63 resultados para Latini, Brunetto, 1220-1295.
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This review focuses on the synthesis, assembly, surface functionalization, as well as application of inorganic nanostructures. Electrochemical and wet- chemical methods are demonstrated to be effective approaches to make metal nanostructures under control without addition of a reducing agent or protecting agent. Owing to the unique physical and chemical properties of the nano-sized materials, novel applications are introduced using inorganic nanomaterials, such as electrocatalysis, photoelectricity, spectrochemistry, and analytical chemistry.
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A series of NIR organic chromophores with donor-pi-acceptor-pi-donor structure are synthesized. Good thermal stability and strong photoluminescence in solid state render them suitable for application in light-emitting diodes. Exclusive near-infrared emission at 1080 nm with external quantum efficiency of 0.28% is obtained from the nondoped OLEDs. The longest electroluminescence wave-length is 1220 nm.
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The alkaloid components in Strychnos nux-vomical L. uncombined and combined with Glycyrrhiza uralensis Fisch have been investigated by electrospray ionization tandem mass spectrometry ( ESI-MSn) and HPLC. The experimental results demonstrated that the number of strychnine and brucine all declined in combined Strychnos nux-vomical L. with Glycyrrhiza uralensis Fisch, and the concentration level of strychnine fell obviously. The results of ESI-MS were identical to those of HPLC, which provided scientific basis for explanation of detoxicity of Glycyrrhiza uralensis Fisch and the reasonable combination of Strychnos nux-vomical L.
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Ti基准晶材料具有热力学稳定的正二十面体构造,表现出特殊的传输特性、贮氢特性和力学特性等,相关研究受到广泛关注.近年,作者所在研究组在Ti基准晶的制备和贮氢性能研究方面取得了一些新进展.综合报道了Ti-Zr-Ni-Cu系准晶相及其复合相材料的制备和贮氢性能.
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A series of nickel(II) complexes bearing two nonsymmetric bidentate beta-ketoiminato chelate ligands have been prepared, and the structures of complexes [(2,6-Me2C6H3)NC(CH3)C(H)C(Ph)O](2)Ni (4a) and [(2,6-Me2C6H3)NC(CH3)C(H)C(CF3)O](2)Ni (4c) have been confirmed by X-ray crystallographic analysis. These nickel(II) complexes were investigated as catalysts for the vinylic polymerization of norbornene. Using modified methylaluminoxane (MMAO) as a cocatalyst, these complexes display very high activities and produce high molecular weight polymers. Catalytic activity of up to 1.16 x 10(4) kg/mol(Ni) .h and the viscosity-average molecular 9 weight of polymer of up to 870 kg/mol were observed. Catalyst activity, polymer yield, and polymer molecular weight could be controlled over a wide range by the variation of the reaction parameters such as Al/Ni molar ratio, norbornene/catalyst molar ratio, monomer concentration, polymerization reaction temperature and time.
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A novel solution-phase method for the preparation of Au@ZnO core-shell composites was described. With this method, the composites were grown without heating that is usually needed in other solution methods. Atomic force microscopy (AFM) results show that the diameter of Au@ZnO core-shell composites is about 10.5 nm. X-ray photoelectron spectroscopy (XPS) was applied to characterize Au@ZnO core-shell composites. The optical properties of Au@ZnO core-shell composites, including UV-vis absorption and photo luminescence (PL), were observed at room temperature.
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Carbon nanotubes (CNTS) coating with europium oxide by a simple method is reported in this letter for the first time. The CNTS were refluxed in a solution of nitric acid containing europium nitrate, and the pH value was subsequently ajusted with ammonia solution. At last, the mixture was filtered and annealed. The TEM micrograph showed that the CNTS were covered with a uniform thin layer with thickness of about 15 nm. The XRD results revealed that the CNTS were coated with europium oxide.
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A detailed petrologic and mineralogic study was carried out on serpentinized peridotites dredged from the southern landward slopes of the Mariana Trench, in order to reveal the serpentinization process of these unusual rocks and to identify the sole presence of the mineral lizardite. The constituent minerals of these southern Mariana forearc peridotites are olivine, amphibole and spinel, as well as serpentine, chlorite and talc. Compared with serpentinite seamounts, the serpentinized peridotites from the southern Mariana forearc are characterized by the absence of magnetite and brucite, and the common presence of talc; besides, the serpentine mineral variety is simplex, only lizardite. Combining mineral chemistry and mineral phase relationships, we conclude that (1) the absence of magnetite in the serpentinized peridotites is due to incomplete serpentinization, other than magnetite, the iron end-member in olivine forms Fe-rich brucite and Fe-rich serpentine; (2) brucite is not stable with high silica activity, reacting with later SiO2-rich fluid and then forming lizardite, leading to a lack of brucite in these serpentinized peridotites; (3) the occurrence of talc is the result of later SiO2-rich fluid reactions with lizardite; and (4) the reason for the sole occurrence of lizardite is that the temperature condition of our study area was not high enough for the formation of antigorite (which is stable at > 500 degrees C). Despite the broad overlap of lizardite and chrysotile in growth temperature, differences in the modes of occurrence of lizardite and chrysotile, such as the scarcity of H2O, low porosity and permeability, as well as the actual situation of initial serpentinization in the study area, result in the absolute prevalence of lizardite over chrysotile in the area. (C) 2009 National Natural Science Foundation of China and Chinese Academy of Sciences. Published by Elsevier Limited and Science in China Press. All rights reserved.
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在过去的几十年间,利用线粒体基因组序列探讨后生动物深层次的系统发育关系已取得初步进展。这主要得益于,线粒体基因组与其它分子标记相比具备诸多优势。迄今为止,超过1,200个后生动物的线粒体基因组已被测定,然而所获得的数据分布极不均衡。 软甲纲历来是甲壳动物分类学和系统发育学研究的重要类群,在形态学特征和分子生物学各方面取得广泛的发展。尽管软甲纲本身作为单系群已得到大多数甲壳动物学家认可,但是软甲纲内部各个类群之间的系统发育关系迄今仍颇有争议。本文报道了凡纳滨对虾Litopenaeus vannamei、中国明对虾Fenneropenaeus chinensis、脊尾白虾Exopalaemon carinicauda、太平洋磷虾Euphausia pacifica和采自南极普里兹湾南极磷虾Euphausia superba的线粒体基因组,其长度分别为15,989 bp、16,004 bp、15,730 bp、16,898 bp和15,498 bp以上(部分非编码区没有测定)。 本研究发现凡纳滨对虾、中国明对虾、脊尾白虾和太平洋磷虾的线粒体基因组包含后生动物线粒体基因组典型的基因组成(13个蛋白质编码基因、22个转运RNA、2个核糖体RNA和一个非编码的AT富含区);然而,南极磷虾与后生动物线粒体基因组典型的基因组成相比,存在1个trnN基因的重复。与泛甲壳动物线粒体基因组的原始排列相比,凡纳滨对虾和中国明对虾线粒体基因组的基因排列完全一致;脊尾白虾的线粒体基因组发生罕见的trnP和trnH易位,从而说明在真虾下目中线粒体基因组的基因排列并不保守;太平洋磷虾线粒体基因组的基因排列出现3个转运RNA的重排 (trnL1、trnL2和trnW);南极磷虾线粒体基因组的基因排列除了出现太平洋磷虾具有的这3个转运RNA重排之外,还有1个trnN的重复和1个trnI基因的重排。另外,在太平洋磷虾线粒体基因组最大的非编码区中存在一个154 bp×4.7的串连重复区域,如此大片段的串联重复区域(>150 bp)在软甲纲动物线粒体基因组中是首次报道。 目前所获得的线粒体基因组数据强有力地支持口足目、对虾科、真虾下目和短尾下目为单系群。通过比较基因排列及蛋白质编码基因核苷酸和氨基酸序列的系统发育分析得知真虾类和龙虾类为腹胚亚目的原始类群,并支持“((Penaeus+Fenneropenaeus)+Litopenaeus)+Marsupenaeus”的系统发育关系。此外,线粒体基因组的数据也强有力地支持磷虾目为单系群。但对于磷虾目在软甲纲中的分类地位及与其它类群的系统发育关系存在一些分歧:基于蛋白质编码基因核苷酸和氨基酸数据的贝叶斯分析强有力地支持磷虾目和十足目近缘,这个结果和传统的分类系统完全一致;然而,基于核苷酸序列的邻接法、氨基酸序列的邻接法和最大似然法均强有力地支持磷虾类和对虾类亲缘关系较近,从而破坏了十足目的单系性,与传统的认识并不一致,但由于自展值的支持率非常高,所以深层次的分析需要进一步加强。 星虫动物属于海洋生物中的一个小门类,自1555年被记载以来,其在后生动物中的分类地位就备受争议。本研究测定了星虫动物门的第一条线粒体基因组:革囊星虫Phascolosoma esculenta的线粒体基因组,全长为15,494 bp,包含13个蛋白质编码基因、22个转运RNA、2个核糖体RNA和1个非编码的AT富含区,所有37个基因在同一条链上编码。与后生动物线粒体基因组的典型组成相比,存在一个trnR基因的缺失和一个trnM基因的重复。比较星虫动物和其它后生动物的线粒体基因组,可以得到以下结论:1)星虫动物和环节动物(包括螠虫动物)的线粒体基因组有相近的基因排列,而且所有基因都在同一链上编码;2)基于蛋白质编码基因的系统发育分析强有力地支持星虫动物和环节动物(包括螠虫动物)组成一个单系群,而将软体动物排除在外。因此,本研究认为以前许多星虫动物和软体动物“共享”的特征,包括发育特征和缺乏分节等,需要重新考虑。
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Metagentiana striata is an alpine annual herbaceous plant endemic to the east of the Qinghai-Tibet (Q-T) Plateau and adjacent areas. The phylogeography of M. striata was studied by sequencing the chloroplast DNA (cpDNA) trnS-trnG intergenic spacer. Ten haplotypes were identified from an investigation of 232 individuals of M. striata from 14 populations covering the entire geographical range of this species. The level of differentiation amongst populations was very high (G(ST) = 0.746; N-ST = 0.774) and a significant phylogeographical structure was observed (P < 0.05). An analysis of molecular variance found a high variation amongst populations (76%), with F-ST = 0.762 (highly significant, P < 0.001), indicating that little gene flow occurred amongst the different regions; this was explained by the isolation of populations by high mountains along the Q-T Plateau and adjacent areas (N-m = 0.156). Only one ancestral haplotype (A) was common and widespread throughout the distributional range of M. striata. The populations of the Hengduan Mountains region of the south-eastern Q-T Plateau showed high diversity and uniqueness of haplotypes. It is suggested that this region was the potential refugium of M. striata during the Quaternary glaciation, and that interglacial and postglacial range expansion occurred from this refugium. This scenario was in good agreement with the results of nested clade analysis, which inferred that the current spatial distribution of cpDNA haplotypes and populations resulted from range expansion, together with past allopatric fragmentation events. (c) 2008 The Linnean Society of London.
Resumo:
Livestock grazing has long been the most widespread land use on the Qinghai-Tibet Plateau, one of the world's highest ecosystems. However, there has been increasing concern during recent decades because of the rapid increase in livestock numbers. To assess the possible influences of grazing on the vast grassland, a long-term grazing experiment in a shrub meadow on the northern Qinghai-Tibet Plateau was carried out. The experiment included five treatments with different stocking rates and one non-grazing (N) treatment. After 17 years of grazing, treatment differences were clear. The species composition differed markedly between grazing intensities, with a decrease in palatable grass species and an increase in unpalatable forbs at higher grazing intensities. The species richness and species diversity, however, were not significantly different between treatments. Vegetation height decreased significantly at higher grazing intensities. Total above,ground biomass declined considerably and the biomass of forbs increased significantly under the higher grazing intensities. The amount of litter was significantly lower under the higher grazing intensities. The results suggest that long-term grazing alters the species composition, vegetation height and biomass production of the alpine grassland ecosystem without significantly changing species richness.
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本文介绍了我们建立的基于Agnet的分布协作式多机器人装配系统-DAMAS,在此基础上研究了多机器人合作的协商协议,采用了改进的合同网协议方法,针对多机器人协商协议的软件实现了,采用了应用前景广阔的分布式对象技术,介绍了机器人合作装配的协商协议的具体实现方法。
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This thesis mainly concentrates on the geochronology, prtrology, elemental geochemistry and Sr-Nd-Pb-Hf isotopic geochemistry of the volcanic rocks in north Da’Hinggan Mountain. By analyzing the data obtained in this study and data from other people, this thesis explored the age distribution, petrology and mineralogy and geochemistry characteristics of the volcanic rocks in north Da’Hinggan Mountain. Furthermore, this thesis speculated upon the source characteristics of these volcanic rocks and their implications for the tectonic evolution and crust accretion. According to the twenty Ar-Ar ages, four zircon U-Pb SHRIMP ages and two Zircon U-Pb LA-ICP-MS ages, the duration of the eruption of the Late Mesozoic volcanic rocks in north Da’Hing Mountain was about 160Ma-106Ma. Most of these volcanic rocks belong to early Cretaceous and the late Jurassic volcanic rocks are only restricted in Manzhouli. The bulk of the late Mesozoic volcanic rocks are high-K calc-alkaline rocks. Only a small portion of these volcanic rocks are shoshonites. These rocks are mainly intermediate or acid and the basic rocks usually have higher alkaline contents. Rock types are very complex in this region. These volcanic rocks have a large TiO2 variation and the Al2O3 and alkaline contents are high. From the point of mineralogy, the plagioclases in these volcanic rocks are oligoclases, andesines and labradorites, and the labradorites are more common. Most pyroxenes in these volcanic rocks are augites which belong to clinopyroxene. The source of the Late Mesozoic volcanic rocks was an enriched lithospheric mantle. When the magma en route to the surface it was contaminated by crust material slightly and had some fractional crystallization. These rocks which mainly belong to high-K calc-alkaline series were one of the results of postorogenic tectonic-magmatic activities. The upwelling in late Mesozoic supplied heat to melt the enriched lithospheric mantle which was resulted from the subduction of paleo-Asian Ocean and/or Mengol-Okhotsk ocean. These late Mesozoic volcanic rocks are also important to the upper crustal accretion of north Da’Hinggan Mountain since the late Mesozoic. These volcanics and the contemporary emplacement of granites and the basaltic underplating in combination fulfilled the crust accretion history in north Da’Hinggan Mountain in Late Mesozoic.