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Physics Lesson 18.2.1 - Parametric Equations in Galilean Transformations

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Welcome to our Physics lesson on Parametric Equations in Galilean Transformations, this is the first lesson of our suite of physics lessons covering the topic of Classical Principle of Relativity, you can find links to the other lessons within this tutorial and access additional physics learning resources below this lesson.

Parametric Equations in Galilean Transformations

Let's suppose there is an observer at rest, who is recording all events occurring in an inertial reference frame S. The origin O of space coordinates and the directions of the three axes X, Y and Z are all known. Using the standard methods, the observer associated to this inertial system measures the coordinates of any point of space. More precisely, he measures the space coordinates (x, y, z) of a material point which can be either at rest or at random motion in this inertial system.

From geometry, it is known that the 3-dimensional space is Euclidian. This means the distance of a point P(x, y, z) from origin O, is calculated through the Pythagorean Theorem.

Physics Tutorials: This image provides visual information for the physics tutorial Classical Principle of Relativity

As you see from the figure, L is the diagonal of the cuboid formed by projections of the point P on each axis and the point P itself. Hence, we can write:

L = √x2p + y2p + z2p

In addition, the observer at rest in S measures the time elapsed through a standard clock. As discussed in the previous tutorial, the time is equal and absolute for all inertial frames of reference. Principally, we assume the observer as able to measure the time through a rigorously periodical process. We denote this time by t and take its origin (t = 0) at any instant, because time is homogenous.

From mathematics, it is known that a parametric equation define a group of quantities as functions of one or more independent variables called parameters. In our case, the time t is the parameter, so we can write general form of the parametric equations of motion as

x = x(t)
y = y(t)
z = z(t)

where x, y and z are the coordinates of the point P at any instant t. Obviously, we know the object's motion when we know all the above three parametric functions at any given instant.

The diagonal L of the cuboid discussed above is usually denoted by r when expressed as a vector. It is known as position vector.

Now, let's consider the random motion of a particle P in a system S related to the Earth (i.e. we assume it as not moveable). The particle's trajectory is shown in the figure below. Then, we observe the same particle from another inertial reference system S'. Just we make sure (for convenience) to take the motion of the system S' in the X-direction of S. Obviously, the system S' moves at constant velocity V in respect to the fixed system S (as S' is inertial).

Let's take as t = 0 the instant in which the origins of the two system converge. It is clear that after a certain time t, the system S' is displaced by

(OO') = V · t

in the positive direction of the X-axis. Therefore, at a given instant t, the particle P will be somewhere in the space and it will have a position vector r in the system S and r' in the system S'.

Physics Tutorials: This image provides visual information for the physics tutorial Classical Principle of Relativity

From properties of vectors, is clear that:

r' = r - V ∙ t

For example, the system S' could have been connected to a train moving at constant velocity in respect to the ground. In the above figure, we also have denoted by v and v' the instantaneous velocity of particle in the systems S and S' respectively.

Remark! Do not confuse the moving velocity V of the inertial reference frame S' in respect to the reference frame S (which is considered at rest) with the velocity of particle (v or v') which represents the velocity of particle in the system S or S'. The first is denoted by an uppercase while the later with lowercase.

Giving that the three components of velocity vector V are (V, 0, 0), we obtain for the parametric equations of the point P in the system S' in respect to the system S:

x' = x - V ∙ t
y' = y
z' = z

When adding the time t as the fourth parameter and giving that t' = t in all inertial frames of reference, we obtain

x' = x - V ∙ t
y' = y
z' = z
t' = t

These equations are nothing else but the equations of Galilean Transformations of Coordinates we obtained in the previous tutorial.

You have reached the end of Physics lesson 18.2.1 Parametric Equations in Galilean Transformations. There are 5 lessons in this physics tutorial covering Classical Principle of Relativity, you can access all the lessons from this tutorial below.

More Classical Principle of Relativity Lessons and Learning Resources

Relativity Learning Material
Tutorial IDPhysics Tutorial TitleTutorialVideo
Tutorial
Revision
Notes
Revision
Questions
18.2Classical Principle of Relativity
Lesson IDPhysics Lesson TitleLessonVideo
Lesson
18.2.1Parametric Equations in Galilean Transformations
18.2.2Galilean Transformations of Velocity
18.2.3The Classical Principle of Relativity
18.2.4The Newtonian System and Speed of Light. The Pseudo-Theory of "Cosmic Ether"
18.2.5Symmetry of the Laws of Classical Physics. The Pseudo-Theory of Cosmic Ether

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