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href="#ulink_85f0f223-9943-5eb1-ae86-20c5a97fc1d5">Equation 1.20) has an interesting and, perhaps, unexpected form. In particular, the origin of the term that has twice the product of an angular velocity and a translational velocity (i.e. images) is not immediately obvious. The origin of all of the acceleration terms in a general expression like that in Equation 1.20 is described below. The description is offered twice – first in a mathematical form then in a graphical form.

      In general, the derivation of an expression for the acceleration of a point (say images) relative to another point (say images) starts with the position vector of images with respect to images and then differentiates it twice. Each differentiation must take account of the angular velocity of the coordinate system being used to express the vectors.

      Let the position vector be

      (1.44)equation

      Then, applying Equation 1.6, the velocity is,

      where the directions of the two components are defined. The rate of change of magnitude term is aligned with the position vector and is thus termed radial and the rate of change of direction component is perpendicular to the position vector and is therefore tangential.

      After collecting terms and substituting images (the angular acceleration vector) for images, we get the well‐known result,

      1  is the radial acceleration. This is nothing more than the second derivative of the distance between and and it is aligned with .

      2  is the tangential acceleration. It is called the tangential acceleration because it is aligned with the direction in which the point would move if it were a fixed distance from and were rotating about (i.e. in a direction perpendicular to a line passing through and ). Notice that is the total derivative of the angular velocity including its rate of change of magnitude and its rate of change of direction. As a result, may not be aligned with .

      3  is the Coriolis acceleration5. The vectorial approach to finding the Coriolis acceleration is in many ways preferable to the scalar approach put forward in many books on dynamics. The magnitude of the radial velocity is often referred to in reference books as and the Coriolis acceleration is seen written as where the reader is left to determine its direction from a complicated set of rules. Consideration of Equations 1.45,1.46,1.47 shows that there are two very different types of terms that combine to form the Coriolis acceleration with its remarkable 2. The two terms are equal in magnitude and direction (i.e. each is ). One of these arises from part of the rate of change of magnitude of the tangential velocity of . The second arises from the rate of change of direction of the radial velocity of .

      4  is the centripetal acceleration. In 2D circular motion. this is commonly written as and points toward the center of the circle. For the general points and used here, the centripetal acceleration points from to .

      Remember that rates of change of magnitude are aligned with the vector that is changing and rates of change of direction are perpendicular to the original vector and are pointed in the direction that the tip of the vector would move if it had the prescribed angular velocity and were simply rotating about its tail.

Schematic illustration of the velocity and acceleration components of the slider.

      Between the inner and outer circles on Figure 1.7 are the components of the acceleration.

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