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Quantitative microstructural characterization of natrojarosite scale formed during high-pressure acid leaching of lateritic nickel ore

机译:红土镍矿高压酸浸过程中形成的钠铁矾垢的定量微观结构表征

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摘要

The build up of scale inside autoclaves during high-pressure acid leaching of nickel laterite ore currently represents a significant industrial problem in processing plants. In this study, the crystallographic microstructure of natrojarosite scale developed on stirring rods inside a high-pressure acid leach autoclave are investigated using electron backscatter diffraction (EBSD). Backscatter electron imaging shows compositional layering of natrojarosite with dispersed minor iron oxide crystals and regularly spaced, parallel layer micro-porosity. Analysis of the scale by EBSD reveals that natrojarosite forms elongate grains with strong (0001) crystallographic preferred orientation with c axes aligned within the plane of the agitator substrate, consistent with unitaxial precipitation from a fluid. The natrojarosite grains contain a complex internal substructure of low-angle (<15°) boundaries that define elongate subgrains and accommodate up to 40° of systematic misorientation across single grains. Low-angle subgrain boundaries do not have simple twin relationships or low-index misorientation axes and are interpreted to have formed as a result of the propagation of crystal defects during growth rather than by syn-growth deformation due to shear stresses between viscous leachate slurry and the agitator inside the autoclave. The presence of extended defects in the scale microstructure has implications for the solubility and reactive stability of mineral processing waste as well as for the development of scale growth inhibitors.
机译:目前,在红土镍矿高压 酸浸过程中高压釜内结垢的形成代表了加工厂中的一个重要的工业问题。在本研究中,使用电子背向散射研究了在高压酸 浸出高压釜内搅拌棒上形成的钠铁矾 水垢的晶体学显微结构。 > 衍射(EBSD)。反向散射电子成像显示了钠铁矾的组成 层,具有分散的次要氧化铁晶体 和规则间隔的平行层微孔。 EBSD对鳞片的分析 显示,钠铁锰铁矿形成细长的 晶粒,具有强烈的(0001)晶体学首选取向 ,c轴在晶面内对齐。搅拌器基板, 与流体的单轴沉淀一致。 natrojarosite 颗粒包含一个低角度 (<15°)边界的复杂内部子结构,该边界定义了细长的子颗粒, 最多可容纳40°跨 单个晶粒的系统性取向错误。低角度亚晶界不具有简单的 孪生关系或低折射率取向错误轴,并且被解释为 >在生长过程中出现晶体缺陷,而不是通过同生生长变形 ,这是由于在高压釜内的粘性渗滤液浆液和 搅拌器之间的剪切应力引起的。氧化皮微观结构中存在扩展缺陷 对矿物加工废料的溶解度 和反应稳定性以及 对氧化皮的发展都具有影响。生长抑制剂。

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    《American Mineralogist》 |2009年第9期|1111-1119|共9页
  • 作者单位

    The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University of Technology, GPO Box U 1987, Perth, Western Australia 6845, Australia;

    CSIRO Minerals (The Parker Centre), PO Box 7229, Karawara, Perth, Western Australia 6152, Australia;

    The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University of Technology, GPO Box U 1987, Perth, Western Australia 6845, Australia;

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