球磨时间对NdFeBDyAlCu合金结构和磁性能的影响

采用机械合金化法制备不同球磨时间的NdFeBDyAlcu合金粉末，研究球磨时间对样品的结构和磁性能影响．随球磨时间的增加，XRD结果显示α—Fe主峰相的强度先减小后增加；SEM结果最示颗粒尺寸明显的变小；VSM结果显示合金粉末球磨5h时的磁性能最好．     

非连续回转面径向跳动误差非接触检测技术研究

结合激光技术与现代电子技术,提出一种能够实现非连续回转面径向跳动误差检测的非接触检测方法。     

钢板厚度对多层波纹转子阻尼器刚度特性的影响

多层波纹钢板转子阻尼器是利用干摩擦作用实现阻尼减振的转子支撑阻尼器,钢板厚度是影响阻尼器特性的主要因素.在Hertz接触分析模型基础上,对多层波纹钢板转子阻尼器的刚度特性进行了研究.给出波纹钢板阻尼器刚度的计算方法和计算实例,并通过静态实验对理论研究进行验证.研究结果表明,波纹钢板阻尼器的刚度在不同圆周方向上变化较小,钢板厚度对阻尼器刚度影响成非线性关系.图12,参8.     

地下商场内火灾烟气运动及控制的大涡模拟

采用湍流大涡模拟方法,对接近于方形的地下商场内的火灾烟气运动及机械排烟进行了数值模拟;研究了机械排烟口的布置和排烟量对火灾烟气排放有效性的影响.结果表明在商场具有防烟分区和挡烟垂壁的条件下,在右侧墙处实施机械排烟比在顶棚处实施机械排烟可取得较好的排烟效果.随着机械排烟量的增大,室内烟气层的高度有明显的上升,从疏散口和自然补风口处流出的烟气速度减小,流入的空气速度增大.     

计算全息三维信息获取的研究

计算全息所用的目标数据一般是通过计算机三维软件模拟获得，这样对于计算全息的应用有一定的限制．提出利用三维激光扫描仪获取计算全息图三维数据的方法，研究了计算全息物光分布和扫描三维数据之间的关系，建立了依据三维物体扫描数据的模拟物光波前分布，并分析了立体数据计算全息消隐问题．     

磨碎玻璃纤维/聚氨酯/环氧灌封材料的形态结构与力学性能

采用真空灌注工艺,制备磨碎玻璃纤维(MG)／聚氨酯(PU)／环氧(EP)灌封材料,并对其力学性能和微观结构进行研究。研究结果表明:随着PU含量的增加,PU／EP共混聚合物的拉伸和冲击强度呈先升后降的变化趋势。当PU含量为15％时,共混聚合物的综合力学性能最佳,拉伸强度为60．57 MPa,冲击强度为23．56 kJ／m2,与EP相比分别提高32．77％和115％。为进一步提高材料的强度,并保持良好韧性,采用添加MG的方法来增强PU／EP。当MG与EP的质量比为1:1时,材料的拉伸强度达到79．72 MPa,与PLJ／EP相比提高31．95％,而冲击强度为17．83 kJ／m2,仍保持较高水平;同时,与相同含量的活性硅微粉相比增强PU／EP材料的拉伸强度和冲击强度分别提高18．91％和11．51％。     

阴极真空电弧沉积MgO薄膜的椭偏光谱研究

采用阴极真空电弧离子沉积技术在硅基片上制备出了MgO薄膜。利用椭圆偏振光谱、原子力显微镜及扫描电子显微镜分别对不同氧流量下制备的MgO薄膜的厚度,光学常数,表面粗糙度及表面形貌进行了分析,并对椭圆偏振光谱的光学粗糙度结果和原子力显微镜的均方根粗糙度结果进行了对比和分析。结果表明,不同氧流量下制备出的MgO薄膜,表面粗糙度及薄膜颗粒随着氧流量的增加而增大。椭偏光谱与AFM得到的表面粗糙度存在线性一致关系,表明椭偏光谱可作为一种很好的无损分析手段。     

用U型管法测定液体的表面张力系数

介绍了用U型管法测定液体表面张力系数的原理和方法。由于采用线阵光电耦合器件(CCD)进行测量,提高了测量精度。     

Molecular dynamics simulation and continuum modelling of granular surface flow in rotating drums

Numerical simulations of granular flows in rotating drums operated at medium to high rates (Fr=0.1― 0.2) have been carried out by using a Molecular Dynamics (MD) algorithm that incorporates inelastic particle interactions, sliding friction and rolling friction. The results indicate that the behavior of granular flow in rotating drums can be classified into two distinct zones: a shear active layer at the bed surface and a quasi-static plug flow region adjacent to the wall. The residence time of a tracer particle in the active layer is approximately a third or a half of that in the plug flow region. The thickness of the active layer at mid-chord is about 0.57―0.61 times that of the plug flow region. It is found that all cases simulated in this work are in the rolling-cascading intermediate regime instead of the pure rolling re-gime. The simulated tangential velocity at the mid-chord is also compared with experimental results reported in the literature and good agreement has been obtained. Based on the MD simulations and experimental results, a continuum approach has also been developed. It is shown that the behavior of granular solids in the plug flow region experiences plastic deformation along the radial direction from the wall with the velocity profiles well described by an exponential function, whereas the active layer velocity follows a simple expression for the Couette shear flow. Discussion has also been made on the granular temperature and concentration profiles.     

Clay minerals in surface sediments of the Pearl River drainage basin and their contribution to the South China Sea

Clay minerals have played a significant role in the study of the East Asian monsoon evolution in the South China Sea by being able to track oceanic current variations and to reveal contemporaneous paleoclimaUc changes prevailing in continental source areas. As one of the most important rivers inputting terrigenous matters to the northern South China Sea, the Pearl River was not previously paid attention to from the viewpoint of clay mineralogy. This paper presents a detailed study on clay minerals in surface sediments collected from the Pearl River drainage basin （including all three main channels, various branches, and the Lingdingyang in the estuary） by using the X-ray diffraction （XRD） method. The results indicate that the clay mineral assemblage consists dominantly of kaolinite （35%-65%）, lesser abundance of chlorite （20%-35%） and illite （12%-42%）, and very scare smectite occurrences （generally 〈5%）. Their respective distribution does not present any obvious difference throughout the Pearl River drainage basin. However, downstream the Pearl River to the northern South China Sea, the clay mineral assemblage varies significantly： kaolinite decreases gradually, smecUte and illite increase gradually. Additionally, illite chemistry index steps down and illite crystallinity steps up. These variations indicate the contribution of major kaolinite, lesser illite and chlorite, and very scarce smecUte to the northern South China Sea from the Pearl River drainage basin. The maximum contribution of clay minerals from the Pearl River is 72% to the northern margin and only 15% to the northern slope of the South China Sea. In both glacials and interglacials, kaolinite indicates that the ability of mechanical erosion occurred in the Pearl River drainage basin.