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Uptake of nickel by synthetic mackinawite

机译:合成马基钠矿对镍的吸收

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摘要

The uptake of aqueous Ni(II) by synthetic mackinawite (FeS) was examined in anaerobic batch experiments at near-neutral pH (5.2 to 8.4). Initial molar ratios of Ni(II) to FeS ranged from 0.008 to 0.83 and maximum Ni concentrations in mackinawite, expressed as the cation mol fraction, were as high as XNi = 0.56 (Fe1 − xNixS; 0 ≤ x ≤ 1). Greater than 99% Ni removal from solution occurred when Ni loading remained below 0.13 ± 0.03 (1σ) mol Ni per mol FeS due to sorption of Ni at the mackinawite surface. Characterization of experimental solids using X-ray diffraction and Raman spectroscopy showed patterns characteristic of nanocrystalline mackinawite; no evidence of nickel monosulfide (α-NiS or millerite), polydymite (Ni3S4), or godlevskite [(Ni,Fe)9S8] formation was indicated regardless of the amount of Ni loading. Slight expansion of the c-axis correlated with increasing Ni content in synthetic mackinawite, from c = 5.07 ± 0.01 Å at XNi = 0.02 to c = 5.10 ± 0.01 Å at XNi = 0.38.Ni K-edge extended X-ray absorption fine structure (EXAFS) spectra of synthetic Ni-bearing mackinawite are similar in phase and amplitude to the Fe K-edge EXAFS spectrum of Ni-free mackinawite, indicating that the molecular environment of Ni2+ in Ni-bearing mackinawite is similar to that of Fe2+ in Ni-free mackinawite. EXAFS data fitting of Ni-bearing mackinawite with XNi = 0.42 indicated a coordination number of 4.04 ± 0.30 and an average Ni_S bond distance of 2.28 Å, in good agreement with the Fe_S bond distance of 2.26 Å in mackinawite, tetrahedral Fe coordination, and slight lattice expansion along the c-axis. At lower Ni loadings (XNi = 0.05–0.11), EXAFS analysis showed a decrease in Ni_S coordination towards CN = 3, which reflects the influence of sorbed Ni. Continued Ni uptake, past the maximum amount of sorption, was accompanied by proportional molar release of Fe to solution. Interstitial occupancy of Ni within the mackinawite interlayer may be transitional to structural substitution of Fe.The Ni-mackinawite solid-solution is described by a one-site binary mixing model: Ln Kd = ln Ke − (W/RT)(1 − 2XNi)where Kd is the distribution coefficient, Ke is the ratio of equilibrium constants for Ni-mackinawite and mackinawite (14.4 ± 1.3), W is an ion interaction parameter, and XNi is the mole fraction of end-member NiS in the solid solution. The experimentally determined value of W is 17.74 ± 1.15 kJ/mol and indicates significant non-ideality of the solid solution.Transformation processes were evaluated by aging Ni-mackinawite with polysulfides and solutions saturated with air. Reaction of Ni-mackinawite with polysulfides led to the formation of pyrite (FeS2) and Ni retention in the solid phase. When Ni-mackinawite was aged in the presence of dissolved oxygen, transformation to goethite (FeOOH) and violarite (FeNi2S4) was observed.
机译:在近中性pH(5.2至8.4)的厌氧分批实验中,研究了合成麦基钠铁矿(FeS)对Ni(II)的吸收。 Ni(II)与FeS的初始摩尔比介于0.008至0.83之间,并且以阳离子摩尔分数表示,马基钠铁矿中的最大Ni浓度高达XNi = 0.56(Fe1-xNixS; 0≤x≤1)。当镍的含量保持在每摩尔FeS 0.13±0.03(1σ)mol Ni以下时,由于镍在马氏体表面的吸附,溶液中的Ni去除率超过99%。使用X射线衍射和拉曼光谱对实验固体进行表征,显示出纳米晶马金刚石的图案特征。没有迹象表明单硫化镍(α-NiS或Millerite),聚poly石(Ni3S4)或高硅镁石[(Ni,Fe)9S8]的形成与镍含量无关。 c轴的轻微膨胀与合成马基钠镍矿中Ni含量的增加有关,从XNi = 0.02时的c = 5.07±0.01Å到XNi = 0.38时的c = 5.10±0.01Å.NiK边缘扩展了X射线吸收精细结构合成含镍马基钠钙石的(EXAFS)光谱在相位和幅度上与无镍马基钠钙石的Fe K-edge EXAFS光谱相似,表明含Ni的Ni 2 + 的分子环境在不含镍的马基诺石中,马基诺石与Fe 2 + 相似。 XNi = 0.42的含镍马基钠钙石的EXAFS数据拟合显示,其配位数为4.04±0.30,平均Ni_S键距为2.28Å,与马基钙钛矿中的Fe_S键距为2.26Å,四面体Fe配位,轻微沿c轴的晶格扩展。在较低的Ni含量下(XNi = 0.05-0.11),EXAFS分析表明Ni_S配位向CN = 3降低,这反映了吸附的Ni的影响。超过最大吸附量持续吸收镍的同时,铁也成比例地摩尔释放到溶液中。镍在马氏体夹层中的间隙占有可能是过渡到Fe的结构取代.Ni-马氏体固溶体通过一点二元混合模型描述:Ln Kd = ln Ke−(W / RT)(1−2XNi ),其中Kd是分布系数, K e 是Ni-马基钠铁矿和马基钠铁矿的平衡常数之比(14.4±1.3), W 是离子相互作用参数, X Ni 是固溶体中末端NiS的摩尔分数。实验确定的 W 值为17.74±1.15 kJ / mol,表明固溶体存在明显的非理想性。通过多硫化物使Ni-马金刚石与多硫化物及空气饱和溶液一起老化,评估了转化过程。镍马基钠铁矿与多硫化物的反应导致黄铁矿(FeS 2 )的形成和镍在固相中的保留。在溶解氧存在下对镍马基钠锰矿进行时效处理时,观察到向针铁矿(FeOOH)和堇青石(FeNi 2 S 4 )的转变。

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