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Revista mexicana de física

versión impresa ISSN 0035-001X

Rev. mex. fis. vol.66 no.5 México sep./oct. 2020  Epub 31-Ene-2022

https://doi.org/10.31349/revmexfis.66.585 

Research

Gravitation, Mathematical Physics and Field Theory

Planar motion with Fresnel integrals as components of the velocity

E. Flores-Garduñoa 

Stefan C. Mancasb 

Haret C. Rosuc 

M. Pérez-Maldonadod 

aInstituto Potosino de Investigación Científica y Tecnológica, Camino a la presa San Jose 2055, Col. Lomas 4a Sección, 78216 San Luis Potosí, S.L.P., México. e-mail: elizabeth.flores@ipicyt.edu.mx

bDepartment of Mathematics, Embry-Riddle Aeronautical University, Daytona Beach, FL 32114-3900, USA. e-mail: mancass.erau.edu

cInstituto Potosino de Investigación Científica y Tecnológica, Advanced Materials Division, Camino a la presa San José 2055, Col. Lomas 4a Sección, 78216 San Luis Potosí, S.L.P., México. e-mail: hcr@ipicyt.edu.mx

dUniversidad Politécnica de San Luis Potosí, Urbano Villalón No 500 Col. La Ladrillera C.P 78363 San Luis Potosí, S.L.P., México. email: maximino.perez@upslp.edu.mx


Abstract

We analyze the two-dimensional motion of a rigid body due to a constant torque generated by a force acting on the body parallel to the surface on which the body moves extending an old note of Ferris-Prabhu [Am. J. Phys. 38, 1356-1357 (1970)] and supplement it with a short discussion of the jerking properties.

Keywords: Planar motion; torque; Fresnel integrals; jerk

PACS: 02.30.Hq; 45.40.Cc; 45.20.D-

1. Introduction

While there are recent surprising applications of Fresnel integrals, such as to rat whiskers [1] and orange peel [2], it is surely much less known that fifty years ago Ferris-Prabhu [3] discussed a two-dimensional motion of a rigid body in classical Newtonian mechanics as an example in which Fresnel integrals occur beyond their usual context of near-field optical diffraction generated by slits and apertures [4-8]. Since the paper of Ferris-Prabhu is a very short note and has also some ambiguous points, we provide here a more detailed analysis of the kinematical quantities of this interesting motion supported by their plots adding also a discussion of its jerked properties.

2. Motion with velocity whose cartesian components are Fresnel integrals

Let us consider a small rigid and compact object of mass M and moment of inertia I on a frictionless surface defined by the cartesian coordinates x and y with the origin placed at the center of mass of the object. We assume the object is initially at rest and apply at time t = 0 a constant force, F, along the positive x direction at the point (x,y) = (0,d), where d is some distance on the y axis smaller than the size of the object in that direction. During the course of motion, the line of application of the force is maintained at the distance d for any instantaneous angle θ made by the force with the x axis, i.e., the force as a vector does not change in the rotating cartesian system defined by the axes x' and y' bound to the body, see Fig. 1.

FIGURE 1 The planar motion of a rigid object considered in this paper at the initial moment and two subsequent instants. 

We are interested in the trajectory of the center of mass of the object under these conditions. Choosing the center of mass as a reference point for the motion is theoretically very convenient because this planar motion is a superposition of translational and rotational motions and for the center of mass the translational motion is due to Newton’s second law, and the rotational motion is due to the torque equation in their standard form.

The torque equation for the motion, as depicted in Fig. 1 is

τ= Iθ¨= Fd, (1)

where I is the moment of inertia of the body, and the dot stands for the time derivative. Denoting K = Fd/I and using zero initial conditions, we find the polar angle θ(t) = (K/2)t 2. We now use this quadratic angle to write the cartesian components of acceleration provided by Newton’s second law

x¨t=FMcosK2t2,

y¨t=FMsinK2t2. (2)

By one integration and assuming zero integration constants, we find the cartesian components of the velocity, expressed in terms of the Fresnel integrals,

Cτ=0τcos(πu2/2)du

And

Sτ=0τsin(πu2/2)du,

where τ=(K/π)t [3]

x˙t=FMπKCKπt,

y˙t=FMπKSKπt. (3)

Since both velocities are zero at t = 0, it confirms that the center of mass undergoes a planar movement as an instant center of rotation. These components are plotted in Fig. 2 for three values of K, together with their renowned Argand plot (the positive part of the clothoid/Cornu/Euler spiral [9]) and the speed v(t) =x˙2+y˙2.

FIGURE 2 The cartesian components of the velocity for K = 1,2,3 (red, green, and blue, respectively), and force and mass taken as unity. The corresponding Argand plots (bottom left) and the speed v(t) =x˙2+y˙2 (bottom right). 

Integrating again with zero integration constants, the cartesian components for the position are

xt=FMπKtCKπt-1πKsinK2t2,

yt=FMπKtSKπt

+1πKcosK2t2-1. (4)

Since F/M is an overall scaling factor, we proceed here by assuming F/M = 1, which does not change the analytical behavior of the solutions. We plot the displacements (4) in Fig. 3 together with the radial displacement r(t) = x2+y2. The plots show a linear behavior that sets in at already moderate instants of time with some superposed ripples which are smaller and almost disappearing at increasing K. This is easy to understand by using the large argument expansion of the Fresnel integrals which we write in the form

Ct~12sgnt+1πtsinπ2t2~121+t sincπ2t2,

St~12sgnt+1πtcosπ2t2~121+t sinc*π2t2, (5)

FIGURE 3 Cartesian displacements w 1x(t) (top left) and w 2y(t) for a rigid particle constrained to a plane under the action of a constant force acting as described in the text forp K = 1,2,3. The position on the surface is r(t) = x2+y2, concerning to the origin at time t (middle left). The fluctuations in the direction of the speed (black arrows) in the course of motion for the same values of K (middle right and bottom). Both force and mass are taken as unity. 

for t >> 1 and where the notation

sinc*π2t2=-cosπ2t2π2t2=sinπ2t2-π/2π2t2

is introduced to emphasize the well-known sinc type ripples in the plateau region of the Fresnel integrals considered as switching functions. The linear rising in the amplitude of the ripples in the large asymptotic Fresnel integrals (5) is by far compensated by the natural damping of the sinc oscillations. In the case of the cartesian displacements (4), we notice that the last oscillatory terms are bounded by their amplitude, 1/K, and so their effect in the plots cannot be perceived. In other words, the displacement plots are dominated by the even functions tC and tS, which asymptotically in the first quadrant are given by

tCt~12t1+t sincπ2t2,

tSt~12t1+t sinc*π2t2, (6)

to which the diminishing effect of the factor π/K  should be added. Using (6) in (4) for F/M = 1, one can see that the graphs of the displacements are essentially the straight lines π/K t/2 with the superposed 1 + t sinc and 1 + t sinc modulations quickly damping down.

3. Some jerk properties

We now point out some jerked properties of this kind of motion. The cartesian displacements x and y present two coupled jerks of the type

x¨=-K~ty¨,

y¨=-K~tx¨, (7)

where K~= FK/M, as can be inferred from the derivatives of (2), although the total acceleration is constant, α = F/M. This is similar to the case of circular motion of arbitrary radius R and angular velocity ω, where the cartesian jerks are given by

x=-ωy¨,

y=ωx¨, (8)

and the centripetal acceleration is αc = ω 2 R.

It is interesting to find out the differential equation satisfied by the jerks, which a priory should be a third-order one [10]. Writing the system (4) in the form

xt=tx˙-1Ky¨,

yt=ty˙+1Kx¨-1K, (9)

and using x¨ from the second equation in the derivative of the first one, we are led to the nonhomogeneous third-order linear differential equation

w+K2t2w˙-K2tw=Kt (10)

This equation has the following linear independent solutions,

w1t=xt,w2t=yt,w3t=πKt-1K. (11)

The first two of them are jerked with intermingled jerks given in (7) and are just the cartesian displacements given in (4) and plotted in Fig. 3. The third linear independent solution is a non jerked, degenerate solution since it is also a solution of the simpler first-order linear equation

K2t2w˙-K2tw=Kt (12)

This solution is discarded because of the initial conditions of the motion.

The importance of the third order differential equation resides in its usage as a (decoupled) definition of the jerks which can be calculated from w1=K2tw1-tw˙1=-Kt sin(Kt2/2) and w2=K2tw2-tw˙2=Kt cos(Kt2/2), respectively.

4. Conclusion

In the planar motion of a rigid body with cartesian velocity components expressed through the Fresnel integrals, the speed tends quickly to a constant value affected by small sinc ripples whose amplitudes are additionally damped by the K parameter. Consequently, there is no surprise that also the trajectory corresponds to a planar motion of almost uniform velocity with only some small undulations. However, these undulations are important as they reveal the jerked features of the motion, that are determined by the third-order nonhomogeneous linear differential equation obtained in this paper.

References

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Received: May 31, 2020; Accepted: July 07, 2020

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