地方高师院校数学史教学中存在的问题与对策

当前地方高师院校数学史课程教学中面临着诸多问题,即重视程度不够、专业师资缺乏、与中学数学教学脱节等.因此,应提高地方高师院校数学史课程的地位,加强数学史师资队伍建设,以及数学史与中学数学的整合,编写适宜的数学史教材,改进数学史课程教学模式,这样才能引导学生体会真正的数学思维过程,创造一种探索与研究的数学学习气氛.     

一种增量式属性约简更新算法

根据关系矩阵表示与计算方法,提出一种基于二叉树的增量式属性约简更新算法,主要考虑对象动态增加情况下属性约简的更新问题.该算法通过快速更新二叉树,在动态求解核的基础上,通过对二叉树进行剪枝,有效地进行增量式属性约简的更新,并就该方法的有效性进行了理论证明与示例分析.     

石河子市大气中多溴联苯醚的含量组成及气粒分配

在石河子市自2008年9月至2009年8月间每周采集大气样品,利用GC-MS分析其中的12种PBDEs,结果显示:石河子市大气中PBDEs的年平均浓度为118±83 pg/m3,低于我国其他较发达城市大气中PBDEs的含量.BDE-209是含量最高的单体,年平均含量占总量的65%,其次是BDE-47和BDE-99,年平均含量分别占总量的9%和7%.气-粒分配的研究结果显示,石河子市大气中PBDEs在气态和颗粒态间的分配并未达到平衡,温度是影响PBDEs在气相与颗粒相间分配的重要因素.比较而言,夏季最为接近平衡状态.     

木薯羧酸酯两性淀粉的制备与合成机理

采用交联、氧化和醚化反应制备羧酸型两性淀粉,通过扫描电子显微镜、X射线衍射、胶体滴定等方法对该淀粉进行表征,并研究了该两性淀粉的合成机理．结果表明：该淀粉的阴、阳离子取代度分别达到0．018和0．033,50℃、6％该两性淀粉糊的黏度为258mPa·s;淀粉羧基离子与淀粉氧负离子存在竞争反应．文中还从微观角度阐明了这些改性反应并未影响淀粉的结晶结构．     

Hopfield自适应异步电动机的直接转矩控制

传统的异步电动机直接转矩控制方法中,电动机低速稳态运行时的电磁转矩、定子磁链和定子电流脉动大,严重影响了整个电动机直接转矩控制系统的性能.为此,文中基于Hopfield神经网络理论和异步电动机动态数学模型,提出了基于Hopfield神经网络的改进异步电动机直接转矩控制方法,有效地降低了电磁转矩、定子磁链和定子电流的波动,达到了改善调速系统低速性能的目的.在此基础上,文中还进行了理论建模和仿真计算,仿真结果表明该方法具有良好的鲁棒性.     

FITC标记的GSTP1蛋白在鼠巨噬细胞中的定位

GSTP1(GSTπ)是人体内谷胱甘肽-S-转移酶(GST)的一种重要的活性亚型,属于机体内源性蛋白,不会引起免疫原反应,在维持细胞的正常机能中发挥着重要作用,也是一种具有临床应用价值的抗氧化剂.本实验室在研究中首先发现GSTP1具有明显的抗炎作用,由此我们设想可以通过增加外源性的GSTP1蛋白来提高其在机体内的水平,以此增强机体的抗炎能力.本实验将薄层色谱扫描和SDS-PAGE相结合用于FITC标记蛋白质的检测,使用激光共聚焦显微镜和流式分析相结合的方法研究了外源GSTP1蛋白在RAW264.7巨噬样细胞和鼠腹腔巨噬细胞中的跨膜转位,结果显示外源GSTP1蛋白能够进入上述细胞.该研究为GSTP1蛋白作为直接使用的药物在抗肿瘤、抗炎、抗氧化等领域的应用提供了实验基础.     

Transmission of oxygen isotope signals of precipitation-soil water-drip water and its implications in Liangfeng Cave of Guizhou,China

According to systemically monitoring results of oxygen （hydrogen） isotope compositions of precipitation, soil waters, soil CO2, cave drip waters and their corresponding speleothems in Liangfeng Cave （LFC） in Guizhou Province, Southwest China, it is found that local precipitation is the main source of soil waters and drip waters, and that the amplitudes of those δ18O values of three waters （precipitation, soil water and drip water） decrease in turn in the observed year, which are 0‰ to -10‰, -2‰ to -9‰ and -6‰ to -8‰, respectively. Moreover, the δ18O values for three waters show a roughly simultaneous variation, namely, that those values are lighter in the rainy seasons, weightier in the dry seasons, and that the average δ18O value of drip waters is about 0.3‰ weightier than that of precipitation, which is modified by surface evaporation processes. We also find that oxygen isotope equilibrium is reached or neared in the formation processes of speleothems in LFC system, and that it is feasible to reconstruct paleotemperature and paleoprecipitation by using δ18O values of speleothems. However, it should be noted that surface evaporation would affect the oxygen isotope values in the study area.     

SHRIMP U-Pb zircon age of tuff at the bottom of the Lower Cambrian Niutitang Formation,Zunyi, South China

A SHRIMP U-Pb zircon geochronology study of the tuff at the bottom of the Lower Cambrian Niutitang Formation at Songlin, Zunyi, South China yielded a mean ^206Pb/^238U age of 518±5 Ma. It is significantly younger than the Re-Os ages of 537--542 Ma for the overlying polymetallic Ni-Mo-PGE-rich layer in the basal Niutitang Formation at Songlin, suggesting that the Re-Os ages might represent that of the original magma chamber for the Ni-Mo-PGE-rich layer rather than the formation age of the strata. The intra-basinal stratigraphic correlation also implies that the absolute age of the Chengjiang biota should be younger than 518±5 Ma. Our new result, together with the SHRIMP U-Pb zircon age for the K-bentonite in the Zhongyicun member of the Zhujiaqing Formation at the Meishucun section, Yunnan Province, provides a temporal constraint for the Lower Cambrian of the Yangtze Platform in South China.     

Three-dimensional fluorescence spectral characteristics of dissolved organic carbon in cave drip waters and their responses to environment changes: Four cave systems as an example in Guizhou Province,China

Understanding the responses of fluorescence spectral characteristics of cave drip waters to modern environment and climate changes is key to the reconstructions of environmental and climatic changes using fluorescence spectral characteristics of speleothems. The fluorescence spectral characteristics of dissolved organic carbon （DOC） in four active cave systems were analyzed with a three-dimensional （3D） fluorescence spectral analysis method. We found that the fluorescence types of DOC were mainly of fulvic-like and protein-like fluorescences, both in soil waters and cave drip waters. The intensity of fulvic-like fluorescence was positively correlated with the concentrations of DOC, suggesting that the DOC of cave drip waters was derived from the overlying soil layer of a cave system. Compared with the other cave systems, the variation range of the excitation and emission wavelengths for fulvic-like fluorescence of cave drip waters in Liangfeng cave system that had forest vegetation was smaller and the excitation wavelength was longer, while its fluorescence intensity varied significantly. By contrast, the excitation and emission wavelengths and fluorescence intensity for that in Jiangjun cave system that had a scrub and tussock vegetation showed the most significant variation, while its excitation wavelength was shorter. This implies that the variation of vegetation overlying a cave appears to be a factor affecting the fluorescence spectral characteristics of cave drip waters.     

三重抗干扰晶闸管触发隔离输出电路

设计了一种抗干扰能力极强的晶闸管触发隔离电路.光耦隔离器件的电源依靠脉冲变压器供电的设计,极大的提高了触发电路的抗干扰能力.