π0与N- (N-)重整化链传播子的"精确"收敛公式与辐射修正

采用中性介子π0与核子(N-)反核子-N强相互作用Lorentz不变耦合模型,对π0与N- (N-)两类重整化链图传播子函数级数收敛性问题作了全面考察与深入研究,并利用链图传播子函数的精确理论计算结果,通过相关理论分析、推导后获得重整化链图传播子函数级数"精确"收敛公式;在此基础上又对两类重整化链图传播子"辐射修正"问题作了理论计算与分析.     

溶胶-凝胶法制备HEC/SiO2杂化材料的工艺研究

以羟乙基纤维素(HEC)、正硅酸乙酯(TEOS)为原料,采用溶胶-凝胶技术合成了HEC/SiO2有机-无机杂化材料.通过探讨水硅比、HEC含量、溶剂量、干燥控制化学添加剂用量、温度等工艺因素对凝胶化过程,特别是材料干燥体积收缩的影响,得出在本实验条件下合成HEC/SiO2有机-无机杂化材料的优化工艺条件.利用红外吸收光谱、紫外-可见光透射光谱以及扫描电子显微镜等测试手段对合成的HEC/SiO2有机-无机杂化材料进行表征.结果表明,HEC作为有机分散相已经均匀地分散到SiO2基相中,制备的HEC/SiO2有机-无机杂化材料透明,无分相,并可能形成了新的化学键.     

单质点弦振子振动分析

利用拉格朗日方程建立了单质点弦振子非线性振动方程,应用微扰法与线化和校正法对单质点弦振子进行了求解;利用MAPLE9.0计算机绘图,分别作出了它们的周期近似解随振幅的变化曲线以及近似解与数值解的变化曲线.所得结论为利用线化和校正法所求得的近似解与数值解比较,具有简单实用、精度高、相对误差低等优点,在求解非线性振动中具有一定的实用价值.     

昆翅在飞行中的动态形变

通过理论模化途径研究昆翅在飞行中的动态形变机制.设计翅气动力试验平台,验证翅准静态形变影响气动力的"柔性楔形效应"理论解释.探讨昆翅的变刚度特性表明,弦向刚度分布规律符合二项式函数时具有优越性和现实性,进而指出昆姻结构的变刚度特性是产生高升力的基本条件.建立了柔性翅的简化力学模型,通过坐标变换法求解在气动力和惯性力共同...     

有外来扩散源条件下DD402单晶合金中的γ’相筏形化

研究了热等静压(HIP)连接DD402单晶合金与FGH95粉末合金的扩散偶中,DD402单晶合金的γ’相筏形化过程.提出了一种新的γ’相筏形化的机理,分析了γ’相筏形化的驱动力问题,建立了γ’相筏形化过程的物理模型.讨论了筏形γ’片层厚度与原始γ’相的尺寸、体积分数以及γ’相形成元素的扩散流量之间的关系.结果表明,单晶合金的γ’筏形化是由于其形成元素的扩散使γ’定向长大.筏形化的过程包括两个阶段:一是γ’粒子的定向连接阶段;二是筏形γ’片层的平坦化.筏形化γ’的初始片层厚度及筏形化方向主要由γ’原始尺寸及晶体取向决定.     

石墨基体等离子喷涂TiC涂层耐烧蚀性能研究

采用等离子喷涂方法在石墨基体上制备出较为致密的Mo黏结层和TiC耐烧蚀涂层,利用SEM,XRD表征氧乙炔烧蚀试验前后涂层的表面形貌与相结构.结果表明:随着烧蚀距离减小,涂层质量烧蚀率呈现先增加后减小的趋势,最终趋于稳定;随着烧蚀时间增大,致密化区域快速增大,涂层质量烧蚀率略有增加.烧蚀过程中涂层经历了点状熔融、线形连接、网状连接和完全致密4个过程.TiC涂层在高温燃流作用下氧化生成TiO2并熔融,在燃流冲刷和表面张力作用下发生黏性流动,形成TiO2致密层,从而减小了机械剥落,降低了涂层质量烧蚀率.     

辽宁省连山关铀矿床绿泥石形成环境与铀矿化关系

采用电子探针分析技术,对产于辽宁省连山关花岗岩型铀矿床深部的绿泥石进行蚀变特征、化学组成、形成环境研究,并初步探讨该矿床中的绿泥石的形成环境与铀矿化关系。指出绿泥石的形成温度为242.54~286.89℃。与铀矿物共生的绿泥石主要是铁镁绿泥石、蠕绿泥石。含矿溶液沉淀时是一个还原环境,绿泥石不仅活化了花岗岩中的铀,同时还为铀矿化提供了良好的沉淀环境。     

Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.     

直接键连C-X(X=H, C)的核自旋偶合常数的理论研究

利用建立的PM3级别上的最大重迭对称性分子轨道法和自然杂化轨道方法,计算了系列烃类化合物的杂化轨道和电荷分布,拟合出计算C-H及C-C偶合常数的简单关系式,研究了各种烃类分子中不同的C-Ｈ键和Ｃ-Ｃ键偶合常数,理论计算值和实验数据都较为吻合．进一步验证了直接键连1JCX(X=C, H)偶合常数主要取决于偶合作用中的Fermi接触相,为从简单价键理论角度解释和计算1JCH和1JCC提供了一种简便直观的方法．计算结果也表明提出的计算方法是可行的．     

关于基因繁殖的反应扩散系统（0，1）解的定态分歧

作者应用谱理论和规范化LyapunovSchmidt约化方法研究了关于基因繁殖的反应扩散系统（0,1）解的定态分歧,在特征值的代数重数为1的情况下,在一定条件下得到了定态方程从二阶非退化奇点处分歧出的正则分歧解.