8.1 概述 8.2 决策的特点和类型 8.3 决策的信息加工模型 8.4 什么是“好”的决策 8.5 决策中的诊断和情景意识 8.6 行动的选择 8.7 改进人的决策

We will start by studying the motion of a particle. We think of particle as a body which has mass, but has negligible dimensions. Treating bodies as particles is, of course, an idealization which involves an approximation. This approximation may be perfectly acceptable in some situations and not adequate in some other cases. For instance, if we want to study the motion of planets it is common to consider each planet as a particle

6.1 概述 6.2 印刷字体的知觉 6.3 整合和自上而下加工的应用 6.4 物体的识别 6.5 理解 6.6 多媒体说明文 6.7 产品警告标记 6.8 语言知觉

In this lecture we will look at some other common systems of coordinates. We will present polar coordinates in two dimensions and cylindrical and spherical coordinates in three dimensions. We shall see that these systems are particularly useful for certain classes of problems Like in the case of intrinsic coordinates presented in the previous lecture, the reference frame changes from point to point. However, for the coordinate systems to be presented below, the reference frame depends only on the position of the particle. This is in contrast with the intrinsic coordinates, where the reference frame is a function of the position, as well as the path

In this lecture we will look at some applications of Newton's second law, expressed in the different coordinate systems that were introduced in lectures D3-D5. Recall that Newton's second law F=ma, (1) is a vector equation which is valid for inertial observers. In general, we will be interested in determining the motion of a particle given

§6～1 风化作用 §6～2 河流的侵蚀、搬运与沉积作用 §6～3 岩溶（喀斯特）作用 §6～4 斜坡与边坡地质作用 §6～5 海岸带地质作用

In this lecture we will consider the equations that result from integrating Newtons second law, F=ma, in time. This will lead to the principle of linear impulse and momentum. This principle is very useful when solving problems in which we are interested in determining the global effect of a force acting on a particle over a time interval Linear momentum We consider the curvilinear motion of a particle of mass, m, under the influence of a force F. Assuming that

• 4.1 概述 • 4.2 物料衡算的基本理论 • 4.3 物料衡算举例 • 4.3.1 物理过程的物料衡算 • 4.3.2 化学过程的物料衡算 • 1.反应转化率、选择性及收率 • (1)限制反应物 • (2)过量反应物 • (3)过量百分数 • (4)转化率x • (5)选择性

So far we have used Newton's second law= ma to establish the instantaneous relation between the sum of the forces acting on a particle and the acceleration of that particle. Once the acceleration is known,the velocity (or position) is obtained by integrating the expression of the acceleration (or velocity). There are two situations in which the cumulative effects of unbalanced forces acting on a particle are of interest to us. These involve:

§3～1 地质年代 一．相对年代与绝对年代 二．地质年代表 三．地方性岩石地层单位 四．我国地史概况 §3～2第四纪地质概述 一．第四纪地质概述 二．第四纪沉积物