Synthesis and characterization of white-light-emitting polyfluorenes containing orange phosphorescent moieties in the side chain

Two orange phosphorescent iridium complex monomers, 9-hexyl-9-(iridium (III)bis(2-(4'-fluorophenyl)-4-phenylquinoline-N, C-2')(tetradecanedionate-11,13))-2,7-dibromofluorene (Br-PIr) and 9-hexyl-9-(iridium(III)bis(2-(4'-fluorophenyl)-4-methylquinoline-N, C-2')(tetradecanedionate-11,13))-2,7-dibromofluorene (Br-MIr), were successfully synthesized. The Suzuki polycondensation of 2,7-bis(trimethylene boronate)-9,9-dioctylfluorene with 2,7-dibromo-9,9-dioetylfluorene and Br-Plr or Br-MIr afforded two series of copolymers, PIrPFs and MIrPFs, in good yields, in which the concentrations of the phosphorescent moieties were kept small (0.5-3 mol % feed ratio) to realize incomplete energy transfer. The photoluminescence (PL) of the copolymers showed blue- and orange-emission peaks. A white-light-emitting diode with a configuration of indium tin oxide/poly(3,4-ethylenedioxythiophene):poly(styrenesulfonate)/PIr05PF (0.5 mol % feed ratio of Br-PIr)/Ca/Al exhibited a luminous efficiency of 4.49 cd/A and a power efficiency of 2.35 lm/W at 6.0 V with Commission Internationale de L'Eclairage (CIE) coordinates of (0.46, 0.33). The CIE coordinates were improved to (0.34, 0.33) when copolymer MIr10PF (1.0 mol % feed ratio of Br-MIr) was employed as the white-emissive layer. The strong orange emission in the electroluminescence spectra in comparison with PL for these kinds of polymers was attributed to the additional contribution of charge trapping in the phosphorescent dopants.

Cure processing modeling and cure cycle simulation of epoxy-terminated poly(phenylene ether ketone) .4. Cure cycle simulation

Epoxy-terminated poly(phenylene ether ketone) (E-PEK) developed in this Institute is a candidate matrix resin for polymer composites as structural materials. Cure cycles for this reaction system were simulated according to the previously established processing model. It is found that for the E-PEK system, the curing process is best completed by a stepwise cure cycle comprising two isothermal processes at different temperatures, T-1 and T-2. The cure cycles over a wide range of processing parameters simulated, based on the established processing model, indicate that the processing window is width-adjustable. Analysis of the mechanical properties of the composite sheets showed that the simulated cure cycles are acceptable and reliable. (C) 1997 John Wiley & Sons, Inc.

棕色田鼠种群繁殖特征及密度制约调节

1992年～1994年在河南灵宝市郊黄土高源农作区春夏秋逐月捕获并解剖棕色田鼠1757只（雌性961只，雄性796只），总性比为1．2073。全年都有繁殖鼠出现，但怀孕率、胎仔数、性比、繁殖指数有明显的季节变化，年间也有一定的差异。不同年龄组的性比、怀孕率、胎仔数、繁殖指数、睾丸下降率不同。种群密度对繁殖特征有明显的调节作用。高密度年份的棕色田鼠的性比、怀孕率和繁殖指数低于低密度年份。高密度区种群的繁殖强度受到抑制，雌鼠怀孕率、睾丸下降率低于低密度种群。

关于中国西南石漠化的若干问题

石漠化是西南岩溶山地脆弱生态系统发生的土地退化。根据已有的经验和研究成果, 深人探讨了中国西南岩溶山地喀斯特石漠化的科学内涵、成因、发展过程、评价指标及防治机理等。土壤和植被是岩溶环境中最为敏感的自然环境要素, 可能是石漠化过程的主要自然成因, 而以土地利用为表现形式的强烈人类活动为驱动力石漠化的发生发展过程即人为过程、生物学过程加速的地学过程。石漠与石漠化, 二者属于完全不同的范畴, 不同空间尺度的石漠化评价应有不同的评价指标、标准和石漠化生态基准的多样性, 以便为石漠化的演化研究及生态重建起一定的参考作用。鉴于石漠化现象在我国现实中存在的客观性、在理论概念上的模糊性及在生态治理中的急迫性, 有必要加强石漠化在不同时空尺度下的驱动机制研究, 特别是人类驱动力的研究, 加强原生岩溶生态系统和受损岩溶生态系统运行规律的研究。

湘南瑶岗仙钨矿床成矿流体地球化学

瑶岗仙钨矿床位于湘东南后加里东隆起和湘、桂、粤北海西—印支坳陷带的交接部位，是南岭地区最典型的石英脉型钨矿床之一。为了深入研究瑶岗仙钨矿的成矿机制，本文在野外地质工作基础上，选取有代表性的样品，进行了氦、氩同位素以及碳、氧、硫稳定同位素研究，探讨了矿床成矿流体的来源，成岩成矿的关系，并初步讨论了矿床的成因模式。论文主要获得以下认识： （1）对瑶岗仙矿区不同硫化物中流体包裹体的氦、氩同位素系统测定表明，该矿床毒砂流体包裹体中3He/4He比值为0.58~2.60 Ra；黄铁矿和黄铜矿流体包裹体中3He/4He比值分别为0.41~1.26 Ra 和0.37~0.43 Ra，黑钨矿流体包裹体中氦同位素组成相对变化较大，其3He/4He比值为0.05~0.49 Ra，这些He同位素组成均明显高于地壳相应值；毒砂流体包裹体中的40Ar/36Ar变化范围在309.94~454.39；黄铁矿流体包裹体中的40Ar/36Ar变化范围在409.12~1822.31；黄铜矿和黑钨矿流体包裹体中的40Ar/36Ar变化范围分别为673~886和325~903，明显高于饱和大气雨水的40Ar/36Ar值。上述氦、氩同位素组成揭示瑶岗仙钨矿床中的成矿流体具有壳、幔两端元混合的特点。结合区域地质构造演化和成矿年代学的研究成果，本文认为瑶岗仙钨矿床的成矿流体是瑶岗仙花岗岩浆分异出的含有地幔He的岩浆流体与大气成因地下水二端元混合的产物。 （2）层解石和方解石的C、O同位素显示，该矿方解石的13CPDB和18OSMOW的变化范围为-2.2‰~ -7.0‰（均值为-4.8‰）和5.6‰~14.4‰（均值为11.3‰）；层解石的13CPDB和18OSMOW的变化范围为-5.5‰~ -6.3‰（均值为-5.8‰）和12.7‰~14.3‰（均值为13.8‰）；该矿方解石、层解石的C、O同位素组成与赣南西华山钨矿床非常类似。这些C、O同位素指示，该矿的成矿流体主要来自岩浆水，后期有少量大气降水的参与。 （3）对瑶岗仙矿区不同硫化物的硫同位素研究表明，该矿硫化物δ34S值的变化范围很窄，为-2.0‰~1.5‰之间，且具有明显的塔式分布。这些特征暗示，该矿的硫来源单一，主要来自岩浆。 （4）瑶岗仙花岗岩过去被视为典型的S型花岗岩，但本文研究发现该花岗岩普遍含有地幔He。结合区域构造背景的最新研究成果，本文认为，原来被认为“由地壳物质重熔形成的”瑶岗仙S型花岗岩体，实际上也是一种岩石圈伸展背景条件下壳幔相互作用的产物，地幔物质和能量的参与在该花岗岩的形成过程中发挥了重要作用。 （5）瑶岗仙钨矿床与矿区复式花岗岩体具有密切时空关系，而且该矿的主要成矿流体和成矿物质均来自矿区花岗岩，故两者亦应具成因联系。

Advanced interatrial block: A well-defined electrocardiographic pattern with clinical arrhythmological implications

3.050 JCR (2013) Q2, 44/125 Cardiac & cardiovascular systems

O discurso de O Portuguez e a Corte portuguesa no Brasil

Relatório apresentado à Universidade Fernando Pessoa como parte dos requisitos para cumprimento do programa de pós-doutoramento em Ciências da Comunicação, vertente Jornalismo

Casa colombiana 2001.

16 hojas.