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

机译:Vicenice八面体的磷化镍: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 [(Ni1.83Fe1.21)3.04P0.96 to (Ni1.71Fe1.28Co0.01)3.00P1.00] lacks detailed and accurate powder data – with only 11 observed reflections down to 1.37 Å. 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 (Ni1.69Fe1.31)3.00P1.00) and a hypothetical Ni3P end-member. Unit-cell dimensions of the synthetic analogue of Ni1.68Fe1.33P0.99 composition from individual peak profile fitting of XRD data collected with Cu radiation are a = 9.0168(2) Å, c = 4.4491(1) Å, V = 361.72(1) Å 3 and those for Ni3P composition are a = 8.9546(1) Å, c = 4.38714(8) Å, V = 351.783(8) Å 3. The space group of the mineral is I and Z = 8. The crystal structure refined from powder data by the Rietveld method is consistent with that refined and published for Fe3P and Ni3P 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:从Butler 陨石[(Ni 1.83 Fe 1.21 3.04 P 0.96 转换为(Ni 1.71 Fe 1.28 Co 0.01 3.00 P 1.00 ] 缺少详细而准确的粉末数据-仅11 观察到的反射低至1.37Å。因此,该阶段没有 晶体结构信息。在这里,我们介绍了在Vicenice IID介质八面体(具有 平均经验公式为(Ni 1.69 Fe 1.31 3.00 P 1.00 )和假定的 Ni 3 个最终成员。 Ni 1.68 Fe 1.33 P 0.99 组成的合成类似物 的单个峰分布 用铜辐射收集的XRD数据的拟合度为a = 9.0168(2) Å,c = 4.4491(1)Å,V = 361.72(1)Å 3 3 P组成的sup>和 分别为a = 8.9546(1)Å,c = 4.38714(8) Å,V = 351.783 (8)Å 3 。矿物 的空间群是I,Z =8。通过Rietveld方法从粉末数据精制的 的晶体结构与精制的 一致。并从单晶数据中公开了Fe 3 P和Ni 3 P合成化合物 以及铁占主导的schreibersite。 < / sup>但是,由于铁 和镍的散射相似,因此我们无法直接从中分离出磷化镍的合成类似物中的位点占有率 。 Vicenice 铁陨石。

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