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Cristallogenèse exploratoire, structure cristalline et propriétés physiques des deux nouveaux composés dans le système PbO-Fe2O3-P2O5

机译:在PbO-Fe2O3-P2O5系统中探索两种新化合物的结晶生成,晶体结构和物理性质

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摘要

A new oxyphosphate compound PbFe3O(PO4)3 has been discovered. Its crystal structure was characterized by single crystal X-ray diffraction (XRD) between 293 and 973 K (monoclinic symmetry P 21/m, a = 7.5826 Å, b = 6.3759 Å, c = 10.4245 Å and  = 99.956 °, Z = 2, at room temperature). DC magnetic susceptibility and specific heat measurements performed on single crystals unveiled an unusual sequence of second order ferromagnetic-like phase transitions at Tc1 = 31.8 K, T2 = 23.4 K and Tc3 ~ 10 K. AC magnetic susceptibility suggests a glassy-like dynamics between ~ 20 K and Tc3. A first extraction of the critical exponents (β,γ,δ) was performed by ac magnetic susceptibility in both PbFe3O(PO4)3 powders and single crystals and the values were found to be consistent with mean-field theory.AFe3O(PO4)3 (A= Ca, Sr and Pb) powder compounds were studied by means of X-Ray diffraction (XRD), from 300 to 6 K in the case of A=Pb, electron-probe microanalysis (EPMA) coupled with wavelength dispersion spectroscopy (WDS), Raman and diffuse reflectance spectroscopies, specific heat and magnetic properties measurements. Magnetization, magnetic susceptibility and specific heat measurements carried out on AFe3O(PO4)3 (A= Ca, Sr and Pb) powders firmly establish a series of three ferromagnetic (FM)-like second order phase transitions spanned over the 32 – 8 K temperature range. Diffuse reflectance measurements reveal two broad absorption bands at 1047 and 837 nm, in both PbFe3O(PO4)3 and SrFe3O(PO4)3 powders, with peak cross sections ~10-20 cm2 typical of spin-forbidden and forced electric dipole transitions.Further exploration of the PbO-Fe2O3-P2O5 system led to the discovery of a new langbeinite phase, Pb3Fe4(PO4)6, the crystal structure of which was solved by room temperature single crystal XRD (P 21 3, Z=4, a=9,7831(2) Å). This phase does not undergo any structural phase transition down to 6 K nor any kind of long range ordering down to 2 K.
机译:已经发现了一种新的含氧磷酸盐化合物PbFe3O(PO4)3。其晶体结构的特征是在293至973 K之间的单晶X射线衍射(XRD)(单斜对称性P 21 / m,a = 7.5826Å,b = 6.3759Å,c = 10.4245Å和= 99.956°,Z = 2,在室温下)。在单晶上进行的直流磁化率和比热测量揭示了Tc1 = 31.8 K,T2 = 23.4 K和Tc3〜10 K时异常的类似于二阶铁磁相变的序列。交流磁化率表明〜之间存在类似玻璃态的动力学20 K和Tc3。通过交流磁化率在PbFe3O(PO4)3粉末和单晶中对临界指数(β,γ,δ)进行了首次提取,发现该值与平均场理论相符.AFe3O(PO4)3 (A = Ca,Sr和Pb)粉末化合物通过X射线衍射(XRD)研究,在A = Pb的情况下从300到6 K,电子探针微分析(EPMA)结合波长色散光谱法( WDS),拉曼和漫反射光谱,比热和磁性能测量。在AFe3O(PO4)3(A = Ca,Sr和Pb)粉末上进行的磁化,磁化率和比热测量牢固地建立了跨越32 – 8 K温度的一系列三个类似铁磁(FM)的二阶相变。范围。漫反射测量结果显示,在PbFe3O(PO4)3和SrFe3O(PO4)3粉末中,在1047和837 nm处有两个宽吸收带,其峰值横截面约为10-20 cm2,这是自旋禁止和强迫电偶极跃迁的典型特征。对PbO-Fe2O3-P2O5系统的探索导致发现了新的朗贝氏体相Pb3Fe4(PO4)6,其晶体结构通过室温单晶XRD解析(P 21 3,Z = 4,a = 9 ,7831(2)Å)。此相不会经历任何低至6 K的结构相变,也不会经历任何低至2 K的长程有序。

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    El Hafid Moulay El Hassan;

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  • 年度 2013
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