Movement Equations 1: Location, Kinematics and Kinetics
By Michel Borel and Georges Vénizélos
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About this ebook
The set of books on Mechanical Engineering and Solid Mechanics, of which this book is the first volume, is an essential tool for those looking to develop a rigorous knowledge of the discipline, whether students, professionals (in search of an approach to a problem they are dealing with), or anyone else interested.
This volume deals with the elements required for establishing the equations of motion when dealing with solid bodies. Chapter 1 focuses on the systems of reference used to locate solid bodies relative to the observer, and demonstrates how to describe their position, orientation, and evolution during their motion. Chapter 2 introduces descriptors of motion such as velocity and acceleration, and develops the concept of torsor notation in relation to these descriptors. Finally, Chapter 3 concerns the notions of mass and inertia, as well as the kinetic torsor and dynamic torsor which consolidate the kinematic and kinetic aspects in a single concept.
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Movement Equations 1 - Michel Borel
1
Location of Solid Bodies
Mechanics is the science of relations between:
– the motion of an arbitrary physical system ( 1_21_10.gif ) in the system of reference ‹λ› from which it is observed;
– and the forces that act upon it.
But the motion of a physical system in space is a very relative notion, which depends in an essential manner on the observer. Before any development concerning the physical system, it is, therefore, fundamental to locate it relative to its observer. This is the focus of the present chapter, in which two considerations will be examined, namely how to represent it in order to locate it, and then how to determine its location.
For all that follows, the physical system considered is the solid body, which is a continuous and rigid (this latter notion will be subsequently specified) material set.
1.1. The notion of system of reference
The system of reference is used in mechanics to set a reference, based on which it is possible to locate a mechanical element (solid body or part of an elastic medium), then to observe the evolution of its location and study its motion.
At the terrestrial scale, the favored domain of mechanics is the physical space seen from a geometrical perspective, as an affine space of a three-dimensional vector space, represented by a basis consisting of three independent vectors; this representation is important because any vector in the geometrical space of terrestrial mechanics can be expressed as a linear combination of these three vectors of the basis.
The principle of the reference system of an element located in this space thus relies on two simultaneous measurements:
– that of the distance between this element and a point in space considered as fixed reference for the motion examined;
– that of the orientation of the segment origin-element
relative to the three independent directions that form the reference trihedron.
The set comprising the point of reference and the system of three independent axes forms a system of reference.
1.2. Frame of reference
1.2.1. Setting up a frame of reference
When a system of reference is used for the study of a motion, it is also called a frame of reference. This notion is of particular importance in the study of motion, since its choice depends on:
– the observer, meaning the context in which the motion evolves;
– the forces that act on the mechanical system under study, as the set of these forces should be inside the environment of reference, in order to be able to apply to this motion the principles that govern it.
1.2.1.1. Choosing the elements of a frame of reference
In principle, the frame of reference used to locate a solid body and follow its evolution should consist of elements that are independant of the body and of the motion to be described. When the latter takes place in the terrestrial environment, the ideal frame of reference meets the following conditions:
– the point of reference chosen as origin of the system of reference is the center of inertia of the solar system.
– its independent directions are symbolized by three axes that are defined by three stars considered to be fixed relative to the motion of the Earth.
It is the solar frame of reference, noted ‹g›, which ultimately illustrates the fundamental notion of the Galilean system of reference, which will be specified later on in this chapter.
This frame of reference is, however, poorly suited for the vast majority of motions taking place in the terrestrial environment, if only because of the measurement of the distance origin-element
, which fixes a scale that is completely disproportionate relative to the dimensions of the body whose motion is studied or to its field of evolution.
Moreover, since the Earth is moving relative to this system of reference, its axes, which would provide three independent directions, cannot be considered fixed for the motion studied. If we resorted to such a frame of reference, we would constantly be in relative motion, which would further complicate the formulation of the problem even though, for most of the motions studied in the terrestrial space, the drive terms are negligible compared with the relative ones; but this is not the case for slow motions such as those of icebergs or the continental