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首页> 外文期刊>Mineralogical Magazine >Jarosite-butlerite intergrowths in non-stoichiometric jarosites: crystal chemistry of monoclinic natrojarosite-hydroniumjarosite phases
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Jarosite-butlerite intergrowths in non-stoichiometric jarosites: crystal chemistry of monoclinic natrojarosite-hydroniumjarosite phases

机译:非化学计量黄钾铁矾中的黄铁矿-钠钙石共生体:单斜钠铁矾-亚氢黄铁矾相的晶体化学

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Monoclinic, non-stoichiometric natrojarosite-hydroniumjarosite solid solution phases have been synthesizedhyd rothermally over a range of temperatures, starting compositions andreaction times, and have been characterized using Rietveld refinement of synchrotron X-ray diffraction data, and chemical andthermal analyses. The H atom locations have been obtainedfrom refinement of neutron diffraction data on a deuterated sample. The results confirm a direct relationship between the monoclinic distortion and the ordering of iron site vacancies in one of two independent iron sites. Ordering of iron vacancies gives rise to domains containing butlerite-like 7 A chains of cornerconnected octahedra and tetrahedra. The formation of these chains within (100) planes results in an expansion of the monoclinic a lattice parameter anda contraction of the c parameter relative to stoichiometric jarosites. The results support a recent model for iron deficiency, whereby an iron vacancy is compensatedby the replacement of four coordinatedOH ~- ions by H_2O molecules, with one of the H_2O molecules coming from deprotonation of H_3O~+. The general formula, basedon intergrowth of stoichiometric jarosite andnon-stoichiometric, butlerite-like regions, is [(Na,H_3O)Fe_3 (SO_4)_2(OH)_6]_(1-y)[(H_2O)Fe_2(SO_4)_2(OH)_2(H_2O)_4]_y.
机译:已经在一定温度,起始组成和反应时间范围内热合成了单斜,非化学计量的萘甲酸铁钠-亚硝酸钠铁矾固溶体相,并使用同步加速器X射线衍射数据的Rietveld精炼以及化学和热分析对其进行了表征。 H原子的位置是从氘化样品上的中子衍射数据的精炼中获得的。结果证实了在两个独立的铁矿场之一中,单斜率畸变与铁矿场空位的排序之间存在直接关系。铁空位的排序产生了包含角连接的八面体和四面体的类似钠钙石的7 A链的域。这些链在(100)平面内的形成导致单斜晶格参数的膨胀和c参数相对于化学计量的黄晶石的收缩。结果支持最新的铁缺乏模型,通过用H_2O分子取代四个配位的OH +离子来补偿铁的空位,其中一个H_2O分子来自H_3O〜+的去质子化。基于化学计量的黄钾铁矾和非化学计量的,类似钠钙石的区域的共生,通式为[(Na,H_3O)Fe_3(SO_4)_2(OH)_6] _(1-y)[(H_2O)Fe_2(SO_4)_2 (OH)_2(H_2O)_4] _y。

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