67 resultados para 8.2 ka event,
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本论文以提高有机/聚合物电致发光材料的发光效率为目的,通过改善发光材料分子的载流子传输平衡、增大分子体积为手段来减小荧光淬灭,设计并合成了一系列新型结构的络合物和聚合物。发现了一种合成五配位8-轻基喳琳铝络合物和双核铝8-轻基喳琳络合物的新方法,在分子中引入了电子和空穴传输基团改善了分子的载流子传输平衡,设计并合成了新型大体积的分子,提高了材料的发光效率,并系统地研究了分子结构与发光波长和发光效率的关系。主要工作如下:1发现了一种合成五配位8-经基喳琳铝络合物和双核铝8-经基喳琳络合物的新方法,克服了没有2一甲基的空间位阻作用很难形成五配位8-轻基喳琳铝络合物的困难。2合成了五配位2-甲基-8-轻基喳琳铝络合物并引入了具有不同空穴传输能力的第二配体。结果表明,与A 1 q;,相比,2-甲基-8-经基喳琳的引入导致了五配位络合物发光的蓝移,同时具有空穴传输能力的三苯胺基团的引入使电致发光器件的效率降低。3设计并合成了五配位8-轻基喳琳铝络合物,同时与Alq做了对比研究。研究发现,这一系列五配位络合物发射绿色荧光,五配位8-轻基喳琳铝络合物的发光波长主要由第一配体决定。4以五配位2-甲基-8-轻基喳琳铝和五配位8-轻基喳琳铝络合物为发光层制备了双层器件。结果表明,五配位8-经基喳琳铝络合物的电致发光波长主要由第一配体决定,第二配体只起到微弱的调节作用;第一配体对器件的发光效率起决定性的作用,第二配体的结构对络合物器件发光效率的影响在同一系列络合物中表现得非常明显。5从增加分子体积能够减小分子之间聚集,增强荧光效率这一观点出发,合成了具有双核铝的8一TTA-基喳琳络合物Me-DAlqz和PPv-DAlq3,用Me-DAlq,作发光层制备了双层器件,并与Alq_3i和AIMq_3作了对比研究。结果表明,DA 1 q,双层器件中的发光效率比Alq_3器件的性能稍高一些,证明了大体积分子能够增加荧光效率的观点。6合成了含有空穴传输性能的三苯胺基团的嗯二吟配体,并用其合 成了金属络合物。这些络合物发射蓝色的荧光,与不带三苯胺的德二哇金属络合物在溶液中发基本相同波长的荧光。但在薄膜和单层电致发光器件中,络合物的荧光发生了不同程度的红移。含三苯胺络合物的单层器件发光效率高于不含三苯胺络合物的单层器件的效率,证实了三苯胺的引入改进了载流子的传输平衡。7合成了系列嗯二哇基团两侧带有蔡环的金属络合物并以这些络合物为发光层制备了双层有机电致发光器件。结果表明,蔡环的引入导致了嗯二哇金属络合物在薄膜状态和电致发光器件中的发光波长比在溶液中的发光波长有了很大的红移。8设计并合成了既具有空穴传输性能又具有电子传输性能的蓝色发光聚合物。用电化学方法证明了它们具有两极性质,表明嗯二哇的引入增加了聚合物的电子传输能力。
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用紫外 -可见 ( UV-Vis)吸收光谱和电化学方法研究 Eu3+ 与微过氧化物酶 -8( MP-8)相互作用的机理 ,发现 Eu3+优先与 MP-8中血红素基团的 2个丙酸基的羧基氧发生强的配位作用 ,导致 MP-8分子中血红素基团的非平面性、暴露程度和电化学可逆性的增加 .过剩的 Eu3+与 MP-8分子中肽链上的含氧基团发生弱的相互作用 ,对血红素基团结构的影响较小
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A new heteropolycomplex, K6H3[ZnW11O40Al] . 9.5H(2)O was prepared and characterized by means of elemental analysis, IR, UV spectroscopy, Al-27 NMR, electrochemistry and X-ray crystallography. The crystal of K6H3[ZnW11O40Al] . 9.5H(2)O is cubic, space group Fm-3m, with lattice constants a=b=c=2. 144 8(2) nm, V = 9.866(2) nm(3), Mo radiation, R = 0.057 8 for 497 independent data with [I>2 delta(I)]. The anion is of alpha-type Keggin structure with C-s symmetry.
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本文用三苯基氢化锡、三对甲苯基氢化锡作为锡氢化试剂与1-乙炔基环辛醇进行反应,合成了两个有机锡化合物:[Z]-1-[2-(三苯基锡基)乙烯基]环辛醇(1)和[Z]-1-[2-(三对甲苯基锡基)乙烯基]环辛醇(2),并测定了1的晶体结构.1和2分别与ICl,Br_2,I_2反应,得到六个有机锡一卤化物和三个有机锡二卤化物(3~11).有机锡二卤化物6和一卤化物5与KOH乙醇溶液反应,分别得到相应的锡氧化物和锡氢氧化物(12,13).有机锡二卤化物8分别与含氮双齿配体[2,2-联吡啶(Bipy),5-硝基-1,10-邻菲罗啉(Nphen),8-羟基喹啉(Oxin)]反应,得到三个相应的配合物(14~16).十六个新化合物通过元素分析、锡含量测定、IR、~1HNMR测定对其结构进行了表征,同时提出了1和2的生成反应历程.
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合成了标题酞菁铜衍生物,并通过元素分析,高压液相色谱,紫外光谱,红外光谱,核磁共振谱,电镜,顺磁共振谱及质谱加以确认。该化合物在稀氯仿溶液和LB膜中各以单,双分子缔合的形式存在。Z型沉积形成的单层LB膜对氨气有很高的灵敏度和选择性。
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采用多速粘度计和Monsanto试验机联用,在表观剪切速率为3×10~(-8)—2.5×10~8s~(-1)时观察了高1,2-聚丁二烯(PB)生胶与顺式1,4-PB,EPDM,SBR 1500在流变性质上的差异。高1,2-PB虽在中等剪切速率下有较高的粘度,但在低、高剪切速率时的粘度均较低,这一特性有利于它的加工。高1,2-PB在低剪切速率下的流动活化能较其他橡胶高,故抗冷流性能优越,易于存放。
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本文研究了双甲基丙烯酸乙二醇酯(EGDMA)对无规1,2-聚丁二烯(1,2-PB)辐射效应的影响。通过辐照1,2-PB和不同EGDMA/1,2-PB比率体系的溶胶分数测定,红外光谱分析及~1H-NMR测试结果,讨论了EGDMA对1,2-PB辐射化学反应(分子间交联及分子内环化)的作用及机理。结果证明,1,2-PB辐射引起的链式交联反应不因EGDMA的存在而改变(无规链反应),但EGDMA的存在将增加1,2-PB的交联引发G(I)值和交联G(c.1)同时导致G(-V)和G(cy)值的减小,抑制或减少,内环化过程。
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Well-dated, high-resolution records of planktonic foraminifera and oxygen isotopes from two sediment cores, A7 and E017, in the middle Okinawa Trough reveal strong and rapid millennial-scale climate changes since similar to 18 to 17 thousand years before present (kyr B.P.). Sedimentation rate shows a sudden drop at similar to 11.2 cal. kyr B.P. due to a rapid rise of sea level after the Younger Dryas (YD) and consequently submergence of the large continental shelf on the East China Sea (ECS) and the retreat of the estuary providing sediment to the basin. During the last deglaciation, the relative abundance of warm and cold species of planktonic foraminifera fluctuates strongly, consistent with the timing of sea surface temperature (SST) variations determined from Mg/Ca measurements of planktonic foraminifera from one of the two cores. These fluctuations are coeval with climate variation recorded in the Greenland ice cores and North Atlantic sediments, namely Heinrich event 1 (H1), Bolling-Allerod (B/A) and YD events. At about 9.4 kyr B.P., a sudden change in the relative abundance of shallow to deep planktonic species probably indicates a sudden strengthening of the Kuroshio Current in the Okinawa Trough, which was synchronous with a rapid sea-level rise at 9.5-9.2 kyr B.P. in the ECS, Yellow Sea (YS) and South China Sea (SCS). The abundance of planktonic foraminiferal species, together with Mg/Ca based SST, exhibits millennial-scale oscillations during the Holocene, with 7 cold events (at about 1.7, 2.3-4.6, 6.2, 7.3, 8.2, 9.6, 10.6 cal. kyr BP) superimposed on a Holocene warming trend. This Holocene trend, together with centennial-scale SST variations superimposed on the last deglacial trend, suggests that both high and low latitude influences affected the climatology of the Okinawa Trough. (c) 2006 Elsevier B.V. All rights reserved.
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A pre-column derivatization method for the sensitive determination of amines using a labeling reagent 2-(11H-benzo[a]-carbazol-11-yl) ethyl chloroformate (BCEC-Cl) followed by high-performance, liquid chromatography with fluorescence detection has been developed. Identification of derivatives was carried out by LC/APCI/MS in positive-ion mode. The chromophore of 1,2-benzo-3,4-dihydrocarbazole-9-ethyl chloroformate (BCEOC-Cl) reagent was replaced by 2-(11H-benzo[a]-carbazol-11-yl) ethyl functional group, which resulted in a sensitive fluorescence derivatizing reagent BCEC-Cl. BCEC-Cl could easily and quickly label amines. Derivatives were stable enough to be efficiently analyzed by HPLC and showed an intense protonated molecular ion corresponding m/z [M+ H](+) under APCI/MS in positive-ion mode. The collision-induced dissociation of the protonated molecular ion formed characteristic fragment ions at m/z 261.8 and m/z 243.8 corresponding to the cleavages of CH2O-CO and CH2-OCO bonds. Studies on derivatization demonstrated excellent derivative yields over the pH 9.0-10.0. Maximal yields close to 100% were observed with three- to four-fold molar reagent excess. In addition, the detection responses for BCEC-derivatives were compared to those obtained using 1,2-benzo-3,4-dihydrocarbazole-9-ethyl chloroformate (BCEOC-Cl) and 9-fluorenyl methylchloroformate, (FMOC-Cl) as labeling reagents. The ratios I-BCEC/I-BCEOC = 1.94-2.17 and I-BCEC/I-FMOC = 1.04-2.19 for fluorescent (FL) responses (here, I was relative fluorescence intensity). Separation of the derivatized amines had been optimized on reversed-phase Eclipse XDB-C-8 column. Detection limits calculated from 0.50 pmol injection, at a signal-to-noise ratio of 3, were 1.77-14.4 fmol. The relative standard deviations for within-day determination (n = 11) were 1.84-2.89% for the tested amines. The mean intra- and inter-assay precision for all amines levels were < 3.64% and 2.52%, respectively. The mean recoveries ranged from 96.6% to 107.1% with their standard deviations in the range of 0.8-2.7. Excellent linear responses were observed with coefficients of > 0.9996. (C) 2006 Elsevier B.V. All rights reserved.
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There are many Archean TTG grey suites in the Wutaishan area, northern Shanxi Province, China. In the past one hundred years, many geologists have done excellent research work in the Wutaishan and its adjacent regions. However, the TTG suites were almost neglected. Located in the northern slope of Mt. Hengshan-namely the Archean Hengshan Island Arc, intruded the Zhujiafang supercrustal rocks at almost 2.5Ga, the Yixingzhai TTG Suite is originated from partial melting of the ancient lower crust upper mantle by REE and trace elements, and the emplacement occurred in an Archean island arc. The rocks are mainly of tonalitic, I type, and calc-alkaline trends are found in the magmatic evolution. At almost 1.8 Ga, the suite was transformed to be dome-like schists in an arc-arc collision event, and the rocks were metamorphosed to an extent of amphibolitic to granulitic facies. The peak metamorphic condition is of 710-760 ℃/0.68-0.72GPa, and the subsequent cooling history is recorded as 560-620 ℃/0.46-0.60GPa. In the center of the Mt. Wutaishan-known as the Archean Wutaishan Island Arc, intruded the Archean Chechang-Beitai TTG Suite, which is of 2.5Ga old and of trondhjemitic and tonalitic, with coexisting I- and S-types and a trondhjemitic magmatic evolution trend. Through REE and trace elements, the suite is believed to be from the partial melting of the ancient lower crust or upper mantle. The 1.8 Ga collision event also made the suite gneissic and the it was metamorphosed to be amphibolitic facies, whose peak condition is approximately of 680 (±50) ℃/0.7Gpa, and the subsequent cooling process is recorded as 680 (±50) ℃、550(±50) ℃、420(±10) ℃. Crustal growth is fulfilled through magmatic intrusion as well as eruption at about 2.5Ga, arc-arc collision at about 1.8 Ga in the Wutaishan area and its environs. Additionally, the biotite-muscovite and muscovite-plagioclase geothermometers are refined, and the biotite-hornblende geothermometer is developed in this dissertation.
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在0.05 mol/L Tris,0.15 mol/L NaCl溶液中,用吸附伏安法研究长春新碱(VCR),其峰电位在-1.68 V(vs. Ag/AgCl),峰电流与1.0*10^{-8}~2.0*10^{-7}mol/L VCR浓度成正比,检测限为7.0*l0^{-9} mol/L,用常规脉冲极谱法、线性扫描和循环伏安法等研究该体系的电化学行为,实验表明,电极还原过程为具有吸附特征的不可逆过程。VCR的吸附符合Frumkin吸附等温式。也研究了VCR与微管蛋白的相互作用。实验表明,VCR与微管蛋白形成一电活性的结合物,这一结合物具有吸附性,且还原过程也为不可逆过程。
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Molecular dynamics (MD) simulations and first-principles calculations are carried out to analyze the stability of both newly discovered and previously known phases of ZnO under loading of various triaxialities. The analysis focuses on a graphite-like phase (FIX) and a body-centered-tetragonal phase (BCT-4) that were observed recently in [0 1 (1) over bar 0]- and [0 0 0 1]-oriented nanowires respectively under uniaxial tensile loading as well as the natural state of wurtzite (WZ) and the rocksalt (RS) phase which exists under hydrostatic pressure loading. Equilibrium critical stresses for the transformations are obtained. The WZ -> HX transformation is found to be energetically favorable above a critical tensile stress of 10 GPa in [0 1 (1) over tilde 0] nanowires. The BCT-4 phase can be stabilized at tensile stresses above 7 GPa in [0 0 0 1] nanowires. The RS phase is stable at hydrostatic pressures above 8.2 GPa. The identification and characterization of these phase transformations reveal a more extensive polymorphism of ZnO than previously known. A crystalline structure-load triaxiality map is developed to summarize the new understanding. (c) 2007 Elsevier Ltd. All rights reserved.
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本文将计算高超声速稀薄气流过渡领域中气动特性的局部方法,推广应用到连续介质中弹头型高超声速再入飞行器气动力特性的快速估算。由激波风洞中M_∞=9.9时,一个8°钝锥的气动力测量结果,导出这一实验条件下的领域系数,并以此来估算不同锥角、不同钝度比及不同外形弹头型再入飞行器的气动力和力矩系数,其结果与无粘数值解及实验结果作了比较,在攻角2°~14°范围内吻合得很好。局部方法可用于弹头型高超声速再入飞行器气动特性的快速预示。
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本文研究低雷诺数情况下偏心圆柱间定常Streaming流动问题,其中内柱以速度U(x)cosωt在静止不可压粘性流体中作小振幅直线简谐振动,外柱则固定不动。