FeS₂ (0.3 - 0.5 g) is added to the boat too. Then the boat is placed at the end of the reactor. After evacuation and sealing, the reactor is placed in a horizontal two-zone furnace. When conducting an experiment, the higher temperature T₂ corresponds to the end of the ampoule with the mixture of the sulfides and the iron halide. The lower temperature T₁ corresponds to the opposite end where the liquid sulfur exists. The value of temperature T₁ determines the saturated vapor pressure of sulfur. Since all the phases of the Fe-S system are characterized by the incongruent sublimation, when only molecular species of sulfur are in equilibrium with the solid sulfides¹⁶, the total pressure p_S should determine both the structure and the nonstoichiometry of the grown iron sulfide crystals. The vapor pressure of sulfur was set in the range from 0.25 to 9.5 bar (360 ≤ T₁ ≤ 640°C).

We used three experimental modes. In the first one the charge of {Fe_1-xS + FeS₂}-mixture is not introduced into the system at all. In this case the crystallization of iron sulfides from the iron halide melts is related to the redox reaction (see below).

In the second and third modes the charge of initial {Fe_1-xS + FeS₂}-mixture is used. In the second mode the temperatures T₂ and T₁ remained steady from the beginning until the end of the experiment. The boat with the substances was held for 20 hours at a temperature ~15°C higher than the melting point of the iron (II) halide (T₂ = 685 - 700°C) to saturate that melt with the iron sulfide. Upon the completion of this heat treatment a number of fine FeS_y single crystals were obtained. In this case the crystal growth takes place at the expense of isothermal recrystallization: the mass transfer from the small crystals to the larger ones via the liquid phase.

In the experiments of the third type the saturation of the melt with iron sulfides and their subsequent crystallization was regulated by varying the temperature T₂. As in the previous (second) mode, the boat with the substances was held for 20 hours at a temperature of 685 - 700°C. Then gradually, within a few hours, the temperature T₂ was reduced to the value 10-15°C below the melting point of iron (II) halide (T_m = 670 - 685°C). The temperature T₁ and, consequently, the pressure of sulfur vapor remained fixed. After the complete crystallization the system was cooled in the off mode furnace. The cooling rate of the hot zone was about 10 K/min.

To isolate the crystallized iron sulfides from halogenides, the resulting heterogeneous mixture was treated with distilled water for leaching the highly soluble halides. The precipitate was successively washed by ethanol and toluene and then dried. During multiple repeated washes, a highly dispersed powder of the initial iron sulfides was almost completely separated from the well grown material.

Annealing experiments. To clarify the stability of marcasite relative to pyrite, a powder samples of pyrite and marcasite mixture were annealed in contact with eutectic KCl-FeCl₂ (38 mol. % FeCl₂, t_eut ≈ 350 °C,¹⁷) or NaCl - KCl - FeCl₂ (12 mol. % NaCl, 48 mol. % FeCl₂, t_eut = 305 ± 2°C¹⁸) melts. Since the reproducible synthesis of marcasite (α-FeS2) is complicated, in our experiments a natural mixture of pyrite and marcasite of the Nizhne-Koshelev hydrothermal deposit (Kamchatka Peninsula) was taken as the starting sample. The chloride mixture amount was such that under the experimental conditions the melt completely covered the FeS₂ powder, which was well wetted by the molten chlorides. After evacuation and sealing, the ampoule with substances was placed in an isothermal section of the furnace at a temperature of 340°C. Then the annealing was carried out. It was completed by cooling in the off mode furnace. The iron sulfides were separated from the chlorides according to the procedure described above.

X-ray phase analysis and electron microscopy. The samples were identified by the X-ray powder diffraction (XRD). The powder patterns were recorded on a Shimadzu XRD-7000 powder diffractometer using monochromatized CuK_α1-radiation. The data were obtained with a sampling rate of 0.05° (2Θ scale) with an exposure time of 6.0 s at the point. Model powder patterns for known structures were calculated according to the published data (PowderCell 2.4 program).

The obtained samples were also investigated by scanning electron microscopy (SEM) using a JEOL JSM-7001F device. For a number of single crystals, a quantitative analysis was carried out with the use of an S8-Tiger X-ray fluorescence analyzer.

3. Results and Discussion

Phase composition and phase transformations. As it was shown by the X-ray studies, the crystals grown from FeCl₂ and FeBr₂ melts at a vapor pressure of sulfur above 0.42 bar represent the only the phase of pyrite β-FeS₂ (Fig. 3). These crystals are characterized mainly by the combined habit of the cube and pentagonal dodecahedron (Fig. 4a). The growth steps are visible on some faces (Fig. 4b). The smoothest faces are formed at the sulfur vapor pressures up to 2 bar, and at the higher pressures the characteristic growth patterns appear on some faces apparently related to the emergence of dislocations (Fig. 4c). The experimental lower limit value of the sulfur vapor pressure (0.42 bar), above which the only phase of pyrite crystallizes at a temperature of 680°C, correlates with the data of^6,19 concerning the P-T dependency for the γ-Fe_1-xS - β-FeS₂ - V equilibrium: 0.39 bar for temperature of 680°C. (That value was calculated using the equation from the work⁶: ln[P/torr] = -40317/[T/K] + 48.000; the data of¹⁹ give practically the same result).

Figure 3
Powder pattern of the FeS_n samples grown at sulfur vapor pressure of 4 bar.

Figure 4
Surface images for the pyrite single crystals, grown by the iron sulfide recrystallization from FeBr₂ melts in a contact with sulfur vapor: P_tot.(Sx) = 1 bar, (a, b) and P_tot.(Sx) = 10 bar (c).

The lattice constant for the cubic pyrite structure (S.G. Pa3) exhibits weak sensitivity to the sulfur vapor pressure during the synthesis. The maximum value of the lattice constant is 0.54130±0.00010 nm and the minimum one is 0.54116±0.00001 nm. So, the pyrite lattice constants are somewhat smaller than it is usually published (for example, 0.547 nm¹¹).

The annealing of the pyrite-marcasite mixture with the eutectic KCl - FeCl₂ melt was carried out at 365, 400, 450 and 500°C for 36 hours. The annealing at the highest temperature (500°C) led to the complete transformation of marcasite into pyrite, the annealing at the lowest temperature (365°C) left the sample practically unchanged. At two intermediate temperature values, an apparent decrease of marcasite phase content in the sample was observed (Figs. 5 and 6). The calculated marcasite volume fractions in the annealed samples are given in Table 1.

Figure 5
Diffraction powder patterns (Cu-Kα1 radiation) of pyrite-marcasite mixtures (1 – initial native sample), which had 36-hours annealing under the KCl–FeCl₂ eutectic melts at the following temperatures: 2 – 365; 3 – 400; 4 – 450; 5 – 500 ºC; а – marcasite α-FeS₂, Pnnm) peaks; b – pyrite (β-FeS₂, Pa3) peaks; * – the notation for the silicates impurities. 6 – 8 – calculated powder pattern: 6 – marcasite α-FeS₂, 7 – pyrite β-FeS₂, 8 – pyrrhotite γ-Fe_1-xS.

Figure 6
The change in the relative intensity of the marcasite reflexes after the 36-hours annealing of pyrite-marcasite mixtures: 1 - 100; 2 - 120; 3 - to 211.

Table 1
Pyrite-phase volume fractions in the pyrite-marcasite mixtures after the 36 h - annealing of the native pyrite-marcasite samples under the KCl - FeCl₂ eutectic melt

tannealing, ºC	Pyrite volume fraction, %
Init. Sample	47.2
365	46.8
400	68.6
450	80.7
500	100.0

To examine the α-FeS₂ → β-FeS₂ transformation at low temperatures, an identical experiment was carried out at 340°C using a more fusible eutectic NaCl - KCl - FeCl₂ and a much longer annealing time (160 h). This experiment, according to X-ray data, led to the complete transformation of marcasite into pyrite (Fig. 5). Thus, metastability of marcasite relative to pyrite is decisively proven (at least for T ≥ 340°C).

In our opinion, the most interesting data were obtained for the samples grown from melts at low sulfur vapor pressures: 0.20 bar or less. In this case the phase of the stoichiometry similar to FeS (with an admixture of pyrite phase) was crystallized from the iron (II) halide melts. The XRD results showed that it is a trigonal phase (S.G. P3₁21) having the defect structure based on γ-Fe_1-xS (S.G. P6₃/mmc, structural type NiAs). This phase was characterized as a type of pyrrhotite-3T²⁰ having the lattice constants: a ∈ [0.68718; 0.68836] nm and c ∈ [1.70692; 1.71082] nm.

As the vapor pressure of sulfur increases, the lattice parameter of the trigonal pyrrhotite decreases. These results are correlated well with the well-known fact that the predominant defects in pyrrhotites are the vacancies in the iron sublattice: an increase in the concentration of these vacancies with an increase in the vapor pressure of sulfur should lead to a decrease in the values of a and c.

The reaction scheme of iron sulfides crystallization for the description of the equilibrium states and the heterophase equilibrium displacement. Taking into account a very noticeable spontaneous electrolytic ionization of the iron halogenides-based melts^21,22, we propose the following hypothesis. We assume that the basis for the formation of iron sulfides from halide melts under the described conditions is the reversible oxidation of liquid iron (II) halides reaction by the free sulfur to free halogens:

(1) $\frac{\mathit{n}}{2}{S}_2^{\left(\mathit{V}\right)}+2X^{-\left(\mathit{L}\right)}=S_{\mathit{n}}^{2-\left(\mathit{L}\right)}+X_2^{\left(\mathit{V}\right)}(X=C1,\mathrm{Br},I\mathrm{),}$

where V is the vapor phase; L is the melt; n = 1 or 2. The reduced species of sulfur (ions S₂^2- or S^2-), released in (1) are bounded by the iron ions(Fe²⁺) to the solid iron sulfide:

(2) $S_{\mathit{n}}^{2-\left(\mathit{L}\right)}+{\mathrm{Fe}}^{2+\left(\mathit{L}\right)}={\mathrm{Fe}}_{\mathrm{Fe}}+{\left(S_{\mathit{n}}\right)}_S,$

where the symbols Fe_Fe and (S_n)_S stand for iron and sulfur in the sublattices of these components in the crystals of pyrrhotite or pyrite. In addition to those above, the quasi-chemical reactions cause the specific defect formation in iron sulfides.

The equilibria (1) and (2) displacement with varying pressure and temperature can lead to the crystallization of iron sulfides or, conversely, to their dissolution in the FeX₂ melts. Moreover, varying the sulfur pressure, we can change the sulfur content in solid sulfides, i.e. - vary the phase composition and nonstoichiometry of these solids. Thus, let us introduce the K_P^# -value²³ for equation (1):

(3) ${\mathit{K}}_{\mathit{P}}^{\#}=\frac{{\mathit{p}}_{x_2}}{{\mathit{p}}_{S_2}};X=C1,\mathrm{Br},I$

The value of K_P^# relates the values of the partial pressures of sulfur and liberated halogen (X₂) vapors in the equation (1) and allows one to determine the value of the chemical potential of sulfur (µ_Sn) in the solid sulfide to within a term depending on the temperature (T), pressure (P) and composition of the liquid phase (x^(L))

(4) ${\mu }_{S\mathit{n}}^{\left(\mathit{S}\right)}=\mathit{RT}\mathit{ln}{\mathit{K}}_{\mathit{P}}^{\#}+\mathit{f}\left(\mathit{T},\mathit{P},{\mathit{x}}^{\left(\mathit{L}\right)}\right)23$

According to (4) it is easy to see that an increase in the sulfur pressure results in a decrease of the chemical potential of sulfur in the sulfide (µ_Sn) and in an increase of the sulfur content (x_S) in it.

Combining the equations (1) and (2) with the assumption of the strict stoichiometry for the pyrrhotite and pyrite phases and simplifying the subscription {Fe_Fe + (S_n)_S} to FeS and FeS₂ formulas, one can obtain equations (5) for n = 2 and (6) for n = 1.

(5) ${\mathrm{FeX}}_2^{\left(\mathit{L}\right)}+S_2^{\left(\mathit{V}\right)}={\mathrm{FeS}}_2^{\left(\mathit{S}\right)}+X_2^{\left(\mathit{V}\right)}(X=C1,\mathrm{Br},I)$

(6) ${\mathrm{FeX}}_2^{\left(\mathit{L}\right)}+\frac{1}{2}{S}_2^{\left(\mathit{V}\right)}={\mathrm{FeS}}^{\left(\mathit{S}\right)}+X_2^{\left(\mathit{V}\right)}(X=C1,\mathrm{Br},I)$

Estimated thermodynamic calculations performed using the data of²⁴ show that for the reactions the enthalpy value (ΔH°) for the equations (5) and (6) must be positive. This means that a decrease in the temperature T₂ should lead to a displacement of the equilibria (5) and (6) to the right and to the crystallization of the iron sulfide of a certain stoichiometry. It is also obvious that an increase in the sulfur vapor pressure should lead to a similar result. The structure of the obtained solid, as well as its composition, should depend both on the temperature of the melt (T₂) and on the sulfur vapor pressure that is set by the cold zone temperature (T₁).

The hypothesis of a significant contribution of the equilibrium (1) to the formation of iron sulfides from iron (II) halides required verification, since it is difficult imagine elemental sulfur oxidizing chlorides and bromides to elemental halogens at any their appreciable concentrations. During such verification, the proposed crystallization mechanism was confirmed by the following experimental results:

1. Pyrite precipitation from the liquid iron (II) bromide during the reaction with the sulfur vapor (see above, the first mode of the crystallization procedure). In case of FeBr₂ and FeI₂ melts the iron sulfides crystal growing can even be achieved without addition of initial FeS_n-charge. Thus, the crystallization of a pure pyrite phase β-FeS₂ was observed under the conditions when the sulfur vapor pressure in an ampoule was set constant (4 atm, which corresponds to T₁ = 450°C), and the FeBr₂ melt was kept for several hours at 680°C. The data from this experiment - the known volume of the ampoule (180 ml) and the mass of the precipitated pyrite (0.3001 g) - make it possible to roughly estimate the K_P^# value at an average temperature of the hot zone of 680°C (for K_P^# see the equations 3 and 4). To approximate K_P^# for X = Br, the required partial vapor pressure of bromine vapor was determined from the ideal gas equation, taking into account the identity n_Br2^(V) = n_FeS2 and the average temperature between T₂ and T₁. The resulting value of K_P^# ≈ 5.10^-3 appears to be somewhat overestimated, since calculations did not take into account the possible solubility of bromine in the hot melt of sulfur, as well as the partial binding of bromine to iron tribromide.

2. Practically irreversible iron sulfides crystallization during the interaction of sulfur vapors with iron (II) iodide melts. During the interaction of the FeI₂ melt with sulfur vapors, iodine vapor was always released. This was determined by the characteristic vapor colour easily distinguishable even against the background of coloured sulfur vapor.

The blackening of the initially red-brown sulfur melt was also observed for the reason of the high solubility of molecular iodine in liquid sulfur. At the same time, the iron sulfides crystallized: at T₁≤400 °C it was a pure pyrite phase, and at T₁ ≤ 300 °C it was a mixture of pyrite and trigonal pyrrhotite 3T-Fe_1-xS. Such crystallization took place even under constant temperature conditions and resulted in complete conversion of the FeI₂ melt into the 3T-Fe_1-xS+ FeS₂ or β-FeS₂ (pyrite) phases.

However, at this stage the practical use of the FeI₂-melts for the crystal growth of iron sulfides of certain composition seems to be doubtful because liberated iodine has a high solubility in liquid sulfur. Indeed, to maintain the vapor pressure of sulfur (P_tot.Sx) constant, one should change the temperature T₁ over the course of experiment, because if the iodine is present in liquid sulfur, then the sulfur vapor pressure value becomes a function of both the temperature and the concentration: P_tot.Sx = f(T₁,x_I2). Moreover, the iodine concentration in the liquid sulfur (x_I2) should be changed with iodine liberation in the gas phase.

3. Oxidizing properties of sulfur condensate that was obtained after recrystallization experiments from the bromide and chloride melts. After the experiments on the recrystallization of iron sulfides from the FeBr₂ and FeCl₂ melts, the excess sulfur was condensed in the free end of the reactor. The removed sulfur was powdered and treated with a concentrated aqueous solution of freshly prepared ferric chloride (II). Then the Fe(III) appearance was observed in the solution (for example with a thiocyanate test). It should be noted that the pure powdered sulfur does not react with the iron (II) salts solutions.

Iron trichlorides and tribromides could be formed according to the reaction (6). Free halogen (Cl₂, Br₂) liberated in Eq. (1), can be partially bonded to volatile iron trihalide:

(6) ${\mathrm{FeX}}_2^{\left(\mathit{L}\right)}+\frac{1}{2}{X}_2^{\left(\mathit{V}\right)}={\mathrm{FeX}}_3^{\left(\mathit{V}\right)}\left(X=C1,\mathrm{Br}\right)$

These volatile species can be condensed in the cold zone and then Fe (III) compounds can be found in aqueous solutions as after the water treatment.

We would like to point out that the proposed scheme (equations 1 and 2) is aimed at the thermodynamic description of the system. First of all, this scheme is intended to show the possibility of growing the crystals of the very sulfide (Fe_1-xS or FeS₂) when we change the pressure of sulfur even if the initial charge of {Fe_1-xS or FeS₂} is absent. At this point we cannot assert that the role of these equations is kinetically significant.

4. Conclusions

Thus, we can consider proven the assumption about an essential contribution of equilibria (1) and (2) to the formation of iron sulfides according to the procedure described in this paper. It should be noted that the possibility of oxidizing halides (Cl^-1; Br^-1) with sulfur (S⁰) was proved both experimentally^25,26 and in thermodynamic calculations²⁶.

The direction of the iron mass transfer - the iron insertion into the growing sulphide phase or its extraction by the halide melt - is determined by the thermodynamic parameters of the experiment (temperature, sulfur vapor pressure, the composition of the melt). This fact suggests that the equilibria considered here are close to selective chemical vapor transport (SCVT). We described SCVT reactions in works^27-29. A distinctive feature of the transport transformations considered in this paper is that these transformations occur with the participation of the liquid phase (molten salts). The low diffusion rates in the liquid (compared to the velocities in the vapor) lead to low rates of formation of the solid phases. In some cases this provides a clear advantage since it makes it possible to perform the crystal growth in a quasistatic regime, obtaining practically equilibrium states. Last but not least, in case of FeBr₂ and FeI₂ melts the iron sulfides crystal growing can even be achieved without addition of initial {Fe_1-xS + FeS₂}-charge.

Let us go back to the experimental proof of the metastability of marcasite with respect to pyrite. In our opinion, the role of the molten iron halides in this annealing experiment is to reduce the kinetic difficulties in the iron transfer between the competing phases of pyrite and marcasite. (Difficulties in the sulfur transfer should be affected much less because of the appreciable saturated sulfur vapor pressure over iron disulphide). As a result, crystals of a more stable phase are allowed to grow by dissolving a less stable phase. Without the presence of a transporting agent, the component transport from one phase to another must have very low speeds; then a phase transformation cannot be observed.

5. Summary

1. A procedure of synthesis of the iron sulphide single-crystals having a given structure and composition is developed and applied. The technique is based on interaction of iron halide melts with sulfur vapors in a closed non-isothermal system at varying pressures of these vapors and allows to regulate the composition and structure of the resulting iron sulphide. In particular, at a relatively low pressure (<0.4 atm), pyrrhotite with a trigonal 3T structure is synthesized. At higher pressure pyrite β-FeS₂ is grown.

2. Reaction routes for the formation of iron sulphides based on the reversible oxidation of sulfur by iron dihalide are proposed and substantiated.

3. On the base of the {pyrite + marcasite} - mixture annealing under the melts of the deepest eutectic compositions of KCl - FeCl₂ and NaCl - KCl - FeCl₂ systems, the instability of the marcasite phase regarding the pyrite one (at least, for T ≥ 340°C) was shown.

6. Acknowledgements

The authors are grateful for the helpful comments which were received from Dr. James McKee and Ms. Marina Berezina, Max-Planck-Institute for Radio Astronomy, Bonn, Germany.

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Publication Dates

• Publication in this collection
  2018

History

• Received
  13 July 2017
• Reviewed
  09 Mar 2018
• Accepted
  26 Mar 2018