In the previous lectures we have described particle motion as it would be seen by an observer standing still at a fixed origin. This type of motion is called absolute motion. In many situations of practical interest, we find ourselves forced to describe the motion of bodies while we are simultaneously moving with respect to a more basic reference. There are many examples were such situations occur. The absolute motion of a passenger inside an aircraft is best

In addition to the equations of linear impulse and momentum considered in the previous lecture, there is a parallel set of equations that relate the angular impulse and momentum. Angular Momentum We consider a particle of mass, m, with velocity v, moving under the influence of a force F. The angular momentum about point O is defined as the \moment\ of the particle's linear

We have seen that the work done by a force F on a particle is given by dw =. dr. If the work done by F, when the particle moves from any position TI to any position T2, can be expressed as, W12=fdr=-(V(r2)-V(1)=V-v2, (1) then we say that the force is conservative. In the above expression, the scalar

In lecture D2 we introduced the position velocity and acceleration vectors and referred them to a fixed cartesian coordinate system. While it is clear that the choice of coordinate system does not affect the final answer, we shall see that, in practical problems, the choice of a specific system may simplify the calculations considerably. In previous lectures, all the vectors at all points in the trajectory were expressed in the

is a vector equation that relates the magnitude and direction of the force vector, to the magnitude and direction of the acceleration vector. In the previous lecture we derived expressions for the acceleration vector expressed in cartesian coordinates. This expressions can now be used in Newton's second law, to produce the equations of motion expressed in cartesian coordinates

In this course we will study Classical Mechanics. Particle motion in Classical Mechanics is governed by Newton's laws and is sometimes referred to as Newtonian Mechanics. These laws are empirical in that they combine observations from nature and some intuitive concepts. Newton's laws of motion are not self evident. For instance, in Aristotelian mechanics before Newton, force was thought to be required in order

简介 一、计算地震作用的方法可以分为静力法、反应谱法(拟静力法)和时程分析法(直接动力法)三大类。 二、我国《抗震规范》要求在设计阶段按照反应谱方法计算地震作用,少数情况才需要采用时程分析法进行补充计算。规范要求进行第二阶段验算的建筑是少数,第二阶段验算采用弹塑性静力分析或弹塑性时程分析方法

13.1胶体及其基本特性 13.2溶胶的制备与净化 13.3溶胶的动力性质 13.4溶胶的光学性质 13.5溶胶的电学性质 13.6溶胶的稳定性和聚沉作用 13.7乳状液(见十二章) 13.8大分子概说 13.9大分子的相对摩尔质量 13.10 Donnan平衡

一、传动装置在机器中的作用 1减速(增速) 2调速 3改变运动形式 4增大转矩 5动力和运动的传递和分配

一、岩溶作用 地下水和地表水对可溶性岩石的破坏和再造作用,包括化学作用过程(溶解和沉淀)和物理作用过程(流水的侵蚀和堆积、重力的塌陷和堆积),但化学作用过程是塑造喀斯特地貌的主要动力