Luminescence of vanadium and rare earth ions in alkaline earth sulfates

The luminescence of samples MeSO₄V, RE (Me = Mg, Ca, Ba) depends strongly on the nature of the Me ions. The amount of association of the V⁵⁺ and RE³⁺ ions can be estimated from the measured quantum efficiencies.     

Antiferromagnetic coupling between rare earth ions and semiquinones in a series of 1:1 complexes

We use the strategy of diamagnetic substitution for obtaining information on the crystal field effects in paramagnetic rare earth ions using the homologous series of compounds with the diamagnetic tropolonato ligand, Ln(Trp)(HBPz(3))(2), and the paramagnetic semiquinone ligand, Ln(DTBSQ)(HBPz(3))(2), (DTBSQ = 3,5-di-tert-butylsemiquinonato, Trp = tropolonate, HBPz(3)= hydrotrispyrazolylborate) for Ln = Sm(iii), Eu(iii), Gd(iii), Tb(iii), Dy(iii), Ho(iii), Er(iii) or Yb(iii). The X-ray crystal structure of a new form of tropolonate derivative is presented, which shows, as expected, a marked similarity with the structure of the semiquinonate derivative. The Ln(Trp)(HBPz(3))(2) derivatives were then used as a reference for the qualitative determination of crystal field effects in the exchange coupled semiquinone derivatives. Through magnetisation and susceptibility measurements this empirical diamagnetic substitution method evidenced for Er(iii), Tb(iii), Dy(iii) and Yb(iii) derivatives a dominating antiferromagnetic coupling. The increased antiferromagnetic contribution compared to other radical-rare earth metal complexes formed by nitronyl nitroxide ligands may be related to the increased donor strength of the semiquinone ligand.     

Local order around rare earth ions during the devitrification of oxyfluoride glasses

Erbium L(3)-edge extended x-ray absorption fine structure (EXAFS) measurements were performed on rare earth doped fluorosilicate and fluoroborate glasses and glass ceramics. The well known nucleating effects of erbium ions for the crystallization of cubic lead fluoride (based on x-ray diffraction measurements) and the fact that the rare earth ions are present in the crystalline phase (as indicated by Er(3+) emission spectra) seem in contradiction with the present EXAFS analysis, which indicates a lack of medium range structural ordering around the Er(3+) ions and suggests that the lead fluoride crystallization does not occur in the nearest neighbor distance of the rare earth ion. Molecular dynamics simulations of the devitrification process of a lead fluoride glass doped with Er(3+) ions were performed, and results indicate that Er(3+) ions lower the devitrification temperature of PbF(2), in good agreement with the experimental results. The genuine role of Er(3+) ions in the devitrification process of PbF(2) has been investigated. Although Er(3+) ions could indeed act as seeds for crystallization, as experiments suggest, molecular dynamics simulation results corroborate the experimental EXAFS observation that the devitrification does not occur at its nearest neighbor distance.     

Complex formation of p-nitrocalix[6]arene with rare earth metal ions.

p-Nitrocalix[6]arene (CALX-N6, L) formed a 1:1 metal complex, ML, with light rare earth metal ions (M3+), such as La3+, Pr3+ and Nd3+ except Ce3+, but formed a 1:2 (M(3+):L) complex, ML2 (the charge of the complex is omitted) with heavy rare earth metal ions, such as Sm(3+)-Lu3+ including Y3+. The conditional stability constants of these 1:1 and 1:2 complexes, KML and KML2, were measured by a ligand displacement method using absorption spectrophotometry in 4% (v/v) acetone aqueous solution at pH 9.65 +/- 0.15 and 25 degrees C.     

Judd-Ofelt analysis and multiphonon relaxations of rare earth ions in fluorohafnate glasses

The optical properties of fluorohafnate glasses doped with Pr³⁺, Nd³⁺, Sm³⁺, Dy³⁺, Ho³⁺, Er³⁺, and Tm³⁺ have been studied. From optical absorption measurements and using Judd-Ofelt theory, JO parameters Ω₂, Ω₄, and Ω₆ have been obtained. The Ω₂ values indicate that fluorohafnate glasses present a less ionic character than fluorozirconates. Multiphonon emission probabilities for several levels of Er³⁺ and Ho³⁺ ions were determined by the difference between the measured rates and the calculated radiative transition probabilities. The results are almost the same as those found in fluorozirconates. Multiphonon emission probabilities are in agreement with the energy-gap law followed by rare-earth ions in crystals and glasses.     

Raman spectroscopic study on the coordination behavior of rare earth ions in N-methylacetamide

The coordination behavior of rare earth (Ln (3+)) ions in N-methylacetamide (NMA) solution has been investigated at room temperature by Raman spectroscopy. The behavior of the symmetric Raman Ln-Cl stretching (nu Ln-Cl) band, and amide I (nu AI), and III (nu AIII) bands of NMA with the rare earth series is discussed in conjunction with the change in the coordination structure occurring in the middle of the rare earth series. A competition for a coordination equilibria between a Cl (-) ion and an NMA molecule from the rare earth chloride-NMA complex might occur in the middle rare earth region. It is demonstrated that the change in the coordination structure of Ln (3+) ions in NMA is due to an elimination of an NMA molecule.     

Operational modes for transient isotachophoretic preconcentration-capillary zone electrophoresis and detectable concentration of rare earth ions.

Operational modes for transient isotachophoretic preconcentration capillary zone electrophoresis (tr-ITP-CZE) were studied by using 5 microM and 0.5 microM rare earth mixtures as analytes in comparison with field-enhanced sample stacking. After examination of several operational modes for tr-ITP, it was found that tr-ITP effectively occured even if both the leading electrolyte and the terminating electrolyte were injected after the sample plug. This was explained as the result of a field-enhanced stacking for both sample components and the leading and terminating ions. The observed theoretical plate numbers were 4-20 times higher than those obtained by normal stacking; and the estimated low limit of detectable concentration of rare-earth elements (REE) was ca. 0.1 microM which was 2.5 times lower compared to normal stacking. For the 0.5 microM sample, a concentration factor of 20 000 could be achieved after only tr-ITP.     

稀土发挥生物效应的机制及其作用物种探讨

稀土在工业、医药领域、基础研究以及在我国的广泛农用引起了人们对其生物效应机理以及可能毒性的关注.在稀土生物学效应机理及毒性的研究中,无论是在动物水平还是细胞层次,引起生物学效应的稀土物种都是一个关键问题,一直存在争议.本文对以动物、细胞为模型的生物效应研究中的实验条件进行分析,对生理条件下引起稀土生物学效应的可能物种提出"稀土离子池"(rare earth ion pool)模型,并对其引起生物学效应的活性物种以及与细胞膜相互作用的方式进行了探讨,以期为阐明复杂生物学体系中稀土化合物的作用机制提供思路.     

混合稀土离子的毛细管电泳电导法分离检测

采用高效毛细管电泳电导检测法分离检测了稀土离子。以醋酸-醋酸钠为背景电解质,4-吗啉乙磺酸（MES）为络合剂,在24kV的高压下,7种稀土离子得到子较好的分离。考察了背景电解质的pH和浓度,络合剂的浓度,分离电压等对稀土离子分离的影响。在选定的实验条件下,7种烯土离子在10min内守成分离检测。     

稀土元素与NEB二元配合物的pH电位法分析

氨三乙氧基三苯甲酸(ＮＥＢ)(ＮＥＢ·ＨＣｌ的分子结构式见下图)作为有立体选择性的配体,它与铀酰离子ＵＯ2(Ⅱ)配位作用已有报导[1]。在对ＮＥＢ质子化常数及二元体系Ｍ(Ⅱ)-ＮＥＢ·ＨＣｌ(Ｍ=Ｃｄ、Ｃｏ、Ｎｉ、Ｃｕ和Ｚｎ)配合物的稳定常数测定的基础上[2],本文在25℃及离子强度为0 2ｍｏｌ/ＬＫＮＯ3的条件下,用精密ｐＨ电位法考察二元体系ＲＥ(ＩＩＩ)—ＮＥＢ(ＲＥ=Ｌａ→Ｎｄ,Ｓｍ→Ｌｕ,Ｙ)中存在的配合物物种及其稳定常数。ＮＥＢ·ＨＣｌ结构式1　实验部分1 1　试剂和仪器ＮＥＢ·ＨＣｌ(Ｈ3Ｌ·ＨＣｌ,Ｌ3-=Ｃ27Ｈ24ＮＯ9)…     

Distribution of components in the rare earth ammonia synthesis catalysts and effect of additives

The distribution of components in the HG-1 ammonia catalyst promoted by rare earth oxide (successfully developed by the authors) was analyzed by electron microprobe photography. The results enable us to explain the effect of additives upon the activity as well as the remarkably high lifetime of catalyst.

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利用荧光浓度指示剂fura-2研究稀土离子的跨膜行为

本文提出了利用fura-2测量细胞内游离稀土离子浓度的定量方法。实验结果表明, 在模拟细胞内离子组成的条件下, 稀土离子La^3^+和Y^3^+与fura-2形成1:1的配合物。其配合物的表观离解常数分别为161nmol.dm^-^3和404nmol.dm^-^3,pH7.05, 有未配对f电子的Nd^3^+, Ho^3^+, Sm^3^+, Dy^3^+,Ce^3^+, Yb^3^+等稀土离子对荧光起萃灭作用。此性质使我们能够定性鉴定它们是否进入了细胞。我们使用如上性质, 利用单细胞阳离子测试系统, 以小鼠骨髓瘤细胞为模式细胞, 研究了上游离稀土离子的跨膜行为及部分体内小分子对稀土离子跨膜行为的影响。实验结果支持游离稀土离子不能通过细胞膜的假设, 而且所研究的体内小分子在生理浓度下对稀土离子的跨膜也无明显作用。     

Photoluminescence properties of multilayer oxide films intercalated with rare earth ions by the layer-by-layer technique

Multilayer oxide films consisting of a TiO-Eu3+-TiO-Tb3+-NbO-Tb3+-NbO-Eu3+ unit which was prepared by the layer-by-layer technique, showed photoluminescence with a high intensity containing both red and green lights.     

Distribution of the rare earth elements in sediments of the Northwestern Iberian Continental Shelf

The temporal and spatial distribution of the REEs was determined, by INAA, in sediment cores collected at Northern Iberian shelf along the area between the Finisterra Cape and the mouth of Minho river, to contribute to the understanding of the origin and sedimentation processes of sediments deposited at the Continental Shelf. The distribution pattern of the REEs were flat and similar to the shales. A negative Eu anomaly was found for all the sections of the analyzed cores. Significant positive correlations between the REE and Zr and Hf contents suggest that zircon is responsible for hosting both light and heavy REEs.     

水杨醛缩邻氨基苯甲酸Schiff碱稀土配合物的合成

报道了水杨醛缩邻氨基苯甲酸及其四种稀土配合物的合成,通过元素分析、IB、UV、1H NMR及热失重分析,确定配合物组成为REL( H2O)C12·H2O( RE=Y、La、Sm、Eu);测试了配合物的荧光性,在激发光源辐射下,Y(Ⅲ)、La(Ⅲ)、Eu(Ⅲ)、Sm(Ⅲ)四种稀土配合物在500-700nm区域产生荧光,λ...