Cycloidal Path of Charged Particle

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Homework Help Overview

The problem involves a charged particle sliding down a frictionless inclined plane under the influence of gravity and a magnetic field, leading to a cycloidal path. The original poster seeks to prove a relationship between the distance along the incline and the vertical displacement of the particle.

Discussion Character

  • Mixed

Approaches and Questions Raised

  • Participants discuss the forces acting on the particle, including gravitational and magnetic forces, and the conditions under which the particle leaves the incline. There are attempts to derive equations of motion and expressions for the distances involved. Some participants question the assumptions made regarding the magnetic field's orientation and its implications for the particle's trajectory.

Discussion Status

There is ongoing exploration of the problem, with various interpretations of the forces and their effects on the particle's motion. Some participants have offered insights into the equations governing the motion, while others are clarifying the conditions under which the particle behaves as described. The discussion remains open, with no explicit consensus reached yet.

Contextual Notes

Participants note the complexity of the problem, including the need for a clear understanding of the magnetic field's orientation and its role in the particle's motion. There are references to the initial conditions and the setup of differential equations, indicating that further clarification may be necessary to resolve ambiguities.

theQmechanic
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Homework Statement



A charged particle (q), mass (m) is released from a frictionless inclined plane of angle θ under influence of Earth's acceleration (g) and magnetic field (B) perpendicular to (g) and plane of motion of particle. The particle slides down distance "l" along incline and then follows a cycloidal path with vertical displacement between highest and lowest point (h). Prove that [itex]l = h\frac{cot^{2}θ}{4}[/itex]



Homework Equations



F= qv[itex]\times[/itex]B


The Attempt at a Solution



In vector notation I took g as -g j. B as -B k.
Took instantaneous velocity as v= vxi + vy j.
Then formed a differential equation to vx and vy in terms of time. The point where it leaves the incline is the point of inflection of the curve. I bashed whatever equations I had to finally get the answer, but after doing this I think there's got to be an easy way to look at this. Can someone help me out?
 
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Wouldn't life be a lot easier for you if the particle does NOT leave the incline ?
[edit] Hmmm... weak moment. B has to be ##\bot## g AND the plane of motion. You don't happen to have a picture at hand ?

Anyway, if the particle stays on the plane and also if it leaves, there has to be a g in one of the relevant equations.
And also in 3: what is your differential eqn? Can you show some of the bashing?
 
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Looks like B is to be perpendicular to g and to the NORMAL of the inclined plane. This appears to be what the OP has assumed, and it would indeed seem to produce a spiral path as it works its way down the incline.

For the first l distance there are 3 forces on the mass: gravity, magnetic and the plane pushing up on the mass. After that, when the mass becomes airborne, the last of these forces is absent. So it seems like you first have to determine l which is when the inclined components of magnetic and gravitational forces add up to zero. That should not be too bad.

Then, determine x and y for the airborne path to get h. I would write F = ma equations in x and y and solve for the locus. That sounds more imposing ...

EDIT: you can solve for just the y motion & then the max - min of this motion should be h I guess. Then compute l/h.

Getting late, may look some more tomorrow but probably others will have joined in by then.
 
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@BvU...h and l both come in terms of m,q,g,B,θ etc. then u take ratio and only θ remains. I'll Show the bashing.

@rude man...it doesn't come to be spiral, i'll show that mathematically.

The F=qvb=ma equation yield the following
[itex]m\frac{d}{dt}(v_{x}i + v_{y}j)=-qBv_{y}i + (qBv_{x}-mg)j[/itex].

Thus,
[itex]\frac{dv_{x}}{dt}= -\frac{qBv_{y}}{m}[/itex] and [itex]\frac{dv_{y}}{dt}=\frac{qBv_{x}}{m} -g[/itex]

[itex]\Rightarrow \frac{d^{2}v_{x}}{dt^{2}}=-(\frac{qB}{m})^{2}(v_{x}-\frac{mg}{qB})[/itex].
Let t=0 when particle is at bottom most point and velocity be [itex]v_{0}i<br /> \Rightarrow v_{x}= (v_{0} -\frac{mg}{qB})cos(\frac{qBt}{m}) + \frac{mg}{qB}[/itex].

Further, [itex]y= (v_{0} - \frac{mg}{qB})\frac{m}{qB}(1-cos(\frac{qBt}{m})))[/itex].
Clearly, [itex]h=\frac{2m}{qB}(v_{0} - \frac{mg}{qB})[/itex]

As can be seen [itex]x= aθ + bsin(kθ) and y=ccos(kθ)[/itex]. Thus it happens to be a cycloid.
 

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OK, I'm inclined to do away with the particle staying on the incline :redface:
Argument: B doesn't do any work, so potential energy at highest point = potential energy at releasing meaning h = l sinΘ, so not the cot2/4. I took ##\vec B \bot## the plane -- as I was told.
So we continue with
  • the assumption ##\vec B## is NOT ##\bot## the plane but in the horizontal negative z direction
  • we look at free fall in a magnetic field with inital condition ##v_0^2 = 2 l g \,sin\theta/ m##. (So ##\vec v_0 \cdot \hat\imath = v_0 \cos\theta## and ##\vec v_0 \cdot \hat\jmath = -v_0 \sin\theta##)
Do we agree so far ?
 
I agree with BvU's v2 = 2l sinθ/m. This is the 'takeoff point'. I now see a system of two diff. eq. in x and y with new initial conditions on vx and vy. I would impose a new coordinate system with x=y=0 at this point to clean up the equations in x and y.

I also got the OP's dvx/dt and dvy/dt equations, but then I don't follow the rest to where he/she gets h. If that h is correct then we have a problem getting the answer, seems like.

I would pursue solving the system of two diff. eq. in x and y, solving for y(t) and getting h that way. (I would use Laplace, but whatever).

@theQmechanic: I used the word 'spiral' loosely. The exact shape is of course determined by the equations. It's undoubtedly a cycloid as you and the question state.
 

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