超微LaMO_3（M＝Fe，Cr，Mn，Co）的导电性与粒度的关系

用Ｓｏｌ－Ｇｅｌ法合成了ＬａＭＯ＿３（Ｍ＝Ｆｅ，Ｃｒ，Ｍｎ，Ｃｏ）超微粉末．Ｘ射线衍射分析表明，不同焙烧温度下所合成的化合物均为单相．ＳＥＭ分析表明，粒子呈球形，室温电阻率测量表明，电阻率随粒度的变化呈两种类型：ＬａＦｅＯ＿３，ＬａＣｒＯ＿３随粒度的增大，电阻率增加；而ＬａＭｎＯ＿３，ＬａＣｏＯ＿３随粒度的增大，电阻率减小．

不同热化学还原LiNbO_3：Ti或Mn晶体杂质电荷态和点缺陷

采用光学吸收和电子顺磁共振（ＥＳＲ）技术表征不同热化学还原ＬＩＮｂＯ３：Ｔｉ，Ｍｌｉ（ＬＮ：Ｔｉ，Ｍｎ）和纯的Ｌｉ／Ｎｂ＝０．９４５一致熔化ＬｉＮｂＯ３（ＬＮ）晶体的热力学还原习性．将ＬＮ：Ｔｉ（厚度为１ｍｍ）样品放在Ｌｉ２ＣＯ３中、６００℃、保温７ｈ，产生６９０ｕｒｎ（～１．８ｅＶ，Ｔ＝６７％）和峰值靠近７８５ｎｍ（Ｔ＝７１％）的７７０￣８１０ｎｍ光学吸收带，它们分别对应于Ｔｉ（３＋）的２Ｔ→２Ｅ跃迁以及室温稳定Ｆ＋心滞有一个电子的氧空位）．经真空１．２Ｐａ，８００℃２ｈ还原后，存在峰值为６７５ｎｍ（Ｔ＝５２％）的４８０～７８０ｎｍ平滑吸收带，它们是Ｔｉ（３＋）、Ｆ心和Ｆ＋心重叠吸收，但是，在Ａｒ气氛下、９００℃、８ｈ处理后，仅能看到峰值在６７５ｎｍ（Ｔ＝５２％）的６００～７８０ｎｍＴｉ（３＋）的弱吸收．来自未处理ＬＮ：Ｔｉ晶体的室温和Ｘ带的ＥＳＲ＄观察到ｇ＝４．３４８，共振磁场０．１５２ＴＨ（ｐ－ｐ）＝０．０１６３Ｔ微波吸收峰，以及四组精细结构Ｂ线（每一ｆｓ线是由６条超精细结构ｈｆｓ组成），ｇ值从３．４６０～１．６７９吸收，它们分别归为于晶体杂质Ｆｅ（３＋）和Ｍｎ（２＋）离子．真空还原后，Ｆｅ（３＋）的

一种新型的Nd：YAP激光眼科治疗机及临床应用

报导一种新型的Ｎｄ：ＹＡＰ激光眼科治疗机。应用于临床，对膜性白内障、青光眼等眼病的治疗取得较满意的治疗效果。

甲烷氧化偶联La-Mn-Li系复合氧化物催化剂的研究

用XRD、IR、XPS和SEM等方法研究了混合氧化物LiLa_(1-x)Mn_xO_2的结构和它们对甲烷氧化偶联的催化性能。结果表明,随着MnO_2的变化,可形成一系列复合氧化物,其中三元复合氧化物La_2Mn_(1-y)Li_yO_4是甲烷氧化偶联的活性相,由于Li~+部分取代Mn~(2+)形成Li~+-O~--Mn(2+)缺陷簇,增加了活性氧种的浓度和再生速度是这种氧化物具有较高甲烷偶联活性的主要原因。脉冲实验证明,CH_4脱氢生成CH_3·偶联生成C_2H_6,进一步氧化脱氢生成C_2H_4都可在催化剂表面完成,而CO和CO_2是在气相反应中生成的。在780℃C_2收率可达23.9%。

溶胶—凝胶法制备LaMO_3超微粉末(M=Cr、Mn、Fe、Co、Ni)

使用溶胶—凝胶法低温合成多组分氧化物玻璃的详细工艺已有报导。我们亦成功地用该法制备出了钕玻璃薄膜和钕玻璃纤维。本文报道利用此法低温合成LaCrO_3、LaMnO_3、LaFeO_3、LaCoO_3、LaNiO_3超微粉末的研究结果。

[n-C_9H_(19)NH_3]_2MCl_4(M=Cu、Mn、Zn、Co)层结构配合物固-固相变的热分析和红外光谱研究

本文用差示扫描量热(DSC)、热重(TG)和红外光谱法研究了标题配合物(简记为C_9M)的热稳定性和固—固相变.讨论了中心金属离子对热稳定性和相变的影响.发现其热稳定性依C_9Co>C_9Mn>C_9Zn>C_9Cu降低.固—固相变数目、相变温度和相变的有序—无序效应主要取决于中心金属离子的种类。Zn组配合物总相变的无序效应比Cu组高,在高温相为完全无序相。C_9Zn配合物低温相变(285K)主要来源于链间相互作用和堆积态的有序—无序变化.高温相为“链熔化”态.

A NOVEL METAL THIAMINE COMPLEX WITH A CYCLIC DIMER FORMED BY METAL-BRIDGED 2 THIAMINE LIGANDS - CRYSTAL-STRUCTURE OF [MN(THIAMINE)CL2(H2O)]2[THIAMINE]2CL4.2H2O

The crystal structure of [Mn(thiamine)Cl2(H2O)]2[thiamine]2Cl4.2H2O has been determined by X-ray diffraction methods. The compound contains a cyclic dimer of a complex cation with two thiamine ligands bridged by two Mn(II) ions across a crystallographic center of symmetry. Each Mn(II) is coordinated by two chloride atoms, a water molecule, a N(1') atom of the pyrimidine from a thiamine and an O(53) atom of the hydroxyethyl side chain from another thiamine. There are two free-base thiamine molecules related by a center of symmetry in the unit cell, which form a base-pair through the hydrogen bonds. Both the independent thiamine molecules in the asymmetric unit assume the common F conformation with phi-T = 10.0(9) and 3.6(10) and phi-P = 85.6(7) and 79.6(7), respectively. The compound provides a possible model for a metal-bridged enzyme-coenzyme complex in thiamine catalysis. Crystallographic data: triclinic, space group P1BAR, a = 12.441(4), b = 13.572(4), c = 11.267(3) angstrom, alpha = 103.15(2), beta 89.03(3), gamma = 115.64(2)-degrees, Z = 1, D(calc) = 1.524 g cm-3, and R = 0.050 for 3019 observed reflections with I > 3-sigma(I).

金属离子在液相氧化中的催化作用——Ⅷ.在丙酸氧化反应中Mn(Ⅲ)-Co(Ⅲ)催化体系不同离子的功能

本文仔细地研究了Mn(Ⅲ)-Co(Ⅲ)催化体系中不同离子在丙酸氧化中的功能:Mn(Ⅲ)离子首先与丙酸作用并被还原成Mn(Ⅱ)离子;Co(Ⅲ)离子可在反应体系中将Mn(Ⅱ)再氧化,而还原了的Co(Ⅱ)离子可为氧再生.这样建立起的氧化还原体系形成了催化循环.

(Ce,Gd,Mn)MgB_5O_(10)磷光体的合成及其发光

本文采用固相反应的方法合成了一系列(Ce,Gd,Mn)MgB_5O_(10)磷光体。观察到合成温度、灼烧时间、原料配比对磷光体的形成和发光亮度有重要影响。X射线衍射分析表明,磷光体结构与LaMgB_5O_(10)相同,属单斜晶系、空间群P2_(1/c)。用EPR确定了磷光体中锰离子为二价。测定了(Ce_(0.2)La_(0.2))MgB_5O_(10),(Gd_(0.7)La_(0.3))MgB_5O_(10),(Mn_(0.05)La_(0.95))MgB_5O_(10),(Ce_(0.2)Mn_(0.05)La_(0.75))MgB_5O_(10),(Gd_(0.95)Mn_(0.05))MgB_5O_(10)、(Ce_(0.2)Gd_(0.8))MgB_5O_(10)和(Ce_(0.2)Gd_(0.75)Mn_(0.05))MgB_5O_(15)等磷光体的光谱。根据光谱数据讨论了(Ce_(0.2)Gd_(0.75)Mn_(0.05))MgB_5O_(10)磷光体中能量传递过程为:Ce~(3+)→Mn~(2+),Gd~(3+)→Mn~(2+)以及Ce~(3+)→Gd~(3+)→Mn~(2+),其中Ce~(...

钙钛矿型铝酸钇(YAP)晶体在还原气氛中的稳定性

关于YAP的相文献上有不同的报导。相图研究说明,在较低温度它将分解成YAG(Y_3Al_5O_(12))和YAM(Y_4Al_2O_9)。Abell等报导分解产物是YAG和未鉴别出来的x相,并推测可能是体系缺氧,而x相不能表示在膺二元体系相图中。我们认为在还原气氛中YAP是不稳定的。本文对石墨加热器处理的YAP晶体粉末通过化学分析和x线相分析进一步证实此推论。

Purification and partial characterization of Mn superoxide dismutase from muscle tissue of the shrimp Macrobrachium nipponense

Superoxide dismutase (SOD; EC 1.15.1.1) is an enzyme that protects against oxidative stress from superoxide radicals in living cells. This enzyme had been isolated, purified and partially characterized from muscle tissue of the shrimp Macrobrachium nipponense. The purification was achieved by heat treatment, ammonium sulfate fractionated precipitation and column chromatograph on DEAE-cellulose 32. Some physiological and biochemical characterization of it was tested. The molecular weight of it was about 21.7 kDa, as judged by SDS-polyacrylamide gel electrophoresis. The purified enzyme had an absorption peak of 278 nm in ultraviolet region, and the enzyme remained stable at 25-45 degreesC within 90 min. However, it was rapidly inactivated at higher temperature. Treatment of the enzyme with 1 mM ZnCl2, SDS and 1 mM or 10 mM mercaptoethanol showed some increasing activity. However, the enzyme activity was obviously inhibited by 10 mM CaCl2, CuSO4, ZnCl2 and 1 mM CaCl2 and 10 mM K2Cr2O7. SOD activity did not show significantly variation after incubated with 1 mM CaCl2, EDTA and 10 MM SDS. The enzyme was insensitive to cyanide and contained 1.03 +/- 0.14 atoms of manganese per subunit shown in atomic absorption spectroscopy, which revealed that purified SOD was Mn superoxide dismutase. (C) 2004 Elsevier B.V. All rights reserved.

He, Ne and Ar isotopic composition of Fe-Mn crusts from the western and central Pacific Ocean and implications for their genesis

The noble gas nuclide abundances and isotopic ratios of the upmost layer of Fe-Mn crusts from the western and central Pacific Ocean have been determined. The results indicate that the He and Ar nuclide abundances and isotopic ratios can be classified into two types: low He-3/He-4 type and high He-3/He-4 type. The low He-3/He-4 type is characterized by high He-4 abundances of 191x10(-9) cm(3.)STP(.)g(-1) on average, with variable He-4, Ne-20 and Ar-40 abundances in the range (42.8-421)x10(-9) cm(3.)STP(.)g(-1), (5.40-141)x10(-9)cm(3.)STP(.)g(-1), and (773-10976)x10(-9) cm(3.)STP(.)g(-1), respectively. The high He-3/He-4 samples are characterized by low He-4 abundances of 11.7x10(-9) cm(3.)STP(.)g(-1) on average, with He-4, Ne-20 and Ar-40 abundances in the range of (7.57-17.4)x10(-9) cm(3.)STP(.)g(-1), (110.4-25.5)x10(-9) cm(3.)STP(.)g(-1) and (5354-9050)x10(-9) cm(3.)STP(.)g(-1), respectively. The low He-3/He-4 samples have He-3/He-4 ratios (with RIRA ratios of 2.04-2.92) which are lower than those of MORB (R/R-A=8 +/- 1) and Ar-40/Ar-36 ratios (447-543) which are higher than those of air (295.5). The high He-3/He-4 samples have He-3/He-4 ratios (with R/R-A ratios of 10.4-12.0) slightly higher than those of MORB (R/R-A=8 +/- 1) and Ar-40/Ar-36 ratios (293-299) very similar to those of air (295.5). The Ne isotopic ratios (Ne-20/Ne-22 and Ne-21/Ne-22 ratios of 10.3-10.9 and 0.02774-0.03039, respectively) and the Ar-38/Ar-36 ratios (0.1886-0.1963) have narrow ranges which are very similar to those of air (the Ne-20/Ne-22, Ne-21/Ne-22, Ar-38/Ar-36 ratios of 9.80, 0.029 and 0.187, respectively), and cannot be differentiated into different groups. The noble gas nuclide abundances and isotopic ratios, together with their regional variability, suggest that the noble gases in the Fe-Mn crusts originate primarily from the lower mantle. The low He-3/He-4 type and high He-3/He-4 type samples have noble gas characteristics similar to those of HIMU (High U/Pb Mantle)- and EM (Enriched Mantle)-type mantle material, respectively. The low He-3/He-4 type samples with HIMU-type noble gas isotopic ratios occur in the Magellan Seamounts, Marcus-Wake Seamounts, Marshall Island Chain and the Mid-Pacific Seamounts whereas the high He-3/He-4 type samples with EM-type noble gas isotopic ratios occur in the Line Island Chain. This difference in noble gas characteristics of these crust types implies that the Magellan Seamounts, Marcus-Wake Seamounts, Marshall Island Chain, and the Mid-Pacific Seamounts originated from HIMU-type lower mantle material whereas the Line Island Chain originated from EM-type lower mantle material. This finding is consistent with variations in the Pb-isotope and trace element signatures in the seamount lavas. Differences in the mantle surce may therefore be responsible for variations in the noble gas abundances and isotopic ratios in the Fe-Mn crusts. Mantle degassing appears to be the principal factor controlling noble gas isotopic abundances in Fe-Mn crusts. Decay of radioactive isotopes has a negligible influence on the nuclide abundances and isotopic ratios of noble gases in these crusts on the timescale of their formation.

云贵高原湖泊近代沉积作用的Fe、Mn、S指示

铁、锰、硫具有强烈的氧化还原敏感性，在湖泊沉积地球化学过程中扮演着重要的角色。铁、锰、硫控制了沉积物中的氧化还原分带，对磷及其它一些微量金属元素的形态和分布具有重要影响。因此本文中我们选择铁、锰、硫来指示湖泊沉积作用中氧化还原过程的变化，为进一步高精度提取环境信息奠定基础。本文对比阿哈湖、洱海和阳宗海，通过铁、锰、硫在湖水、孔隙水和沉积物体系内的垂直剖面特征分析，阐述了三湖沉积物中氧化还原过程的区别、氧化还原边界层对铁锰循环的控制作用以及铁-锰-硫对重金属的控制作用，深入探讨了铁、锰、硫及微量元素记录的早期成岩改造特征及其对湖泊沉积作用的指示意义，进一步阐明了沉积物中的有机质降解规律及早期成岩机制，获得了如下结论：1．阿哈湖水中铁、锰出现季节性释放，锰的季节性释放强度比铁大；在冬季和夏季，阿哈湖沉积物界面铁、锰均出现富集。冬季的富集程度强于夏季，锰的富集程度远远强于铁。沉积物表层由冬季的黄褐色转变为夏季的黑色，表示铁、锰氧化物层转变为FeS层。2．洱海沉积物中，铁、锰均在沉积物一水界面出现富集，界面以下，铁、锰的含量逐渐递降。铁、锰在孔隙水中产生扩散迁移，而在沉积物表层形成富集，说明洱海沉积物表层处于较好的含氧状况，氧化还原边界层处于沉积物中；阳宗海沉积物孔隙水中铁锰峰值均位于界面2cm处，而沉积物中铁在表层出现亏损，表明夏季阳宗海表层处于缺氧状态，氧化还原边界层位于湖水中。3．铁、锰的界面扩散和沉降通量在不同湖间差异较大。但锰的扩散通量占沉降通量的比例高于铁，锰在界面的沉积后再迁移程度和沉积记录的改造程度比铁显著。湖泊中铁、锰在有机质降解过程的驱动下，围绕沉积物一水界面形成氧化还原循环。其中锰的循环相当激烈，铁则较为缓和。铁、锰界面循环受氧化还原边界层和沉积物—水界面的双重控制。4．三湖沉积物界面处均存在硫酸盐的还原作用。洱海硫酸盐由于其含量较低以及表层良好的含氧状况因此不可能成为有机质降解的主要氧化剂，而阳宗海和阿哈湖则情况相反。阿哈湖沉积物柱芯好氧菌和SRB的分布进一步证实了表层处硫酸盐在SRB的参与下强烈的还原作用，同时说明有机质的好氧和厌氧降解并不是完全对立的；水体向沉积物内部扩散是高硫酸盐浓度湖泊的主要清除作用，而对于低硫酸盐含量湖泊而言，水体浮游生物如藻类吸收和同化作用应是水体硫酸盐的主要清除机制。5．三湖沉积物硫主要都以黄铁矿存在。阳宗海的AVS含量较高，AVS和FeS_2在界面的富集进一步证实了在阳宗海沉积物界面存在着强烈的硫酸盐还原作用；阿哈湖沉积物中硫酸盐的还原与季节无太大联系。在夏季和冬季，沉积物表层均表现出明显的SO_4~(2-)还原作用。只不过随着氧化还原边界层的迁移，SO_4~(2-)还原作用的范围也随之发生迁移。铁氧化物作为电子受体参与有机质分解的过程中，水铁矿和纤铁矿等Feo首先被还原而溶解出来。同时，Feo和Fec是可以互相转化的，针铁矿和赤铁矿等晶体铁氧化物可以向水铁矿和纤铁矿转化。6．三湖中Corg都表示出明显的降解趋势，证明了沉积物表层存在的早期成岩作用。洱海表现出“沉降一降解一堆积”三阶段分布特征，而阳宗海和阿哈湖沉积物中Corg表现出“降解一堆积”二阶段分布特征；洱海沉积物中有机质的选择性分解不明显，C／N指示沉积物有机质主要来自无纤维束的陆源植物；阿哈湖沉积物中C／N很高，均>20，且随深度增加呈现上升的趋势，说明阿哈湖沉积物中有机质含易降解的低N和难降解的高C，有机质主要来源于陆源输入。7．洱海和阳宗海沉积物中均存在明显的重金属再迁移现象。洱海沉积物中铁、锰循环对Pb、Cu的迁移影响很大；颗粒物的吸附一解析作用是影响Cd迁移的主要因素；洱海沉积物中可迁移释放的Ni含量并不高。8．阳宗海沉积物孔隙水中Ni、Cu、Cd均与铁、锰表现出良好的相关性，铁、锰氧化物的还原是造成它们在孔隙水表层富集的主要控制因素。而Pb与铁、锰呈现微弱的正相关。Pb、Cd相对于Cu、Ni的释放趋势较强，再迁移作用较剧烈。Pb、Cd在表层孔隙水中与一些有机、无机化合物络合，由于沉积物的吸附作用而再次沉降到沉积物表层形成富集。沉积物中重金属的再迁移主要受有机质降解、铁锰氧化物还原和硫化物沉积控制，但是不同的湖泊控制因索各不相同。