2015 Volume 55 Issue 12 Pages 2694-2696
The kinetics of the dissolution of nitrogen into molten Fe–Mn–C alloys through the isotope exchange reaction at 1673 K was investigated. The rate of nitrogen dissolution into a molten Fe–Mn–C alloy at low oxygen concentrations ([mass% O] < 0.001) indicated a first-order reaction with respect to the partial pressure of nitrogen. In a molten Fe–Mn–C alloy, Mn had a positive effect on the dissolution rate of nitrogen owing to a strong thermodynamic affinity with nitrogen, while carbon produced the opposite effect. The present work on nitrogen dissolution in molten Fe–Mn–C alloys was compared to previous studies on the carbon-free Fe–Mn binary alloy, providing empirical evidence for the proportionality of the rate constant to the square of the Mn alloying element activity. It should also be noted that nitrogen dissolution into the molten Fe–Mn–C alloy could be described using a parallel reaction model for the ideal mixing between Fe and Mn, which is also discussed in detail.
The industrial importance of nitrogen dissolution in molten steels with high alloy additions has recently led to substantial interest in the kinetics of interfacial reactions in molten ferro-alloy systems. Several previous studies on the interfacial reaction of nitrogen on liquid steel have indicated that the rate of interfacial reaction can be reasonably estimated using Langmuir’s ideal isotherm model for a first-order reaction. The isotope exchange technique showed that the rate of nitrogen dissolution was strongly dependent on the surface coverage by surface active elements such as O,1,2,6) S,1,6) Se,2) and Te,2) which retarded nitrogen dissolution on the surface. Recent studies suggest that Al,3,5) Si,3,5) B,3,6) and Cu5) can also retard nitrogen dissolution, whereas Ti,4) Zr,4) V,4) and Cr4) can accelerate this dissolution, owing to an affinity with the nitrogen in liquid iron alloys.
Considering the increase on the stacking fault energy of TWIP steel with nitrogen content,7) nitrogen dissolution into a Fe–Mn–C alloy should be controlled during the steelmaking process. Ono et al.5) and Han et al.6) estimated that the rate constant of nitrogen dissolution increases with increasing manganese content in a Fe–Mn binary alloy up to 15 mass%, since Mn has a stronger thermodynamic affinity with nitrogen than iron. Han et al.6) suggested an increasing rate constant of nitrogen dissolution with manganese content that changes at approximately 6 mass% of Mn content, owing to changes in the liquid structure of the molten Fe–Mn alloy. Although fundamental studies on the interfacial reaction rates in several binary ferro-alloys have been conducted,3,8) nitrogen dissolution into a molten Fe–Mn–C alloy has yet to be fully understood due to its high vapor pressures.
In the present study, the effect of manganese and carbon on the dissolution rate of nitrogen into molten Fe–Mn–C ternary system within a wide range of Mn and C at 1673 K has been investigated to clarify the interfacial dissolution behavior of nitrogen using the isotope exchange reaction.
Since the nitrogen dissolution reaction on the surface can be expressed by Eq. (1), its reaction rate, R (in mol/cm2·s), can be defined by Eq. (2), as follows:
(1) |
(2) |
(3) |
(4) |
The experimental apparatus and employed procedure was similar to those used in a previous investigation of nitrogen isotope exchange reactions described in detail elsewhere.6) A nitrogen isotope (98% 30N2, Cambridge Isotope laboratories, Inc., MA, USA) was mixed with UHP N2 (99.999% 28N2) at a ratio of 3:97, where the partial pressure of the combined nitrogen was maintained at 0.3 atm using an Ar (99.9999%) carrier gas.
Reagent-grade carbon (99.999%), manganese chips (99%), and electrolytic iron were mixed in an Al2O3 crucible at 1673 K. The total oxygen was controlled below 10 ppm. A quadrupole type mass spectrometer (model HPR 20, HIDEN Analytical LTD, Warrington, UK) was used in order to analyze the fraction of each outgoing gas component.
After equilibration, the crucible was withdrawn from the furnace and rapidly quenched under Ar. Nitrogen and oxygen were measured using a LECO® TC-300 analyzer, and carbon content was determined using a LECO® CS-200 analyzer. Manganese was analyzed using X-ray fluorescence spectroscopy (XRF, S4 Explorer; Bruker AXS, Wisconsin, USA).
The elementary reaction involved in the dissolution of nitrogen into molten metal can be described as follows:
(5-a) |
(5-b) |
(5-c) |
(5-d) |
(5-e) |
(6) |
(7) |
If molten Fe–Mn alloy, where Mn is substitutional element, was ideal mixing states between iron and Mn on the surface,6) it can be reasonably assumed by Eq. (8) using a parallel reaction model for nitrogen adsorption on a molten Fe–Mn alloy.
(8) |
In the Fe–Mn–C ternary system, the nitrogen dissolution rate on the bare surface considering the low initial oxygen content ([mass% O] < 0.001) and the stabilization of sulfur in the form of MnS11) can ignore the effect of oxygen and sulfur.
The effect of manganese in molten Fe–Mn–C on the rate constant of nitrogen dissolution at 1673 K, compared with previous studies,3,4,5,6,8) is shown in Fig. 1. The rate constant increases with increasing Mn, V, and Cr content, each of which has a stronger affinity with nitrogen than iron.13,14) The carbon in molten Fe–Mn–C alloy retarded the rate of nitrogen dissolution at various fixed manganese contents at 1673 K, as shown in Fig. 2. The effect of carbon on the rate constant of nitrogen dissolution was previously explained by its sole effect on the activity of nitrogen in the metal, thus implying that carbon typically had no effect on dissolution kinetics.14) This was correlated to the negligible effects on the activity of the vacant site described in Eq. (7).4,15) However, the addition of carbon to the molten Fe–Mn–C significantly influenced the rate constant of nitrogen dissolution on the surface of manganese, owing to its strong interaction with Mn. Since the effect of carbon on nitrogen activity is negligible, the rate constant of nitrogen dissolution, which was affected by the addition of carbon, should be considered in terms of effects on the activity of other elements within the molten Fe–Mn–C ternary system.
Dependence of the rate constant of nitrogen dissolution in molten Fe (–C) on additional element content (i = Mn, Si, Cr, V, Ni) at 1673 K.
Dependence of the rate constant of nitrogen dissolution in molten Fe–Mn–C ternary system on carbon content at 1673 K.
Figure 3 shows the kFe–i–C/
(9) |
(10) |
The relationship kFe–i–C/k°Fe (=a□2) as a function of (a) ai and (b) ai2 at 1673 K.
The estimated rate constant of nitrogen dissolution on molten Fe–Mn–C ternary system at 1673 K.
The effect of manganese and carbon on the dissolution rate of nitrogen into molten Fe–Mn–C ternary system has been investigated for a wide range of Mn and C contents at 1673 K. The resulting data was used to clarify the interfacial dissolution behavior of nitrogen using the isotope exchange reaction. The following conclusions were drawn:
(1) The rate of nitrogen dissolution into molten Fe–Mn–C ternary system subject to low oxygen concentration (mass% O] < 0.001) indicated a first-order reaction with respect to the partial pressure of nitrogen.
(2) Mn in the molten Fe–Mn–C alloy had a positive effect on the dissolution rate of nitrogen, owing to a strong thermodynamic affinity with dissolved nitrogen, while carbon showed the opposite effect.
(3) Since the activity of the vacant site, a□, at the metal surface directly corresponds to the activity of the component elements on that surface, the rate constant of nitrogen dissolution on molten Fe–Mn–C ternary system at 1673 K can be expressed using the parallel reaction model.
This work was supported by the BK21 and the Industrial Strategy Technology Development (No. 10033389, Development of e-FERA Technology) through a grant provided by the Ministry of Knowledge Economy.