Varying hydrochloric acid concentration affects the observed reaction rate with magnesium but not the standard enthalpy change.
the verdict
INSUFFICIENT LEANING
refutedsupported
the weight of evidence
3 sources for · 0 against
The retrieved literature confirms that varying hydrochloric acid concentration affects reaction and leaching rates involving magnesium, but does not provide direct evidence concerning the standard enthalpy change of the reaction.
The kinetics of hydrochloric acid leaching of oxidized magnesite–iron nickel ores from the Gornostaevskoye deposit (Eastern Kazakhstan) were investigated. The ore has high contents of Mg (14.25 wt.%), Fe (10.8 wt.%) and Si (24.32 wt.%), with a Ni content of 0.87 wt.%. The optimal process parameters were determined as follows: S:L = 1:4, temperature = 85–90 °C, leaching duration = 120 min, HCl concentration = 18%, and stirring rate = 400 rpm. The extraction rates of Ni, Mg and Fe were 91.03%, 97.88% and 93.04%, respectively. The pregnant leach solution contained 1.98 g L-1 Ni, 35.31 g L-1 Mg and 25.12 g L-1 Fe. Kinetic modeling indicated that the leaching of Ni, Fe, and Mg followed a mixed-control mechanism, with activation energies of 76.07 kJ mol-1 for Ni, 125.45 kJ mol-1 for Fe, and 119.33 kJ mol-1 for Mg, confirming that the chemical reaction was controlled. Thermodynamic analysis revealed that pimelite, nickel silicate hydrate, and antigorite are the most reactive phases under hydrochloric acid leaching, on the basis of their highly negative ΔG values. The established mineral dissolution sequence, namely, pimelite > Ni − silicate hydrate > nepouite > antigorite > lizardite > talc > wüstite > hematite, reflects the combined influence of structural accessibility and thermodynamic favorability.
Kinetic modeling indicated that the leaching of Ni, Fe, and Mg followed a mixed-control mechanism, with activation energies of 76.07 kJ mol -1 for Ni, 125.45 kJ mol -1 for Fe, and 119.33 kJ mol -1 for Mg, confirming that the chemical reaction was controlled. Thermodynamic analysis revealed that pimelite, nickel silicate hydrate, and antigorite are the most reactive phases under
The advantages of using HCl as a lixiviant are the easier production of metal chloride solutions containing Ni, Fe and Mg and the possibility of regenerating free hydrochloric acid from its spent solution 10 ; therefore, hydrochloric acid was chosen as a leaching reagent 27 since the ore minerals are completely exposed and impurities such as iron and magnesium are easier to remove from chloride media. The authors in Ref 28 .
On the basis of these results, 85 °C was selected as the optimum leaching temperature for further experiments, as it provided the highest recovery rates for all target metals. Effect of acid concentration The effects of hydrochloric acid concentration on the leaching of nickel (Ni), iron (Fe), and magnesium (Mg) from laterite ore were investigated over the range of 6–21 wt.% HCl. The experiments were performed at a fixed leaching time of 120 min, a temperature of 85 °C, a solid-to-liquid ratio of 1:4, and a stirring speed of 400 rpm. The results are presented in Fig. 8 . Fig. 8 Effect of acid concentration on Ni, Fe, and Mg leaching from laterite (S:L = 1:4, τ = 120 min, t = 85 °C, 400 rpm).
In the present study, these models were applied to experimental leaching data for nickel (Ni), iron (Fe), and magnesium (Mg) extracted from lateritic ore under optimized hydrochloric acid conditions. The kinetic expressions vary depending on the reaction order and can be expressed in the following forms (Eqs. (8)-(11)): The zero-order pseudohomogeneous model assumes a constant leaching rate, independent of the concentration of unreacted material. It is typically applicable when the reagent is present in large excess or when surface reaction sites are quickly replenished. 8 In the half-order pseudohomogeneous model , the rate is proportional to the square root of the unreacted fraction.
The applicability of the pseudo-second-order model to acid leaching of multi-phase solids is justified by its underlying assumption of surface-controlled reactions involving chemical interactions between protons and reactive sites. Similar to sorption systems, the leaching of nickel, iron, and magnesium from laterite ore occurs via proton exchange mechanisms that are governed by valence forces, consistent with previous reports on heterogeneous dissolution kinetics (Ho & McKay, 1999) 41 . Hixson and Crowell model The Hixson–Crowell model 42 describes the dissolution rate of solid particles by accounting for changes in surface area as a function of particle size reduction.
The lower β for Mg indicates more sustained leaching activity, potentially because of higher accessibility and lower surface heterogeneity. Thermodynamic analysis Thermodynamic calculations allow prediction of the energetic feasibility and stability of phases involved in leaching processes, as well as determination of the optimal conditions for the selective extraction of target components from multicomponent ores. In this study, changes in the standard Gibbs energy (ΔG) and enthalpy (ΔH) were calculated for the leaching reactions of various silicate and oxide minerals typical of nickel-containing ores using the HSC Chemistry 10.0 program.
The prevailing rate of nickel leaching is also evidenced by the lowest value of activation energy (Table 1 ) compared with magnesium and iron. Notably, lizardite can also act as a source of nickel. The authors of 53 reported that the reaction of sulfuric acid in the sulfation–roasting–leaching process with serpentines, particularly lizardite, is more thermodynamically probable than that with phyllosilicates (goethite). In our case, under the conditions of ore containing a large amount of lizardite (Fig. 4 ), hydrochloric acid leaching is also effective for extracting nickel from laterite ores. The main carriers of Mg are antigorite (Mg₄₈Si₃₄O₈₅(OH)₆₂), talc and lizardite.
These values highlight the suitability of hydrochloric acid as a leaching reagent for complex multicomponent laterite ores, enabling efficient metal recovery while offering the advantages of chloride system regeneration and improved impurity removal. Kinetic modeling using the shrinking core model (SCM) revealed that the dissolution process is controlled by a mixed mechanism combining surface chemical reactions and diffusion through the product layer.
The purpose of this paper is to review the theory of mass transfer, with and without chemical reaction, and to show how it can be applied in the prediction of uniform corrosion rates. As an example, experimental data reported1 for the rate of dissolution of magnesium cylinders in hydrochloric acid solutions were analyzed. A mechanism for the reactions and the transport of ions to or from the metal surface was suggested, and the model was used in the prediction of data with considerable success. Application of this method in other corrosion systems is presently under investigation, in an effort to broaden its usefulness and to determine its limitations.
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