教师专业化背景下的一体化教师教育模式初探

在界定教师专业化的内涵与标准的基础上，分析了教师专业化的必然趋势和要求，最后结合别国的经验，探讨了作为教师专业化实现途径之一的一体化教师教育模式的建构策略。     

常温常压等离子体氟碳纳米颗粒膜表征

通过介质阻挡放电在大气压条件下进行等离子体聚合,获得了氟碳聚合物薄膜。并用红外光谱、X射线光电子能谱、扫描电镜以及静滴接触角界面张力测量仪等测试方法研究了膜的化学结构、表面物理形态与放电条件之间的关系。实验结果表明,聚合物膜是一种由纳米颗粒堆积而成的多孔膜。通过选择控制放电的功率、时间以及单体的流量,可以得到含FC或FCO官能团的聚合物膜。经该聚合物涂层后的棉织物具有超级拒水拒油性能,比表面能可降为2.429×10-2J/m2,而且透湿指数为0.9997,涂层后织物透湿性几乎没有变化。     

Cr 3+改性膨润土用于处理特定有机废水的实验研究

制备了Cr 3 改性膨润土并用于吸附苯酚、对苯二酚和苯胺.研究了吸附过程的适宜条件、投样量、样品稳定性及再生情况.以COD为综合指标检测了处理垃圾渗滤液的实验效果,并与常见的吸附剂进行了简单的经济技术对比.对可能的机理进行了探讨.     

基体的梯度结构对涂层硬质合金性能的影响

通过控制烧结气氛制备了均质和梯度结构的硬质合金基体，并用化学气相沉积制成涂层硬质合金及切削刀片。采用光学显微镜和扫描电镜观察，通过显微硬度抗弯测试和切削试验对均质基体和梯度基体的涂层硬质合金的组织特征与性能进行对比研究。研究结果表明，梯度结构的硬质合金基体可以提高涂层硬质合金的抗弯强度；相对于均质基体的涂层硬质合金刀片，梯度基体的涂层硬质合金刀片在保持耐磨性能的同时能显著提高抗冲击性能。基体涂层合金的组织结构及断口特征显示，梯度基体表层韧性区可阻碍裂纹的扩展。     

电弧喷涂铝涂层的抗高温空气氧化性能

采用电弧喷涂技术在Q235钢基体上制备铝涂层。用Q235钢、铝涂层和封孔铝涂层3种试样进行400℃和500℃涂层氧化和失效试验，并绘制了氧化动力学曲线。结果表明，在500℃以下，在Q235钢基体上电弧喷涂铝涂层和封孔铝涂层可以提高试样的抗氧化能力，但只是在短期内有效。在相同的温度下，封孔铝涂层试样氧化速度最低，铝涂层试样和Q235钢试样的氧化速度大约分别是它的2倍和3倍。氧化过程中，氧化气体渗透到涂层内部，Al2O3膜不断生成、破碎和剥落，并在涂层颗粒机械结合部位堆积，产生的张应力造成涂层的内聚强度降低，塑性和密封性能变差，防腐作用减弱，这是涂层氧化和失效的主要原因。     

新型中和缓蚀剂对常减压塔顶H2S—HCI—H2O腐蚀作用的影响

研究了新型中和缓蚀剂SF-121B和BZH-1在常减压蒸馏塔顶H2S-HCl-H2O腐蚀系统中的缓蚀效果，结果表明：随着H2S浓度增加，腐蚀速率增加；温度升高，溶液pH值下降，腐蚀增加。中和缓蚀剂SF-121B和BZH-1的缓蚀效果优于目前工业常用的7019。SF-121B与氨水复配在保持较好缓蚀效果的同时，可减少操作成本。     

金属基体表面热熔敷玻璃涂层耐蚀性研究

利用斑点试验、点蚀试验、电化学测试及扫描电镜等方法 ,研究了熔敷温度、保温时间和稀土添加量等工艺参数对热熔敷法制备的玻璃涂层耐蚀性的影响 ,探讨了添加稀土提高玻璃涂层耐蚀性的机理。试验结果表明 ,采用热熔敷法制备的玻璃涂层有较好的耐蚀性。随着熔敷温度的提高和保温时间的延长 ,形成了一定量的晶相后会降低涂层的耐蚀性。试验结果表明 ,熔敷温度为 70 0℃、保温 5min后能够得到耐蚀性良好的玻璃涂层。添加稀土提高了釉料的软化温度和熔融釉料的粘度 ,阻止了结晶形核和晶核长大 ,减少了晶相 ,同时提高了涂层的电极电位 ,使涂层耐蚀性显著提高。当稀土含量为 2 %时 ,涂层的耐蚀性较好。     

Recent development of organic electron transport materials

This article reviews the recent development of organic electron transport materials applied in the fields of organic photoconductors, light-emitting diodes, field-effect transistors and solar cells. Several technologies for charge carrier mobility measurement are summarized and compared, and a series of basic principles for designing high-performance organic electron transport materials are suggested as well.     

Initial organic geochemical investigation on Late Neoproterozoic-Early Cambrian sediments in the Yangtze region, China

Totally 19 samples of typical Upper Proterozoic-Lower Cambrian sedimentary rocks were collected and analyzed for an organic geochemical investigation. Almost all these rocks have high TOCs, super-maturities and similar biomarker distribution. As an exception, however, the Sinian Nantuo Tillite shows much lower TOCs and little phytane and pristane in comparison with those in other strata, which implies a very faint photosynthetic process, and a restricted euphotic zone and quite limited sunlight within the sedimentary water column during the Sinian glaciation age in the western Yangtze region providing an evidence for palaeo-oceanic environment of the Neoproterozoic Snowball Earth age.     

Isotopic evolution of the terminal Neoproterozoic and early Cambrian carbon cycle on the northern Yangtze Platform, South China

Profound geotectonic, climatic and biological changes occur during the terminal Neoproterozoic and its transition into the early Cambrian. These are reflected in temporal variations of the chemical and isotopic composition of seawater. We are studying a sequence of sedimentary rocks at the Shatan section, northern Yangtze Platform, Sichuan Province of China. This succession comprises, in ascending stratigraphic order, predominantly calcareous sediments of the Sinian upper Dengying Formation and black shales of the lower Cambrian Guojiaba Formation (time equivalent of Niutitang Fm.). Paleoenvironmental setting represents shallow-water shelf deposits. The objective of our study is to provide temporal records for the isotopic compositions of organic and carbonate carbon throughout this time interval. Organic carbon isotope values display a range between -35.8‰ and -30.1‰ with clear stratigraphic variations. Carbonate carbon isotope data vary between -3.5‰ and +0.5‰. These secular variations are interpreted to reflect perturbations of the global carbon cycle, specifically changes in the fractional burial of organic carbon. However, local conditions have further affected the isotopic signals.