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Varying hydrochloric acid concentration affects the observed reaction rate with magnesium but not the standard enthalpy change.
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INSUFFICIENT LEANING
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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.

Evidence for · 3
2023 · cited by 11
Magnesium chloride hexahydrate crystal (MgCl_2.6H_2O) is an intermediate product used to obtain Mg metal from its ores. This work aims to produce purified MgCl_2.6H_2O crystals from natural Egyptian serpentine. Serpentine samples were collected from the Eastern Desert in Egypt and prepared for leaching with HCl solutions. Reaction temperature (°C), leaching time (h), solid/liquid ratio (g/mL), and acid concentration (M) were studied. The optimum leaching conditions achieved 97.6% MgO recovery optimized at particle size less than 75 µm (100%), 95 °C of the reaction temperature for three hours with solid-to-liquid ratio 1:5, and 5 M of HCl concentration. The serpentine dissolution kinetics were studied depending on the solid–liquid reaction and activation energy model. The resultant liquor was purified and crystallized. The kinetic studies indicated that product layer diffusion is the most likely rate-controlling step for serpentinite dissolution in the HCl solution. Similar content being viewed by others Hydrometallurgical Leaching of Manganese Using Hydrochloric Acid in The Presence of Thiourea from Um Bogma Area, Sinai, Egypt Article 14 November 2024 Preparation of Magnesium Chloride from Magnesite Dust Using Hydrochloric Acid Leaching and Spray Drying Article 06 July 2022 Removal of Magnesium from Liquor Produced by Nickel Mining by Crystallization Chapter © 2017 Explore related subjects Discover the latest articles, books and news in related subjects, suggested using machine learning. After leaching, the soluble magnesium chloride salt is separated from the insoluble residue and purified [ 2 ]. Commonly used lixiviants are hydrochloric acid [ 12 , 13 , 14 ], sulfuric acid [ 3 , 8 ], and other inorganic and organic acids. Several investigations into serpentinite rock have been done to understand its dissolution characteristics better. Singh et al. investigated the effect of solvent concentration, sample size, reaction temperature, and reaction time on Mg extraction that was explored using three acids: HCl, H 2 SO 4 , and HNO 3 . The activation energy was calculated for the dissolution kinetics of Mg, which follows the product layer diffusion process with 17.45 kJ·mol −1 (0–30 min) and 14.12 kJ·mol −1 (60–120 min) [ 15 ]. Abou El-Leef et al. investigated the best conditions for leaching Mg 2+ ions from serpentine ore using sulfuric acid. They found that the rate of magnesia dissolution in H 2 SO 4 acid solutions was regulated by a chemical reaction on the surface of the serpentine ore The following conditions were used to study the effect of the temperature on MgO recovery by leaching with aqueous HCl solution: Reaction time is 1 h, solid-to-liquid ratio is 1:5 g/ml, and acid concentration is 5 M. The results are shown in Fig. 2 a, which reveal that MgO recovery increases as temperature increases. The optimum temperature is 95 °C, which results in a MgO recovery of 86.5%. Fig. 2 Full size image Effect of leaching parameters on MgO recovery: Reaction temperature ( a ), Reaction time ( b ), Solid/liquid ratio ( c ), and Hydrochloric acid concentration ( d ) 3.2.2 Effect of Reaction Time The reaction time effect was studied at different time periods (1-4 h), where temperature, solid/liquid ratio, and acid concentration were set at 95 °C, 1:5 g/mL, and 5 M to optimize the recovery of MgO at the optimum reaction time. Figure  2 b shows that the interaction of serpentine with hydrochloric acid is a high-rate spontaneous reaction. The mole ratio of MgO to HCL was kept at a constant value while changing the ratios of solid (ore) and liquid (solution) by adopting the HCl concentration. Figure  2 c indicates that a higher solid-to-liquid ratio (1:20) results in a lower magnesium chloride concentration (83.4%) because of the decreased corresponding acid concentration. The low concentration of magnesium salts resulting from the increasing solid-to-liquid ratio leads to intensive energy consumption during the evaporation and crystallization step in the magnesium salt production process. It is worth mentioning that the reaction time required to achieve a certain degree of conversion of the magnesium is not an independent quantity, but it mainly depends on the size of the serpentinite particles and on the concentration and temperature of the acid. 3.3 Kinetic Analysis Experimental studies reveal that the Mg recovery from serpentine ores depends on the varied parameters of the applied process synchronized with its dissolving behavior. Material dissolving behavior is determined by the interaction between the acid reactant and the solid. This reaction is determined by the solid–liquid reaction model and the energy of activation. There are mainly three methods, product layer developed on the surface of the particle, film diffusion, or chemical reaction caused by unreacted ore, controlling the solid–liquid reactions. The slowest step of these methods controls the reaction rate. The dissolution characteristics of serpentinite rocks have been studied by many researchers, as shown in Table 2 . This research work conducted experiments with particle size 100%-200 mesh of the sample, 5 M acid concentration of 5 M, and at various applied temperatures in the reaction. The results of the experiments are presented in Fig. 3 for various times and temperatures. 6 Full size image Block flow diagram for preparation of magnesium chloride hexahydrate from serpentine ore 4 Conclusions This study concluded the optimum leaching conditions of Egyptian serpentine ores to achieve 97.6% MgO recovery at particle size less than 75 µm (100%), 95 °C of the reaction temperature for 3 h with solid-to-liquid ratio 1:5, and 5 M of HCl solution concentration. This study found that serpentine ore dissolution kinetics depended on the solid/liquid reaction model and activation energy. The kinetic studies proved that product layer diffusion could be the most appropriate rate-controlling step for the serpentine dissolution by HCl.
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More for · 2
2025 · cited by 10
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.
1968 · cited by 5
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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first checked01 Aug 2026
judged → COMMON KNOWLEDGE · 9501 Aug 2026
held for human review08 Aug 2026
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