阴影法和差分干涉法在分层流密度测量中的应用

本文讨论了用阴影法和差分干涉法测量水-盐两层分层界面上的密度分布。此外,还对一任意密度分布的分层流体作了测量和计算。

Optical near-field simulation of Sb thin film thermal lens and its application in optical recording

Using the finite-difference-time-domain method, the near-field optical distribution and properties of Sb thin film thermal lens are calculated and simulated. The results show as follows. Within the near-field distance to the output plane of thermal lens, the spot size is approximately 100 nm, and its intensity is greatly enhanced, which is higher than that of incident light. The spot shape gradually changes from ellipse to round at the distance of more than 12 nm to the output plane. The above-simulated results are further demonstrated by the static optical recording experiment. (C) 2005 American Institute of Physics.

中国家鸡的起源探讨

测定了6个家鸡品种30个个体的线粒体D-环区539bp的碱基序列,并与GenBank中的红原鸡、灰原鸡、绿原鸡、黑尾原鸡及鹌鹑的相应序列作比较分析,构建了分子系统树。结果表明,原鸡属4个种间差异较大,其中家鸡与泰国及邻近地区红原鸡关系最近,与印尼红原鸡、黑尾原鸡、灰原鸡、绿原鸡及鹌鹑的关系依次变远。提示中国家鸡可能起源于泰国及邻近地区的红原鸡。结果还显示,该地区红原鸡的两个亚种(G.g.gallus和G.g.spadiceus)间的遗传分化程度显著低于家鸡亚种内的分化程度,这两个亚种似乎可以归为同一亚种。

利用可协变衬底制备生长氧化锌薄膜材料的方法

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辐射诱发肿瘤细胞旁效应的免疫学实验研究

目的　研究用自然杀伤 (NK)细胞活性的变化检测肿瘤细胞Yac Ⅰ在6 0 Coγ射线照射后是否存在旁观者效应 (旁效应 ) ,以及其旁效应剂量学和时间效应特征。方法　以健康ICR小鼠脾NK细胞活性为生物终点 ,检测NK细胞对不同条件培养肿瘤细胞Yac Ⅰ的活性 ,用培养基介导法观察旁效应 ,同时 ,培养不同时间观察其时间规律。结果　每个剂量组NK细胞活性的均值与对照细胞NK细胞活性均值差异有显著性 (P <0 0 5 )。照射后分别培养 0和 2 4h ,各剂量组间的NK细胞活性均值差异无显著性。结论　6 0 Coγ射线照射能诱发肿瘤细胞Yac Ⅰ的旁效应。旁效应在低剂量时较为明显。

Geological records of marine environmental changes in the southern Okinawa Trough

Indexes of sediment grain size, sedimentation rates, geochemical composition, heavy minerals, benthic foraminiferal fauna, indicator species of the Kuroshio Current, paleo-SST and carbonate dissolution of core E017 conformably suggest a great marine environmental change occurring at about 10.1-9.2 cal. kaBP in the southern Okinawa Trough, which may correspond to the strengthening of the Kuroshio Warm Current and re-entering the Okinawa Trough through the sea area off northeast Taiwan. The invasion of Kuroshio current has experienced a process of gradual strengthening and then weakening, and its intensity became more fluctuation during the last 5000 years. Compared to the transition of sediment grain size, geochemical composition and heavy minerals, the foraminiferal faunas show a 900-year lag, which may indicate that the invasion of Kuroshio Current and the consequent sea surface and deep-water environmental changes is a gradual process, and fauna has an obvious lag compared to environment altering. The carbonate dissolution of the Okinawa Trough has had an apparent strengthening since 9.2 cal. kaBP, and reached a maximum in the late 3000 years, which may be caused by the deep-water environmental changes due to the invasion of Kuroshio Current.