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首页> 外文期刊>Mineralogical Magazine >Nickelphosphide from the Vicenice octahedrite: Rietveld crystal structure refinement of synthetic analogue
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Nickelphosphide from the Vicenice octahedrite: Rietveld crystal structure refinement of synthetic analogue

机译:Vicenice八面体中的磷化镍:合成类似物的Rietveld晶体结构细化

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The original description of nickelphosphide from the Butler meteorite [(Ni_(1.83)Fe_(1.21))SIGMA3.04P_(0.96) to (Ni_(1.71)Fe_(1.28)Co_(0.01))SIGMA3.00P_(1.00)] lacks detailed and accurate powder data - with only 11 observed reflections down to 1.37 A. Consequently, no crystal structure information for this phase is available. Here we present the crystal structure for a synthetic analogue of the phase found in the Vicenice IID medium octahedrite (with a mean empirical formula of (Ni_(1.69)Fe_(1.31))SIGMA3.00P_(1.00)) and a hypothetical Ni3P end-member. Unit-cell dimensions of the synthetic analogue of Ni_(1.68)Fe_(1.33)P_(0.99) composition from individual peak profile fitting of XRD data collected with Cu radiation are a =9.0168(2) A, c = 4.4491(1) A, V= 361.72(1) A~3 and those for Ni_3P composition are a = 8.9546(1) A, c =4.38714(8) A, V = 351.783(8) A~3. The space group of the mineral is I4-bar and Z= 8. The crystal structure refined from powder data by the Rietveld method is consistent with that refined and published for Fe_3P and Ni_3P synthetic compounds as well as Fe-dominant schreibersite from single-crystal data. However, because of the similarity of the scattering of iron and nickel, we were not able to refine directly the site occupancies in the synthetic analogue of the nickelphosphide from the Vicenice iron meteorite.
机译:缺少从巴特勒陨石[(Ni_(1.83)Fe_(1.21))SIGMA3.04P_(0.96)到(Ni_(1.71)Fe_(1.28)Co_(0.01))SIGMA3.00P _((1.00)]的磷化镍的原始描述准确的粉末数据-仅观察到11个反射信号,低至1.37A。因此,该阶段没有晶体结构信息。在这里,我们介绍在Vicenice IID中等八面体中发现的相的合成类似物的晶体结构(平均经验公式为(Ni_(1.69)Fe_(1.31))SIGMA3.00P_(1.00)),并假设一个Ni3P末端-会员。由Cu辐射收集的XRD数据的单个峰轮廓拟合得出的Ni_(1.68)Fe_(1.33)P_(0.99)组成的合成类似物的晶胞尺寸为a = 9.0168(2)A,c = 4.4491(1)A ,V = 361.72(1)A〜3,Ni_3P组成为a = 8.9546(1)A,c = 4.38714(8)A,V = 351.783(8)A〜3。矿物的空间群为I4-bar,Z =8。通过Rietveld方法从粉末数据中精炼的晶体结构与针对Fe_3P和Ni_3P合成化合物以及单晶的Fe占优势的菱铁矿精炼和公布的晶体结构一致。数据。但是,由于铁和镍散射的相似性,我们无法直接从Vicenice铁陨石合成的磷化镍的合成类似物中直接改善位点占有率。

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