正常人脐静脉内皮细胞的原子力显微镜观察

目的:利用原子力显微镜(AFM)在单细胞水平分析正常人脐静脉内皮细胞的形貌特征和机械性质,为了解内皮细胞结构与功能的关系奠定基础.方法:新鲜人脐静脉内灌注质量分数为0.25%胰蛋白酶消化,获得人脐静脉内皮细胞(HUVECs),M199培养基进行培养,免疫细胞化学检测内皮细胞第Ⅷ因子的表达.将体外培养的HUVECs用质量...     

温度不均匀性对吸收池中气体吸收的影响

为研究温度不均匀性对低温控制吸收池中气体吸收的影响,建立了桌面不锈钢体低温控制吸收池体积分数标定装置,并使用自行编制的大气辐射传输软件ARH iRS进行模拟计算.实验结果和数值模拟计算结果表明,长1m,充满1.01×105Pa二氧化碳(CO2)气体的吸收池,由于吸收池内外温差导致内部温度不均匀分布(吸收池中轴向温度呈中心对称分布,且吸收池中间的气体温度较低,两端靠近窗片处的温度比中心温度高276~278 K),温度不均匀分布对吸收池气体吸收透射比的影响不大于0.05%,对反演体积分数的影响不超过0.80%,能够满足体积分数定标的需要.     

基于PID神经网络自动换挡过程油门调速

提出了一种在AMT换挡过程中运用PID神经网络进行油门调速的方法.通过台架实验,建立了东风康明斯EQB235-20柴油发动机的油门实验模型,同时在Matlab平台上对PID神经网络进行训练,使其输出逼近理想油门实验模型.将训练后的PID神经网络移植入ECU,进行发动机调速实验.实验表明,PID神经网络有响应速度快、鲁棒性好、收敛特性好的特点,提高了车辆的自适应能力.     

质酸金的合成及性质研究

为获得透明质酸新的功能,对其进行结构修饰.以氯金酸、透明质酸钠为原料合成质酸金.通过元素分析、冷场扫描电子显微镜、傅里叶变换红外光谱和核磁共振分析对其结构进行了表征,对肺癌细胞A549、肝癌细胞BEL7402增殖影响进行了研究.结果表明,在高剂量下对肝癌细胞BEL7402的增殖有明显的抑制活性,对肺癌细胞A549的增殖有边缘抑制活性.     

几种不同周期性单元的PBG天线的设计与仿真

提出了几种不同周期性单元的PBG结构的贴片天线.采用有限元法对其进行仿真分析,通过相互对比,研究出这几种不同PBG结构对贴片天线性能的影响.结果表明,在贴片天线中增加PBG结构能减少天线的回波损耗,提高天线的增益和辐射效率.并得出周期性单元的形状和数目对其特性的影响.     

环境污染物PFOS可致人脑微血管内皮细胞骨架蛋白改变

目的:探讨全氟辛烷磺酰基化合物(PFOS)引起的人脑微血管内皮细胞(HBMEC)骨架蛋白(F-actin)排列变化.方法:培养正常的人脑毛细血管内皮细胞,不同浓度PFOS作用30分钟,利用免疫荧光染色的方法检测细胞骨架蛋白F-actin的变化.结果:PFOS可使细胞骨架蛋白F-actin发生重排,这与PFOS的浓度有关.     

围绝经期综合征舌苔脱落细胞凋亡调控蛋白与肝郁病理的相关性

通过研究围绝经期综合征舌苔脱落细胞调控蛋白与肝郁病理的相关性,为临床诊疗提供实验依据.本研究采用随机数字表法,选取50例健康妇女作为对照组,150例围绝经期综合征患者作为观察组,证素辨证计算肝郁积分,巴氏染色检测舌苔脱落细胞的成熟指数(MI)和成熟价值(MV),流式细胞仪检测舌苔脱落细胞凋亡指数,免疫组化检测舌苔脱落细胞调控蛋白.结果显示,围绝经期综合征肝郁积分明显高于健康妇女:肝郁病理改变,与舌苔脱落细胞MI的中层细胞数量呈正相关,与舌苔脱落细胞MI的表层细胞数量及MV呈负相关:肝郁病理改变,与舌苔脱落细胞凋亡指数、Fas、Bax的阳性率呈正相关,与舌苔脱落细胞中Bcl-2的阳性率呈负相关.提示肝郁病理是围绝经期综合征的核心病机之一,肝郁病理与舌苔脱落细胞的成熟度、凋亡指数及凋亡调控蛋白相关.     

Preparation of monoclonal antibody based indirect competitive ELISA for detecting 19-nortestosterone residue

19-Nortestosterone (NT) has been illegally used in horse racing to boost physical performance, and in animal husbandry to accelerate weight gain. To monitor the abuse of NT, our goal was to develop a commercial enzyme linked immunosorbent assay (ELISA) kit. For this purpose, hybridomas were prepared by fusing NS0 mouse myeloma cells with splenocytes isolated from immunized BALB/c mouse. Noncompetitive and competitive indirect ELISA were used to screen positive cell clones. To optimize the indirect competiti...     

Coral reef ecosystems in the South China Sea as a source of atmospheric CO<Subscript>2</Subscript> in summer

Field measurements of air-sea CO2 exchange in three coral reef areas of the South China Sea (i.e. the Yongshu Reef atoll of the Nansha Islands, southern South China Sea (SCS); Yongxing Island of Xisha Islands, north-central SCS; and Luhuitou Fringing Reef in Sanya of Hainan Island, northern SCS) during the summers of 2008 and 2009 revealed that both air and surface seawater partial pressures of CO2 (pCO2) showed regular diurnal cycles. Minimum values occurred in the evening and maximum values in the morning. Air pCO2 in each of the three study areas showed small diurnal variations, while large diurnal variations were ob-served in seawater pCO2. The diurnal variation amplitude of seawater pCO2 was ~70 μmol mol–1 at the Yongshu Reef lagoon, 420–619 μmol mol–1 on the Yongxing Island reef flat, and 264–579 μmol mol–1 on the reef flat of the Luhuitou Fringing Reef, and 324–492 μmol mol–1 in an adjacent area just outside of this fringing reef. With respect to spatial relations, there were large differences in air-sea CO2 flux across the South China Sea (e.g. ~0.4 mmol CO2 m–2 d–1 at Yongshu Reef, ~4.7 mmol CO2 m–2 d–1 at Yongxing Island, and ~9.8 mmol CO2 m–2 d–1 at Luhuitou Fringing Reef). However, these positive values suggest that coral reef ecosystems of the SCS may be a net source of CO2 to the atmosphere. Additional analyses indicated that diurnal variations of surface seawater pCO2 in the shallow water reef flat are controlled mainly by biological metabolic processes, while those of deeper water lagoons and outer reef areas are regulated by both biological metabolism and hydrodynamic factors. Unlike the open ocean, inorganic metabolism plays a significant role in influencing seawater pCO2 variations in coral reef ecosystems.     

Evolution of the East Asian monsoon and its response to uplift of the Tibetan Plateau since 1.8 Ma recorded by major elements in sediments of the South China Sea

Evolution of the East Asian monsoon and its response to uplift of the Tibetan Plateau has been investigated in the study of global change. Core sediment samples drilled in the South China Sea during ODP Leg184 are the best materials for studying long-term variability of the East Asian monsoon. R-mode factor analysis of major elements in the fine grain-sized carbonate-free sediments (<4 μm) of the upper 185 mcd splice of ODP Site 1146 drilled during Leg184 in the South China Sea shows that Ti, TFe2O3, MgO, K2O, P, CaO, and Al2O3 are representative of a terrestrial factor. The variation in the terrestrial factor score is subject to chemical erosion in the source region and thus indicates the evolution of the East Asian summer monsoon. The terrestrial factor score has three stepwise decreases at ~1.3 Ma, ~0.9 Ma, and ~0.6 Ma, indicating the phased weakening of the East Asian summer monsoon is related to wholly stepwise, quick uplifts of the Tibetan Plateau since 1.8 Ma. The periodic fluctuation of the terrestrial factor score since ~0.6 Ma indicates that the glacial-interglacial cycles have been the main force driving the evolution of the East Asian monsoon. As in the case of Chinese loess, the long-term evolution of the East Asian monsoon recorded in sediments of the South China Sea reflects a coupled effect of the glacial-interglacial cycle and uplift of the Tibetan Plateau.