齿面润滑压力和油膜厚度的数值分析

采用梯度－牛顿联合法对直齿圆柱齿轮传动进行了弹流润滑数值分析，得出了沿齿廓各啮合点的弹流压力分布及最小油膜厚度，为齿轮传动的摩擦学设计提供了初步的理论依据。     

考虑剪切的变厚度圆板及环形板的弯曲问题

根据E.Reissner平板理论,考虑横向剪切变形的影响,推导出在集中载荷下变厚度圆板和均布载荷下变厚度圆环板的弯曲方程。应用摄动法,求出了四级解析解。计算简便,精确度高。     

推杆式活齿传动中活齿—导槽副润滑状态分析

推导并建立了推杆式活齿减速器传动中活齿—导槽副的润滑方程。首次揭示了活齿承受油膜劝压力的分布规律,以及活齿在运动周期里,油膜压力和最小油膜厚度的变化规律。     

钢-铝固液相复合板界面层厚度建模

采用人工神经网络方法建立了钢－铝固液相复合中助焊剂质量分数,铝液温度,模具温度,压力与界面层厚度间的关系型,并结合最大剪切强度的复合工艺参数得出了钢－铝固液相压力复合的最佳界面界厚度的１０．０μｍ。     

复合路面沥青面层最佳厚度

应用三维有限元分析技术,分析了沥青罩面层厚度对反射裂缝的影响,给出了单双反裂裂缝的分界罩面厚度,提出了最佳脱开宽度和最佳罩面厚度的概念。试验路观测结果不仅验证了力学分析结果,同时显示,双裂缝的宽度基本上等于沥青罩面层的厚度。综合力学分析和试验路观测结果,给出了复合路面沥青罩面层的最佳厚度,为工程应用提供参考。     

Study on crustal, lithospheric and asthenospheric thickness beneath the Qinghai-Tibet Plateau and its adjacent areas

Based on the results of pure dispersions of Rayleigh wave tomography in the Qinghai-Tlbet Plateau and its adjacent areas, tsklng S wave velocities from previous linear inversion as the initial model, using the simulated annealing algorithm, a nonlinear simultaneous inversion has been carried out for S wave velocity and thickness of different layers, including the crust, the lithosphere and the asthenosphere. The results indicate： The crustal thickness shows strong correlation with geology structures sketched by the sutures and major faults. The crust is very thick in the Qinghal-Tibet Plateau, varying from 60 km to 80 kin. The Ilthospherlc thickness in the Qinghai-Tibet Plateau Is thinner （130-160 kin） than Its adjacent areas. And two blocks can be recognized, divided by an NNE strike boundary running between 90°E-92°E inside the plateau. Its asthenosphere is relatively thick, varies from 150 km to 230 kin, and the thickest area is located in the western Qiangtsng. India has a thinner crust （32-38 kin）, a thicker lithosphere of 190 km and a rather thin asthenosphere of only 60 kin. Sichuan and Tarlm basins have the crust thickness less than 50 kin. Their Iithospheres are thicker than the Qinghai-Tibet Plateau, and their asthenospheres are thinner. A discussion has been made on the character and formation mechanism of the typical crust-mantle transition zone in the western Qiangtsng block.     

等厚干涉法测量应用实验研究

利用等厚干涉测量头发丝的直径,可以训练学生的实验操作技巧,加深对实验原理的掌握,丰富了实验内容,避免了实验结果的千篇一律,同时激发了学生的实验兴趣.     

Determination of the optical thickness and effective particle radius of clouds from transmitted solar radiation measurements

A method is presented for determining the optical thickness (τc) and effective particle radius (re) of stratiform cloud layers from transmitted solar radiation measurements. A detailed study shows that the cloud optical thickness and effective particle radius of water clouds can be determined from transmission function measurements at 0.75 and 2.13 μm, provided that the scaled optical thickness τ′0.75>1 and re>5 μm. The wavelengths adopted by our study are similar to the channels of the moderate resolution imaging spectrometer (MODIS). The proposed method is invalid for optically thin clouds since transmission at 2.13 μm is less sensitive to re. The retrieval errors of τ′0.75 and re monotonically decrease with increasing τc. For clouds having τ′0.75≥2, the retrieval errors of τ′0.75 and re are below 10% and 20%, respectively. Transmissions at 0.75 and 1.65 μm can also be used to retrieve τc and re.     

厚度对ZnS薄膜结构和应力的影响

用射频磁控溅射法在单晶Si基片上制备了4种不同厚度的ZnS膜,采用XRD和光学干涉相移法对薄膜的微结构和应力进行研究。结构分析表明,不同厚度的ZnS膜均呈多晶状态,并有明显的(220)晶面择优取向,晶体结构为立方晶型(闪锌矿)结构;随着薄膜厚度的增加,平均晶粒尺寸随之增大;薄膜的晶格常数在不同厚度下均比标准值稍大。应力分析表明,随着膜厚的增加,ZnS膜的应力差减小,在厚度为768 nm时的选区范围内应力差最小,应力分布较均匀。     

钢筋混凝土梁裂缝分布受保护层厚度影响试验研究

基于河口海岸水动力二维数值计算模拟,建立风暴潮与天文潮耦合作用的数值模型,通过多次台风引起的增水和综合潮位的模拟验证,证实该模型可适用于杭州湾海域,能够准确模拟强潮海湾内风暴潮和综合潮波的传播.应用该模型计算了秦山核电厂处可能最大热带气旋引起的增水,结果表明,过程最大增水随遭遇的天文潮位降低而增大,增幅可达85%,综合高潮位则随遭遇的潮位降低而下降;在平均海平面条件下最大增水比高潮位增水约大50%,也大干我国登陆最强的超强台风引起的增水.分析指出在强潮海区,基准洪水位组合中的可能最大风暴潮增水取发生在高潮位时的最大增水较合理.