Ce~（3＋）在钙钛矿型KMF_3（M＝Mg、Ca、Sr、Ba）基质中的发光特性

采用高温固相反应法，在Ａｒ气氛中合成了ＫＭＦ３（Ｍ＝Ｍｇ、Ｃａ、Ｓｒ、Ｂａ）基质化合物和掺杂Ｃｅ３＋的磷光体。经Ｘ射线衍射分析确定，ＫＭｇＦ３和ＫＣａＦ３属于立方晶系、钙钛矿型结构，ＫＳｒＦ３和ＫＢａＦ３具有类似的结构。测定了ＫＭＦ３∶Ｃｅ３＋的发光光谱，观察到与其结构对应的分为二种不同的光谱结构，讨论了Ｃｅ３＋的取代格位

A STUDY OF SURFACE OXYGEN SPECIES FROM LA-ME-O (ME=MG, CA, SR, BA) CATALYSTS FOR METHANE OXIDATIVE COUPLING

CO2-TPD was used to study the surface basicity of La-Me-O mixed oxides and O-2-TPD, CH4-TPD were employed to study the surface active oxygen species. Comparing the CO2-TPD with O-2-TPD, we can see that the basicity of catalyst is in parallel with the catalystic activity. The stronger basicity is more profitable for the catalyst to adsorb oxygen to form active oxygen species and to activate CH4 by breaking a C-H bond, By comparing the catalytic activity, the results showed that La-Ba-O(La/Ba=7/3) catalyst had the strongest basicity, and it gave the highest CH4 conversion and C-2 selectivity, The results from the pulse reaction showed that the lattice oxygen participated in the OCM reaction without gas oxygen, and it was the selective oxygen species.

甲烷氧化偶联La－Me－O（Me＝Mg，Ca，Sr，Ba）系催化剂表面氧种的研究

利用ＣＯ_２－ＴＰＤ法考察了Ｌａ－Ｍｅ－Ｏ（Ｍｅ＝Ｍｇ，Ｃａ，Ｓｒ，Ｂａ）系催化剂的表面碱性，并用Ｏ_２－ＴＰＤ、ＣＨ_４－ＴＰＤ法对该体系的表面活性氧种进行了表征，并与催化性能相关联。结果表明，Ｌａ－Ｂａ－Ｏ催化剂由于表面强碱性中心数目多，产生活性氧种的数目也多，有利于甲烷的活化，因而具有最高的甲烷转化率和Ｃ_２烃选择性。脉冲反应表明，在无气相氧存在下，表面晶格氧参与了氧化偶联，而且是选择氧化的活性氧种。

稀土离子和肌质网(Ca~(2+)+Mg~(2+))-ATP酶相互作用的研究

研究了稀土离子对肌质网(Ca~(2+)+MG~(2+))-ATP酶活性的影响及其作用机制,结果表明,低浓度Gd~(3+)对肌质网膜上(Ca~(2+)+Mg~(2+)),ATP酶有激活作用,较高浓度Gd~(3+)抑制其活性,Gd~(3+)抑制纯化酶的活性,低浓度Gd~(3+)对磷脂酸(FA)、心磷脂(CL)重组酶有激活作用,而对磷脂酰胆碱(PC)、磷脂酰胆碱(PC)与磷脂酰乙醇胺(Pe)混合物(PC/PE)及磷脂酰丝氨酸(PS)重组酶无激活作用,低浓度Tb~(3+)对肌质网膜与纯化酶上Ca~(2+)结合位点的影响不同。

A STUDY OF SITE OCCUPATION OF EU-3+ IN ME2Y8(SIO4)6O2 (ME=MG, CA, SR)

Alkaline earth (Mg, Ca. Sr) yttrium silicate oxyapatites doped with Eu3+ show red luminescence with comparable intensity. In this system of phosphors, the Eu3+ ions enter 4f sites and 6h sites simultaneously according to the fluorescence spectra, in which

溶胶－凝胶法合成（Mg，Ca）O－SiO_2∶Eu~（3＋），Bi~（3＋）发

以Ｍｇ（ＮＯ３）２、Ｃａ（ＮＯ３）２、Ｅｕ（ＮＯ３）３、Ｂｉ（ＮＯ３）３、ＬｉＮＯ３和Ｓｉ（ＯＣ２Ｈ５）４为反应物，采用溶胶－凝胶法，在比较低的温度下，首次合成０．７０１ｍｏＩＭｇＯ－０．１７５ｍｏｌＣａＯ－１．２５ｍｏＩＳｉＯ２∶０．０６ｍｏｌＥｕ（３＋），０．００２ｍｏＩＢｉ（３＋）（加入Ｌｉ＋作为电荷补偿剂）发光体。得到了最佳合成条件。研究了由溶胶向凝胶转变和凝胶向发光晶体的转变过程。探讨了发光体在不同激发波长激发下的发光特性以及在激活剂、敏化剂不同掺杂量下的发光行为。讨论了在（Ｍｇ（ａ）Ｏ－ＳｉＯ２基质中Ｂｉ（３＋）对Ｅｕ（３＋）的能量传递和敏化作用。

10种外眼病泪液中Ca,Mg,Zn,Fe元素测定

检测10种外眼病141例、178眼泪液中的Ca、Mg、Zn、Fe含量。结果显示,翼状胬肉和泡性角结膜炎泪液中的Ca,复发单疱病毒性角膜炎(HSK)泪液中的Ca、Mg、Zn、Fe,慢性结膜炎泪液中的Ca、Fe含量均明显低于对照组(P<0.001～0.05)。提示这4种外眼病的病因可能与泪液Ca、Mg、Zn、Fe含量不足有关。

火焰原子吸收光谱法测定明胶中Mg、Ca、Cu、Fe等杂质

明胶是感光工业基本原料之一,其质量的好坏直接影响照像性能,因此对明胶中的杂质进行分析研究具有重要的实际意义。本文采用火焰原子吸收光谱法测定明胶中Mg、Ca、Cu、Fe四个元素。明胶样品经灰化除去有机成分后进行酸溶,然后定容到

稀土对Al-Mg-Si合金性能影响和稀土作用机理研究

本文研究了稀土对铝镁硅合金性能的影响通过添加稀土改善合金的综合性能,提高合金的成品率,表面光泽性和致密度,讨论了稀土对铝镁硅合金的作用机理,为稀土在铝镁硅合金型材中的推广应用提供了有力的实验依据。

ICP-OES测定浮游有孔虫的Mg/Ca比值及其在SST分析中的应用

海洋是驱动大气环流的主要“引擎”，海表温度（SST）又是揭示海洋环境变化的重要参数。利用有孔虫Mg/Ca比值恢复SST具有较高精密度，是目前恢复SST较成功的方法之一。本论文旨在建立一套有效的有孔虫清洗方法和ICP-OES测试有孔虫Mg/Ca比值的分析方法。 文中分析了53份西菲律宾海区(N18°40.23′，E135°37.11′；水深3225m)表层沉积物中浮游有孔虫Globigerinoides ruber（白色）Mg/Ca比值。结合本研究区的特点，文中使用的清洗方法是有孔虫Mg/Ca比值测试常用的“Mg”清洗方法，主要是由以下步骤构成：①用超纯水和甲醇在超声波水浴中清洗，②显微镜下剔除深色硅酸盐颗粒，③用氧化试剂去除有机质(加入30%H2O2和0.1M NaOH溶液在90℃左右的沸水浴中加热)，④酸洗(250μl 0.001N HNO3 超声波水浴中清洗10S)。清洗干净的样品经超纯硝酸溶解成溶液后，利用电感耦合等离子体发射光谱(ICP-OES)对其进行Mg/Ca比值的分析测试。仪器操作条件如下：辅助气流量（Ar）为0.5L/min（0.5L/min-1.5L/min），雾化器压力为0.2Mpa（0-0.4Mpa），泵速为20rpm（0-125rpm），高频输出功率（RF）为1150W（750W-1500W），火焰高度为15.5mm（8-21mm），通过多次重复测量一组Mg/Ca=3.333mmol/mol的标准溶液，其Mg/Ca短期精密度<0.5%,长期精密度为1%。53份样品之间Mg/Ca比值的RSD为2.7%，利用Lea(2000)建立的太平洋地区浮游有孔虫G. ruber(白色)的Mg/Ca与SST的校正公式:Mg/Ca(mmol/mol) ＝0.30exp[0.089×SST(℃)]，得到本研究区的SST为28℃±0.3℃。

Characteristics of anodic coatings oxidized to different voltage on AZ91D Mg alloy by micro-arc oxidization technique

With increasing applied voltage, three types of anodic coatings, passive film, micro-spark ceramic coating and spark ceramic coating were made by micro-arc oxidization (MAO) technique on AZ91D magnesium alloy in alkali-silicate solution. The structure, composition characteristics and the electrochemical properties of coatings were also studied with SEM, XRD and EIS (electrochemical impedance spectroscopy) technique, respectively. It is found that the electrochemical properties are closely related to the structure and composition characteristics of the anodic coatings. At the same time, the characteristics of the three types of anodic coatings differ significantly, among them, the micro-spark ceramic coating, prepared in the voltage range of 170similar to220V exhibits compact, homogeneous structure and highest corrosion-resistance.

大别（超）包产到户铁岩和阜新火山岩铂族元素斌存规律研究

The platinum-group elements (PGE), including Os, Ir, Ru, Rh, Pt and Pd, axe strongly siderophile and chalcophile. On the basis of melting temperature, the PGE may be divided into two groups: the Ir group (IPGE, >2000°C) consisting of Os, Ir and Ru, and the Pd group (PPGE, <20GO°C) consisting of Rh, Pt and Pd. Because of their unique geochemical properties, PGE provide critical information on global-scale differentiation processes, such as core-mantle segregation, late accretionary history, and core-mantle exchange. In addition, they may be used to identify magma source regions and unravel complex petrogenetic processes including partial melting, melt percolation and metasomatism in the mantle, magma mixing and crustal contamination in magma chambers and melt crystallization.Compared with other rocks, (ultra)mafic rocks have lower REE content but higher PGE content, so PGE have advantages in studying the petrogeneses and evolution of them. In this study, we selected (ultra)mafic rocks collected in Dabie Orogen and volcanic rocks from Fuxin Region. Based on the distribution and behaviour of platinum-group elements, combined with other elements, we speculate the magma evolution and source mantle of these (ultra)mafic rocks and volcanic rocks.Many (ultra)mafic rocks are widely distributed in Dabie Region. According to their deformation and metamorphism, we classed them into three types. One is intrusive (ultra)mafic rocks, which are generally undeformed and show no or little sign of metamorphism, such as (ultra)mafic intrusions in Shacun, zhujiapu, Banzhufan, qingshan, Xiaohekou, Jiaoziyan, Renjiawan and Daoshichong. The other one is ultrahigh pressure metamorphic (ultra)mafic rocks, some of them appeared as eelogites, such as complex in Bixiling and adjacent Maowu. Another one is intense deformed and metamorphic, termed as tectonic slice, alpine-type (ultra)mafic rocks. The most representative is Raobazhai and Dahuapin. However, there are many controversies about the formation of those (ultra)mafic rocks. Here, we select typical rocks of the three types. The PGE were determined by inductively coupled plasma mass spectrometry (ICP-MS) ater NiS fire-assay and tellurium co-precipitation.The PGE tracing shows that three components are needed in the source of the cretaceous (uitra)mafic intrusions. They could be old enriched sub-continental lithospheric mantle, lower crust and depleted asthenospheric mantle. The pattern of PGE also shows the primitive magma of these intrusions underwent S saturation. According to palladium, we can conclude that the mantle enrich in PGE. Distribution of PGE in Bixiiing and Maowu (ultra)mafic rocks display they are products of magmas fractional crystallization. The (ultra)mafic rocks in Bixiiing and Maowu are controlled by various magmatic processes and the source mantle is depleted in PGE. Of interest is that the mantle produced UHP (ultra)mafic rocks are PGE-depleted, whereas the mantle of cretaceous (ultra)mafic intrusions are enrich in PGE. This couldindicate that the mantle change from PGE-enriched to PGE-depleted during120-OOMa, which in accord with the time of tectonic system change in the East China. At the same time, (ultra)mafic intrusions in cretaceous took information of deep mantle, which means the processes in deep mantle arose structural movement in the crust The character of PGE in alpine-type (ultra)mafic rocks declared that the rocks had experienced two types of metasomatic processes - hydrous melt derived from slab and silicate melt. In addition, we analyze the platinum-group elements in volcanic rocks on the northern margin of the North China Craton, Fuxin. The volcanic rocks characterized by negative anomalies of platinum. This indicates that platinum alloys, which may host some Pt resided in the mantle. The PGE patterns also show that Jianguo alkali basalts derived from asthenospheric mantle source, but wulahada high-Mg andesites derived from lithospheric mantle.

生物壳体Sr／Ca、Mg／Ca、^87Sr／^86Sr比值在恢复古气候、古环境中的应用—以小渡口剖面为例

生物壳体的Sr/Ca、Mg/Ca比值能反映其沉积水体的Sr/Ca、Mg/Ca比值，在一定条件下反映水体的盐度、温度，并分别与宿生水体的盐度、温度呈正比关系。生物壳体的^87Sr/^86Sr比值是恢复盆地古水文条件的一种重要手段。本文以著名的泥河湾盆地小渡口剖面的第28层为实例，力图通过对有孔虫、介形虫、腹足类生物壳体Sr/Ca、Mg/Ca比值与^87Sr/^86Sr比值的对比研究，并结合前人所作的中更新世古地理特征研究，来恢复生物壳体沉积时泥河古湖水的温度、盐度，进而进行古气候、古环境的恢复。研究结果表明：在0.97-0.94Ma间，古泥河湾湖为一陆相湖泊，湖水的温度、盐度变化趋势相吻合，均呈低－高－低的演化特征，可能对应着盆地水体的扩展－退缩－扩展变化。其中，在0.96-0.95Ma间，古泥河湾湖具有较高的温度、盐度特征。生物壳体的Sr/Ca、Mg/Ca比值能反映其沉积水体的Sr/Ca、Mg/Ca比值，在一定条件下反映水体的盐度、温度，并分别与宿生水体的盐度、温度呈正比关系。生物壳体的^87Sr/^86Sr比值是恢复盆地古水文条件的一种重要手段。本文以著名的泥河湾盆地小渡口剖面的第28层为实例，力图通过对有孔虫、介形虫、腹足类生物壳体Sr/Ca、Mg/Ca比值与^87Sr/^86Sr比值的对比研究，并结合前人所作的中更新世古地理特征研究，来恢复生物壳体沉积时泥河古湖水的温度、盐度，进而进行古气候、古环境的恢复。研究结果表明：在0.97-0.94Ma间，古泥河湾湖为一陆相湖泊，湖水的温度、盐度变化趋势相吻合，均呈低－高－低的演化特征，可能对应着盆地水体的扩展－退缩－扩展变化。其中，在0.96-0.95Ma间，古泥河湾湖具有较高的温度、盐度特征。