控制量变化率受限时的MRAS鲁棒变结构控制

本文研究了控制量变化率受限时的MRAS控制。在文献[1～3]的启发下,本文提出了控制量变化率受限时的MRAS鲁棒变结构控制问题;给出了控制器结构、控制律、自适应律,分析了系统的稳定性和渐近收敛性。     

a-Si:H的光电导衰退与微结构的关系

目前,主要流行的两类微观机制模型——“负有效相关能模型”和“断键模型”——都表明a-Si:H的光诱导变化与其微观结构有关.本文研究了不同制备工艺条件对a-Si:H微结构的影响,和样品的光电导衰退依赖于微结构的关系.最后,从S—W效应的微观机制作了简短讨论.     

数据库技术在滚齿机挂轮选择中的应用

利用数据库技术选择滚齿机上的差动挂轮,只需在计算机上输入待加工齿轮的螺旋角β、模数m_n和滚刀的头数K,即可自动检索到既满足精度要求,又是机床所具备的若干组差动挂轮的齿数。文中介绍了建库的方法及程序。     

压电石英晶体在有机液体—水混合体系中的特性

用晶体振荡器研究了压电石英晶体在一系列有机液体与水混合体系中的振荡性能,确定:在此类体系中的晶体频移与纯有机液体或电解质水溶液中的晶体频移变化规律不一致,系与液体的密度、粘度及介电常数有关,符合下一通式:△F=c_1d~(1/2)+c_2η~(1/2)-c_3ε_0+c_0,但电导率无显著影响.检测池外壁接地可显著降低介电常数的影响并提高频率稳定性.温度对频移的影响与体系的含水量有关.     

精密切削加工中表面粗糙度的在线检测

本文研制了一种光纤表面粗糙度在线测量系统,通过涡流测微仪和步进马达控制系统,可以补偿由于工件尺寸变化、机床导轨几何误差和主轴部件的振动造成的光纤探头和被测工件表面之间的距离变化,使光纤测量仪的输出只反映已加工表面粗糙度的变化。该测量系统能识别出金刚石刀具切削铝合金时,影响加工表面粗糙度的主要因素是积屑瘤和振动。同时还可以用在线监测加工表面粗糙度的方法来监测刀具的磨损。     

黑洞温度、熵变化率和时间尺度的压缩

研究了动态黑洞的温度、熵变化率与事件视界附近“时间尺度压缩因子”之间的关系。给出了计算稳态及动态黑洞温度和墒变的简单公式．     

脉冲磁场对种子生物效应的研究

本文报道多种频率的脉冲磁场作用于蔬菜种子，提高种子活力，进而研究脉冲磁场的生物效应实验表明：脉冲磁场强度在一定的阈值内，作用一定的时间，种子活力将提高，出现正的生物效应（刺激效应），而超过这一阈值范围．种子将出现负的生物效应（抑制效应）．     

Radiolarian record to paleoecological environment change events over the past 1.2 MaBP in the southern South China Sea

This note studies the Radiolarian fossil groups since 1.2 MaBP in ODP leg 184 site 1143, the southern South China Sea (SCS). The result shows that radiolarian abundance experienced a significant variation: before 0.9 MaBP it remained at the extremely low level, but increased with low extent between 0.9–0.65 Ma, which corresponded to the Mid-Pleistocene Transition stage, and it increased rapidly after 0.65 MaBP. During the whole process, the average abundance became higher and higher in each stage, and showed regularly periodic fluctuations. The obvious increase after 0.65 MaBP is inferred to result from the enhanced upwelling in this region, which was induced by the intensified monsoon circulation after the “Mid-Pleistocene Transition”. An outstanding result of the spectral analyses is that a long oscillation of ∼ 0.2 Ma cycle was found in the records of radiolarian abundance and complex diversity, which corresponds well to the result of other paleoceanographic indexes. This probably indicated a special cycle characteristic of paleoecological environment evolution in this area. In addition, all of the radiolarian indexes show an obvious boundary in about 0.47 MaBP, indicating the abrupt variation of the community structure and radiolarian abundance level before and after 0.47 MaBP. So we suppose that there existed a distinct change event of oceanic ecology environment during that period.