描述有源矩阵液晶显示系统液晶显示器件电光特性的简化模型

本文提出了一个描述扭曲向列型（TN）液晶显示器件电光特性的简化模型。根据模型，可以很容易地计算出各类参数液晶显示器件的电光特性。理论计算与实验数据符合的很好。因此该模型可用于有源矩阵（Active Matix)液晶显示系统的模拟程序。     

STUDY ON THE PERMEABILITY OF MICROCAPSULES

In the present study,microcapsules with disperse dye solutions and a direct dye solution ascore materials were prepared by the complex coaeervation method and the interfacialpolycondensation method respectively.Experiments and theoretical analysis showed that there wasan exponential relationship between the diffusion time and the release rate of the core material intothe surrounding medium.A concise equation to calculate the permeability constant was derivedand verified by the experimental results.By means of duplex focus on the inner and outer diametersof a microcapsule,the average wall thickness of microcapsules was measured.     

离心泵旋转叶轮内部流场变分有限元解及粘性修正

本文探索研究离心泵旋转叶轮内部流场的数值模拟,为在水泵内部流场计算设计领域引进和推广有限元法提供一种有效手段,同时为水泵叶轮反问题计算设计、优化设计及CAD打下一个良好基础.计算结果表明:本文所建立的计算方法是可行的.     

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。     

Thermodynamic evolution of lithosphere of the North China craton： Records from lower crust and upper mantle xenoliths from Hannuoba

Lithospheric thinning in East China attracts much attention of geologists. In many cases where a lithospheric thinning is inferred, the trigger for instability is a preced-ing episode of crustal thickening by the continental colli-sion[1]. Lithospheric processes (e.g. lithospheric thinning) could be recorded by the thermal history of the lower crustal and upper mantle xenoliths. Xu et al.[2] suggested that the cooling (from >1200 to 850℃) recorded by spinel harzburgite from Northeast China …     

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.