ISIJ International
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Fundamentals of High Temperature Processes
Thermodynamic Activity of SiO2 in CaO–SiO2–Al2O3–MnO–MgO System Molten Slags
Jian-Bin Chen Huai-Zhuang LuanHong-Hong HuangMing-Hui ZhaoWen-Bo PanZhi-Yu Chen
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2022 Volume 62 Issue 7 Pages 1341-1351

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Abstract

To understand the thermodynamic characteristics of the reaction between Al and SiO2 during the continuous casting process of the high-aluminum steel, the activity coefficients of SiO2 and MnO in molten slags of (18–43%) CaO-(33–64%) SiO2-(9–21%) Al2O3-(2–3%) MgO-(<2.4%) MnO were measured at 1400°C, 1450°C and 1500°C by the experiments of the Si and Mn equilibrium between liquid copper and molten slag in the graphite crucible under the mixed gas atmosphere of CO and Ar. The effects of SiO2, Al2O3, the basicity, the radio of CaO/Al2O3 and the temperature on the activity coefficients of SiO2 and MnO in molten slag were discussed. The quadratic regression relationships among the activity coefficient of SiO2 or MnO, the concentration of component, the basicity and the temperature were investigated by the regression analysis method.

1. Introduction

During the production of high-aluminum steel, SiO2 in the slag will be reduced by the aluminum in the high-aluminum molten steel, which will have an important impact on the quality of the continuous casting slabs and the molten steel. Therefore, no matter the inclusion control and the slagging in the process of the secondary refining, or the control of the composition and performance of the mold flux during the continuous casting process of the high-aluminum steel, the activity coefficient and the activity of SiO2 in the CaO–SiO2–Al2O3–MnO–MgO slags are required when the thermodynamics of the reaction at the metal-slag interface are analyzed, especially the data at 1400 to 1500°C.

There have been many researches reports on the activity of SiO2 in the CaO–SiO2–Al2O3 slag system. According to the equilibrium concentration of SiO2 in the slag and Si in the molten metal obtained from the equilibrium experiment at 1425°C to 1700°C, the activity of SiO2 in CaO–SiO2(30–60%)-Al2O3(≤20%) slags was calculated by Fulton and Chipman1) from the known standard free energy data of the reaction and the activity of Si in the metal. Taylor’s research group2,3) determined the activity of SiO2 in the CaO-(32–70%) SiO2-(0–41%) Al2O3 slags based on the measured CO partial pressure of the equilibrium of the reduction reaction of SiO2 to SiC by carbon. The activities of SiO2 in CaO-(36–60%) Al2O3-(<12%) SiO2 slags and in CaO-(48–54%) Al2O3-(4.5–6.5%) SiO2 slags were measured by Ozturk and Fruehan,4) and Park et al.5) used the reaction equilibrium of Si between Fe–C–Si alloy and slag in a graphite crucible at 1600°C under the Ar + CO mixed gas or pure CO for 10 to16 hours, respectively. Kang et al.6) changed the reference metal to Cu and studied the activity of SiO2 in CaO-(36–56%) Al2O3-(4–11%) SiO2 and in CaO-(35–52%) Al2O3-(3–9%) SiO2-10%MgO slags through the reaction equilibrium of Si between the liquid copper and the slag at 1600°C. Kume et al.7) used the reaction equilibrium of the reduction of SiO2 by Ca, Al and Mg to study the activity of SiO2 in CaO-(0.085–0.562) Al2O3-(0.071–0.876) SiO2 (in mole fractions) slags and in CaO-(0.41–0.64)SiO2-(0.11–0.51) MgO (in mole fractions) slags. So far, a large amount of data on the thermodynamic properties of SiO2 in the CaO–Al2O3–SiO2 slags involved in the various processes of the ferrous metallurgy have been accumulated.1,2,3,4,5,6,7,8,9,10,11,12,13,14,15,16) In these studies, the temperature was mainly 1550–1600°C,1,2,3,4,5,6,7,8,9,11,13,14,15) but a small number of studies involved the temperatures of 1400–1500°C.1,10) But the results of the activity of SiO2 obtained differed as much as two or three orders of magnitude. According to the phase diagram of CaO–SiO2,17) there will be the decomposition of 3CaO·2SiO2 (C3S2) (1464°C), the eutectic reaction between CaO·SiO2 (CS) and 2CaO·SiO2 (C2S) (1460°C), and the eutectic reaction between CaO·SiO2 (CS) and SiO2 (1436°C) in the range of the temperature of 1400–1500°C when the SiO2 concentration is 35–80% (%CaO/%SiO2 = 0.25–2.3). The temperature of 1400–1500°C closes to the melting point of CaO·SiO2 (CS) (1544°C). What effects will these characteristics have on the thermodynamic properties of SiO2?

This research is aimed at CaO–SiO2–Al2O3 slags with MgO and MnO of continuous casting mold flux. The activity coefficients of SiO2 and MnO in molten slag of CaO-SiO2-Al2O3-(<2.4%) MnO-(2–3%) MgO were measured through the reaction equilibrium of Si and Mn between the metal Cu and the slag in the graphite crucible for 30 hours under Ar + CO mixed gas atmosphere at the temperature of 1400°C, 1450°C and 1500°C, respectively. The effects of the components, the basicity and the temperature on the activity coefficients and the activities of SiO2 and MnO in the slags were investigated. The relationships among the activity coefficient of SiO2 or MnO, the concentrations of components in the slag, the basicity and the temperature were also studied by the regression analysis method.

2. Experimental

The experimental device and the experimental process used in this research have been reported in detail in the determination of MnO and FeO activity.18,19) But in order to measure the temperature of the melt in the crucible more accurately, the thermocouple was moved from the bottom of the crucible into the corundum crucible. The number of reaction crucibles in the corundum crucible was increased to six. The blowing flow rate was increased to ensure that the atmosphere above the melt met the experimental requirements.

99.9% copper powder was used as the reference metal in the experiment, and the slag was prepared by the combination of chemical reagents with purity 98% CaO, AR grade SiO2 and Al2O3, 98.5% MgO and 99.5% MnO. The ingredients of the mixed slag are shown in Table 1. The reaction crucible was a graphite crucible with a size of 36 mm inner diameter, 40 mm outer diameter, and 57.5 mm high. During the experiment, six graphite crucibles containing 15 g of copper powder and 25 g of premixed slag material were placed in a corundum crucible. The temperature in the corundum crucible was raised to the preset temperature (1400°C, 1450°C and 1500°C, respectively) under the protection of Ar gas with a flow of 1200 mL·min−1 and a purity of 99.999%. After this status had been stood for 15 min to homogenize the composition and temperature, the Ar gas flow rate was adjusted to 500 mL·min−1, and a 99.995% purity CO gas with the flow rate of 200 mL·min−1 was passed into the corundum crucible above the six graphite crucibles (the partial pressure of CO gas PCO is 0.286 atm). And then timing started after standing for another 30 minutes. After the counted time had reached 30 h, six crucibles were all taken out from the furnace one by one and were cooled down in an Ar gas stream. A XRF method was used to determine the content of each component in the slag sample. Metal Cu samples were analyzed for the content of Si and Mn by ICP-AES method.

Table 1. Charge compositions, mass%.
No.Temperature/°CAl2O3SiO2CaOMnOMgO
1140011.4061.7521.853.002.00
214009.5039.9045.603.002.00
3140012.3539.9042.753.002.00
4140013.3062.7019.003.002.00
5140014.2554.1526.603.002.00
6140016.1539.9038.953.002.00
7140019.9545.6029.453.002.00
8140017.1046.5531.353.002.00
9140020.0035.7139.293.002.00
10140020.0041.6733.333.002.00
11140020.0046.8828.133.002.00
12140020.0037.5037.503.002.00
13140020.0042.8632.143.002.00
14140020.0039.4735.533.002.00
15140020.0044.1230.883.002.00
16140020.0045.4529.553.002.00
17140020.0040.5434.463.002.00
18140020.0050.0025.003.002.00
19145019.0039.9036.103.002.00
20145018.0543.7033.253.002.00
21145017.1046.5531.353.002.00
22145013.3062.7019.003.002.00
23145017.1054.1523.753.002.00
24145020.0039.4735.533.002.00
25145020.0037.5037.503.002.00
26150017.1046.5531.353.002.00
27150014.2554.1526.603.002.00
28150011.4061.7521.853.002.00
29150013.3062.7019.003.002.00
30150017.1054.1523.753.002.00
31150019.9545.6029.453.002.00
32150020.0040.5434.463.002.00
33150020.0039.4735.533.002.00
34150020.0037.5037.503.002.00
35150020.0035.7139.293.002.00
36150020.0034.0940.913.002.00
37150020.0032.6142.393.002.00

The equilibrium time of reaction of Si and Mn in the system has been found to be 22 hours through the preliminary experiments, so the equilibrium time in the experiments was taken as 30 hours.

3. Experimental Results

The following reaction equilibrium was determined under the experimental conditions.   

( Si O 2 ) +2C( s ) = [ Si ] in Cu +2CO( g ) (1)
  
K 1 = a Si p CO 2 a C 2 a SiO 2 = γ Si x Si p CO 2 γ SiO 2 x SiO 2 (2)
Where γSi and aSi are the Raoultian activity coefficient and activity of Si in the liquid copper in reference to the pure liquid silicon, respectively; γSiO2 and aSiO2 are the Raoultian activity coefficient and activity of SiO2 in the molten slag in reference to pure solid silica, respectively; xSi and xSiO2 are the mole fractions of Si in the liquid copper and SiO2 in the molten slag, respectively; aC is the activity of carbon, and aC = 1 in the case of using a graphite crucible; pCO is the partial pressure of CO; K is the equilibrium constant of the reaction (1), which can be calculated from the standard free energy change of the reaction (3) under the selected standard state of activity.   
Si O 2 ( quartz ) +2C( s ) =Si( l )    +2CO( g ) ΔG°=728   853-377.27T ( J/mol ) (3) 20)

The Raoultian activity coefficient of Si in the liquid copper is equal to that of an infinite dilute solution of Si in the liquid copper, γSi = γ Si(l)   in   Cu at the very low concentration of Si.   

ln γ Si(l)   in   Cu =- 7   549 T +0.0143 (4) 21)

Then the activity coefficient of SiO2 in the slag can be derived from Eq. (2) as follows:   

γ Si O 2 (s) = p CO 2 K 3 γ Si x Si x Si O 2 | x Si 0 (5)

Similarly, there is the reaction equilibrium for MnO as follows:   

MnO( s ) +C( s ) =Mn( l ) +CO   ( g ) ΔG°=286   604-170T ( J/mol ) (6) 20)

The activity coefficient of MnO in molten slag can be obtained by Eq. (7).18)   

γ MnO(s) = p CO K 6 γ Mn x Mn x MnO | x Mn 0 (7)
Where γMnO is the Raoultian activity coefficient of MnO in the molten slag in reference to pure solid manganese oxide, γ Mn is the Raoultian activity coefficient of Mn in an infinite dilute solution of Mn in the liquid copper in reference to the pure liquid manganese.   
ln γ Mn(l)   in   Cu =- 981 T +0.0159 (8) 21)

The activity coefficients and the activities of SiO2 and MnO in the experimental slags are shown in Table 2, respectively.

Table 2. Equilibrium concentrations in metal and slag, and the activity coefficient and the activity of SiO2 and MnO.
No.Temperature /°CMetal (mass%)Molten slag (mass%)Activity coefficientActivity (×10−3)
SiMnAl2O3SiO2CaOMgOMnOγSiO2(s) (×10−3)γMnO(s)aSiO2aMnO
114000.200.739.5051.8234.502.001.748.6860.1054.5541.569
214000.0221.219.7840.6045.412.541.371.2430.2260.5052.621
314000.0661.3212.7641.0642.162.511.173.6350.2841.5152.861
414000.100.4812.9763.3518.592.112.393.5190.0502.3201.051
514000.110.5814.2854.2526.402.292.304.4890.0622.5281.258
614000.0321.1116.3440.7038.572.431.561.7400.1750.7332.400
714000.130.6416.8154.7423.392.302.205.2090.0713.0021.395
814000.140.9617.4046.7431.462.361.796.5710.1313.2082.076
914000.0171.0819.7536.5339.272.451.630.0530.1620.0202.348
1014000.0691.0619.7142.5333.342.361.600.1840.1610.0832.301
1114000.0480.6519.7247.1528.192.242.200.1150.0720.0581.417
1214000.0271.1819.9138.3437.482.401.460.0800.1960.0322.550
1314000.0450.8819.8343.7731.772.301.890.1170.1130.0541.917
1414000.0891.2919.9540.2335.622.491.300.2500.2400.1062.787
1514000.0360.7119.8544.6930.592.292.060.0920.0840.0431.553
1614000.0920.8919.9246.2129.212.331.870.2240.1150.1101.928
1714000.0811.1620.1541.2234.312.431.460.2220.1920.0972.512
1814000.130.7419.9950.5524.712.192.050.2900.0870.1561.612
1914501.701.5920.2839.4737.002.490.3422.9580.6249.5321.889
2014500.521.4219.2941.9934.902.440.866.7760.2262.9911.731
2114500.921.2617.6047.1031.592.330.9710.5640.1765.2041.510
2214500.680.7013.3263.0419.102.231.695.9500.0573.9020.851
2314500.851.0017.6654.5623.332.291.568.3370.0864.8031.197
2414500.431.4620.0541.1435.342.390.825.6880.2422.4611.771
2514501.601.6020.6537.6038.662.480.2522.4530.8458.8771.881
2615000.281.0217.1347.3830.982.431.620.8600.0490.4260.705
2715000.660.9614.4654.4426.622.271.751.7860.0431.0090.667
2815001.401.2110.1150.7735.292.111.124.0910.0862.1060.827
2915000.520.7413.0263.0318.722.322.021.2330.0290.8100.524
3015000.500.8817.2654.6323.472.271.851.3330.0370.7670.614
3115000.230.9920.0146.4129.282.241.640.7220.0470.3550.695
3215000.361.3920.2841.3434.592.410.981.2630.1100.5510.967
3315000.591.6020.3040.2936.012.450.592.1230.2110.9011.110
3415000.391.5520.1538.6637.852.390.601.4790.2030.6011.086
3515000.281.6320.1836.9739.572.420.491.1110.2620.4311.141
3615000.311.7220.2134.8841.782.480.401.3050.3390.4761.201
3715000.231.7420.2633.4043.182.430.351.0140.3930.3541.219

4. Discussions

4.1. About the Structure of the Molten Slag

It can be known from textbooks that when the temperature is not too high from the melting point, the pressure is not too low, and the gasification temperature is much higher than the research temperature, the short-range order theory of silicate melt believes that the melt structure is close-range order. The arrangement and spacing of neighbors are similar to those in solid crystals. When the crystal is heated to the melting point and melted into a melt, there are still a certain number of relatively regularly arranged particles around the particles. Only when it is far away from the center particles, the regular arrangement is gradually disappeared. The structural feature of the melt is short-range order and long-range disorder.

According to the polymer structure theory of silicate melts, the high temperature still does not completely destroy the covalent bonds in the original solid state when a considerable number of strong covalent bonds are in the structure. The remaining covalent bonds combine the melt component atoms into a large number of “polymers” with different polymerization degrees, which are highly dispersed and coexist with each other. There are Si O 4 4- (monomers), S i 2 O 7 6- (dimers), S i 3 O 10 8- (trimers), S i n O 3n+1 2n+2- (n-mers) and three-dimensional fragments [SiO2]n and other anions, and the free metal cations in the silicate melt. The type and quantity of polymers in the silicate melt are mainly related to the composition and temperature of the melt.

Based on the above two theories, it is believed that even if the compound molecules in the molten slag do not exist in the solid state, they will exist in the molten slag in the form of “clusters” related to the compound in the solid state. The types of compounds that may exist in the molten slag can obviously be obtained from the phase diagrams of the relevant slag series. The components that do not generate complex compounds with other oxides are called free components, such as free CaO. Obviously, when a component in the slag exists in a free form, the activity of the free component must be higher than that of the component in the form of a certain complex compound type “cluster”. The higher the stability of the complex compound, the lower the activity of the oxide component in this compound type “cluster”. However, according to polymer structure theory of silicate melts, free CaO can be ionized into Ca2+ and O2− ions, so as to exist in the molten slag in the form of ions.

The following will explain the experimental results based on the above viewpoint.

4.2. Effects of SiO2

Figures 1 and 2 show the effects of SiO2 in the slag on the activity coefficients of SiO2 and MnO at 1400°C and 1500°C, respectively. The reported results4,5,6,18,22,23,25,26) are also illustrated in the figures for comparison. It can be seen from Fig. 1 that when SiO2<52%, the activity coefficient of SiO2 in the slag at 1500°C is higher than the value of 1400°C. At 1400°C and when SiO2<52%, the activity coefficient of SiO2 increase with the increase of SiO2. At 1400°C and when SiO2>54%, the activity coefficient of SiO2 decreases with the increase of SiO2 and its value is far higher than the value when SiO2<52%. The transition point of concentration of the changes for the activity coefficient of SiO2 is about 52–54% SiO2 at 1400°C. At 1400°C and when SiO2>54%, the activity coefficient of SiO2 is also higher than the value at 1500°C. The activity coefficient of SiO2 increases with the increase of SiO2 at 1500°C. It can be seen that the interaction between temperature and basicity has an effect on the activity coefficient of SiO2.

Fig. 1.

The effect of SiO2 on the activity coefficient of SiO2 at 1400°C and 1500°C.

Fig. 2.

The effect of SiO2 on the activity coefficient of MnO at 1400°C and 1500°C.

The composition points of the equilibrium slag with CaO/SiO2<0.65 at 1500°C in Fig. 1 (the points with “▲” in Fig. 1) are located in the CaO·SiO2 (CS) + SiO2 phase zone in the CaO–SiO2 binary phase diagram and in the concentration triangle of the CS–SiO2–CaO·Al2O3·2SiO2 (CAS2) in the CaO–SiO2–Al2O3 ternary phase diagram.17) The experimental temperature (1500°C) is near the melting temperature of CS (1544°C) and the decomposition temperature of C3S2 (1475°C). The change of the activity coefficient and the activity of SiO2 in the slag should be related to these factors. With the increase of SiO2, the molar ratio of CaO:SiO2:Al2O3 in the slag change from 1:1.48:0.52 to 1:3.14:0.33, as shown in Table 3. The formation of CAS2 type clusters in every 100 grams of molten slag consumes 0.26 to 0.39 mol of SiO2 calculated based on the Al2O3 content in the molten slag. The generation of CS type clusters in every 100 grams of molten slag will consume 0.33 to 0.55 mol of SiO2 calculated based on the CaO content in the molten slag. Because the concentrations of MnO and MgO in the molten slag are very low and are basically the same, and the composition points fall in the concentration triangle of the CS–SiO2–CAS2 in the CaO–SiO2–Al2O3 ternary phase diagram, the consumption of SiO2 combined with MnO and MgO is temporarily ignored. Since CaO may exists in complex compounds such as CS and CAS2 at the same time, the CaO consumed to generate CAS2 can no longer exist in CS. Therefore, the number of moles of SiO2 in molten slag is first subtracted the SiO2 consumed to generate CAS2. Then the SiO2 consumed to generated CS (formed by the remaining CaO combining with SiO2) is subtracted. If C2AS or C3S2 is also generated, it continues to subtract the SiO2 consumed to generate C2AS or C3S2. The number of moles of the SiO2 that remains in the molten slag is finally gotten. It is represented by “nSiO2 remained” and is listed in the last column of Table 3. SiO2 remained in the molten slag increase from 0.05 to 0.59 mol with the increase of SiO2. Therefore, the activity coefficient of SiO2 in the molten slag increases with the increase of SiO2, just like the results of many researchers.1,2,3,5,9,11)

Table 3. The phase zone in the CaO–SiO2–Al2O3 phase diagram where the experimental point in Fig. 1 is located, the ni/nCaO ratio and the nSiO2 consumed by the formation of complex compounds.
No.Temp./°CsymbolConcentration trianglenAl2O3/nCaOnSiO2/nCaOnSiO2 for CSnSiO2 for CAS2nSiO2 remained
51400CS-SiO2-CAS20.301.920.470.280.29
71400CS-SiO2-CAS20.402.180.420.330.33
41400CS-SiO2-CAS20.383.180.330.250.60
91400CS-CAS2-C2AS0.280.870.700.39−0.29
121400CS-CAS2-C2AS0.290.950.670.39−0.23
141400CS-CAS2-C2AS0.311.050.640.39−0.16
171400CS-CAS2-C2AS0.321.120.610.40−0.12
101400CS-CAS2-C2AS0.331.190.590.39−0.08
131400CS-CAS2-C2AS0.341.290.570.39−0.03
151400CS-SiO2-CAS20.361.360.550.390.00
161400CS-SiO2-CAS20.381.480.520.390.05
111400CS-SiO2-CAS20.381.560.500.390.09
181400CS-SiO2-CAS20.441.910.440.390.20
311500CS-SiO2-CAS20.381.480.520.390.05
261500CS-SiO2-CAS20.301.430.550.340.07
271500CS-SiO2-CAS20.301.910.470.280.29
301500CS-SiO2-CAS20.402.170.420.340.32
291500CS-SiO2-CAS20.383.140.330.260.59
371500C3S2-CS-C2AS0.260.720.770.40−0.41
361500CS-CAS2-C2AS0.270.780.750.40−0.36
351500CS-CAS2-C2AS0.280.870.710.40−0.29
341500CS-CAS2-C2AS0.290.950.670.40−0.23
331500CS-CAS2-C2AS0.311.040.640.40−0.17
321500CS-CAS2-C2AS0.321.120.620.40−0.13

Note: “nSiO2 for CS “ refers to the number of moles of SiO2 consumed when CaO·SiO2 is produced, and is calculated based on the number of moles of CaO; “nSiO2 for CAS2” refers to the number of moles of SiO2 consumed when CaO·Al2O3·SiO2 is produced, and is calculated based on the twice the number of moles of Al2O3 because the number of moles of Al2O3 is lower than that of CaO. “nSiO2 Remained” refers to the number of moles of SiO2 remained SiO2 without combination with other oxides, which is calculated by the nSiO2 in slag subtracting the SiO2 consumed to generate CS and CAS2, without repeating the calculation of the amount of CaO in these two compounds.

When CaO/SiO2>0.84 at 1500°C (the points with “▼” in Fig. 1), except for one slag sample falling on the concentration triangle of the C3S2-CS-C2AS, the other composition points all fall within the concentration triangle of the CS-CAS2-C2AS. At this time, SiO2 in the slag may form CS (CaO·SiO2) type, CAS2 (CaO·Al2O3·2SiO2) type and/or C2AS (2CaO·Al2O3·SiO2) type, and/or C3S2 (3CaO·2SiO2) type clusters with other oxides. There is no the SiO2 which formed the compound with other oxides. However, it can be seen from Table 3 that the negative value of the “nSiO2 remained” gradually decreases with the increase of SiO2. So, the activity coefficient of SiO2 increases.

The composition points of the equilibrium slag with CaO/SiO2<0.49 at 1400°C in Fig. 1 (the point with “■”) are located in the CaO·SiO2 (CS) + SiO2 phase zone in the CaO–SiO2 binary phase diagram and in the concentration triangle of the CS–SiO2–CAS2 in the CaO–SiO2–Al2O3 ternary phase diagram.17) The experimental temperature (1400°C) is slightly lower than the eutectic temperature (1436°C) of this two-phase zone. As shown in Table 3, with the increase of SiO2 concentration, SiO2 remained in the molten slag in every 100 grams of molten slag increases from 0.29 to 0.60 mol. Therefore, the activity coefficient of SiO2 in the slag should increase with the increase of SiO2 concentration, just like the results when CaO/SiO2<0.65 at 1500°C and the results of many researchers.1,2,3,5,9,11) The result that the SiO2 activity coefficient decreases with the increase of SiO2 concentration when CaO/SiO2<0.49 at 1400°C in Fig. 1, whether can be explained as: with the increase of SiO2, the SiO2 that is not formed the complex compounds will continue to generate some silicon-oxygen anions with more complex structure, so the activity coefficient of SiO2 decreases. At 1500°C and %CaO/%SiO2<0.65, the high temperature causes the silicon-oxygen anions with a complex structure to disintegrate, and the structure of silicon-oxygen anions is simplified. Therefore, the SiO2 activity coefficient increases with the increase of SiO2 concentration.

When CaO/SiO2>0.49 and the temperature is 1400°C, the composition points all fall within the CS-CAS2-C2AS concentration triangle (the point with “●” in Fig. 1). It can be seen from Table 3 that the “nSiO2 remained” keeps increasing as the increases of SiO2, but the concentration of the remaining SiO2 in the slag is not high enough. The generated Si–O anions are not much enough to form complex ion clusters with a very complex structure. So, the SiO2 activity coefficient increases with the increase of the SiO2 concentration. At 1400°C, the transition point of concentration of the changes for the activity coefficient of SiO2 is about 52–54% SiO2. The maximum nSiO2 remained for this concentration is 0.29, and the molar ratio of nSiO2:nCaO is 1.92 at mass%Al2O3 = 20. It is speculated that at this concentration ratio at 1400°C, the structure of SiO2 in the molten slag will have a relatively large change.

The MnO combines with SiO2 to form not only MnO·SiO2 type clusters easily, but also more stable CaO·MnO·2SiO2 type clusters. The activity coefficient of MnO in the slag reduces with the increase of SiO2, as shown in Fig. 2. But when CaO/SiO2 = 0.98–1.27 at 1400°C, SiO2 forms CS type clusters with CaO, and even CAS2 type clusters with CaO and Al2O3. The number of SiO2 which used to form MnO–SiO2 type clusters with MnO is relatively reduced. So, the activity coefficient of MnO increases as SiO2 increases. This is different from the change of the activity coefficient of MnO when CaO/SiO2 = 0.84–1.29 at 1500°C. Because the high temperature of 1500°C makes CAS2 clusters unstable and even it is difficult for the CAS2 clusters to be formed. SiO2 is more inclined to form MnO–SiO2 clusters with MnO. Hence, the activity coefficient of MnO decreases still with the increase of SiO2.

4.3. Effects of Al2O3

When SiO2 = 33.27–54.74% and basicity CaO/SiO2 = 0.42–1.27, the activity coefficient of SiO2 in the slag decreases with the increase of Al2O3 at 1400°C and 1500°C, as shown in Fig. 3. Because the Al2O3 concentration in the equilibrium slag in Fig. 3 is lower than that of the molar ratio of Al2O3 to SiO2 in CaO·Al2O3·2SiO2 (CAS2) and in 2CaO·Al2O3·SiO2(C2AS), the SiO2 is continuously consumed to form the stable CAS2 and C2AS type clusters as Al2O3 increases. Hence, the activity coefficient of SiO2 decreases with the increase of Al2O3. When the basicity and the SiO2 are the same, the activity coefficient of SiO2 at 1400°C is slightly higher than the value at 1500°C (the points with “■●” in Fig. 3 is higher than the point with “◆”). It can also be seen that the interaction between temperature and basicity has an effect on the activity coefficient of SiO2.

Fig. 3.

The effect of Al2O3 on the activity coefficient of SiO2 at 1400°C and 1500°C.

The activity coefficients of MnO at 1400°C and 1500°C decrease both slightly with the increase of Al2O3, as shown in Fig. 4. Al2O3 is easy to form MnO·Al2O3 type clusters with MnO as Al2O3 increases, and even forms 2MnO·Al2O3·5SiO2 type clusters with MnO and SiO2 easily. Therefore, the activity coefficient of MnO at 1500°C decreases slightly with the increase of Al2O3. At 1400°C, the effect of Al2O3 on the activity coefficient of MnO is related to the basicity and SiO2 content. Hence, the interaction of Al2O3 with basicity and SiO2 complicates the change of the activity coefficient of MnO.

Fig. 4.

The effect of Al2O3 on the activity coefficient of MnO at 1400°C and 1500°C.

4.4. Effects of Basicity

The activity coefficient of SiO2 in the slag decreases with the increase of basicity (R = %CaO/%SiO2) at 1400°C and 1500°C, as shown in Fig. 5. As the basicity increases, SiO2 in the molten slag forms CaO·SiO2 (CS) type clusters with CaO, even CAS2 type clusters with CaO and Al2O3. So, the activity coefficient and the activity of SiO2 in the slag decreases, as shown in Fig. 5.

Fig. 5.

The effect of the basicity on the activity coefficient of SiO2 at 1400°C and 1500°C.

The activity coefficient of MnO in the slag increases with the increase of basicity at 1500°C, as shown in Fig. 6, but there is a transition point around the basicity of 0.6 to 0.7. When the basicity is greater than 0.7, the slope of the change in the activity coefficient of MnO increases. At 1400°C, the increasing of the activity coefficient of MnO with the increase of the basicity is the overall trend. However, when Al2O3 = 19.69–20.15% and SiO2 = 33.27–50.55%, the change of activity coefficient of MnO has a maximum point when the basicity is around 0.9–1.0.

Fig. 6.

The effect of the basicity on the activity coefficient of MnO at 1400°C and 1500°C.

At 1500°C, as the basicity increases, SiO2 forms CS type clusters with CaO, and even forms CAS2 and C2AS type clusters with CaO and Al2O3. The MnO, which is used to form MnO·SiO2 (MS) type clusters with SiO2, is decrease. So, the activity coefficient of MnO in the slag increases. In addition, from the viewpoint of ionic of the molten slag structure, as the basicity increases, the O2− concentration in the molten slag increases, which also increases the activity coefficient of MnO in the slag. It can be seen from Fig. 6 that when the basicity is higher than the transition point of 0.7, the SiO2 in the equilibrium slags in the experiments is lower, but the Al2O3 is higher. After SiO2 has formed CS, CAS2 and C2AS type clusters, there is less SiO2 and more MnO in the slag, so the activity coefficient of MnO increases faster with the increase of the basicity.

4.5. Effects of the Ratio of CaO/Al2O3

At 1400°C, the activity coefficient of SiO2 decreases with the increase of the ratio of CaO/Al2O3, as shown in Fig. 7. At 1500°C, when the basicity CaO/SiO2 = 0.29–0.67, the activity coefficient of SiO2 increases with the increase of the CaO/Al2O3 ratio. At 1500°C, when the basicity CaO/SiO2 = 0.67–1.29, the activity coefficient of SiO2 decreases with the increase of the CaO/Al2O3 ratio.

Fig. 7.

The effect of the ratio of CaO/Al2O3 on the activity coefficient of SiO2.

At high basicity, it can be seen from Fig. 7 that Al2O3 in the slag is almost unchanged. As the ratio of CaO/Al2O3 increases, CaO increases. Then SiO2 forms CS-type clusters with CaO, even CAS2 and C2AS-type clusters. Therefore, the activity coefficient of SiO2 decreases with the increase of the ratio of CaO/Al2O3. When the basicity is low, the strong acid slag has high SiO2. Although SiO2 forms Al2O3·SiO2 type clusters with Al2O3, even CAS2 type or C2AS type clusters, the number of the clusters containing Al2O3 decreases with the increase of CaO/Al2O3. The activity coefficient of SiO2 increases with the increase of the CaO/Al2O3 ratio.

As the ratio of CaO/Al2O3 increases, SiO2 forms CS type clusters with CaO, and even forms CAS2 type or C2AS type clusters, and then the number of MnO-SiO2 type clusters which has been formed decreases. Hence, the activity coefficient and the activity of MnO increase, as shown in Fig. 8. In addition, the O2– concentration in the slag increases with the increase of CaO/Al2O3 ratio, which also increases the activity coefficient and the activity of MnO. Corresponding to the change of the activity coefficient of SiO2, at low basicity (%CaO/%SiO2 = 0.29–0.67) at 1500°C, it can be seen from Fig. 8 that at this time Al2O3 is lower and SiO2 is higher. As the ratio of CaO/Al2O3 increases, the Al2O3 decreases, and the number of the more stable clusters of Al2O3-containing type decreases. And then the SiO2 combined with MnO increases, so the activity coefficient and the activity of MnO increase little. When the basicity is high (%CaO/%SiO2 = 0.67–1.29), Al2O3 is higher and SiO2 is lower. As the ratio of CaO/Al2O3 increases, SiO2 forms CS, CAS2 and C2AS type clusters with CaO, and the rest SiO2 is combined with MnO. The remained number of SiO2 which is used to form the clusters with MnO is small, so the slope of the increase of the activity coefficient and the activity of MnO is relatively large.

Fig. 8.

The effect of the ratio of CaO/Al2O3 on the activity coefficient of MnO.

4.6. Effects of the Temperature

The effects of temperature on the activity coefficient of SiO2 are related to the basicity (R = %CaO/%SiO2) of the slag, as shown in Fig. 9. When the basicity is lower (R≤0.67, acidic slag), the activity coefficient of SiO2 is lower at 1500°C than at 1400°C. When the basicity is higher (R>0.8), the activity coefficient of SiO2 is higher at 1500°C than at 1400°C.

Fig. 9.

The effect of temperature on the activity coefficient of SiO2 in the slag.

It can be seen from the Fig. 9 that the activity coefficient of SiO2 is higher at 1450°C than at 1400°C or 1500°C when SiO2, Al2O3 and basicity are basically the same. This may be related to the fact that the eutectic temperatures of the two-phase zones of C3S2 + CS and of SiO2 + CS are just around 1450°C.

The effect of temperature on depolymerization is greater at higher silica contents because such melts are in a state of high level of polymerization.20) As the temperature rises, the polymer of Si–O anions in molten slag ( S i n+1 O 3n+4 2(n+2)- ) disintegrate as follows:37)   

S i n+1 O 3n+4 2(n+2)- + O 2- =Si O 4 4- +S i n O 3n+1 2(n+2)- (9)

The concentration of O2- ions in the slag is reduced. The activity coefficient of MnO decreases when CaO/SiO2<0.88, as shown in Fig. 10. When CaO/SiO2>0.96, the disintegration of Si–O complex anions in the molten slag is small, and the O2− concentration increases as the increases of the basicity. Hence, the activity of MnO increases.

Fig. 10.

The effect of temperature on the activity coefficient of MnO in the slag.

4.7. The Relationship between the Activity Coefficient and Concentration

According to the above discussion, the activity coefficients of SiO2 and MnO in the slag are related to the concentration, basicity and temperature. The interactions between the composition & the basicity and between the basicity & the temperature also affect the activity of SiO2 and MnO greatly. To obtain the relationship between the activity coefficient of SiO2 and MnO in the slag and the concentration, all the data in Table 2 are used to obtain the quadratic regression relationship, as shown in Eqs. (10), (11), (12), (13).

At 1673 K, when SiO2 = 36–64%, Al2O3 = 9–20%, MgO = 2–3% and MnO <2.4%,   

log γ Si O 2 =-239.216+1.643(%CaO)+3.491(%Si O 2 ) +2.419(%A l 2 O 3 )+0.827(%MnO)+2.156(%MgO) +0.00426 (%CaO) 2 -0.0129 (%Si O 2 ) 2 -0.0253 (%A l 2 O 3 ) 2 +0.385B×(%A l 2 O 3 )±0.168 (α=0.05,   R=0.99,   Adj. R 2 =0.95) (10)
  
log γ MnO =-14.062+0.131(%CaO) +0.137(%Si O 2 )+0.164(%A l 2 O 3 )-0.396(%MnO) +0.250(%MgO)+1.544× 10 -4 (%CaO) 2 +5.180× 10 -6 (%Si O 2 ) 2 -5.469× 10 -4 (%A l 2 O 3 ) 2 -0.00450B×(%A l 2 O 3 )±0.00877   (α=0.05,   R=1.000,   Adj. R 2 =0.998) (11)

At 1773 K, when SiO2 = 33–63%, Al2O3 = 9–20%, MgO = 2–3% and MnO <2%,   

log γ Si O 2 =-59.053+0.0670(%CaO)+1.497(%Si O 2 ) -0.319(%A l 2 O 3 )-0.580(%MnO)+0.919(%MgO) +0.00220 (%CaO) 2 -0.0103 (%Si O 2 ) 2 +0.0123 (%A l 2 O 3 ) 2 +0.355B×(%A l 2 O 3 )±0.0489 (α=0.05,   R=0.99,   Adj. R 2 =0.94) (12)
  
log γ MnO =-11.444-0.557(%CaO)+0.321(%Si O 2 ) -0.0214(%A l 2 O 3 )-0.557(%MnO)+0.0971(%MgO) +9.936× 10 -4 (%CaO) 2 -0.00235 (%Si O 2 ) 2 +2.919× 10 -4 (%A l 2 O 3 ) 2 -0.105B×(%A l 2 O 3 )±0.0233 (α=0.05,   R=1.000,   Adj. R 2 =0.997) (13)

When the effect of the temperature is considered, the regression relationship can be obtained as follows at 1673 K–1773 K when SiO2 = 33–64%, Al2O3 = 9–21%, MgO = 2–3% and MnO <2.4%:   

log γ Si O 2 =-187.984+3.679× 10 4 × 1 T +0.825(%CaO)+2.795(%Si O 2 )+1.442(%A l 2 O 3 ) -0.0917(%MnO)+2.518(%MgO)+0.0115 (%CaO) 2 -0.0130 (%Si O 2 ) 2 -0.0153 (%A l 2 O 3 ) 2 +0.596B ×(%A l 2 O 3 )-2.255× 10 4 B× 1 T ±0.294   (α=0.05,   R=0.93,   Adj. R 2 =0.82) (14)
  
log γ MnO =-14.728+1.573× 10 4 × 1 T -0.143(%CaO)+0.309(%Si O 2 ) -0.140(%A l 2 O 3 )-0.585(%MnO) +0.323(%MgO)+0.00196 (%CaO) 2 -0.00292 (%Si O 2 ) 2 +0.00197 (%A l 2 O 3 ) 2 +0.117B×(%A l 2 O 3 )-1.169× 10 3 B× 1 T ±0.0401   (α=0.05,   R=0.99,   Adj. R 2 =0.99) (15)
where B = (mass%CaO + mass%MnO + mass%MgO)/mass%SiO2. From the |t Stat| or the P-value of regression analysis, the order of the effect of various factors on the activity coefficient of SiO2 is: 1/T, SiO2, the interaction of basicity B and Al2O3 (B × Al2O3), CaO2, SiO22, Al2O3, MgO, the interaction of basicity B and the reciprocal of temperature, Al2O32, CaO, MnO. 1/T has a very significant effect on the activity coefficient of SiO2. SiO2, the interaction of basicity B and Al2O3 (B × Al2O3), CaO2, SiO22 have a significant effect on the activity coefficient of SiO2. The order of the effect of various factor on the activity coefficient of MnO is as follows: 1/T, MnO, SiO22, the interaction of basicity B and Al2O3 (B × Al2O3), CaO2, SiO2, MgO, Al2O32, Al2O3, CaO, the interaction of basicity B and the reciprocal of temperature. 1/T, MnO, SiO22, the interaction of basicity B and Al2O3 (B × Al2O3), CaO2 has a very significant effect on the activity coefficient of MnO. SiO2 has a significant effect on the activity coefficient of MnO.

Therefore, in the study of the calculation model of the activity of the components in the slag, the quadratic terms of the concentration of each component27,28,29) or even a more complex terms30,31,32,33,34,35,36) are often included. It is also necessary to consider the interaction between the components. Regarding the calculation models of the activities of the components in the slag, the most famous are the ionic solution model (Temkin model), the regular solution model (Lumsden Model27,28,29,36)), the molecular ion coexistence model,30,31,32) and the modified quasi-chemical solution model.33,34,35) Both in the Temkin model and in the Lumsden model, the presence of Si–O complex anions in the molten slag and its influence on the activity are not considered, and both models are generally suitable for high-basicity slags. The various structure forms of the Si–O complex anion of silicate molten slag are considered in the Masson model, but the Masson model can only be applied to binary system slag generally. The existence of complex compound molecules and simple ions in the molten slag is considered in the molecular ion coexistence model, but the existence and influence of complex anions such as Si–O is not considered. The influence of the more complex Si–O complex anions in the low-basicity slag is not considered in the quasi-chemical solution model also. From the mathematical expression point of view, Eqs. (10), (11), (12), (13), (14), (15) are similar to the regular solution model, and both include the first and quadratic terms of the component concentration in the slag. But the quadratic term in the regression formula (Eqs. (10), (11), (12), (13), (14), (15)) contains the interaction of the components themselves, the interaction between basicity and components, and the interaction between basicity and temperature. In order to reduce the number of interactions between components, the interaction between basicity and components is used to reflect the interaction between components and to simplify the regression formula. Figure 11 shows the comparison between the calculated values of the molecular ion coexistence model (MIC Model), of the quasi-chemical model (calculated by FactSage software), and that of the Eqs. (10), (12) and (14) and the experimental values. It can be seen from the Fig. 11 that the calculated values of Eqs. (10) and (12) are in good agreement with the experimental values. The calculated values of the molecular ion coexistence model and the quasi-chemical model are much larger than the experimental values, even up to 1 to 2 orders of magnitude. Therefore, the existing models need to be further improved for strong acid slag.

Fig. 11.

Comparison of the measured activity of SiO2, calculated activity of SiO2 by the regression equation and by the models.

5. Conclusions

The activity coefficients of SiO2 and MnO in (18–43%) CaO-(33–64%) SiO2-(9–21%) Al2O3-(2–3%) MgO-(<2.4%) MnO slags were determined through the chemical equilibrium experiments of Si and Mn in the liquid copper and the molten slag in a mixed gas atmosphere of CO and Ar at temperatures of 1400°C, 1450°C and 1500°C, respectively. The effects of SiO2, Al2O3, basicity, the ratio of CaO/Al2O3 and temperature on the activity coefficients of SiO2 and MnO were discussed. The quadratic regression relationships between the activity coefficients of SiO2 or MnO, the concentration, the basicity in the slag and the temperature were obtained by the regression analysis method. The results show:

(a) At 1400°C and 1500°C, the change of the activity coefficient of SiO2 with the increase of SiO2 is complicated, and it is related to the concentration of the component, the basicity and the temperature. When SiO2>40%, the activity coefficient of MnO in the slag at 1400°C and 1500°C decrease with the decrease of SiO2.

(b) When SiO2 = 33.27–54.74%, basicity CaO/SiO2 = 0.42–1.27, the activity coefficient of SiO2 in the slag decreases with the increase of Al2O3 at 1400°C and 1500°C. The activity coefficients of MnO decrease slightly with the increase of Al2O3 at 1500°C.

(c) When Al2O3 = 12.76–20.3%, as the basicity increases, the activity coefficient of SiO2 in the slag decreases at 1400 and 1500°C.

(d) When SiO2, Al2O3 and basicity are basically the same, the activity coefficient of SiO2 and MnO at 1450°C is higher than that of 1400 and 1500°C.

Acknowledgements

The author expresses his gratitude to the funding support by National Natural Science Foundation of China (No. 51874198).

References
 
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