如果水流运动的速度不高,即使紊流状态的水流,用常规的水 力学方法或工程流体力学方法即可对其水力特性进行描述。 但如果水流运动速度足够高,以至于水流紊动强烈和剧烈 掺气,并可能导致空蚀破坏、结构震动、局部区域雾流强 降雨、急流冲击波及滚波等现象的单独或综合出现,此时 的水流称为高速水流

1.包含内容: (1)问题(文字描述) (2)问题应用背景(文字描述+视频片段、图片或动画表现) (3)涉及的知识点(不包含知识点的详细内容) (4)解题方法(建立模型,文字+音频描述) (5)解题过程(详细过程,多种媒体表现)

一、经济:废井田 二、政治和军事:争霸→兼并 三、政治制度:宗法分封→专制官僚 四、社会:世袭→流动 五、学术:贵族→民间 六、结论:

一、FLAC3D软件简介 二、FLAC3D的基本原理 三、FLAC3D的前后处理 四、流-固耦合分析 五、接触单元与应用 六、完全非线性的动力分析 七、自定义本构模型的基本方法 八、结构单元及应用

Lecture D34 Coupled Oscillators Spring-Mass System(Undamped/Unforced)

Lecture D32: Damped Free Vibration Spring-Dashpot-Mass System k Spring Force Fs =-kx, k>0 Dashpot Fd =-cx, c>0 Newton's Second Law (mx =EF) mx +cx+kx (Define)Natural Frequency wn=k/m,and

Solution General solution x(t)= A cos wnt +B sin wnt or, x(t)=Csin(wnt+φ) Initial conditions

When the only force acting on a particle is always directed to- wards a fixed point, the motion is called central force motion. This type of motion is particularly relevant when studying the orbital movement of planets and satellites. The laws which gov- ern this motion were first postulated by Kepler and deduced from observation. In this lecture, we will see that these laws are a con- sequence of Newton's second law. An understanding of central

In this lecture, we will consider how to transfer from one orbit, or trajectory, to another. One of the assumptions that we shall make is that the velocity changes of the spacecraft, due to the propulsive effects, occur instantaneously. Although it obviously takes some time for the spacecraft to accelerate to the velocity of the new orbit, this assumption is reasonable when the burn time of the rocket is much smaller than the period of the orbit. In such cases, the Av required to do the maneuver is simply the difference between the

In this lecture, we will derive expressions for the angular momentum and kinetic energy of a 3D rigid body. We shall see that this introduces the concept of the Inertia Tensor. Angular Momentum We start form the expression of the angular momentum of a system of particles about the center of mass