ANODIC-OXIDATION OF HYDRAZINE ON GLASSY-CARBON ELECTRODES IN ACETONITRILE

The anodic oxidation kinetics of hydrazine on glassy carbon electrodes in acetonitrile were examined by cyclic voltammetry, a rotating ring-disc electrode technique and chronoamperometry. The experimental results of the rotating ring-disc electrode prove that hydrazine is oxidized to HN=NH, which cannot be oxidized further in acetonitrile. Hydrazine molecules are adsorbed on the electrode surface. One-third of the adsorbed hydrazine molecules are oxidized to HN=NH and the other two thirds act as proton acceptors. A possible mechanism of hydrazine oxidation is proposed.

HIGH-TEMPERATURE SUPERCONDUCTOR, YBA2CU3O7-X AS ALL-SOLID-STATE LITHIUM CELL

The utility of the high-temperature superconductor, YBa2Cu3O7-x as the cathode material for an all-solid-state lithium cell has been examined. The capacity of YBa2Cu3O7-x is 223 mA h g-1 and the discharge efficiency is > 92%. Measurements of a.c. impedance show that the charge-transfer resistance at the interface of the electrolyte/cathode is very low and increases with the depth-of-discharge of the battery. Studies using X-ray photoelectron spectroscopy (XPS) reveal that the cathode becomes doped with Li+ ions as the cell discharges.

SYNTHESES OF BIS(TERT-BUTYLCYCLOPENTADIENYL)LANTHANOID CHLORIDE COMPLEXES AND CRYSTAL-STRUCTURES OF BIS(TERT-BUTYLCYCLOPENTADIENYL)CHLORO(BISTETRAHYDROFURAN)-PRASEODYMIUM AND BIS(TERT-BUTYLCYCLOPENTADIENYL)-CHLOROTETRAHYDROFURANYTTERBIUM

Reaction of lanthanoid trichloride with two equivalents of sodium t-butylcyclopentadienide in tetrahydrofuran affords bis(t-butylcyclopentadienyl)lanthanoid chloride complexes (t-BuCp)2LnCl. nTHF (Ln = Pr, Nd, n = 2; Ln = Gd, Yb, n = 1). The compound (t-BuCp)2PrCl.2THF (1) crystallizes from THF in monoclinic space group P2(1)/c with unit cell dimensions a = 15.080(3), b = 8.855(2), c = 21.196(5) angstrom, beta = 110.34(2)degrees, V = 2653.9 angstrom-3 and D(calcd) = 1.41 g/cm3 for Z = 4. The central metal Pr is coordinated to two t-BuCp ring centroids, one chlorine atom and two THF forming a distorted trigonal bipyramid. The crystal of (t-BuCp)2YbCl.THF (2) belongs to the monoclinic crystal system, space group P2(1)/n with a = 7.726(1), b = 12.554(2), c = 23.200(6) angstrom, beta = 97.77(2)degrees, V = 2229.56 angstrom-3, D(calcd) = 1.50 g/cm3 and Z = 4. The t-BuCp ring centroids, the chlorine atom and the oxygen atom of the THF describe a distorted tetrahedron around the central ion of ytterbium.

4f金属化合物催化苯乙烯和双烯烃的共聚——共聚反应的主要特征和聚合物的表征

在配位聚合反应的研究中,值得注意的研究课题之一是将稀土催化剂引入到苯乙烯和双烯烃的共聚反应。这一新课题的研究不仅对阐明4f金属配位聚合反应机理,且对开发新型稀土催化剂和共聚物,都有重要意义.例如,共聚物中顺式-1,4含量的多少,对它们的各种性能有明显的影响。

[Sm(CH_3CN)_9]·(AlCl_4)3·CH_3CN的合成和晶体结构

关于过渡金属乙腈配合物的合成和催化性能的研究在文献中已有很多报道。但是,含稀土元素的这类配合物的合成及催化性能的研究直到1986年才见报道。Thomas利用金属Eu和NOBF_4在乙腈中的反应制得了配合物[Eu(CH_3CN)_3(BF_4)_3]_x。本文报道了新乙睛稀土配合物[Sm(CH_3CN)_9]·(AlCl_4)_3·CH_3CN的合成及其晶体结构与分子结构。 (一) 实验 所有操作都在氩气保护下进行。无水SmCl_3用NH_4Cl法制得。AlCl_3经升华后使用。CH_3CN经P_2O_5干燥蒸馏。IR用Perkin-Elmer FTS-20红外光谱仪测定。

Establishment of a micro-particle bombardment transformation system for Dunaliella saliva

In this study, we chronicle the establishment of a novel transformation system for the unicellular marine green alga, Dunaliella salina. We introduced the CaMV35S promoter-GUS construct into D. saliva with a PDS1000/He micro-particle bombardment system. Forty eight h after transformation, via histochemical staining, we observed the transient expression of GUS in D. salina cells which had been bombarded under rupture-disc pressures of 450 psi and 900 psi. We observed no GUS activity in either the negative or the blank controls. Our findings indicated that the micro-particle bombardment method constituted a feasible approach to the genetic transformation of D. salina. We also conducted tests of the cells' sensitivity to seven antibiotics and one herbicide, and our results suggested that 20 mu g/ ml of Basta could inhibit cell growth completely. The bar gene, which encodes for phosphinothricin acetyltransferase and confers herbicide tolerance, was introduced into the cells via the above established method. The results of PCR and PCR-Southern blot analyses indicated that the gene was successfully integrated into the genome of the transformants.

Additional pandaloid shrimps from the South China Sea (Crustacea : Decapoda : Caridea), with description of one new species

The present paper reports 22 pandaloid shrimp species from the South China Sea and its adjacent area, including two new records of the South China Sea, 14 new records of the Nanshan Islands, and one new speices. Heterocarpus chani, new species, type localities from the Philippines and Nansha Islands, is distinguished from its allied species, H. gibbosus Bate, 1888, H. tricarinatus Alcock & Anderson, 1894 and H. lepidus De Man, 1917, by the third maxilliped with a short rudimentary exopod.

高原鼢鼠四肢骨的进化适应性分析

通过对比分析了高寒草甸生态系统的高原鼢鼠(Myospalax baileyi)、高原鼠兔(Ochotona curzoniae)及根田鼠(Microtus oeconomus)的四肢骨,结果表明,地下啮齿动物高原鼢鼠的四肢骨比地面种类高原鼠兔和根田鼠的对应骨骼粗壮,显示其较强的挖掘能力.与挖掘效率相关的尺骨挖掘动力臂系数,高原鼢鼠为0.361 7,而高原鼠兔和根田鼠不到0.17.高原鼢鼠与其他两物种的四肢骨重量分布也明显不同:高原鼢鼠的前肢骨重量超过后肢骨,而高原鼠兔及根田鼠则正好相反;高原鼠兔及根田鼠的桡尺骨重量在四肢骨中最低,而高原鼢鼠的桡尺骨重量在四肢骨中则最高.这些特征反映了地下啮齿动物为了适应地下生活方式,其四肢骨骼系统已经发生了显著变化,这对于研究地下啮齿动物的进化适应性问题具有重要意义.

柱前衍生-反相高效液相色谱荧光测定及质谱鉴定土壤和苔藓中的脂肪酸

合成新型荧光衍生试剂1-[2-(对甲苯磺酸酯)乙基]-2-苯基咪唑[4，5．f]9，10-菲(TSEPIP)，将其作为柱前衍生化试剂，在Eclipse XDB-Cs色谱柱上，采用梯度洗脱实现了30种游离脂肪酸(FFA)衍生物的基线分离。利用柱后在线的串联质潜以APCI大气压化学电离源正离子模式实现了各组分的质谱定性。对土壤与两种苔藓(狭叶绢藓、曲尾藓)中FFA组分的定量结果表明，苔藓植物从土壤中富集了大量的游离脂肪酸。荧光检测的激发和发射波长分别为λ_(ex)=260 mn，λ_(em)=380 nm。绝大多数脂肪酸的线性回归系数大于0．9993，检出限为3．2～37 fmol。建立的方法具有良好的重复性，对实际样品测定结果满意。

高寒草甸植被生育期耗水量和耗水规律的分析

用1991～1993年在高寒草甸地区植被生育期测定的土壤水分资料，联系土壤水分平衡方程，讨论高寒草甸植被生育期的耗水量和耗水规律的特征，结果表明，草甸地区植被生育期5月20日～9月15日，３年平均耗水量约为361.0ｍｍ；全年牧草地上净初级生物量与耗水量具有一定的相关性；植被生育期内气温、降水的协调配合能提高牧草地上净初级生物量。5～9月，植被耗水量变化量单峰型曲线，3年平均表明，７月耗水量最高，５月最低。

我国牛科（Bovidae）中3种动物的染色体组型比较分析

比较分析我国牛科中３种动物（即羚牛、绵羊、黄牛）的染色体组型，从染色体数目和形态上比较它们之间的差异，并讨论这３种动物彼此之间的进化亲缘关系和进行杂交育种的可能性，为畜牧育种培养新类型提供细胞遗传学的依据。

Effects of temperature on CO2 exchange between the atmosphere and an alpine meadow

The alpine meadow ecosystem on the Qinghai-Tibetan Plateau is characterized by low temperatures because of its high elevation. The low-temperature environment may limit both ecosystem photosynthetic CO2 uptake and ecosystem respiration, and thus affect the net ecosystem CO2 exchange (NEE). We clarified the low-temperature constraint on photosynthesis and respiration in an alpine meadow ecosystem on the northern edge of the plateau using flux measurements obtained by the eddy covariance technique in two growing seasons. When we compared NEE during the two periods, during which the leaf area index and other environmental parameters were similar but the mean temperature differed, we found that NEE from 9 August to 10 September 2001, when the average temperature was low, was greater than that during the same period in 2002, when the average temperature was high, but the ecosystem gross primary production was similar during the two periods. Further analysis showed that ecosystem respiration was significantly higher in 2002 than in 2001 during the study period, as estimated from the relationship between temperature and nighttime ecosystem respiration. The results suggest that low temperature controlled the NEE mainly through its influence on ecosystem respiration. The annual NEE, estimated from 15 January 2002 to 14 January 2003, was about 290 g CO2 m(-2) year(-1). The optimum temperature for ecosystem NEE under light-saturated conditions was estimated to be around 15 degrees C.

Effect of N fertilizer on the productivity and nutritive values of perennial grass mixtures in the alpine region of Qinghai-Tibetan Plateau, China

A study was conducted on grass mixtures that included smooth bromegrass (SB) + drooping wild ryegrass (DW), smooth bromegrass + Siberian wild ryegrass (SW) + crested wheatgrass (CW) and smooth bromegrass + Siberian wild ryegrass + drooping wild ryegrass + crested wheatgrass in the alpine region of Qinghai-Tibetan Plateau. The study was conducted from 1998 to 2000 to investigate the effects of N application rates and growing year on herbage dry matter (DM) yield and nutritive values. Herbage DM production increased linearly with N application rates. The effect of N application on DM yields was greater (P < 0.05) in the 2nd and 3rd production years than in the establishment year. Dry matter yields of SB + SW + CW and SB + SW + DW + CW can reach as high as 15 000 kg ha(-1) at 345 kg ha(-1) N rate in the 3rd growing year. With increased N application rates, crude protein (CP) contents and 48 h in sacco DM degradability of grasses increased (P < 0.05). No effect (P > 0.05) of N application was detected on organic matter (OM) and acid detergent fibre (ADF) concentration. It can be concluded that for increased biomass production in the alpine region of the Qinghai-Tibetan Plateau, a minimum of 345 kg N ha(-1) should be applied to grass stands in three split application of 115 kg N ha(-1), in early June, early July and late July

内蒙古龙头山Ag-Pb-Zn多金属矿床成矿模式及找矿模型

The recent years research indicated that middle-south section of Da Hinggan Mountains metallogenic belt has two periods(Hercynian and Yanshanian) characteristics of metallogenesis, as well as the most of ore deposits in the area closely relate to Permian strata. Longtoushan ore deposit discovered in 2004 is an Ag-Pb-Zn polymetallic ore deposit born in Permian and located in the east hillside of the metallogenic belt, which has considerable resources potentials. It has important research value for its good metallogenic location and blank research history. Base on the detail field geology studies, the geology characteristics of "two stages and three kinds of metallogensis" has established. According to further work through geochemistry research including trace element, REE, S, Pb and Sr isotope, as well as petrography, microtemperature measurement, Laser Raman analysis and thermodynamics calculation of fluid inclusion, origin and characteristic of the ore-forming material and fluid has been discussed. And a new technology of single pellet Rb-Sr isochrones has been tried for dating its born time. Bae on above work, study of ore deposit comparison has been carried out, and metallogesis controlling factor and geological prospecting symbol have been summarized. Finally, metallogenic model and prospecting model have been established. According to above, the next step work direction has been proposed. Main achievement of the paper are listed as follow: 1.Longtoushan ore deposit has experienced two metallogenic periods including hot-water sedimentation period and hydrothermal reformation period. There are three kinds of metallizing phase: bedded(or near-bedded) phase, vein-shaped phase and pipe-shaped phase. The mian metallogenic period is hot-water sedimentation period. 2.Ore deposit geochemistry research indicated that the metal sulfides have charcateristic of hot-water sedimentation metallogensis, but generally suffered later hydrothermal transformation. The barite mineral isotope content is homogenous, showing the seabed hot-water sedimentation origin characteristic. Wall rock, such as tuff is one of metallogenic material origins. Both of Pb model age and Rb-Sr isochrone research older age value than that of strata, possibly for been influenced by hydrothermal transformation, and interfusion of ancient basis material. 3.There are two kinds of main metallogenic fluid inclusion in barite of the Longtoushan ore deposit, which are rich gas phase( C type) and liquid phase (D type). Their size is 2～7um, and principal components is H2O. Both kinds of fluid inclusion have freezing point temperature -7.1～-2.4℃ and -5.5～-0.3℃, salinity 4.0～10.6wt% and 0.5～8.5wt%, homogeneous temperature 176.8～361.6℃ and 101.4～279.9℃, which peak value around 270℃ and 170℃, respectively. Density of the ore-forming fluid is 0.73～0.97g/cm3, and metallogenic pressure is 62.3×105～377.9×105Pa. Above characteristic of the fluid inclusion are well geared to that of ore deposit originated in seabed hot-water sedimentation. 4.Through the comparison research, that Longtoushan ore deposit has main characteristic of hot-water sedimentation ore deposit has been indicated. Ore-forming control factor and prospecting symbol of it has been summarized, as well as metallogenic model and prospecting model. Next step work direction about prospecting has also been proposed finally.