Mossbauer spectra of Fe-57 in a thick film of YBa2(Cu0.97Fe0.03)(3)O7-x irradiated by a large dose of gamma-rays

Mossbauer spectra of Fe-57 in a thick film YBa2(Cu0.97Fe0.03)(3)O7-x irradiated by a large dose of gamma-rays from Co-60 have been measured. The variation of the relative intensities of some subspectra of Fe-57 in the. Mossbauer spectra of the thick film YBa2(Cu0.97Fe0.03)(3)O7-x after irradiation can be observed. This variation indicates that the change of the coordination environment around some Fe atoms in the lattice occurs due to irradiation. The relative intensity of subspectrum D1(Fe) at the Cu(1) site decreases and that of subspectrum D4(Fe) at the Cu(1) site increases. This may be because of the possible oxygen atom hopping between the coordination environments of D1(Fe) and D4(Fe) in the lattice caused by irradiation. The effect of irradiation on the coordination environment around the Fe atom at the Cu(2) site is not appreciable. (C) 1997 Elsevier Science B.V.

Investigation on molecular and crystal structures of metal complexes with aminopolycarboxylic acids .1. Synthesis and structure of Na-2[Fe-III(ida)(2)](2)center dot 3H(2)O

The crystal structure of the title complex salt has been determined by single-crystal X-ray structure analysis. The crystal data areas follows; Monoclinic, P2(1)/c, a=15.6480(10)Angstrom, b=16.7870(10)Angstrom, c=10.347(2)Angstrom, beta=90.790(10), V=2717.7(6)Angstrom(3), Z=3, and R=0.0333 for 4789 unique reflections. The complex anion has a pseudo-octahedral structure distorted more than the Cr-III and Co-III analogs, in which each, iminodiacetato ligand (ida(2-)) is coordinated in a facial fashion with the two N atoms in a cis configuration, resulting in an unsym-fac structure.

THE STUDY OF MOSSBAUER-EFFECT IN EUBA2CU3O7-Y

EuBa2(Cu1-xFex)3O7-y has been investigated by the Fe-57 and Eu-151 Mossbauer effect. The Fe-57 Mossbauer spectra of the EuBa2(Cu1xFex)3O7-y without or with DC electric current (the current strength I = 0.5A) around the superconducting transition temperature have been measured. The results indicate that the isomer shift (IS) and the quadrupole splitting (QS) of the Fe replacing the Cu(2) vary neither with increasing the Fe content nor with the small DC eletric current passing the superconductor and that the IS and the QS of the Fe replacing the Cu(1) vary with the Fe content. Especially, the IS and the QS of the Fe (D3) replacing the Cu(1) are changed when the small electric current passes the superconductor at 80K.

高温超导体EuBa_2(Cu_(1-x)Fe_x)_3O_(7-y)的穆斯堡尔谱学新研究

利用~(57)Fe和~(151)Eu穆斯堡尔效应对EuBa_2(Cu_(1-x)Fe_x)_3O_(7-y)高温超导体作了研究。在液氮温区,分别测量了样品中有和无电流通过时的~(57)Fe穆斯堡尔谱,结果表明取代了Cu(2)位置的Fe的同质异能位移和四极分裂与通过超导体的电流无关,而取代Cu(1)位置的Fe的穆斯堡尔谱参数则与电流有关。不同Fe含量样品的穆斯堡尔谱分析表明,超导电性和穆斯堡尔谱参数都与Fe的含量有关。

BIOMIMITICS OF OXIDASE AND OXYGENASE THE ELECTRONIC SPECTRA AND THE OXYGEN UPTAKE KINTICS FOR MPc AND MTPP (M = Fe, Co, Cu, Pc AND TFP - ARE DIANIONS OF PHTHALOCYANIN AND TETRAPHENYLPORPHYRINE, RESPECTIVELY)

The reaction rates of MTPP with oxygen in air are Inas than that with pure oxygen, the ratio is roughly the same as to the partial presence of imygen in air, The influences of S-ligand etbanethiol and O- litand Vc on the above Systems have also been investigated, the former makes the MP hands having more changes and the reaction rate constants becoming greater, the latter has less influence.

Microstructure and wear properties of laser clad Fe based amorphous composite coatings

A FeNiSiBV amorphous composite coating was developed by laser cladding of metallic powders on AISI 1020 low carbon steel substrate. The coatings were studied using X-ray diffraction, transmission electron microscopy and scanning electron microscopy. The coating reveals different microstructures along the depth of the coating. The transition zone exhibits good metallurgical bonding between the substrate and the coating. The layer consists of amorphous phase in majority and nanocrystalline phase/crystalline phase in minority. Accompanied with the nanocrystalline phase, the amorphous phase is concentrated in the middle of the coating. The crystalline phase in the coating is identified as Fe2B. A gradient distribution of the microhardness ranges from 1208 HV0.2 to 891 HV0.2 in the coating along the depth. The coating shows higher microhardness and better wear property than the substrate.

高效液相色谱法分离测定Fe(Ⅱ)和络合物Fe(Ⅱ)-PDT的两种几何异构体

铁在自然界中广泛分布，其环境和生态效应主要取决于它们的理化性质、形态、溶解性以及与溶解有机质的结合程度。氧化还原性敏感元素铁在自然界主要以Fe(Ⅱ) 和Fe(Ⅲ)两种价态存在。铁在水环境中的地球化学循环作用主要通过其自身的各种价态之间转化以及与周围其他物质(微量元素,营养盐,有机质)之间的相互作用来实现的。不同形态的铁具有不同的理化性质，其环境效应和生物有效性都是不同，不同形态的铁还可对其他重金属在水体中的循环迁移、赋存形态和生物有效性等均产生不同程度的一定的影响。因此，为铁的环境地球化学行为提供更为准确的信息，就必须进行铁的形态分析，由于Fe(Ⅱ)的氧化还原敏感性，故对铁进行形态分析的前提就是准确测定Fe(Ⅱ)的含量，用普通分光光度法测定Fe(Ⅱ)特别是低含量的Fe(Ⅱ)时，结果的不准确性以及高检出限等缺点都严重制约了准确测定环境中Fe(Ⅱ)的含量。为克服用普通分光光度法测定Fe(Ⅱ)时易受样品溶液其他组分的基体干扰以及灵敏度低等缺点，我们采用了用3-(2-吡啶基)-5,6-二苯基-1,2,4-三嗪（PDT）作为柱前衍生试剂，反相离子对高效液相色谱法来测定Fe(Ⅱ)。由于络合物Fe(II)-PDT存在两种几何异构体，故在建立反相离子对高效液相色谱法来测定Fe(Ⅱ)的同时，我们进一步研究了PDT及Fe(II)-PDT的两种几何异构体色谱分离与测定的实验研究，取得了如下进展： 1．研究了有机萃取分光光度法测定Fe(Ⅱ)，实验中发现加入离子对试剂四溴酚酞乙酯钾(TPBE-K)，由于TPBE和Fe(Ⅱ)-PDT络合物生成三元离子缔合物，导致最大特征吸收波长红移，由555nm增加至610nm，三元离子缔合物[Fe(PDT)3] [TBPE]2的摩尔吸收系数由2.4×104 l•mol-1•cm-1增加至1.9×105 l•mol-1•cm-1，显著改善了方法的灵敏度，降低了检出限，在Fe(Ⅱ)含量为0~0.3μg/ml范围内，方法的线性关系良好，线性方程为y＝0.3582x＋0.01，R2＝0.9974，检出限为0.96ng/ml(S/N＝3)，达到ng/ml水平，成功应用于测定泉水及表层湖水的Fe(Ⅱ)及总铁含量。 2．将3-(2-吡啶基)-5,6-二苯基-1,2,4-三嗪(PDT)作为衍生显色络合试剂应用于分光光度法来测定Fe(Ⅱ)已得到较为充分的报道。在上述研究基础上，首次研究了将PDT作为柱前衍生络合试剂，应用于反相离子对高效液相色谱法来测定Fe(Ⅱ)，不仅克服了常规络合衍生分光光度法过量络合剂干扰试验结果的缺点，而且进一步优化选择了检测波长，由于HPLC的应用，突破了在分光光度法中只能在可见波长范围内选择检测波长为555nm，将检测波长选择在Fe(Ⅱ)-PDT吸收更强烈的紫外区295nm处，使得灵敏度得到了显著提高。在Fe(Ⅱ)浓度为0～3.5×10-6mol/l时，峰面积A和峰高H均和标准溶液的浓度C(×10-7mol/l)的线性关系良好,线性回归方程分别为：A=7.4951x-0.0785(R2=0.9999) 和H=0.5126x- 0.0915(R2=0.9997)，方法的检测限为0.35ng/ml (S/N＝3)。本方法测定Fe(Ⅱ)时，不需复杂的前处理步骤，如固相萃取、有机溶液萃取等，直接柱前衍生HPLC方法测定，方便、快速且灵敏度高，低于众多分光光度报道的检出限水准7～170ng/ml范围。 3．由于络合物Fe(II)-PDT存在面式和经式两种几何异构体，故在建立起反相离子对高效液相色谱法来测定Fe(Ⅱ)新方法的同时，进一步研究了PDT及Fe(II)-PDT的两种几何异构体色谱分离及测定实验研究，关于这方面的试验研究，目前来说还没有相关的研究报道，所以将反相离子对高效液相色谱法应用到分离及测定PDT及Fe(II)-PDT的两种几何异构体中，这也是本论文的第二个创新之处。在本实验中，所用的色谱固定相为普通的反相键合C8柱，但由于优化选择了最佳流动相条件，使得PDT及Fe(II)-PDT的两种几何异构体直接在C8柱上得到完全的基线分离。讨论了流动相中有机改性剂乙腈不同比例、不同种类的离子对试剂(高氯酸钠和十二烷基硫酸钠)及不同浓度对PDT和Fe(II)-PDT两种几何异构体的色谱行为的影响。根据不同试验条件下，对所获得的色谱参数(容量因子、分离度、选择性因子、保留时间等)进行了较为深入的分析，据此探讨了色谱分离异构体过程的机理。 4．在上述实验的基础之上，引入更能灵活的调节洗脱强度和被分离物质分离度的三元流动相(乙腈/甲醇/水=20/50/30)，优化选择了三元流动相中有机改性剂的比例以及离子对试剂的种类及浓度，使得异构体的分离度和选择性因子均得到满意结果。对一系列不同浓度的Fe(II)-PDT异构体分离，面式和经式异构体的面积和浓度之间的线性关系在4~25×10-7mol/l范围内良好，线性关系分别为：y = 3.6333x - 2.3378(R2 = 0.9957，经式异构体)，y = 1.8219x - 1.0783(R2 = 0.9964, 面式异构体)。面式和经式异构体的检测限分别为4.28ng/ml和3.44ng/ml (S/N＝3)。 5．进一步研究发现Fe(II)-PDT的两种几何异构体之间存在相互转化的动态平衡，故根据异构体含量随时间的变化就可以探讨在转变过程中的动力学和热力学参数。用高效液相色谱法研究了异构体转变过程中色谱峰高和面积随时间的变化，并依此首次得出了两种几何异构体相互转化可逆过程中的热力学和动力学参数，如熵变、焓变、自由能变化、反应速率常数等，对两种几何异构体之间的动力学转变平衡机理进行合理的解释提供了有益的参考。各不同温度下(30℃，35℃，40℃，45℃)，反应时间在3倍半衰期以内，两种几何异构体之间的相互转变平衡均符合动力学一级反应。各不同温度下Xeln[(Xe-X0)/Xe-X)]随时间变化的线性关系良好，分别为：y=0.0821x+0.7288(R2=0.9911,T=45℃)；y = 0.0486x + 0.598(R2 = 0.9987, T=40℃); y = 0.0216x + 0.5861(R2 = 0.9987, T=35℃)；y = 0.0124x + 0.591(R2 = 0.9988, T=30℃)。 首次将PDT作为柱前衍生络合试剂，应用于反相离子对高效液相色谱法来测定环境中的Fe(Ⅱ)，且无需复杂的样品前处理过程(固相萃取，有机溶液萃取等浓缩富积过程)，克服了普通分光光度法检测限高、易受样品基体效应的干扰等缺点；在建立起的高效液相色谱法测定Fe(Ⅱ)的基础上，进一步对络合物Fe(II)-PDT的两种几何异构体色谱分离及动力学转变实验研究，则是对建立起的反相离子对高效液相色谱法测定Fe(Ⅱ)试验研究基础上的进一步延伸和扩展，是对测定Fe(Ⅱ)的高效液相色谱法的机理的进一步认识和探讨。PDT作为柱前衍生络合试剂首次应用于高效液相色谱测定Fe(Ⅱ)为铁的环境地球化学工作者提供了一种灵敏度高的测定Fe(Ⅱ) 的新途径，为环境样品中Fe(Ⅱ)含量的准确测定提供保证，对铁的环境地球化学研究，如铁形态分析、铁的水-沉积物界面行为等提供更翔实可靠的信息。

中元古代昆阳群Fe-Cu-REE矿床地球化学研究-以武定迤纳厂矿床为例

稀土元素成矿与地壳的构造运动密切相关，稀土在中元古代具有大规模暴发性成矿特征。云南武定迤纳厂稀土铁铜矿床为昆阳群因民组出现稀土富集成矿的典型代表。本论文选择迤纳厂矿床为主要研究对象，系统研究矿床不同类型岩（矿）石和矿物的稀土元素地球化学特征，探讨富稀土的成矿流体、成矿物质来源和稀土元素成矿时代，揭示昆阳裂谷初期因民组稀土元素富集的地球化学机制。主要认识如下：1、迤纳厂矿床产于昆阳裂谷初期形成的禄丰一武定火山断陷盆地中。早中元古界昆阳群分布于绿汁江岩石圈断裂和小江一易门断裂的夹持地带，呈狭长状展布。迤纳厂矿床赋矿地层为昆阳群因民组上段的硅质白云岩和碱性火山岩（粗面安山岩）。矿体产出形态和矿石的结构构造等均显示矿体与赋矿地层同沉积特征；出现独立矿物氟碳饰矿、独居石及褐帘石，磷灰石、萤石、菱铁矿等矿物中也含有一定量的稀土，沿矿体走向和垂向稀土元素变化不大。2、矿体顶、底板围岩（石榴石黑云母片岩、钠长黑云母片岩等）的原岩为碱性火山岩（粗面安山岩），相对富集大离子亲石元素Ba、Cs、Rb、K、LRE日及贫Zr、Sr、Ti、Hf、HEE，为早元古代末期一中元古代早期交代富集地慢低程度部分熔融所形成的碱性火山岩。矿石稀土总量高（645-4443）×10-6，强烈富集轻稀土（（La/Tb）N＝17.3-81.1），稀土元素分布特征明显不同于矿区正常沉积的硅质白云岩和后期侵入的钠长石英斑岩及火山角砾岩，而与矿体顶、底板碱性火山岩中稀土元素配分特征基本一致，暗示稀土成矿物质来源与碱性火山岩有密切的关系；3、矿石中微量元素组合及变化特征与现代海底正在喷出的热液和热液沉积物中元素组合有较大的可比性，明显不同与火成碳酸岩型稀土矿床中的特征元素组合；在微量元素判别图解（Al-Fe-Mn、Fe／Ti-Al／（Al+Fe＋Mn）、U-Th、Y-P2O5等）中，逸纳厂矿石均投影在热水沉积区，矿石的Y／Ho值与黑烟囱值接近，表明成矿流体为高温、还原性质，稀土成矿可能以热水沉积作用方式为主；4、对矿石中主要矿物萤石、菱铁矿、磁铁矿、石英、方解石的稀土元素特征研究表明，矿石沉积时不同矿物中稀土元素分布特征基本相同，主要受成矿流体中稀土分布特征制约。而后期变质作用形成的矿物，其稀土元素分布主要受矿物晶体结构控制。同期成矿流体从早期到晚期（块状矿石→条带状矿石），轻重稀土分异变小，稀土总量增加，条带状矿石中稀土含量最高；矿石黄铜矿6345值变化在一任3％0到2g％。范围，显示慢源硫特征；菱铁矿6r3C（8％-9.1%）、δ18O（-11.17%-15.37）‰指示成矿流体具岩浆来源和有机质的脱梭酸分解作用参与；成矿流体中稀土元素可能主要以（RE（CO3）3F）4-、（既（CO3）3F2）、（RE（F，Cl万等形式迁移，当温度降低时沉淀出氟碳饰矿等稀土矿物；5、矿石和萤石单矿物 Sm-Nd等时线年龄分别为1621士110Ma和15：38士43Ma，与矿区碱性火山岩错石的U-Pb年龄1676Ma、因民组顶部石英正长斑岩的错石U-P1。年龄1685Ma基本一致，也与因民组地层年龄1765M。较为接近，反映成矿时代为早元古代晚期和中元古代早期：这一时间也与一早元古代晚期一中元古代早期昆阳裂谷初始裂陷阶段，大量来自于地幔的碱性火山岩喷发事件相吻合。矿石。Nd（t）:-2.87-3.60，萤石单矿物εNd（t）：-3.93-5.90，变化范围较窄并全为负值，接近0，指示源区为富集地幔。同时结合矿床形成的构造一地质环境及矿体产出的地质形态，认为逛纳厂稀土铁铜矿床可能是在昆阳裂谷初期，在碱性火山岩浆喷发的间歇期，来自地幔富稀土、挥发份的成矿流体由火山喷流一同生沉积方式形成的矿床。6、昆阳群因民组地层中出现的稀土富集、成矿与我国的白云鄂博稀土REE-Fe-Nb超大型矿一床和澳大利亚的olympic Dam Cu-U-Au-Ag-REE超大型矿床，在成矿时代、产出大地构造背景、成矿物质来源等方面具有较大的相似性，均体现成矿受控于中元古代1.5Ga超大陆聚合前或随后裂解初始阶段伴随的非造山型碱性岩浆或热液作用，稀土来源于超大陆拼合前因板块俯冲交代而形成的富集地幔。

Regeneration behaviors of Fe/Si-2 and Fe-Mn/Si-2 catalysts for C2H6 dehydrogenation with CO2 to C2H4

The catalytic performance of Fe/Si-2 and Fe-Mn/Si-2 catalysts for conversion of C2H6 with CO2 to C2H4 was examined in a continuous-flow and fixed-bed reactor. The results show that the Fe-Mn/Si-2 catalyst exhibits much better reaction activity and selectivity to C2H4 than those of the Fe/Si-2 catalyst. Furthermore, the coking-decoking behaviors of these catalysts were studied through TG. The catalytic performances of the catalysts after regeneration for conversion of C2H6 or dilute C2H6 in FCC off-gas with CO2 to C2H4 were also examined. The results show that both activity and selectivity of the Fe-Mn/Si-2 catalyst after regeneration reached the same level as those of the fresh catalyst, whereas it is difficult for the Fe/Si-2 catalyst to refresh its reaction behavior after regeneration.

Direct synthesis of highly ordered Fe-SBA-15 mesoporous materials under weak acidic conditions

Iron-substituted SBA-15 (Fe-SBA-15) materials have been synthesized via a simple direct hydrothermal method under weak acidic conditions. The powder X-ray diffraction (XRD), NZ sorption and transmission electron microscopy (TEM) characterizations show that the resultant materials have well-ordered hexagonal meso-structures. The diffused reflectance UV-vis and UV resonance Raman spectroscopy characterizations show that most of the iron ions exist as isolated framework species for calcined materials when the Fe/Si molar ratios are below 0.01 in the gel. The presence of iron species also has significant salt effects that can greatly improve the ordering of the mesoporous structure. Different iron species including isolated framework iron species, extraframework iron clusters and iron oxides are formed selectively by adjusting the pH values of the synthesis solutions and Fe/Si molar ratios. (c) 2005 Elsevier Inc. All rights reserved.