红泥聚氯乙烯(RM-PVC)复合材料光稳定性机理

纯PVC在紫外光照射下也易脱去HCl而生成共轭双键,RM-PVC优良耐光老化机理主要是,红泥中的Fe_2O_3,能强烈地吸收紫外光,以及红泥中的钙、硅等其它一些成分也能一定程度地吸收紫外光,从而使基体PVC基本上免遭光能作用而降解、破坏。     

肿瘤病人红细胞膜唾液酸和岩藻糖含量的研究

本文测定健康人66例,胃癌、肺癌、肝癌病人共64例的红细胞膜唾液酸和岩藻糖含量。发现健康人上述两项指标没有性别和年龄的差异。与健康组比较,各癌症组红细胞膜唾液酸显著增多(p<0.001),而岩藻糖显著减少(p<0.001),但含量较分散、与健康者重叠较大。红细胞膜唾液酸与岩藻糖之比、各癌症组都高于健康组(p<0.001);以高于健康组M+2SD 者为阳性,则胃癌组、肺癌组和肝癌组的阳性率分别为79.2％,95.0％和80.0％,对肿瘤理论研究和临床诊断颇有价值。     

《红楼梦》中的女性悲剧

《红楼梦》是一出为天下女儿们悲歌哭泣的大悲剧。这些在封建社会末世中最无力把握自己命运的女子,让人共掬一把悲悼怜悯之泪。她们的爱情婚姻、人生道路、性格命运的悲剧结局充分展示了人间美好事物与美好感情的惨遭毁灭。     

从《红楼梦》对联翻译看意美、形美和音美

文章通过分析《红楼梦》译文不同版本对对联翻译的不同处理方式，指出对联作为中国文化的一种古老的形式，在其翻译时最重要的是注重“意美”，其次是“形美”，再其次是“音美”。     

基于HYCOM模拟的南海西北部环流

为研究北部湾在内的南海西北部海域环流结构的时空特征,本文基于Hybrid Coordinate Ocean Model(HYCOM)模式和气象强迫数据,通过三重嵌套模拟研究南海西北部环流在风力强迫下的结构及其时空分布特征,结果表明:(1)南海西北部流场受季风影响较大,冬季基本为西南向流,夏季基本为东向流,流场结构复杂,外海涡旋众多,Ekman运动特征较为明显;(2)北部湾流场呈现出较强的密度流特征,冬季基本为气旋式环流,夏季同时存在较小尺度的气旋式和反气旋式环流; 7月湾口表层的气旋式环流结构向下直接影响到海底;(3)北部湾的海表面盐度受蒸发降雨影响较大,盐度分布西低东高,这与湾口和琼州海峡入侵的南海高盐海水有关;(4)在热盐作用和季风驱动下,琼州海峡的表、底层流冬季为西向流,夏季为东向流,冬季广东沿海地区的富营养化海水可能通过琼州海峡影响广西近海海域环境质量。     

试论《红楼梦》中宝黛爱情描写的意义

宝黛爱情的描写是贯穿《红搂梦》全书的中心故事，它在突破旧有的郎才女貌、一见钟情、才子佳人、怜才爱色的爱情模式的同时，向我们展现了全新的闪烁看朴素民主思想的爱情观。而这两位叛逆者的爱情由于为统治阶级所不容和家族势力的迫害，以及主人公自身所带有的人文知识分子的特性，导致了他们爱情的悲剧结局。这个爱情悲剧突破了以往夫贵妻荣的大团圆模式，它的悲剧力量将永远震撼人们的心灵。     

The phorbol ester TPA induces metamorphosis in Red Sea coral planulae (Cnidaria: Anthozoa)

Controlled experiments on the metamorphosis of marine invertebrate larvae require artificial inducers. These inducers can be used for studying the involvement of known signal transduction pathways in settlement and metamorphosis. The ability of the tumor-promoting phorbol ester TPA (12-O-tetradecanoylphorbol-13-acetate) to induce metamorphosis in planulae of the Red Sea soft coral speciesHeteroxenia fuscescens, Xenia umbellata, Dendronephthya hemprichii, Litophyton arboreum andParerythropodium fulvum fulvum, and the stony coralStylophora pistillata, was examined by using various concentrations of TPA. The chemical induced metamorphosis in all six species. The effect was unspecific and concentration-related. For all the corals except forX. umbellata the highest mean percentages of metamorphosis were obtained with 8.1×10^–7–10^–9 M TPA. ForX. umbellata, the percentage of metamorphosis was lower, and was obtained within a wider TPA concentration range. The present results, along with previous studies on Hydrozoa and Scyphozoa, demonstrate that TPA is the first common artificial inducer for these classes of Cnidaria. TPA is known to activate the enzyme protein kinase C (PKC) and therefore plays an important role in studying the phosphatidylinositol signal transduction system. Evidence for the involvement of this pathway in triggering metamorphosis has already been reported for Hydrozoa and Scyphozoa. Our results suggest that PKC is also involved in initiating metamorphosis in Anthozoa.     

Al（Ⅲ）—EGTA—PR—CPB显色体系的研究

在pH5.0-5.9的微酸性溶液中.铝(Al).乙二醇二乙醚二氨基四乙酸(EGTA)、邻苯三酚红(PR)和阳离子表面活性剂溴化十六烷基吡啶(CPB)迅速反应,形成一蓝色配位化合物,最大吸收波长于615nm处。该配位化合物的组成为Al(Ⅲ)∶EGTA∶PR∶CPB=1∶1∶3∶12,表观摩尔吸光系数为5.9×10~4dm~3·mol~(-1)·cm~(-1).25cm~3溶液中,0-8μg含量范围内的Al(Ⅲ)遵守比尔定律,17种常见离子和5种阴离子不干扰Al(Ⅲ)的测定。     

海面杂波的仿真

海浪引起的雷达反射信号即海面杂波对于欲探测目标的雷达图像造成干扰,此种干扰无法建立精确的数学模型。在舰船指控系统的陆基演练中,要求模拟海上战术环境,本文提出海情仿真的工程近似仿真方法。     

Deep crustal structure of Baiyun Sag,northern South China Sea revealed from deep seismic reflection profile

This paper discusses deep crustal architecture of the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea based on velocity analysis, time-depth conversion and seismic interpretation of the deep seismic reflection profile DSRP-2002. The profile was acquired and processed to 14 S TWT by the China National Offshore Oil Corp. (CNOOC) in 2002. It extends across the Baiyun Sag of the Pearl River Mouth Basin, from the northern continental shelf of the SCS to the deepwater province. As the first deep seismic reflection profile in the Pearl River Mouth Basin, this profile reveals seismic phases from basement down to upper most mantle. The Moho surface appears in the profile as an undulating layer of varying thickness of 1-3 km. It is not a single reflector interface, but a velocity gradient or interconversion layer. The crust thins stepwisely from the shelf to the continental slope and the abyssal plain (from north to south), and also thins under depocenters. The crustal thickness is only 7 km in the depocenter of the main Baiyun Sag, which corresponds to a Moho upwelling mirroring the basement topography. In the lower slope and the ocean-continental transition zone of the southernmost portion of the profile, three sub-parallel, NW-dipping strong reflectors found at depths around 10--21 km are interpreted as indications of a subducted Mesozoic oceanic crust. Crustal faults exist in the northern and southern boundaries of the Baiyun Sag. The intense and persistent subsidence of the Baiyun Sag might be related to the long-term activity of the crustal faults.