脉宽调制逆变器中谐波消除法的仿真研究

用计算机仿真技术分析了电压源脉宽调制(PWM)逆变器输出波形中的谐波消除法,给出了去除两个、四个及五个较低次谐波分量的解及波形,并把它们应用到一台典型的感应电动机上。最后进行了样机实验,结果证明是理想的。     

磁化等离子体中的涡旋湍流和反常扩散

研究磁化等离子体中短波漂移阿尔芬波涡旋结构．采用涡旋气体动力学模型，估计出等离子体涡旋湍流谱，并求出反常扩散系数．研究结果表明，涡旋湍流产生的反常扩散系数与扰动场振幅的平方根成正比．     

介质损耗测试方法的研究

以傅立吸叶级数分离基波相位的方法为依据，采用先进的单片计算机技术，提出了一种新的测量方法，理论分析和仿真结果表明，这种数字测量方法检测方便，系统组成简单，智能化程度高，适用于介质损耗角正切较大的简易测量，最后给出了用ＭＣＳ０８０９８单片机组成的数字测量系统的硬件结构图。     

阻尼对弹性管道中孤波运动的影响

本文用微扰理论的研究方法,求出了阻尼较小但不能忽略的情况下,弹性管内流体运动非线性问题中孤立波随时间的演变规律.结果表示阻尼使孤波逐渐变矮,增宽、发生形变且波的传播速度减慢,能量逐渐耗散,最后导致孤波消失。     

澜沧—耿马大震前后尾波Q值的研究

本文根据Aki的尾波散射理论,对澜沧-耿马大震前后近10年的时间,在大震区域及外围的7个地震台近2000多张地震记录图的尾波进行测量,得出Q值随时间变化的结果表明:澜沧、耿马两次大震前有1～3年左右的低Q值异常期;在临近大震前1年左右,Q值处于回升阶段;震后Q值明显增大.并结合澜沧-耿马地区区域地质构造图,试图分析Q值在断层错动中随时间变化的特征;澜沧、耿马7.6、7.2级两次大震是分别孕育的双主震并且可能是澜沧7.6级大震的发生触发了耿马7.2级大震的发生。     

浅水风波波高,波周期分布

通过浅水风波试验，探讨了浅水波高、波周期的分布形式，重点分析了水深因素对波高、波周期分布的影响，给出了浅水波高、波周期分布的表达式，并确定了浅水特征波高间的关系。     

几种疑难心电波形的自动识别方法探讨

本文提出几种疑难心电波形的识别方法,该方法的特点在于将医生读图的经验引入识别过程,设定可能性识别判据,从而显著提高了自动诊断系统对于预激综合症、完全性左、右束支传导阻滞和心肌梗塞等病种的诊断准确性。     

Coupling and propagating of mesoscale sea level variability between the western Pacific and the South China Sea

The coupling and propagating features of mesoscale sea level variability between the western Pacific (WP) and the South China Sea (SCS) were studied based on time series analyses of satellite altimeter measured, along-track sea surface height anomalies (SSHA) along 21°N and the slope of the northern SCS. The analyses show that mesoscale sea level fluctuations in the WP have rather limited coherent effects on the SCS, and no statistically significant propagation of mesoscale variability through the Luzon Strait was observed except in the 45-day band. Evidence suggests that the 45-day fluctuation is very much likely a character of the Kuroshio originating from its low-latitude beginning. It is also sug- gested that the westward propagating Rossby waves will deform when they encounter the dynamical barrier of the Kuroshio. The Kuroshio will then acts on the SCS in its own way. The SCS is a relatively isolated system in the sense of coupling and propagating of oceanic mesoscale waves.     

福建东山湾海浪现场观测的统计特征

为分析福建省南部港湾──东山湾的波浪特征,采用S4型压力式方向波浪仪观测获取现场一个月的风浪过程资料,对其进行了统计分析和频谱分析,给出了波高和周期分布,特征波要素与频谱关系,结果表明:实测波高分布与瑞利分布基本相符;波浪谱的显著部分在狭窄的频率内,对应3、5、6、7级风谱峰密度值(m2s)分别为0.084 3、0.372 8、0.941 8、1.837 7,随着风速的增加,谱能也显著地增加,谱曲线下面的总面积增大,谱的显著部分波及的频率范围也扩大,且谱的显著部分沿低频率的方向推移,对应风浪的波高及周期范围增大.     

Nonlinear interactions between gravity waves and background winds

Using the nonlinear propagating gravity waves (GW) model in the two-dimensional compressible atmosphere and the linear GW theory, the process of GW propagation in different background winds, e.g. the direction of the background wind is opposite to (dead wind) or the same as (tail wind) the direction of the horizontal phase velocity of GW, is studied. The results show that the dead wind prolongs the vertical wavelength and accelerates GW propagation. Therefore, GW propagates up to a higher height becomes instable in a short time and eventually induces an inverse jet flow. Then, the vertical wavelength is becoming short due to the nonlinear interactions between GW and the inverse jet flow. The vertical wavelength and group velocity decrease after GW propagates into the tail wind. The initial instable time is delayed. Although most of GW is trapped in the instable region, some of GW propagates above the instable region. Compared with GW propagation in the tail wind, the nonlinear interactions between GW and the dead wind are also strong. In contrast, the linear GW theory predicts that GW can propagate freely in the dead wind. The vertical wavelength simulated by the nonlinear numerical model is different from that predicted by the linear theory greatly after GW propagates into the dead wind.