A new oxide ion conductor: La3GaMo2O12

A new oxide ion conductor, La3GaMo2O12, with a bulk conductivity of 2.7 X 10(-2) S.cm(-1) at 800 degrees C in air atmosphere was prepared by the traditional solid-state reaction. The room temperature X-ray diffraction data could be indexed on a monoclinic cell with lattice parameters of a=0.5602(2) nm, b=0.3224(1) nm, c= 1.5741(1) nm, beta= 102.555(0)degrees, V=0.2775(2) nm(3) and space group Pc(7). Ac impedance measurements in various atmospheres further support that it is an oxide ion conductor. This material was stable in various atmospheres with oxygen partial pressure P(O-2) ranging from 1.0 X 10(5) to 1.0 X 10(-7) Pa at 800 degrees C. A reversible polymorphic phase transition occurred at elevated temperatures as confirmed by the differential thermal analysis and dilatometric measurement.

Studies on preparation of iron phenanthroline and 8-hydroxyquinoline complexes/Y zeolite, characterization and catalytic hydroxylation of phenol

Iron phenanthroline - and 8 - hydroxyquinoline complexes /Y zeolite, denoted a FePhen/Y and FeOx/Y respectively, were prepared; The formation of the metal complexes mentioned above within the cages of Y zeolite and their crystal structures were determined by elemental analyses, diffuse reflectance UV-Vis,SEM,BET,and XRD methods; The influence of experimental parameters upon phenol conversion and product selectivities were investigated as well.

铁邻菲咯啉、8-羟基喹啉配合物/Y型分子筛的制备、表征及催化苯酚羟化的研究

制备了铁邻菲咯啉、8-羟基喹啉配合物/Y型分子筛(简记为FePhen/Y,FeO_x/Y).用元素分析,TG-DTA,UV-Vis,IR,SEM,BET,及XRD等方法确定了分子筛笼中金属配合物的生成及其晶体结构,考察了实验参数对苯酚转化率及产物选择性的影响.

INTERACTIONS OF RARE-EARTH LENS WITH BOVINE BLOOD CU(ZN)-SUPEROXIDE DISMUTASE

The interactions of lanthanium trichloride and terbium trichloride with bovine blood Cu (Zn)-superoxide dismutase [Cu(Zn)-SOD] in the aqueous solution of hexamethylenetetrarnine buffer (pH = 6.3) have been studied by using fluorescece, CD and ESR spectra. The results indicated that rare earth ions were coordinated to the carboxyl groups of acidic amino acid residues which were far from active center of the Cu(Zn)-SOD molecule and only lightly disturbed the secondary structure of the enzyme protien, and made the coordination structure of enzyme-bound CU2+ come from the rhombchedron to the axial shape at 77 K and the activity of Cu(Zn)-SOD enzyme was not nearly changed at room temperature.

稀土离子与牛血Cu(Zn)-SOD的作用

采用ESR、CD谱和荧光光谱研究了pH=6.3时六次甲基四胺-HCl缓冲溶液中LaCl_3和TbCl_3与Cu(Zn)-SOD的配位作用和结构。Cu(Zn)-SOD可增强Tb~(3+)的荧光发射,Tb~(3+)与Cu(Zn)-SOD有多个配位位置,其中有2个强结合位点,La~(3+)与Tb~(3+)可竞争Cu(Zn)…SOD上相同结合位点,77K下La~(3+)与Tb~(3+)使Cu(Zn)-SOD的Cu~(2+)活性中心的配位环境由菱形对称结构向轴对称结构转变,使Cu(Zn)-SOD的局部结构变松散,但对SOD酶活性基本无影响,表明稀土离子主要与酶蛋白分子中的酸性氨基酸羧基配位,对酶蛋白二级结构仅产生微弱扰动,对活性中心空间结构影响较小,基本不影响Cu(Zn)-SOD酶活性。

用NMR方法研究杂多酸HPA-23与谷胱甘肽的作用

早在70年代初,人们就发现杂多酸具有抗病毒活性.例如钨锑酸钠[NaSb_9W_(21)O_(86)]~(18-)有可能成为潜在的抗病毒化合物.非常有趣的是最近报道[NH_4]_(18)[NaSb_9W_(21)O_(86)]·24H_2O(结构代号为HPA-23)具有很高的抗爱滋病病毒活性,在法国已进入临床应用.但从分子水平研究杂多酸化合物抗病毒的机理,目前尚未见到国内外报道.而作为病毒可以广义地看作由一个蛋白外壳包裹,内部则为核酸.爱滋病病毒同样由两层蛋白所包裹,与宿主细胞发生吸附作用主要是通过外层包络蛋白(GP120),该蛋白的活性组分是一个由8个氨基酸组成

SYNTHESIS, THERMAL-STABILITY AND X-RAY CRYSTAL-STRUCTURE OF THE BIS(CYCLOPENTADIENYL)YTTERBIUM NAPHTHOXIDE DERIVATIVE (C5H5)2YB(OC10H7)(THF)

Cp3Yb (Cp = C5H5) reacts with a-naphthol (HNP) in THF to form Cp2Yb(NP)(THF) (1), which crystallizes in the space group P2(1)/n with unit cell dimensions a = 8.084(2), b = 15.996(6), c = 15.973(7) angstrom, beta = 98.95(3), V = 2040.3 angstrom and D(calc.) = 1.69 g cm-3 for Z = 4. Least-squares refinement based on 2242 observed reflections converged to a final R value of 0.081. The average Yb-C(Cp) distance is 2.60(2) angstrom and Yb-O(THF) and Yb-O(NP) distances are 2.30(1) and 2.06(1) angstrom, respectively. The title compound loses the coordinated THF molecule readily by heating under vacuum to give dimeric [Cp2Yb(NP)]2 (2), which undergoes disproportionation to give Cp3Yb and Yb(NP)3 on heating above 230-degrees-C.

电感耦合等离子体原子发射光谱分析中导数光谱法研究——Ⅱ.数据平滑和扫描步长的影响

数据平滑和扫描步长是两个重要求导条件。本工作用五点三次多项式平滑技术对扫描数据进行平滑处理以消除随机噪音,但平滑次数增大会导致信号失真从而使导数光谱的分辨能力降低。扫描步长减小能提高导数光谱的分辨能力,但同时导致导数光谱灵敏度减小。导数光谱中干扰物等效浓度IEC的大小是上述因素的综合反映。本文以IEC为考察指标,讨论了平滑次数和扫描步长的优化。

Phenomenon of micro-droplets formation on metals during the deliquescence of salt particles in atmosphere

CORROSION; MECHANISM; WATER; ZINC

Cryopreservation of flounder (Paralichthys olivaceus) sperm with a practical methodology

A simple and convenient protocol for the cryopreservation of the flounder (Paralichthys olivaceus) sperm was established for "on the spot" cryopreservation of large quantities of semen. The use of three cryoprotectants, dimethyl sulphoxide (DMSO), glycerol (Gly) and methanol was tested in the method. The percentage of motile sperm present in semen after it had been frozen and thawed in the presence of DMSO, Gly or methanol was 60.5 +/- 3.6, 79.17 +/- 4.5 and 13.25 +/- 4.7%, respectively. The fertilization rates of this sperm were 67.06 +/- 15.1, 76.20 +/- 10.0 and 44.93 +/- 22.6%, while the hatching rates of eggs fertilized with this sperm were 37.40 +/- 8.3, 48.18 +/- 25.7 and 23.35 +/- 10.8%, respectively. It was found that Gly and DMSO were better cryoprotectants than methanol, with Gly giving the best overall results. Under scanning electron microscopy, it could be seen that while the majority of the frozen-thawed sperm remained morphologically normal, some exhibited lost or dilated mitochondria, swollen mid-pieces, broken tails, or damaged cell membrane, which probably caused the decrease in motility and fertility of the frozen-thawed sperm. (C) 2003 Elsevier Science Inc. All rights reserved.

马里亚纳海沟南部橄榄岩的研究：地幔楔中含水流体－橄榄岩的相互作用

弧下地幔楔是俯冲板片物质向地表折返的必经之地，对地幔楔橄榄岩的研究是研究“俯冲工厂”运行机制的重要环节。为了深入了解俯冲作用对弧下地幔楔橄榄岩的影响，本文对马里亚纳岛弧南部前缘的橄榄岩进行了岩石、矿物学和地球化学研究。根据矿物组成将这些橄榄岩分为两组：含辉石的Group1和不含辉石的Group2。矿物学和地球化学特征表明这些橄榄岩是弧下地幔楔高度部分熔融的残余，并叠加后期含水流体－橄榄岩的相互作用。全岩组成和矿物组成均表明马里亚纳岛弧南部前缘橄榄岩经历了比深海橄榄岩更高程度的部分熔融作用。并且，与橄榄石和斜方辉石相比，单斜辉石的亏损程度更高，暗示后期含水流体的渗入引起了马里亚纳岛弧南部前缘橄榄岩的局部熔融。后期含水流体－橄榄岩的相互作用使马里亚纳弧下地幔楔发生Ca、Na的相对富集；并使单斜辉石在发生局部熔融的同时发生LILE和LREE以及Zr的相对富集；还明显改变了尖晶石的矿物组成；同时导致角闪石、斜方辉石等新的矿物相的形成。含水流体－橄榄岩相互作用下角闪石的形成是一个受温度影响的长期过程，早期高温条件下形成的角闪石还参与了橄榄岩的局部含水熔融作用。含水流体普遍富含Al、Ca和Na，对各种微量元素的溶载能力随着其温度的升高而升高，相对低的HREE和HFSE溶载能力暗示其源于俯冲板片的脱水作用。

五种红树植物光合产量模型及对环境因子的响应

以木榄（Bruguiera gymnorriza）、白骨壤（Avicennia marina）、桐花树（Aegiceras corniculata）、秋茄（Kandelia candel）和海漆（Excoecaria agallocha）为对象，以光合作用对环境因子的响应为主线，建立了从叶片水平到群体冠层水平上的光合产量模型，探讨了从器官、个体到群体的光合产量对环境因子响应的定量关系。 将Farquhar提出的单叶片光合作用生理生化模型与气孔导度B-B模型相结合，建立了光合作用－气孔导度耦合模型。模型模拟结果与实际测量结果具有较好的一致性。在温度为25.0℃，光合有效辐射为1000μmol•m-2s-1 的条件下，当外部CO2浓度倍增到720μmol•mol-1时，白骨壤、木榄、桐花树、秋茄、海漆的光合速率分别提高22.56%，17.13%，18.43%，18.63%和18.41%。在大气CO2浓度和光合有效辐射通量密度不变的条件下，光合作用速率对温度的响应呈单峰型曲线，即有一个最适温度，5种红树植物的最适温度值均为26.5℃左右。大气CO2浓度和温度固定不变（分别为350μmol•mol-1和25.0 ℃）时，光合作用对光合有效辐射的响应符合Michaelis-Menten反应曲线，模型在PAR<1800μmol•m-2s-1时模拟精度较高（P<0.01）。 在典型晴天条件下，5种红树植物的光合速率日变化都出现两个极大值（分别在11时和15时左右），中午前后光合速率较低，模型模拟光合速率日变化与实测数值日变化趋势一致。本模型能较好地模拟5种红树植物光合产量以及对环境因子的响应，模拟预测精度较高（P<0.01）。 以Ross和Nilson叶倾角分布模型为基础，分别建立了直接辐射和散射辐射在冠层内传输的子模型。冠层内的消光系数均有明显的日变化，且上午8时之前和下午16时之后随时间变化较大。在典型晴天条件下，单位土地面积日合成干物质总量（折合为CH2O）白骨壤为15.840g•m-2d-1，对于木榄、桐花树、秋茄、海漆其相应的值分别为 22.254 g•m-2d-1， 23.610 g•m-2d-1，24.525 g•m-2d-1和25.996 g•m-2d-1 。

高寒草甸牧草产量和草场载畜量模拟研究及对气候变暖的响应

高寒草甸地区温度是限制牧草地上年产量提高的主要因素。利用这一点, 引进牧草产量与生长期间的产量积温比概念, 建立高寒草甸牧草产量的估算模式。其估测值与实测值的拟合率较高, 相对误差平均只有2% , 说明模式的建立具有较好的应用价值。研究还表明, 现实状况下高寒草甸地区牲畜理论负载能力约为2. 54 个羊单位。在未来气候变暖(假设气温升高2 ℃, 降水不变) 的情景下, 草场生产力将有所降低, 相应的草场理论载畜量降低至1. 04 个羊单位。

藏东及滇东南新生代钾质岩浆作用及其深部制约

The dissertation focuses on the petrology, geochemistry of the volcanic rocks in east Tibet and southeast Yunnan. It lucubrates the Magmatic process, forming mechanism and the possible tectonic settings of the volcanic rocks. The volcanic rocks of Nangqen basin in east Tibet, Qinghai province are mainly Cenozoic intermediate-acid shoshonites. The rocks are LREE enriched and the LREE/HREE = 3～34; (La/Yb)_N = 18.17-53.59, and ΣREE 222～1260μg/g. There are no Eu anomaly, and Nb, Ta, Zr, Hf, Ti are markedly depleted. The isotopic composition is ~(87)Sr/~(86)Sr = 0.70497～0.70614, ~(206)Pb/~(204)Pb = 18.622～18.974, ~(208)Pb/~(204)Pb = 38.431～38.996, ~(207)Pb/~(204)Pb = 15.511～15.613, respectively. K-Ar age of the whole rocks and the single mineral are between 32.0-36.5Ma. Based on the trace elements and isotopic elements, we get the conclusion that the partial melting is one of the dominated forming mechanisms for the volcanic rocks in Naneqen basin. The magma did not experience the crustal contamination en route to the surface; however, the complex mixture took place in the upper mantle before the melt was formed. There are at least two kinds of mixed sources that can be identified. The basalt in southeast Yunnan province is studied. They are distributed in Maguan, Tongguan, and Pingbian County, which is located on the both sides of the Red River belt, and the ultrabasic xenolith are cursory introduced. The volcanic rocks belongs to the alkali series, which can be subdivided into trachybasalt and basanite(Ol normal molecule >5). The volcanic rocks are characteristics by high Ti and low Mg#. According to the magma calculation model, the original rocks of the basalt in southeast Yunnan province are Spinel Lherzolite in Tongguan, Garnet Lherzolite in Pingbian and Maguan, while Togguan undergoes 2-5 percent and percent of partial melting, whereas volcanism in Maguan and Pingbian was so complex to calculate. The fractional crystallization took place during the magma evoltion in southeast Yunnan. The basalt is enriched in LREE with LREE/HREE=9.23-20.19. All of the trace elements display weak Nb, Ta peak, and the depletion of Zr, Hf and Ti in Maguan and pingbian represent the presence of Garnet in the source. The composition of the isotope ratio are ~(87)Sr/~(86)Sr = 0.70333-0.70427, ~(143)Nd/~(144)Nd = 0.512769-0.512940, ~(206)Pb/~(204)Pb = 18.104-18.424, ~(207)Pb/~(204)Pb = 15.483 -15.527; ~(208)Pb/~(204)Pb = 37.938-38.560, respectively, which shows the characteristics of the HIMU type OIB. The volcanic rocks of the southwest Yunnan are derived from the enriched, OIB type mantle sources by synthesizing all the data from trace and isotope elements. It is similar to that of the volcanic rocks in Hawaii, a typical kind of the mixtures of the recycled oceanic crust plume and depleted asthenosphere. To sum up, the volcanic rocks in southeast Yunnan are formed by the intraplate hotpot volcanism.