首页> 外文期刊>Dalton transactions: An international journal of inorganic chemistry >Mixed-valence phosphato-hydrogenphosphato-iron network compounds ~1_∞{[C_4N_2H_(11.6)]_(1.5)[Fe~(II)Fe~(III)(PO_4)(H_(0.8)PO_4)_2]·H_2O} and ~3_∞[Fe~(II)_5Fe~(III)_2(PO_4)_2(H_(0.5)PO_4)_4]: structure elucidation with the help of Mossbauer spectro
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Mixed-valence phosphato-hydrogenphosphato-iron network compounds ~1_∞{[C_4N_2H_(11.6)]_(1.5)[Fe~(II)Fe~(III)(PO_4)(H_(0.8)PO_4)_2]·H_2O} and ~3_∞[Fe~(II)_5Fe~(III)_2(PO_4)_2(H_(0.5)PO_4)_4]: structure elucidation with the help of Mossbauer spectro

机译:价氢-磷酸氢铁-铁络合物〜1_∞{[C_4N_2H_(11.6)] _(1.5)[Fe〜(II)Fe〜(III)(PO_4)(H_(0.8)PO_4)_2]·H_2O}和〜3_∞[Fe〜(II)_5Fe〜(III)_2(PO_4)_2(H_(0.5)PO_4)_4]:借助Mossbauer光谱进行结构解析

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摘要

The mixed-valence iron phosphates ~1_∞{[C_4N_2H_(11.6)]_(1.5)[Fe~(II)Fe~(III)(PO_4)(H_(0.8)PO_4)_2]·H_2O} and ~3_∞[Fe~(II)_5Fe~(III)_2(PO_4)_2(H_(0.5)PO_4)_4] (2) have been synthesized by hydrothermal methods. Their crystal structures were determined by single-crystal X-ray diffraction and Mossbauer spectroscopy. Mossbauer spectroscopy suggests the Fe centers in compound 1 to be mostly in a trapped, mixed-valence +2 and +3 oxidation state from which the average protic hydrogen occupation on HPO_4 and piperazinedium is calculated to be 0.8. At 4 K there is an intervalence tunneling process between part of the Fe~(2+) and Fe~(3+) atoms. Compound 1 contains linear strands of corner-sharing {FeO_4} and {PO_4} tetrahedra. The Fe atoms are bridged by Fe-O-P-O-Fe and Fe-O-Fe linkages. The strands are held together by hydrogen bonding interactions involving the piperazinedium and the water molecules of crystallization as well as complementary H-bonds between the HPO_4-groups. The iron phosphate 2 is found from Mossbauer spectroscopy to be a trapped mixed-valence system with about 30% Fe~(3+)/70% Fe~(2+) which translates perfectly into Fe~(II)_5Fe~(III)_2 from which a total of two protic hydrogens on phosphate has been calculated. The crystal quality permitted the protic hydrogens in 1 and 2 to be found and their positions freely refined. At 4.2 K the Fe~(3+) is completely and Fe~(2+) partially magnetically ordered in 2. Compound 2 is a three-dimensional framework constructed from edge- and corner-sharing {FeO_6} octahedra and {FeO_5} trigonal bipyramids together with the {PO_4} tetrahedra. Temperature-variable magnetic measurements confirm the oxidation state assignments for 1 and 2 through a matching experimental and calculated values for μ_(eff) 300 K.
机译:混合价磷酸铁〜1_∞{[C_4N_2H_(11.6)] _(1.5)[Fe〜(II)Fe〜(III)(PO_4)(H_(0.8)PO_4)_2]·H_2O}和〜3_∞ [Fe〜(II)_5Fe〜(III)_2(PO_4)_2(H_(0.5)PO_4)_4]已通过水热法合成。它们的晶体结构通过单晶X射线衍射和Mossbauer光谱法确定。 Mossbauer光谱表明,化合物1中的Fe中心大部分处于俘获,混合价+2和+3氧化态,据此,质子在HPO_4和哌嗪鎓上的平均氢占据率为0.8。在4 K处,部分Fe〜(2+)和Fe〜(3+)原子之间存在间隔隧穿过程。化合物1包含角共享{FeO_4}和{PO_4}四面体的线性链。 Fe原子通过Fe-O-P-O-Fe和Fe-O-Fe键桥接。这些链通过涉及哌嗪鎓和结晶水分子的氢键相互作用以及HPO-4-基团之间的互补H键保持在一起。从Mossbauer光谱学中发现磷酸铁2是一种捕获的混合价体系,具有约30%Fe〜(3 +)/ 70%Fe〜(2+),可以完美地转化为Fe〜(II)_5Fe〜(III) _2,据此计算出磷酸盐上总共两个质子氢。晶体质量允许发现1和2中的质子氢,并且可以自由调节其位置。在4.2 K时,Fe〜(3+)完全被磁化,而Fe〜(2+)在2中部分磁化。化合物2是三维结构,由{FeO_6}八面体和{FeO_5}三角形的边角共享双锥体和{PO_4}四面体。温度可变的磁测量结果通过匹配的实验值和计算得出的μ_(eff)300 K值来确认1和2的氧化态分配。

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