Mssbauer谱学及其在熔渣铁离子行为研究中的应用张丽君

综述了M¨ossbauer谱学原理、基本参数和测定方法 ;分析了熔渣中铁离子行为 ,并从化学和谱学角度阐述了Fe2 +、Fe3 +tet 和Fe3+oct 离子的M¨ossbauer谱特征 ;讨论了铁离子行为与熔渣碱度、渣中全铁量及Na2 O、Al2 O3 含量的关系 ;提出该领域的研究前景     

[Fe_3O(Ala)_6(H_2O)_3](ClO_4)_7和[Fe_3O(Gly)_6(H_2O)_3](NO_3)7·3H_2O的顺磁共振谱及变温磁化率研究

本文通过对 [Fe3 O(Ala) 6(H2 O) 3 ](Cl O4) 7和 [Fe3 O(Gly) 6(H2 O) 3 ](NO3 ) 7· 3H2 O的 ESR谱的解析及变温磁化率的研究 ,得出它们的 ESR谱具有各向同性的特点 ;朗德因子分别为 2 .0 19和 1.997;两种配合物中铁离子间有反铁磁相互作用     

[Fe3O（Ala）6（H2O）3]（ClO4）7和[Fe3O（Gly）6（H2O）3]（NO3）7·3H2O的顺原共振谱及变温磁化率研究

本文通过对[Fe 3O(Ala) 6(H 2O) 3](ClO 4) 7和[Fe 3O(Gly) 6(H 2O) 3](NO 3) 7·3H 2O的ESR谱的解析及变温磁化率的研究,得出它们的ESR谱具有各向同性的特点;朗德因子分别为2.019和1.997;两种配合物中铁离子间有反铁磁相互作用.     

[Fe3O(Ala)6(H2O)3](ClO4)7和[Fe3O(Gly)6(H2O3)(NO3)7)·3H2O]顺磁共振谱及变温磁化率研究

本文通过对[Fe 3O(Ala) 6(H 2O) 3](ClO 4) 7和[Fe 3O(Gly) 6(H 2O) 3](NO 3) 7·3H 2O的ESR谱的解析及变温磁化率的研究,得出它们的ESR谱具有各向同性的特点;朗德因子分别为2.019和1.997;两种配合物中铁离子间有反铁磁相互作用.     

多金属氧酸盐α-Na_6H〔GeW_9Fe_3(H_2O)_3O_(37)〕·16H_2O的合成和光谱

合成了多金属氧酸盐 α- Na6H〔 Ge W9Fe3 (H2 O) 3 O3 7〕· 16 H2 O,通过元素分析、红外、紫外、光电子能谱、极谱和穆斯堡尔谱等手段进行了表征 ,并讨论和研究了该配合物的谱学性质     

一种用于同位素分离在线穆斯堡尔谱学的PPAC

研制了一种用于同位素分离在线穆斯堡尔谱学的平行板雪崩计数器，计数器仅重40g。用它测量由穆斯堡尔共振吸收后放出的内转换电子，采用85％^119Sn同位素增丰的SnO2作为阴极吸收材料，测得的穆斯堡尔谱的信噪比为11，是一种适合在线穆斯堡尔实验的计数器。对该计数器的性能进行了讨论。A Parallel Plate Avalanche Counter （PPAC） with weighted about 40 g was developed for isotope separator on-line Moessbauer Spectroscopy. It detects the internal conversion electrons emitted from the resonance Moessbauer nuclide. The signal-to-noise ratio of the spectra reaches 11 for 85% enriched ^119SnO2 cathode and absorber. It is an effective detector for on-line Moessbauer experiments. The perform ance of the counter was discussed in detail.     

多金属氧酸盐α-Na6H[GeW9Fe3(H2O)3O37]·16H2O的合成和光谱

合成了多金属氧酸盐α-Na6H[GeW9Fe3(H2O)3O37]16H2O，通过元素分析、红外、紫外、光电子能谱、极谱和穆斯堡尔谱等手段进行了表征，并讨论和研究了该配合物的谱学性质。     

钕、钐-邻苯二甲酸-1,10-邻菲咯啉配合物的合成及谱学性质

合成了稀土钕、钐的邻苯二甲酸 1,10 邻菲咯啉二元、三元配合物 ,通过元素分析、1HNMR、中红外光谱、差热 热重分析 ,确定了配合物的组成为RE2 L3 ·2H2 O ,RE2 L3 phen·2H2 O(RE :稀土离子 ,L :邻苯二甲酸根 ,phen :1,10 邻菲咯啉 ) ,讨论了配合物的谱学性质 ,并对配合物的远红外光谱、拉曼光谱进行了归属研究。     

La_(2/3)Ca_(1/3)Mn_(1-x)Fe_xO_3化合物铁掺杂效应的Mssbauer谱研究

利用固相反应方法制备了名义成分为La2 / 3Ca1 / 3Mn1 -xFexO3(0 .0 1≤x≤ 0 .2 0 )的一系列样品 .在整个掺杂范围内晶体结构没有明显变化 .在室温下测量了各样品的M ssbauer谱 ,拟合结果表明 +3价高自旋态的铁离子占据锰的八面体晶位 ,随Fe掺杂量的增加 ,铁离子的 3d电子出现局域化趋势 ,并伴随Fe O配位体畸变程度的增强 .本文对此进行了讨论 .     

稀土与桂皮酸、2,2''''-联吡啶三元配合物合成、表征及荧光性质

以2,2'-联吡啶(bipy)、桂皮酸(HL)为配体与稀土离子(RE=Tb, Gd, Eu, Sm, Nd)在乙醇溶液中合成了三元稀土配合物. 通过元素分析、摩尔电导、紫外光谱、红外光谱、差热-热重分析, 确定了配合物的组成为REL3·bipy. 并讨论了配合物的谱学性质及EuL3和EuL3·bipy·H2O的荧光性能. EuL3的荧光强度比EuL3·bipy·H2O的荧光强度强4.5倍.     

The relaxation dynamics, iron valence state, and M?ssbauer effect in PFN ceramics

The dielectric properties, X-ray emission spectra, and M?ssbauer effect in ceramics made of PbFe_1/2Nb₁/₂O₃ (PFN) compound were studied. The relaxation dynamics revealed above Curie temperature TC at a frequency of 3 × 10⁻²–10⁵ Hz is described in detail. Analysis of the X-ray emission and M?ssbauer spectra showed that at room temperature (T = 300 K), the iron ions in PFN are mainly in the high-spin valence state Fe³⁺. The M?ssbauer spectral parameters obtained at T = (300, 353, and 393 K) indicate an octahedral environment for Fe³⁺ in both the ferroelectric and paraelectric phases.     

Investigation of the transition of acrylate cation exchangers from solidlike into highly elastic state under hydration

The transition from solid-like (glassy) state into the (elastic) state with high intramolecular mobility under hydration was investigated for two⁵⁷Fe³⁺-substituted cation exchangers (SGK ?7 and SG ?1 m with acrylic and methacrylic nature of chains). The transition was observed as sharp change of Mössbauer lineshape (appearance of quasielastic components) and decrease of Mössbauer effect probability. The region of hydration degrees in which the transition occurs in both systems varies from 1 to 3–4 H₂O molecules per ?COOH group depending on cross-linkage concentration in a nonmonotonous way.     

Magnetic interaction in ferrous antimonite, FeSb2O4, and some derivatives

Ferrous antimonite, FeSb(2)O(4), which is isostructural with Pb(3)O(4), and some lead-?and cobalt-doped variants of composition FeSb(1.5)Pb(0.5)O(4) and Co(0.5)Fe(0.5)Sb(1.5)Pb(0.5)O(4) have been examined by (57)Fe and (121)Sb?M?ssbauer spectroscopy. Antimony is present as Sb(3+). The presence of Pb(2+) on the antimony site induces partial oxidation of Fe(2+) to Fe(3+). There is no Verwey-type transition in which electrons are shared between iron in different oxidation states. The quasi-one-dimensional magnetic structure gives rise to situations in which weakly coupled Fe(2+) ions can coexist in a non-magnetic state alongside Fe(3+) ions in a magnetically ordered state.     

Response of La0.8Sr0.2CoO3-δ to perturbations on the CoO3 sublattice

Emission and transmission M?ssbauer studies of La_0.8Sr_0.2CoO_3-δ perovskites doped with ∼0.02 stoichiometric units of oxygen vacancy or 2.5% iron corroborate the occurrence of electronic phase separation in these systems. The effect of the small perturbation of the CoO₃ sublattice with either iron ions or oxygen vacancies on the bulk magnetization as well as on the M?ssbauer spectra is in good agreement with the double exchange based cluster model. The magnetoresistance does not show any peak near the Curie temperature, but reaches -84% in a field of 7.5 T at T = 8 K. Below T_C ≈ 180 K the M?ssbauer spectra distinctly include the contribution from paramagnetic and ferromagnetic regions, providing direct evidence for phase separation. No contribution to the spectra from Fe⁴⁺ ions can be observed, which is an unambiguous evidence that at low concentration iron (either directly doped or formed from ⁵⁷Co by nuclear decay) is accommodated in the cobaltate lattice as Fe³⁺ ion.     

M?ssbauer study of contaminated soils by industrial activity in Paramonga city, Region Lima Provinces, Peru

In this work we characterize soils from the Paramonga city, Region Lima Provinces in Peru, which are contaminated by residual chemicals (Br, As and Sr) from sugar and paper industry in the city. Four samples were collected, labelled as S1, S2, S3 and S4 and analized by X-ray diffraction (XRD), energy-dispersive X-ray fluorescence (EDXRF) and M?ssbauer spectroscopy. For all the samples, the chemical analysis by EDXRF revealed the presence of Fe, Mn, Cu, Zn, K, Br, Sr. The XRD detected the presence of quartz as principal phase and copper sulfide and potassium magnesium as secondary phases. The M?ssbauer spectra at room temperature (RT) for all the samples exhibit sextets which reveal the presence of an iron oxide or hydroxide. The fitting M?ssbauer for both samples S1 and S4 have three doublets corresponding to iron in paramagnetic phases and a magnetic component of around 35.50?T corresponding to goethite, α-FeOOH. Sample S2 have two magnetic phases with internal fields of 37?T and 34.6?T which correspond to the goethite and other incorporated element in the structure. The sample S3 have three magnetic fields of H1?=?36.8?T, H2?=?33.6?T and H3?=?34.8?T which correspond to hydroxide iron, pyrrhotite and goethite respectively.     

Exchange bias in iron oxide nanoclusters

Iron oxide nanoclusters have been prepared by the gas-phase aggregation technique to form thin film structures with very high exchange bias values (up to 3000?Oe at low temperatures). Composition has been analysed by x-ray absorption and M?ssbauer spectroscopies in order to elucidate the actual origin of the observed magnetic behaviour. The formation of a metal-oxide core-shell arrangement to explain the observed exchange bias has to be discarded since results show no metallic iron content and the main presence of α-Fe(2)O(3). The observed weak ferromagnetism and exchange bias are in agreement with the obtained size of α-Fe(2)O(3) nanoparticles: weak ferromagnetism because of the well-known spin canting in this antiferromagnetic structure and exchange bias because of the interaction between different spin sublattice configurations promoted by the modification of iron coordination in α-Fe(2)O(3) nanoparticles. Moreover, the preparation method is proposed for tuning both magnetization and exchange bias values by modification of the preparation conditions of α-Fe(2)O(3) nanoparticles, which open new possibilities in the design of new materials with required properties.     

Measurement of local magnetic fields in the CuO2 planes of CuBa2YCu2O7-delta superconductors

A fully oxygenated Cu(1)Ba2YCu(2)2O7-delta sample having 0.167 at % of the Cu atoms replaced by enriched 57Fe was synthesized. As confirmed by 57Fe M?ssbauer spectroscopy approximately 16% of the Fe atoms entered the superconducting Cu(2)O2 planes. M?ssbauer spectra recorded at various temperatures between 77 and 373 K exhibited the presence of a weak magnetic hyperfine interaction in the Fe atoms entering the CuO2 planes. The nonzero internal field obtained from the M?ssbauer data increased following a Brillouin-type behavior, from the estimated Néel-like temperature of approximately 400 K down to 96 K where it reached approximately 1.5 T. Upon further cooling below T_{c} the internal field decreased fast down to approximately 0.4 T at 77 K. The presence of the internal field is believed to be related to magnetic correlations among the CuO2-plane atoms, i.e., to reflect local antiferromagnetic coupling between the Cu atoms.     

Cation distribution in Eu-Sc-Fe garnets

The cation distribution has been studied with ⁵⁷Fe Mössbauer spectroscopy in the garnet system Eu_3?ySc_2+yFe₃O₁₂ with y = 0.0, 0.2 and 0.5. It is shown that the previously proposed cation distribution is not correct. The problem of possible impurities in the investigated system is discussed in detail. Several possible cation distributions are considered compatible with Mössbauer data. Mössbauer results combined with the composition dependence of lattice constants show that the tetrahedral sites are accessible to Sc³⁺ ions. The system studied is a second example of a garnet structure in which Sc³⁺ ions are found at the tetrahedral sites. A small fraction of Sc³⁺ ions for the samples y = 0.2 and 0.5 is also found at the dodecahedral sites.     

Synthesis,magnetic properties and Mössbauer spectroscopy for the pyrochlore family Bi2BB′O7 with B=Cr and Fe and B′=Nb,Ta and Sb

The samples Bi₂BB′O₇, with B=Cr and Fe and B′=Nb, Ta and Sb were prepared by solid state method. The crystallographic structure was investigated on the basis of X-ray powder diffraction data. Rietveld refinements show that the crystal structure is cubic, space group Fd-3m. The Bi³⁺ cation on the eight-coordinate pyrochlore A-site shows displacive disorder, as a consequence of its lone pair electron con?guration. There is also a considerable A-site disorder shown by Rietveld Analysis and confirmed in the case of the iron containing samples with Mössbauer spectroscopy. The magnetic measurements show paramagnetic behavior at all temperatures for the Cr oxides. The Fe pyrochlores show antiferromagnetic order around 10 K.