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首页> 外文期刊>Minerals Engineering >Acid leaching of metals from deep-sea manganese nodules - A critical review of fundamentals and applications
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Acid leaching of metals from deep-sea manganese nodules - A critical review of fundamentals and applications

机译:深海锰结核中金属的酸浸-基本原理和应用的严格审查

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摘要

The mass% metal composition of deep sea nodules ranges from 10-28% Mn, 4-16% Fe, 0.3-1.6% Ni, 0.02-0.4% Co, and 0.1-1.8% Cu in mixed oxide matrices with alumina and silica. The concentrations of base metal ions in sea water of pH ~ 8 of the order 10 ~(-3)-10~2 nmol/kg are shown to be dependent on the solubility products (Kg.) of carbonate sediments. Cations of higher softness have higher pK_(SP) and lower solubility. Previously reported leach results of nodules in H_2SO_4 and HC1 under atmospheric pressure and temperatures in the range 30-90 °C and in the absence or presence of SO_2, Na_2SO_3, NaCl and CaCl_2 are used in the present study to compare, contrast and rationalise the leaching behaviour of metal values. Leach efficiency of metals increases with increasing acid concentration, and Cu(II) and Zn(II) follow the same trend in HC1. Potential-pH diagrams of base metal oxides show a higher stability of mixed metal oxides such as ferrites, magnetite and manganite, which causes partial dissolution of high-valent oxides in the absence of reducing agents. Application of a shrinking core kinetic model in both H_2SO_4 and HC1 media predicts a proton diffusivity of D_H~+ ~ 10~(-11) cm~2 s~(-1) for the dissolution of Ni from nodules. This value is of the same order as D_H~+ for the high pressure acid leaching of Ni from limonitic laterite. A linear correlation between leaching efficiencies of Fe and Ni appears to be a result of co-dissolution of these metals from NiO.Fe_2O_3 or NiFeOOH. The first order dependence of initial dissolution rates of Cu(II) with respect to H~+ concentration in H_2SO_4, and the beneficial effect of background chloride ions, suggests a dissolution mechanism: CuO -> Cu(OH)Cl_(ads/aq) -> CuSO_4. The Cu(II) ions in solution can also affect Ni(II) dissolution from oxide by cation exchange mechanism. The presence of SO_2 or Na_2SO_3 as reducing agents facilitates the acid leaching of high-valent oxides of Mn and Co and other metals incorporated in the mixed oxide matrix. Whilst Fe(II) ions formed during the reductive leaching of Fe(III)-oxides accelerate the dissolution of Mn(III)/(IV) oxides, the resultant Mn(ll) ions accelerate the dissolution of high-valent Co-oxides. Leaching efficiency in HCl increases with temperature. As for the SO_2/H_2O system thermodynamic calculations predict a decrease in concentration of H~+ and HSO_3~- at high temperatures, which retards leaching efficiency. The SO_2/H_2O/air leach system enhances metal dissolution due to the production of H_2SO_4 via the transition metal catalysed oxidation of SO_2 to H_2SO_4.
机译:在具有氧化铝和二氧化硅的混合氧化物基体中,深海结核的金属成分的质量百分比范围为:10-28%Mn,4-16%Fe,0.3-1.6%Ni,0.02-0.4%Co和0.1-1.8%Cu。海水中pH〜8的贱金属离子浓度约为10〜(-3)-10〜2 nmol / kg,这取决于碳酸盐沉积物的溶解度产物(Kg。)。较高柔软度的阳离子具有较高的pK_(SP)和较低的溶解度。本研究使用先前报道的H_2SO_4和HC1中的结节在大气压力和30-90°C的温度下以及不存在或存在SO_2,Na_2SO_3,NaCl和CaCl_2的浸出结果进行比较,对比和合理化。金属值的浸出行为。金属的浸出效率随酸浓度的增加而增加,而HCl中Cu(II)和Zn(II)的趋势相同。贱金属氧化物的电势-pH图显示混合金属氧化物(例如铁氧体,磁铁矿和锰矿)的稳定性更高,这导致在没有还原剂的情况下部分溶解高价氧化物。在H_2SO_4和HC1介质中应用收缩核动力学模型可以预测D_H〜+〜10〜(-11)cm〜2 s〜(-1)的质子扩散率,从而可以从结节中溶解镍。该值与从镍红土红土中高压酸浸出镍的D_H〜+数量级相同。 Fe和Ni的浸出效率之间存在线性关系,这似乎是这些金属从NiO.Fe_2O_3或NiFeOOH中共溶解的结果。 Cu(II)初始溶解速率相对于H_2SO_4中H〜+浓度的一阶依赖性以及背景氯离子的有益作用提示了溶解机理:CuO-> Cu(OH)Cl_(ads / aq) -> CuSO_4。溶液中的Cu(II)离子还可通过阳离子交换机制影响Ni(II)从氧化物中的溶解。作为还原剂的SO_2或Na_2SO_3的存在促进了Mn和Co以及混合氧化物基质中掺入的其他金属的高价氧化物的酸浸。虽然在还原浸出Fe(III)-氧化物过程中形成的Fe(II)离子加速了Mn(III)/(IV)氧化物的溶解,但生成的Mn(II)离子却加速了高价Co-氧化物的溶解。 HCl中的浸出效率随温度的升高而增加。至于SO_2 / H_2O系统的热力学计算表明,高温下H〜+和HSO_3〜-的浓度会降低,这会降低浸出效率。 SO_2 / H_2O /空气浸提系统通过过渡金属催化的SO_2氧化为H_2SO_4产生H_2SO_4,从而提高了金属的溶解度。

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