2013 Volume 53 Issue 5 Pages 761-767
An empirical model has been developed based on optical basicity to calculate the sulfide capacity of metallurgical molten slag. The model estimated sulfide capacities agree well with the experimental data for CaO–MgO–FeO–MnO–TiO2–Al2O3– SiO2–CaF2 multicomponent slags. It is found that the abilities of increasing sulfide capacity in MO–SiO2 (M=Ca, Mg, Fe and Mn) melts follow the order: MnO>FeO>CaO>MgO. Also, substitution of CaO for CaF2 decreases the sulfide capacity and substitution of TiO2 for SiO2 increases the sulfide capacity.
Metallurgical slag plays a significant role in removing the sulfur (undesirable element) in the metal during pyrometallurgical processes. The dissolution behavior of sulfur in molten slag was first quantitatively defined by Fincham and Richardson1) as “sulfide capacity”. In order to accurately control the sulfur content in metal, knowledge of sulfide capacity of slag is required. To date, numerous experimental1,2,3,4,5,6,7,8,9,10,11,12,13,14,15,16,17,18,19,20,21,22,23,24,25,26,27,28,29,30,31,32,33,34,35,36,37,38,39,40,41,42,43,44) and theoretical studies45,46,47,48,49) have been carried out. Theoretical models can make up for the shortage of available experimental data and extend our ability for prediction. Thermodynamic models were proposed by -Reddy and Blander,45) Moretti and Ottonello,46) Kang and Pelton.47) These models calculate the sulfide capacity solely from the knowledge of thermodynamic activity calculated by different slag polymer models. The precisions of sulfide capacities are determined by the precisions of activity calculations. However, these models are inconvenient to be used for their complexity and/or commercial use. Furthermore, these models cannot calculate the sulfide capacity of slags containing CaF2. KTH model36) considers all the complex polymeric ions as dissociated simple species. Good agreement is obtained when estimating the sulfide capacity of CaO–MgO–FeO–MnO–Al2O3–SiO2 slag by the KTH model. However, too many parameters need to be optimized in this model.
The optical basicity, a measure of basicity or the capacity of the oxides to donate electrons was first proposed by Duffy and Ingram,50) and used to relate slag composition to viscosity,51) electrical conductivity,52) activity53) and phosphide capacity of the slag.48) Sosinsky and Sommerville48) first proposed a simple sulfide capacity prediction model using optical basicity. Young et al.49) found Sosinsky and Sommerville’s relationship is not sufficiently accurate particularly in the high basicity region. Thereby, a new sulfide capacity model was proposed.49) However, its accuracy is also very low. Therefore, in the present study, a new optical basicity model is proposed to improve the calculation accuracy of sulfide capacity.
The dissolution behavior of sulfur in oxide slags is usually described by the following sulfur-oxygen exchange chemical reaction,1)
(1) |
(2) |
(3) |
(4) |
(5) |
(6) |
(7) |
(8) |
Systems | References | |
---|---|---|
Group I | CaO–SiO2 | [1],[2],[3],[4],[5],[6] |
MgO–SiO2 | [1],[7],[8] | |
CaO–Al2O3 | [1],[9],[10],[11],[12],[13] | |
CaO–MgO–SiO2 | [7],[14] | |
CaO–Al2O3–SiO2 | [1],[4],[10],[13],[14],[15],[16],[17],[18] | |
MgO–Al2O3–SiO2 | [8],[19] | |
CaO–MgO–Al2O3 | [17],[19] | |
CaO–MgO–Al2O3–SiO2 | [20],[14],[16],[21],[22],[23],[24],[25],[26],[27],[28] | |
Group II | MnO–SiO2 | [2],[5],[6],[8] |
MnO–Al2O3 | [8] | |
CaO–MnO–SiO2 | [2],[5],[6],[29] | |
MgO–MnO–SiO2 | [8],[30] | |
MnO–Al2O3–SiO2 | [8],[19] | |
CaO–MgO–MnO–SiO2 | [30] | |
CaO–MgO–MnO–Al2O3 | [24] | |
CaO–MnO–Al2O3–SiO2 | [24],[25] | |
CaO–MgO–MnO–Al2O3–SiO2 | [24],[25],[31] | |
Group III | FeO | [32],[33] |
FeO–SiO2 | [1],[34] | |
CaO–FeO–SiO2 | [35],[36] | |
MgO–FeO–SiO2 | [36] | |
FeO–MnO–SiO2 | [36] | |
CaO–MgO–FeO–Al2O3–SiO2 | [23],[27],[37] | |
CaO–MgO–FeO–MnO–Al2O3–SiO2 | [36] | |
Group IV | FeO–TiO2 | [32] |
MnO–TiO2 | [38] | |
CaO–MgO–TiO2 | [39] | |
CaO–FeO–TiO2 | [40] | |
CaO–SiO2–TiO2 | [39] | |
FeO–SiO2–TiO2 | [40] | |
CaO–MgO–SiO2–TiO2 | [39] | |
CaO–FeO–SiO2–TiO2 | [40] | |
CaO–Al2O3–SiO2–TiO2 | [39] | |
CaO–MgO–Al2O3–SiO2–TiO2 | [21],[26],[27] | |
CaO–MgO–FeO–Al2O3–SiO2–TiO2 | [27] | |
Group V | CaO–SiO2–CaF2 | [41],[42],[43],[44] |
CaO–Al2O3–CaF2 | [16],[43] | |
CaO–MgO–SiO2–CaF2 | [42] | |
CaO–MnO–SiO2–CaF2 | [42] | |
CaO–Al2O3–SiO2–CaF2 | [16],[42] |
Comparisons between calculated and measured sulfide capacity values for CaO–MgO–FeO–MnO–TiO2–Al2O3–SiO2–CaF2 slag.
The strict theoretical relations between composition and terms E and A in Eq. (6) are hard to deduced. Therefore, an empirical treatment will be adopted to represent the experimental data of sulfide capacity. In order to express the nonlinear relation between the logarithm of sulfide capacity and optical basicity, the present model assumes that the activation energy term E is the linear function of the reciprocal of optical basicity (the estimation results show that this treatment works well). Mills et al.51) also used the reciprocal of optical basicity to describe the activation energy of viscosity. The temperature compensation effect54) is also considered, which is widely used to relate activation energy with pre-exponent factor (using a linear relationship) in the van’t Hoff or Arrhenius type equation. Therefore, in the present model, both E and A in Eq. (6) will be the linear functions of the reciprocal of optical basicity.
(9) |
(10) |
After obtaining values of m and n, the apparent optical basicity values of transition metal oxides MnO, FeO and TiO2 are optimized in turn with the measured sulfide capacity data of Groups II, III and IV shown in Table 1, respectively. Apparent optical basicity of CaF2 is determined by fitting the experimental data of Group V in Table 1. It should be pointed out that when calculating optical basicity of slag containing CaF2 by Eq. (8), Ni for CaF2 is 1 since two fluorine ions can be considered equivalent to one oxygen ion. Table 2 shows the optical basicity of different components, and by using them the sulfide capacity of CaO–MgO–FeO–MnO–TiO2–Al2O3–SiO2–CaF2 system can be calculated according to Eq. (10).
Comparisons of calculated and measured sulfide capacities for slag systems in Groups I, II, III, IV and V are shown in Figs. 2, 3, 4, 5, 6, respectively. The model calculated sulfide capacities agree well with the measured values. In the following sections, variation of sulfide capacity with composition for some binary and ternary systems will be given to show how the sulfide capacity varies with composition.
Comparisons between calculated and measured sulfide capacity values for CaO–MgO–Al2O3–SiO2 slag.
Comparisons between calculated and measured sulfide capacity values for slag containing MnO.
Comparisons between calculated and measured sulfide capacity values for slag containing FeO.
Comparisons between calculated and measured sulfide capacity values for slag containing TiO2.
Comparisons between calculated and measured sulfide capacity values for slag containing CaF2.
The sulfide capacity variations of MO–SiO2 (M=Ca, Mg, Fe and Mn) systems with the mole fractions of MO at 1773 K and 1923 K are shown in Fig. 7, in which the experimental data are also included for comparison. It can be seen that calculated sulfide capacities agree well with the measured values. Furthermore, the sulfide capacity of different MO–SiO2 binary systems with same content of MO at the same temperature follows the order: MnO–SiO2>FeO–SiO2> CaO–SiO2>MgO–SiO2. The reason for this order is that sulfide capacity is determined by both the concentration of free oxygen that is bond with metal cation M only and the stability of the sulfide MS.55) High concentration of free oxygen and higher stability of the sulfides can increase the sulfide capacity. The order of free oxygen concentrations in binary MO–SiO2 slags with the same contents of SiO2 is FeO–SiO2>MnO–SiO2>MgO–SiO2>CaO–SiO2, while order of the sulfide stability is: CaS>MnS>FeS>MgS. Both factors contribute to the order of sulfide capacity for binary MO–SiO2 system.
Comparisons between calculated and measured sulfide capacity values for MO–SiO2 (M=Ca, Mg, Fe, Mn) slag.
Influence of MO (M=Fe, Mn) content on sulfide capacity of MO–TiO2 system at 1773 K is shown in Fig. 8. Increasing MO content can lead to the increase of sulfide capacity of MO–TiO2 system. It also can be concluded from Fig. 8 that MnO has a stronger ability of increasing sulfide capacity than FeO.
Comparisons between calculated and measured sulfide capacity values for MO–TiO2 (M=Fe, Mn) slag.
The iso-log(CS) curves at 1773 K for CaO–MgO–SiO2 system is plotted using the present model in Fig. 9, and the experimental data are also included for comparison. It can be seen that the substitution of CaO by MgO can decrease the sulfide capacity. The iso-Log(CS) curves at 1923 K for CaO–MnO–SiO2 and MgO–MnO–SiO2 systems are plotted in Figs. 10 and 11, respectively. For a given (constant) SiO2 content, CS in both melts will increase as increasing MnO content.
The iso-Log(CS) curves of CaO–MgO–SiO2 slag at 1773 K. (■) Ref. 14; (—) iso-Log(CS) curves calculated by the present model.
The iso-Log(CS) curves of CaO–MnO–SiO2 slag at 1923 K. (■) Ref. 5; (—) iso-Log(CS) curves calculated by the present model.
The iso-Log(CS) curves of MgO–MnO–SiO2 slag at 1923 K. (■) Ref. 8; (—) iso-Log(CS) curves calculated by the present model.
From the iso-Log(CS) curves of CaO–Al2O3–SiO2 melt at 1773 K shown in Fig. 12, it can be seen that in the region of low basicity, substitution of Al2O3 for SiO2 can increase the sulfide capacity greatly, while in the region of high basicity the substitution can only slightly increase sulfide capacity. The reason for this may be that Al2O3 is an amphoteric oxide which can behave as a basic oxide under the condition of low basicity, and as an acidic oxide under the condition of high basicity. Increasing the content of the basic oxide could increases the concentration of free oxygen which is very important for increasing the dissolution of sulfur in slag (increases the sulfide capacity). The present model uses the reciprocal of optical basicity in Eq. (9), so in the range of high optical basicity, the sulfide capacity increment at same increment of optical basicity will decrease. Therefore, though the model does not consider the amphoteric behavior information of Al2O3, it can still embody this variation phenomenon.
During the pyrometallurgical processes, CaF2 is always added to enhance the fluidity and desulfurization ability of the slag. So, it is significant to understand its influence on the sulfide capacity. The iso-Log(CS) curves of CaO–CaF2–SiO2 melt at 1776 K and 1473 K are shown in Fig. 13. At a given (constant) SiO2 content, the sulfide capacity of CaO–CaF2–SiO2 melt decreases when increasing the content of CaF2. Therefore, CaF2 has a weaker ability to increase the sulfide capacity compared to CaO. However, it can be seen from Fig. 13 that when adding CaF2 to CaO–SiO2 melt while keeping the ratio of CaO to SiO2 constant, there will be an increase in sulfide capacity.
From the iso-Log(CS) curves of CaO–TiO2–SiO2 melt at 1773 K shown in Fig. 14, it can be concluded that sulfide capacity of CaO–TiO2–SiO2 system increases when SiO2 is replaced by TiO2 for a given (constant) CaO content. It is known to all that Ti is a multivalence element, which has the valences of 2+, 3+ and 4+. The proportions of different TiOx oxides are determined by oxygen fugacity, temperature and basicity.56) So, the coexistences of several TiOx oxides in melt are also the reason for model discrepancy from the measured values. It was pointed out that at ambient pressure the reduced valences are favor by high temperature, but the proportions of them in air become significant only above 2273 K.56) So, it is assumed that all the Ti present as TiO2 because all the sulfide capacity data for TiOx containing slags used in this study are measured below 1873 K. Mysen56) reviewed the spectroscopic data on titania bearing glasses and found that more than one structural position of Ti4+ might be possible. Or, TiO2 may act either as a network modifier or a network former. If it behaves as a network modifier, it can obviously increase sulfide capacity relative to SiO2 because it can decrease the degree of polymerization and help increase the free oxygen content. Even if TiO2 acts as a network former like SiO2, because the Ti4+ ion is larger than the Si4+ cation, the Ti–O–Ti bond is expected to be weaker than Si–O–Si bond. Thus, substitution of TiO2 for SiO2 will decrease the degree of polymerization, and thereby increase sulfide capacity. Accordingly, replacement of SiO2 by TiO2 for a given (constant) CaO content will increase sulfide capacity regardless of the acid or base behavior of TiO2.
The iso-Log(CS) curves of CaO–TiO2–SiO2 slag at 1773 K. (■) Ref. 39; (—) iso-Log(CS) curves calculated by the present model.
(1) With about sixty optimized parameters, KTH model can give a good estimation results for CaO–MgO–FeO–MnO–Al2O3–SiO2 systems. The calculated sulfide capacities by KTH model and our model of Groups I, II and III in Table 1 are compared with the measured values as shown in Fig. 15. It is indicated that with only eight adjustable parameters, our model can still obtain good results.
Comparisons between calculated and measured sulfide capacity values for CaO–MgO–FeO–MnO–Al2O3–SiO2 slag.
(2) The apparent optical basicity of FeO is optimized to be 1.00 in the work of Young et al.49) Obviously, this value is unreasonable because if the optical basicity of FeO is the same as that of CaO, the sulfide capacity of CaO–FeO–SiO2 melt should not change when FeO is substituted for CaO at constant SiO2 content. However, according to the experimental results this is not true. It is found that when CaO is replaced by FeO for a given (constant) SiO2 content in CaO–FeO–SiO2 melt, the sulfide capacity increases.36) Hence, the optimized optical basicity value of 1.24 for FeO is more reasonable and is able to rationalize the observation.
(3) In the definition formula of sulfide capacity (Eq. (3)), both the influences of activity coefficient of sulfur ion and activity of free oxygen ion are included. Generally, the optical basicity could reflect the activity of free oxygen ion, while in the present model both the two terms are expressed by the sulfide capacity. Therefore, the optimized apparent optical basicity values of FeO, MnO, TiO2 and CaF2 are also incorporated the influence of sulfur ion. So, the presently derived optical basicity values for these components may be applicable only to the sulfide capacity estimation, not to other ones such as the phosphate capacity.
The concept of optical basicity is used to model the sulfide capacity of CaO–MgO–FeO–MnO–TiO2–Al2O3–SiO2–CaF2 melt, and good estimation results are obtained. The model assumed a linear relationship between the logarithm of sulfide capacity and the reciprocal of optical basicity of the slag. Apparent optical basicity of FeO, MnO, TiO2 and CaF2 are optimized in this study. The order of sulfide capacity for MO–SiO2 binary systems for a given (constant) SiO2 content and temperature is MnO–SiO2>FeO–SiO2>CaO–SiO2>MgO–SiO2; substitution of CaO by CaF2 decreases the sulfide capacity and substitution of SiO2 by TiO2 increases the sulfide capacity.
The authors wish to express their thanks to the financial supports from China Postdoctoral Science Foundation (2012M510318) and the Chinese Natural Science Foundation (51174022 and 51234001).