一类高维非线性方程(组)自相似解的简易求法

对(2 1)维非线性偏微分方程进行相似变换后,根据相似变量不变性原理,提出了一个相似变量的复合变换,从而把(2 1)维偏微分方程最终化成常微分方程.将该方法用于KP方程、ZK方程、高维Burgers方程组,均得到了具有Palinlevé性质的常微分方程.通过进一步的分析求解得到KP方程和ZK方程的自相似渐进解,尤其是得到了高维耦合Burgers方程组的精确解.     

一种基于改进互信息的文本分类方法

用改进的互信息公式进行特征选择,通过三种文本分类方法验证了改进的公式具有较高的准确率、召回率和F1值,从而证明改进的互信息公式的有效性.     

输水线路一干郭河与沙坡河倒虹吸工程地质评价

经过张峰水库输水线路一干工程地质勘测,就输水线路一干郭河与沙坡河倒虹吸工程地质条件进行了分析与评价。     

固定化双菌串联发酵生产1，3-丙二醇

以葡萄糖为底物，利用分别固定化的酵母Candida krusei ICM-Y-05和肺炎杆菌Klebsiella pneumoniae ZJU 5205串联发酵生产1,3-丙二醇。实验结果表明，由C.krusei发酵而得粗甘油只需经简单离心后即可被K.pneumoniae所利用。将C.krusei包埋于NaCS/PDMDAAC生物微胶囊中，并于气升式反应器中发酵，所得发酵液直接流入固定床反应器，同时向固定床反应器补充微量元素，发酵培养经NaCS/PDMDAAC生物微胶囊包埋的K.pneumoniae，产物即为1,3-丙二醇。三批次发酵实验结果表明，1,3-丙二醇/葡萄糖的最终摩尔转化率为0.295。     

Al—Ti—CN细化工业纯铝工艺参数测定

继Al—Ti—C中间合金之后,又开发了Al—Ti—CN中间合金,通过大量细化工业纯铝试验,从中间合金加入量、加热温度、保温时间等工艺试验,找出Al—Ti—CN中间合金细化工业纯铝的最佳工艺.对Al—Ti—CN用于工业生产提供有益参数.     

非等间距GM(1,1)模型背景值构造方法及应用

背景值是影响灰色系统理论建模精度的重要因素之一。为提高灰色模型的预测精度,对非等间距GM(1,1)模型中的背景值构造进行了研究,提出了用x(1)(t)在区间[ki,ki 1]上的中点实际值作为背景值。该背景值计算简洁,适应性强,提高了非等间距GM(1,1)模型精度,拓广了非等间距GM(1,1)模型的适用范围。并应用改进的非等间距GM(1,1)对钛合金疲劳强度随温度变化的关系进行建模,取得了满意的效果,数据拟合精度高达98.8%。建模结果表明了该文提出的方法的有效性。     

溶剂对TS-1催化丙烯环氧化反应的影响

溶剂对钛硅分子筛TS-1催化丙烯环氧化反应具有重要影响,该文对甲醇、异丙醇和仲丁醇3种醇溶剂及丙酮、乙腈和四氢呋喃等有机溶剂中环氧化反应活性进行了研究,实验结果活性顺序为:甲醇>异丙醇>仲丁醇>乙腈>丙酮>四氢呋喃。以催化反应机理为基础,通过电子效应、空间位阻效应、溶剂极性、物理扩散和分配、溶剂氧化副反应、环氧丙烷(PO)醚化副反应、催化剂失活和丙烯溶解度等多种因素分析了溶剂对环氧化反应的影响。电子效应、空间位阻效应和溶剂极性是影响反应的重要因素,研究工作为今后同类反应溶剂的选取提供理论根据和指导,为PO清洁生产工艺的进一步工业化奠定基础。     

抗白粉病的小麦-黑麦1BL/1RS易位系99/2439的cDNA文库构建

用pGEMT-easy质粒载体构建了经白粉茵诱导0.5h、1.0h、12h、24h和48h的小麦-黑麦1BL/1RS易位系99/2439叶片cDNA文库1个.文库宿主茵为E. coliDH10B,诱导文库平均插入片段为1kb左右.     

Water isotope variations in the snow pack and summer precipitation at July 1 Glacier, Qilian Mountains in northwest China

This paper presents the stable isotope data of the snow pack and summer precipitation collected at the July 1 Glacier, Qilian Mountains in northwest China and analyses their relationships with meteorologi- cal factors. On an event scale, there is no temperature effect on the δ 18O values in the summer pre- cipitation, whereas the amount effect is shown to be clear. By tracing the moisture transport history and comparing the precipitation with its isotopic composition, it is shown that this amount effect not only reflects the change in moisture trajectory, which is related to the monsoon activities, but is also associated with the cooling degree of vapor in the cloud, the evaporation of falling raindrops and the isotopic exchange between the falling drops and the atmospheric vapor. As very little precipitation occurs in winter, the snow pack profile mainly represents the precipitation in the other three seasons. There are low precipitation δ 18O ratios in summer and high ratios in spring and autumn. The Meteoric Water Line (MLW) for the summer precipitation is δ D = 7.6 δ 18O 13.3, which is similar to that at Delingha, located in the south rim of the Qilian Mountains. The MWL for the snow pack is δ D = 10.4 δ 18O 41.4, showing a large slope and intercept. The deuterium excess (d) of the snow pack is positively correlated with δ 18O, indicating that both d and δ 18O decrease from spring to summer and increase from early autumn to early spring. This then results in the high slope and intercept of the MWL. Sea- sonal fluctuations of d in the snow pack indicate the change of moisture source and trajectory. During spring and autumn, the moisture originates from continental recycling or rapid evaporation over rela- tively warm water bodies like Black, Caspian and Aral Seas when the dry westerly air masses pass over them, hence very high d values in precipitation are formed. During summer, the monsoon is responsi- ble for the low d values. This indicates that the monsoon can reach the western part of the Qilian Mountains.