Boyd R. Davis, Michael S. Moats, Shijie Wang, Dean Gregurek, Joël Kapusta, Thomas P. Battle, Mark E. Schlesinger, Gerardo Raul Alvear Flores, Evgueni Jak, Graeme Goodall, Michael L. Free, Edouard Asselin, Alexandre Chagnes, David Dreisinger, Matthew Jeffrey, Jaeheon Lee, Graeme Miller, Jochen Petersen, Virginia S. T. Ciminelli, Qian Xu, Ronald Molnar, Jeff Adams, Wenying Liu, Niels Verbaan, John Goode, Ian M. London, Gisele Azimi, Alex Forstner, Ronel Kappes and Tarun Bhambhani (eds.)Extraction 2018The Minerals, Metals & Materials Serieshttps://doi.org/10.1007/978-3-319-95022-8_25
Fundamental Process Equilibria of Base and Trace Elements in the DON Smelting of Various Nickel Concentrates
Pekka Taskinen1, Katri Avarmaa1, Hannu Johto2 and Petri Latostenmaa3
(1)
Department Chemical Engineering and Metallurgy, School of Chemical Engineering, Aalto University, P.O. Box 16100, 00076 Aalto, Finland
(2)
Outotec Research, Kuparitie 10, 28101 Pori, Finland
(3)
Boliden Harjavalta, Teollisuuskatu 1, 29200 Harjavalta, Finland
The converter-less nickel matte
smelting
technology (DON) adopted more than 20 years ago in Boliden Harjavalta smelter has been since that applied successfully to the processing of large number of nickel
sulphide concentrates of various Ni-to-Cu ratios and MgO contents. The operational point of the technology is far from the conventional primary nickel smelting
in the smelting
-converting route. Therefore, a careful scouting of distribution
equilibria
of the base and trace elements in the smelting
conditions of DON process has been conducted, in order to obtain quantitative information about the equilibria
and thermodynamic properties of the nickel
mattes at low iron
concentrations, less than 10 wt% [Fe] in matte. The series of investigations has included novel experimental
and analytical techniques for increasing the reliability and sensitivity of the phase equilibria
as well as the element distribution
observations carried out in typical high-grade nickel matte
smelting
conditions.
Keywords
Nickel matteIron silicateMagnesiaPrecious metalsPlatinum group metals
Introduction
An access to high-MgO raw materials for nickel smelting
directed Outokumpu in the late 1980s to development of a new primary smelting
technology for nickel matte
, based on the flash smelting
concept. The fundamental novel idea was the expansion
of slag
volume generated in the smelting
step, by oxidation
the feed mixture to much lower iron
concentrations in the produced matte than the conventional practice [1]. This involved a new flow sheet, closing internal circulation of the slag
and matte between the converting and slag
cleaning thus improving the metal value recoveries, in particular that of cobalt
, and lowering environmental impact
of the nickel matte
smelting
. The elimination of converters and the entire converting step had several side effects to the industrial operation, including e.g. lower fugitive emissions and smaller CAPEX [2]. It also required modifications in the refinery flow sheet [3]. The current operational practices will be described elsewhere in this Conference [4].
Fundamentals of nickel smelting
are much less scrutinised than those of copper smelting
[2–5]. In 1995 only limited information existed, about the fundamentals of matte-slag
equilibria
, when the direct nickel matte
smelting
was taken into industrial use, and the data on properties of trace elements at low iron
concentrations in the matte below 15 wt% Fe were non-existent. In high-iron
mattes, the previous focus had been in nickel
losses to slag
and recoveries of selected trace elements, typically cobalt
[6].
The knowledge in early ‘90 s upon nickel
mattes in the converting was largely based on a review
of Kellogg [7] and the prior experimental
data. Font et al. [8] and Henao et al. [9] presented new experimental
data on the slag
-matte-gas equilibria
in MgO crucibles and about selected trace elements. The scope was in conventional matte making and its conditions. Certain details on trace elements in nickel matte
converting related to platinum
group element distributions were studied [10]. For helping to understand the coupled phenomena in converting, process dynamics modelling has also been used [11, 12].
This presentation gives an overview on the recent studies of the slag
-matte equilibria
carried out with a novel experimental
technique, allowing accurate observations about phase equilibria
, their assays and the distributions of minority elements deporting them between matte to be recovered and slag
where many elements will be discarded at low concentrations to various slag
products.
Experimental
The experimental
technique was based on gas equilibration of small matte-slag
samples on a solid substrate in flowing CO
-CO2-SO2-Ar mixtures of controlled compositions. The experimental
conditions were selected so that sulphur dioxide pressure in the furnace
in all conditions was P(SO2) = 0.1 atm. This was a modification of a technique used earlier in many geochemical applications [13], and adopted by Jak et al. [14] for metallurgical slags and slag
-metal equilibria
. The experimental
set up as well as the techniques used for confirming the state of equilibrium reached in the experiments of this work have been presented earlier in detail in the literature [15–17].
The experimental
breakthrough in the analytical techniques for the trace elements was the use of laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) directly from the polished sections, without separating the different phases of samples prior to the phase composition analyses. Combined with the electron microprobe X-ray analysis (EPMA) it allowed accurate chemical analyses in the whole range from several wt% to sub-ppm concentrations. The technique used also involved a statistical evaluation of the composition of each phase so that 8–10 points were measured on well-quenched domains of the sample and in addition to the average composition, its standard deviation will also be reported [15]. Those were the first metallurgical slag
samples analysed with LA-ICP-MS technique and a lot of effort was put on the possible systematic errors arising from samples, from different composition domains than the geological specimens studied earlier [18].
An indication of the consistence of the two direct analytical methods is the good agreement for such elements present at concentrations above the detection limits of both the methods. An example is shown in Fig. 1 where cobalt
concentrations of various iron silicate
slags by LA-ICP-MS and EPMA are plotted as a function of iron
concentration in the nickel matte
at 1350–1450 °C. The agreement between two independent techniques is good, and the obtained standard deviation of the results is ± 0.01 wt% between the different techniques.
The experimental
series consisted of equilibration experiments at 1350–1450 °C for gas-matte-slag
samples in fused quartz
crucibles and with constant Ni-Cu ratios of 0, 2:1 and 4:1 (w/w). The studied sulphide mattes were synthetised in situ in the equilibration furnace
from pure Cu2S, FeS and Ni3S2 powders. They initially contained 1 wt% of each trace element which were distributed between the slag
, matte and gas phases during the high-temperature
equilibration period. The main process between the gas, iron silicate
slag
and nickel
-copper matte was the adjustment of iron
distribution
by two independent system variables, based on the overall reaction (1):
(1)
Thus, the prevailing sulphur and oxygen pressures as independent variables define the distribution
of iron
between the nickel matte
and slag
, as well as ‘the matte grade’ defined in this study as iron
concentration of the sulphide matte. As a parallel reaction within the slag
, iron
oxides distribute between the oxidation
stages as
(2)
but the advancement of reaction (2) was not considered experimentally, as EPMA is sensitive to the elements only and no information about their oxidation
states can be obtained.
Results
The slag
assay in matte-slag
equilibrium at silica
saturation was examined as a function of the matte grade and magnesia
concentration. The EPMA results of iron
concentrations at 1400 °C from 3 to 12 wt% are plotted on an isothermal constrained Gibbs triangle FeOx-MgO-SiO2 in P(O2) = 0.01 Pa in Fig. 2. The oxygen pressure range in the two mattes with [Ni]:[Cu] = 2 and 4 (w/w) had no major impact to the silica
saturation boundary, as can be seen in the graph. It shows about 1 wt% higher silica
solubility
in contact with matte than the assessed copper
- and nickel
-free iron silicate
slag
system in the Mtox database [19] used in the calculations.
The experimental
liquidus
composition data allow also estimation of the temperature
dependency for the silica
saturation boundary at fixed magnesia
concentrations, Fig. 3. The used magnesia
concentrations in the two experimental
series with [Ni]:[Cu] = 4 and 2 (w/w) are not completely overlapping, in particular at the highest MgO concentration. The experimental
technique used and the small differences sin the initial MgO compositions causes the recognisable scatter in the liquidus
line projection shown in Fig. 3.
The solubility
of sulphur in the slag
was studied as a function of temperature
, iron
concentration of matte and MgO concentration of the slag
. MgO concentration of the slag
has a clear effect on the sulphur solubility
, as can be seen in Fig. 4. It is clearly also equally affected by the iron
concentration of the matte in a fixed atmospheric point, which also reveals the activity of iron
in the system. This indicates that the nickel
-to-copper ratio has relatively small impact to the iron
activity of matte in the current composition range.
The distribution
coefficient of a component Me was defined in this study as ratio of its concentration in the nickel matte
divided by that in the slag
, i.e.
(3)
The above referred fact that iron
activity in nickel
-copper-iron sulphide mattes at constant iron
concentration is not strongly a function of the [Ni]:[Cu] -ratio is also seen in the behaviour of the distribution
coefficient of iron
at low iron
concentrations, Fig. 5. Magnesia
concentration of slag
, affecting the iron
activity of the slag
in each oxygen pressure [17] and thus the matte composition in each equilibrium condition has been used as parameter in Fig. 5. The de-ironisation of nickel
mattes proceeds thus in a similar way from mattes with a high and low copper
concentration, over a wide range of [Ni]:[Cu] ratios, down to 2–3 wt% iron
. The removal
of iron
from the nickel
-copper mattes occurs at high iron
concentrations essentially without major slagging of copper
or nickel
, and independently of the copper
concentration of the matte, as scrutinised in industrial converter blows already by Browne [20].
The thermodynamic properties of nickel
and copper
in the matte vary when it is de-ironised in the smelting
, and, as a consequence, when the Ni-Cu ratio of the feed mixture of the smelter fluctuates along with time. This causes changes in their matte-to-slag
distribution
coefficients. That feature at 1400 °C is demonstrated in Fig. 6a and b for nickel
and copper
at (MgO) = 0, and in Fig. 7a, and b for nickel
, at three magnesia
concentrations of the slag
.
MgO additions to the slag
favour the distribution
of copper
and nickel
to the sulphide matte. The effect is small but clear in all studied concentrations of magnesia
. The distribution
coefficient is affected slightly also by the used boundary condition of this study, when (Fe):(SiO2)
ratio of the slag
decreases with increasing MgO, as pointed out earlier, e.g., by Takeda [21] and Strengell et al. [16].
As suggested earlier (e.g., Teague et al. [6]) the reason of more favourable distributions between matte/metal and slag
is the increase of the activity coefficient of less basic oxides, by formation of stronger MgO-SiO2 bonds in the slag
when magnesia
is added.
The distribution
coefficients of the trace elements cobalt
and gold
between the nickel
-copper mattes as a function of its iron
concentration and slag
are shown in Figs. 9 and 10, respectively. The nickel
-to-copper ratio of nickel
sulphide matte in these studies was [Ni]:[Cu] = 4 (w/w). As can be concluded from Fig. 10, the solubility
of palladium
from the nickel
mattes containing 1 wt% Pd in the iron silicate
slag
is very low (< 1 ppm).
MgO clearly affects low concentrations of cobalt
in iron silicate
slags when upper iron
concentration range of this study is concerned, see Fig. 8. Below ≈ 3 wt% iron
in the matte, the impact of magnesia
cannot be found any more. The MgO-free data obtained are in good agreement with Toscano and Utigard [22].
The PGM and PM distributions measured in copper
(Cu-Fe) and nickel
(Cu-Ni-Fe) matte-metal equilibria
suggest that nickel
mattes are more favourable collectors of precious and platinum group metals
than copper
mattes, as shown in Fig. 9. Nevertheless, the obtained distribution
coefficients in both the cases are very high.
The presence of basic oxides in the slag
affects the distributions of the precious and platinum group metals
very much. As Fig. 10 indicates, the impact of MgO on the distribution
coefficient of gold
is about factor of 5 larger when its concentration in silica
saturated iron silicate
slag
is increased from 0 to about 8 wt% (MgO). We did observe a similar trend in the distribution
behaviours of palladium
and platinum
, as well [17]. Also here, increasing silica
concentration of the iron silicate
slag
has a positive influence on the distributions [21].
Conclusions
Due to the absence of data on nickel
-copper-iron mattes in low iron
concentrations, below 15 wt% [Fe] and in the operational window of DON process, an experimental
program was carried out for measuring base metal and trace element distributions. The variables used were iron
concentration of the matte, its nickel
-to-copper ratio, magnesia
concentration of the slag
and temperature
. Magnesia
of the slag
in these conditions, in a fixed atmosphere, has a clear impact to iron
concentration of matte, as a feedback from iron
activity of the slag
[17].
The common substance in nickel
sulphide concentrates’ gangue, MgO [24, 25], improves favourably recoveries of the base metals to the sulphide matte. A particularly large impact of MgO was found to be on those elements, which are weak oxide formers, as typically the precious and some platinum group metals
.
A comparison of the current observations at silica
saturation with the computational phase diagram Fe-O-MgO-SiO2 based on Mtox database [19] indicates a good agreement. This suggests that the assessed data of Mtox database reproduces reliable phase property data for the industrial nickel matte
smelting
slags in DON smelting
conditions in the flash smelting
furnace
(FSF) [26].
Font et al. [8] presented distribution
data for selected trace elements in MgO crucibles at 1300 °C (i.e. in olivine saturation). They compared their observations as a function of P(SO2), with mattes of different [Ni]:[Cu] ratios and iron
concentrations, including the limiting ‘binary’ matte systems Cu2S-FeS and Ni3S2-FeS. Their results indicate the effects of prevailing P(SO2) on the dissolution of the base metals into iron silicate
slags. The impact of MgO on the distributions is not visible, due to olivine saturation where silica
concentration of the slag
still is a free variable, as indicated in Fig. 1, and was less accurately controlled in those experiments.
As atmospheric SO2(g) links together the sulphur and oxygen pressures in the equilibrium systems. The high-SO2 environments thus represent higher oxygen pressures in a fixed matte composition, according to reaction
(4)
where sulphur pressures in the slag
-matte equilibria
are controlled by the matte and its assay. Therefore, in the environments of flash smelting
, when slag
and matte are formed below the reaction shaft, on the FSF settler bath surface, from the oxidation
products the settler reactions generate essentially pure sulphur dioxide gas and the local prevailing P(SO2) ≈ 1 atm [23]. This is also the universal boundary condition for the sulphide matte and slag
forming reaction process in the flash smelting
furnace
settlers, independently of the oxygen enrichment.
The results by Font et al. [8] imply that the matte-slag
distribution
coefficients for As and Sb increase when iron
concentration of copper
-nickel matte
decrease, and the highest values for As, Bi and Sb were always obtained in copper
-free mattes. This pattern, based on the present experimental
observations, is more complicated if the effect of magnesia
on the slag
assay and its silica
will be taken into account. There seems to be no data concerning the non-saturated magnesia
-bearing iron
silicates.
Acknowledgements
The authors are indebted to Boliden Harjavalta Oy for its dedication and SIMP program by Tekes and Dimecc Oy for funding this extensive study.