Chapter 4 – Motion in 3 Dimensions F ma or Fx mx Fy my Fz mz if the Fx x is the function of x only and Fy y is the function of y only and Fz z is the function of z only, then there is nothing new, just 3 equations, one for each direction. However, if variables other that x and its derivative appear in Fx and likewise for Fy and Fz then there is a significant complication. For this case, we have coupled D.E. that may ever be non-linear. The work energy principle is still true: F dr T path that is the change in Kinetic energy of a particle is equal to the line integral of the resulting force acting on the particle along the path the particle moves. If the resulting forces are all conservative, the line integral will be independent of path and depend only on the end points. Page 2 of 6 3/8/2016 The test tosee if a force is conservative is that xF 0 or i x Fx j y Fy k 0 z Fz The derivation of this idea that is the integrations of a vector along a path being independent of path is a special case of Stokes Theorem which states: F dr area F n da Stokes Theorem is true whether F is conservative or not. But if the integral on the LHS is to be zero, one must have F 0. This is a very powerful theorem. It states that a line integral around a perimeter is the same as a surface integral over the area inside the perimeter. Page 3 of 6 3/8/2016 Potential Energy In one dimension, the potential energy is dV related to the force by F . dx In three dimensions, this becomes: V V V F i j k V x y z The Del operator is defined in rectangular coordinates to be: i j k x y z Some terminology and properties of Del are: V is said to be the gradient of V The gradient is a vector that gives the maximum change in V. It is perpendicular to lines of V = constant. Page 4 of 6 3/8/2016 F is called the curl of F . If F 0 , then F can be written as F V because V 0 , that is the curl on any gradient is always zero. F is called the divergence of F . Page 5 of 6 3/8/2016 Curvilinear Coordinates (back of book, page A12) To be able to use the equations in Appendix F one needs to understand what the “h”s are. The equation that defines them is: dr e1h1du e2h2dv e3h3dw This is an orthogonal coordinate system with coordinates u, v, and w that have unit vectors associated with them of e1, e2 , e3. Notice that to get h1 , one holds v and w constant and generates a length element. In an xyz coordinate system, the length along the x axis is dx, so h1 1. For cylindrical coordinates, one has x R cos , y R sin , z Z The u, v, and w are R, , and Z. If and Z are constant, the differential length generated by letting R increases in just dR , so h1 1. Page 6 of 6 3/8/2016 If R and Z are constant and is allowed to increase, the length generated is Rd , so h 2 R. And if R and are constant and Z increases, one gets dz h3 1. In other words, if two of the dimensions are held constant and the third is allowed to change, one has the d distance generated hu du , in the eu direction.