利用微气囊扰动进行流动控制的数值模拟研究

探讨一种可以用来模拟“三角翼上分布微气囊，从而控制流动获得滚转力矩”的数值方法。为微型飞机的气动设计提供一种工具。研究的内容包括：考虑微气囊的三角翼网格生成、流场NS方程计算、微气囊不同布局对流动的扰动等。     

Emergence of a Habitable Planet

We address the first several hundred million years of Earth’s history. The Moon-forming impact left Earth enveloped in a hot silicate atmosphere that cooled and condensed over ∼1,000 yrs. As it cooled the Earth degassed its volatiles into the atmosphere. It took another ∼2 Myrs for the magma ocean to freeze at the surface. The cooling rate was determined by atmospheric thermal blanketing. Tidal heating by the new Moon was a major energy source to the magma ocean. After the mantle solidified geothermal heat became climatologically insignificant, which allowed the steam atmosphere to condense, and left behind a ∼100 bar, ∼500 K CO₂ atmosphere. Thereafter cooling was governed by how quickly CO₂ was removed from the atmosphere. If subduction were efficient this could have taken as little as 10 million years. In this case the faint young Sun suggests that a lifeless Earth should have been cold and its oceans white with ice. But if carbonate subduction were inefficient the CO₂ would have mostly stayed in the atmosphere, which would have kept the surface near ∼500 K for many tens of millions of years. Hydrous minerals are harder to subduct than carbonates and there is a good chance that the Hadean mantle was dry. Hadean heat flow was locally high enough to ensure that any ice cover would have been thin (<5 m) in places. Moreover hundreds or thousands of asteroid impacts would have been big enough to melt the ice triggering brief impact summers. We suggest that plate tectonics as it works now was inadequate to handle typical Hadean heat flows of 0.2–0.5 W/m². In its place we hypothesize a convecting mantle capped by a ∼100 km deep basaltic mush that was relatively permeable to heat flow. Recycling and distillation of hydrous basalts produced granitic rocks very early, which is consistent with preserved >4 Ga detrital zircons. If carbonates in oceanic crust subducted as quickly as they formed, Earth could have been habitable as early as 10–20 Myrs after the Moon-forming impact.     

飞机主操纵系统疲劳试验载荷谱小操纵位移频次问题研究

针对飞机全机主操纵系统疲劳试验载荷谱中小操纵位移频次影响问题进行了分析和讨论,确定了某机全机主操纵系统小操纵位移频次的级别。同时,在原某机全机主操纵系统疲劳试验载荷谱的基础上再次对其小操纵位移频次进行了计算,去掉了这一级别以下对全机主操纵系统疲劳试验无影响的小操纵位移频次,从而完善了主操纵系统疲劳试验载荷谱。另外,对小操纵位移频次问题研究结果在其全机主操纵系统疲劳试验中的实施效果进行了阐述。     

基于特征模型的全系数自适应控制系统稳定性研究

讨论了基于特征模型的黄金分割加逻辑微分自适应控制律组成闭环系统的稳定性问题。针对参数未知、线性定常或慢时变的二阶不稳定对象,本文给出了在采样周期满足一定条件下,上述闭环系统渐近稳定的充分条件,其中包含对于时变参数变化范围和非线性阻尼系数的约束条件。     

企业经济效益综合评价与分级管理方法

本文针对财政部设计的企业经济效益评价指标体系，用多目标优化方法的思想对其进行优化处理，并且数理统计方法将各指标值折算成分数以符合人们的习惯；同时，用数理分析等方法将所得的评价序列进行分级归类管理。     

大型真空热试验中的摄像观察技术

为完成在大型真空热试验中对飞船表面及舷窗的摄像观察提出了实施方案,分析并解决了普通摄像设备在真空—低温下使用的关键的技术问题,满足了试验要求.     

大型空间模拟器真空测量的自动化

介绍了大型空间模拟器真空测量自动化的实施和特点,以及真空度的描述方法,对真空测量自动化的进一步发展提出了设想。     

滚珠丝杠螺距误差补偿法提高数控机床定位精度的研究

在详细论述、对比了实现数控机床滚珠丝杠螺距误差补偿的硬件、软件方法的原理基础上,对滚珠丝杠螺距误差软件补偿法可有效提高数控机床的定位精度进行了试验验证。     

圆柱齿轮齿廓偏差及螺旋线偏差精度控制研究

在齿轮加工过程中,热处理变形是影响齿轮精度的主要原因之一.通过分析CA457桥从动圆柱齿轮在渗碳淬火热处理中齿廓偏差、螺旋线偏差的变化数据,得出齿廓偏差、螺旋线偏差的变形规律.根据渗碳淬火后基圆半径和螺旋角的变形均呈增大趋势,修改加工刀具的设计齿廓和齿轮的设计螺旋线,降低热处理前产品的工艺精度,保证了热处理后产品的合格率.在创造良好经济效益的同时也为同类产品提供了设计依据.     

区域极点及方差约束下的航天器拦截控制：静态输出反馈情形

本文提出并讨论了具有选通窗约束的航天器拦截控制问题，指出航天器拦截控制的稳暂态性能指标可表现为系统稳态状态方差及闭环区域极点的形式。然后，基于配置控制的思想，本文完整地给出了期望静态反馈控制器的存在条件及其解析表达式，并举例说明所提设计方法的直接性与有效性