Wilkin Richard T, Beak Douglas G
U.S. Environmental Protection Agency, National Risk Management Research Laboratory, Ground Water and Ecosystems Restoration Division, 919 Kerr Research Drive, Ada, OK 74820, United States.
Chem Geol. 2017 Jun 25;462:15-29. doi: 10.1016/j.chemgeo.2017.04.023.
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 = 0.56 (Fe Ni S; 0 ≤ ≤ 1). Greater than 99% Ni removal from solution occurred when Ni loading remained below 0.13 ± 0.03 (1) 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 (NiS), or godlevskite [(Ni,Fe)S] formation was indicated regardless of the amount of Ni loading. Slight expansion of the -axis correlated with increasing Ni content in synthetic mackinawite, from = 5.07 ± 0.01 Å at = 0.02 to = 5.10 ± 0.01 Å at = 0.38. Ni -edge extended X-ray absorption fine structure (EXAFS) spectra of synthetic Ni-bearing mackinawite are similar in phase and amplitude to the Fe -edge EXAFS spectrum of Ni-free mackinawite, indicating that the molecular environment of Ni in Ni-bearing mackinawite is similar to that of Fe in Ni-free mackinawite. EXAFS data fitting of Ni-bearing mackinawite with = 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 -axis. At lower Ni loadings ( = 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: where is the distribution coefficient, is the ratio of equilibrium constants for Ni-mackinawite and mackinawite (14.4 ± 1.3), is an ion interaction parameter, and is the mole fraction of end-member NiS in the solid solution. The experimentally determined value of 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 (FeS) and Ni retention in the solid phase. When Ni-mackinawite was aged in the presence of dissolved oxygen, transformation to goethite (FeOOH) and violarite (FeNiS) was observed.
在近中性pH值(5.2至8.4)的厌氧间歇实验中,研究了合成马基诺矿(FeS)对水溶液中Ni(II)的吸收情况。初始Ni(II)与FeS的摩尔比范围为0.008至0.83,以阳离子摩尔分数表示的马基诺矿中最大Ni浓度高达 = 0.56(Fe Ni S;0 ≤ ≤ 1)。当Ni负载量低于0.13 ± 0.03(1)mol Ni/mol FeS时,由于Ni在马基诺矿表面的吸附作用,溶液中Ni的去除率大于99%。使用X射线衍射和拉曼光谱对实验固体进行表征,结果显示出纳米晶马基诺矿的特征图案;无论Ni负载量多少,均未发现形成硫化镍(α-NiS或针镍矿)、辉镍矿(NiS)或戈德列夫斯基矿[(Ni,Fe)S]的证据。随着合成马基诺矿中Ni含量的增加, 轴略有膨胀,从 = 0.02时的 = 5.07 ± 0.01 Å增加到 = 0.38时的 = 5.10 ± 0.01 Å。含Ni马基诺矿的Ni - 边扩展X射线吸收精细结构(EXAFS)光谱在相位和幅度上与无Ni马基诺矿的Fe - 边EXAFS光谱相似,这表明含Ni马基诺矿中Ni的分子环境与无Ni马基诺矿中Fe的分子环境相似。对 = 0.42的含Ni马基诺矿进行EXAFS数据拟合,结果表明配位数为4.04 ± 0.30,平均Ni_S键距为2.28 Å,这与马基诺矿中Fe_S键距2.26 Å、四面体Fe配位以及沿 轴的轻微晶格膨胀情况良好吻合。在较低的Ni负载量( = 0.05 - 0.11)下,EXAFS分析表明Ni_S配位向CN = 3减少,这反映了吸附Ni的影响。超过最大吸附量继续吸收Ni时,会伴随着等量的Fe以摩尔比释放到溶液中。马基诺矿层间Ni的间隙占据可能向Fe的结构取代转变。Ni - 马基诺矿固溶体由单一位点二元混合模型描述: 其中 是分配系数, 是Ni - 马基诺矿和马基诺矿平衡常数的比值(14.4 ± 1.3), 是离子相互作用参数, 是固溶体中终态成员NiS的摩尔分数。实验测定的 值为17.74 ± 1.1kJ/mol,表明固溶体存在显著的非理想性。通过用多硫化物和空气饱和溶液对Ni - 马基诺矿进行老化处理来评估转变过程。Ni - 马基诺矿与多硫化物反应导致黄铁矿(FeS)的形成以及Ni保留在固相中。当Ni - 马基诺矿在溶解氧存在下老化时,观察到向针铁矿(FeOOH)和硫镍铁矿(FeNiS)的转变。