Activity-composition relations of MnO in MnO-CrO x -CaO-SiO2-containing melts

The MnO activities in (MnO-CrO _x -CaO-SiO₂)-containing melts, which were saturated with the (Mn, Cr)₃O₄ spinel phase, were determined at 1500 °C under an oxygen partial pressure of 10^−8.99 atm. This was done by equilibrating the samples with platinum. The activity of MnO in the melt was then calculated from the activity coefficient of manganese in the resultant Pt-Cr-Mn alloy. Darken’s quadratic formalism for ternary metallic solutions was used to calculate the activity coefficient of manganese in the Pt-Cr-Mn system, in which platinum was considered to be the solvent. It was found that an increase in the concentration of MnO in the melt increases both the MnO activity and the activity coefficient of MnO. For a constant MnO concentration in the (MnO-CrO _x -CaO-SiO₂)-containing melts, the activity of MnO can be increased by increasing the basicity of the melt. In order to obtain high-manganese recoveries from (MnO-CrO _x -CaO-SiO₂)-containing melts into an alloy phase, basic slags in which the activity coefficient of MnO is high should therefore be used.     

Phase Transformations and Grain Growth in β-stabilized TiAl Alloys

Solid-state phase transformations and grain growth of an intermetallic γ-TiAl alloy were investigated in-situ using high-temperature laser scanning confocal microscopy (HTLSCM). During isothermal annealing in the single β-phase region, significant grain coarsening was observed. On cooling beneath the β-transus temperature with different rates, a CCT diagram was evaluated for the initiation of β to α phase transformation and changes in the morphology were observed.     

Determining actual LNAPL plume thickness: review and case study in a fractured aquifer

Determining the thickness of a LNAPL (light non-aqueous phase liquid) hydrocarbon plume in the fractured rock surrounding a borehole is a very important aspect in determining the quantity and degree of contamination of the groundwater and soil, as well as deciding on applicable remediation measures. This review aims to compare some of the field and empirical methods to eventually propose a method of confirming the plausibility of the determined thickness. General insight is supplied relating to the occurrence of groundwater in the Earth’s crust, the basic principles of multiphase flow and the properties of the three fluids of importance, being water, Jet A-1 fuel and air. From the methods applied, the field bail-down method of Hughes et al. and the mathematical approach according to CONCAWE supplied reasonable results, with the Zillox and Muntzer equation providing no rational outcome due to changing water levels from regular bailing of the LNAPL. Furthermore, practically none of these methods have been developed for deep, fractured aquifers. By plotting regular depths to water and fuel on the abscissa axis with free product thickness on the ordinate, the depth to water and depth to fuel linear plots will intersect where the free product thickness equals zero. This indicates the static water level (i.e., the ground water level prior to hydrocarbon contamination) and by subtracting this from the free product depth, a maximum product thickness is obtained.      

In-situ observations of phase transformations in titanium

An in-situ laser-scanning confocal microscopy study has been undertaken on the phase transformations in highpurity titanium. Observations of the β-Ti to α-Ti were observed to proceed with a pronounced Widmanstätten plate morphology due to the large β-Ti grain size. An anomalous transformation was also observed, with the α-Ti growing with a defined ledge-like surface relief. The observed transformation morphologies are discussed with reference to the crystallography of the regions, analyzed using electron-backscatter diffraction.     

In Situ Characterization of Lattice Structure Evolution during Phase Transformation of Zr‐2.5Nb

The α–β phase transformation behavior of Zr‐2.5Nb (in mass%) has been characterized in real time during an in situ neutron diffraction experiment. The Zr‐2.5Nb material in the current study consists, at room temperature, of α‐Zr phase (hcp) and two β phases (bcc), a Nb rich β‐Nb phase and retained, Zr rich, β‐Zr(Nb) phase. It is suggested that this is related to a quench off the equilibrium solubility of Nb atoms in the Zr bcc unit cells. Vegard's law combined with thermal expansion is applied to calculate the composition of the β‐phase, which is compared with the phase diagram, revealing the system's kinetic behavior for approaching equilibrium.     

Engulfment Behavior of Inclusions in High-Carbon Steel: Theoretical and Experimental Investigation

Previous studies on inclusions behavior at the front of the solidifying steel shell have mainly focused on low-carbon steels. However, with the increasing applications of high-carbon steel in recent years because of its superior properties, it is crucial to understand this behavior in high-carbon steel. Most of the high-carbon steels are deoxidized by silicon, calcium treated, and contain higher sulfur percentage. Also, higher carbon content has a determining influence on the viscosity and surface tension, which will affect the inclusion behavior. In this study, we have investigated the engulfment behaviors of inclusions in front of the solidifying interface in high-carbon steels using concentric solidification method. The critical velocity of the growing shell, at which the particle is engulfed in the solidifying shell, instead of being pushed by this shell, was determined. The inclusion identified in this study is a bi-component form of CaO-SiO₂-based oxide and CaS. It was revealed that engulfment behavior is strongly affected by convection of liquid steel that originates from carbon push out in high-carbon steels. This study provides new crucial information to produce high-carbon steel with fewer inclusions, which opens new application pathways for this emerging grade of steel.