气刀操作条件对密相栓流气力输送的影响

以高密度聚乙烯为对象,进行了密相栓流气力输送的中试研究,结果表明:输送压力、气刀的操作周期、充气时间与断气时间的比值对输送气速、输送能力、固气比等均有较大的影响.     

增速箱系统动态激励下的响应分析

齿轮啮合动态激励是齿轮系统产生振动和噪声的基本原因，齿轮系统在内部动态激励下的响应分析，对齿轮系统的设计和使用具有重要的意义。针对增速箱系统，采用三维接触有限元法得出啮合齿对的时变刚度曲线，根据齿轮精度级确定的齿轮偏差模拟得出齿面误差曲线，得出了刚度激励和误差激励。应用Ⅰ-DEAS软件建立了增速箱有限元动力分析模型，分析计算出了增速箱的固有频率和箱体、传动轴的动态响应。结果表明，增速箱系统在使用中不会引起共振，且振幅不大，能满足系统的使用要求。     

^4He^＋离子在C和Cu上能量沉积系数的理论计算

利用部分地考虑能量损失的角关联的改进离子输运双群模型，计算了＾４Ｈｅ＾＋离子垂直入射到Ｃ和Ｃｕ上的能量沉积参数，改进了早期的离子输运双群模型。     

徐州红色鲢鱼的初步研究

对红色鲢鱼和白色鲢鱼进行比较研究,结果表明,除体色差别外,两者在体形、咽骨咽齿、消化管相对长度、鳍式和鳞式等方面均无显著差异。可以认为红鲢是白鲢的红色变异体,并对色变的原因做了些推测。     

氯化镁用于染料废水的脱色研究

研究了MgCl_2处理若干种类的活性染料及分散染料的脱色效果,比较了MgCl_2/Ca(OH)_2、Al_2(SO_4)_3.PAC、FeSO_4/Ca(OH)_2的脱色效果。探讨了MgCl_2的脱色机理。实验结果表明,MgCl_2的脱色效果与染料种类、脱色的pH条件,脱色剂的用量有关;MgCl_2的脱色率随pH值升高而增加,对于活性染料废水,当pH=12.5左右时脱色率达最佳;对于分散染料废水,pH=12.0左右时脱色率达最佳;MgCl_2/Ca(OH)_2的脱色效果优于 PAC、Al_2(SO_4)_3、FeSO_4/Ca(OH)_2的脱色效果;MgCl_2的脱色机理为:(1)Mg~(2+)能与含有—OH,—SO_3H、—COOH基因的染料化合物起反应,生成稳定的螯合物,该螯合物在碱性条件下通过混凝作用从水中分离出来;(2)MgCl_2在高pH值下依靠水解生成的Mg(OH)_2胶体沉淀物对染料分子的吸附和卷扫沉降作用达到脱色目的。     

铁路沿线山岬对电波传播特性影响分析

利用波导分析理论及介质表面阻抗的概念,分析了电波在非理想表面的山岬中的传播特性．同时,对频率为９００ ＭＨｚ 的电波在非理想表面的矩形山岬内的传播特性进行了理论计算与分析．计算分析结果表明,环境媒质的相对介电常数对电波传播特性的影响较其它环境参数对电波传播特性的影响要明显得多．非理想表面介质增加了电波传播能量的损耗,缩短了纵向传播距离．在传播的横截面上,水平方向的电场衰减呈现波动分布．     

Perceiving distance accurately by a directional process of integrating ground information

By itself, the absolute distance of an object cannot be accurately judged beyond 2-3 m (refs 1-3). Yet, when it is viewed with reference to a flat terrain, humans accurately judge the absolute distance of the object up to 20 m, an ability that is important for various actions. Here we provide evidence that this is accomplished by integrating local patches of ground information into a global surface reference frame. We first show that restricting an observer's visual field of view to the local ground area around the target leads to distance underestimation, indicating that a relatively wide expanse of the ground surface is required for accurate distance judgement. Second, as proof of surface integration, we show that even with the restricted view, the observer can accurately judge absolute distance by scanning local patches of the ground surface, bit by bit, from near to far, but not in the reverse direction. This finding also reveals that the surface integration process uses the near-ground-surface information as a foundation for surface representation, and extrapolation to the far ground surface around the target for accurate absolute distance computation.     

线型聚能装药射流形成过程的数值模拟

聚能射流形式过程的研究对于正确认识射流侵彻理论具有重要的意义。根据线型聚能药的结构特点,利用DYNA3D显式有限元程序对线型聚能射流的形成过程进行了数值模拟。模型探讨了线型聚能装药爆炸的诸多重要物理特性,如药型罩的压垮、射流形成和拉伸以及体杵体的“体缩”现象。还分析了线型聚能射流形成过程中速度、密度、温度等参数的分布特性,得出了射流有逆向速度梯度和杵体存在“体缩”现象听结论,其结果与现有的理论分成果基本一致。     

区域前兆台网的管理

简要介绍了广东前兆台网“十五“项目的部署情况。根据国家地震前兆台网中心的工作要求,制定了相应的区域前兆台网中心和台站的规章制度,对中心和台站进行规范化管理。该工作仍在不断改进和完善中,目的是要按质、按量、按时地提供前兆数据。     

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.