Solving a Point Particle on a Semi-Sphere: M and m's Role

  • Thread starter Thread starter benf.stokes
  • Start date Start date
  • Tags Tags
    Particle Point
Click For Summary

Homework Help Overview

The problem involves a point particle of mass m placed on top of a semi-sphere of mass M and radius R, which is on a frictionless surface. The objective is to determine the angle at which the particle loses contact with the semi-sphere as it begins to slide down.

Discussion Character

  • Exploratory, Assumption checking, Problem interpretation

Approaches and Questions Raised

  • Participants discuss the relevance of masses M and m in the solution, with some suggesting they may be red herrings. Others question how the motion of the hemisphere affects the problem and whether the initial interpretations of the problem were correct.

Discussion Status

The discussion is ongoing, with various interpretations being explored. Some participants have provided hints regarding the relationship between the motions of the hemisphere and the sliding mass, while others are attempting to reconcile their solutions with the problem's requirements.

Contextual Notes

There is ambiguity in the problem statement regarding the roles of M and m, leading to confusion about their necessity in the solution. Participants are also grappling with the implications of the frictionless surface and the motion of the hemisphere.

benf.stokes
Messages
67
Reaction score
0

Homework Statement



A point particle of mass m placed on top of a semi-sphere of radius R and mass M, which is based on a frictionless surface. At one instant, the particles begin to slide over the semi-sphere.
Obtain an equation for the angle at the point where the particle loses contact with the semi-sphere.
How do M and m get into the picture?

Thanks

Homework Equations



[tex]m\cdot g\cdot \cos(\theta) - N = m\cdot \frac{v^2}{R}[/tex]
[tex]m\cdot g\cdot R+0= \frac{1}{2}\cdot m\cdot v^2+m\cdot g\cdot R\cdot \cos(\varphi)[/tex]

The Attempt at a Solution



[tex] \mbox{Using conservation of mechanical energy comes:}[/tex]

[tex] m\cdot g\cdot R+0= \frac{1}{2}\cdot m\cdot v^2+m\cdot g\cdot R\cdot \cos(\varphi)[/tex]

[tex] \mbox{Solving for v^2 gives:}[/tex]

[tex] v^2 = 2\cdot g\cdot R\cdot (1-\cos(\varphi))[/tex]

[tex] \mbox{Using the centripetal force condition yields:}[/tex]

[tex] m\cdot g\cdot \cos(\theta) - N = m\cdot \frac{v^2}{R}[/tex]

[tex] \mbox{When contact is lost N = 0:}[/tex]

[tex] v^2 = g\cdot R\cdot \cos(\theta) \hspace{1 pt} \mbox{being \theta \hspace{0.5 pc} \mbox{the angle at which contact is lost and so:}}[/tex]

[tex] 2\cdot g\cdot R\cdot (1-\cos(\theta)) = g\cdot R\cdot \cos(\theta) \hspace{0.5 pc} \mbox{which upon solving gives:}[/tex]

[tex] \theta=\cos^{-1}(\frac{2}{3})[/tex]

[tex] \mbox{But I don't know where do M and m figure in this solution.}[/tex]
 
Last edited:
Physics news on Phys.org
the question is, do they have to be there ? .. have a look at your solution and tell us what do you conclude from it?
 
.Sometimes questions contain red herrings
 
In my solution M and m don't appear, so they would be irrelevant to the question. But why would my instructor introduce M and m then int he question?
 
benf.stokes said:
In my solution M and m don't appear, so they would be irrelevant to the question. But why would my instructor introduce M and m then int he question?

I suppose to see if you're on the ball.M never appears in the solution and m cancels out.As I said they are red herrings.:biggrin:
 
benf.stokes said:
In my solution M and m don't appear, so they would be irrelevant to the question. But why would my instructor introduce M and m then int he question?
Hint: The hemisphere is on a frictionless surface. (You solved a different problem.)
 
Doc Al said:
Hint: The hemisphere is on a frictionless surface. (You solved a different problem.)

The way I read the question is that the surface on which M slides is frictionless.I got the same answer as benf.
 
Dadface said:
The way I read the question is that the surface on which M slides is frictionless.
Right! (I thought I just said that.)
I got the same answer as benf.
Did you take into account the motion of the hemisphere?
 
Doc Al said:
Right! (I thought I just said that.)

Did you take into account the motion of the hemisphere?

Sorry I meant the surface on which m slides.Looking at the question again it seems that benf and myself both misinterpreted it(but it does have a trace of ambiguity,that's my excuse anyway).Because of the way I read the question I did not consider any movement of M.:blushing:
 
  • #10
How do I take in account the motion of the hemisphere??
 
  • #11
benf.stokes said:
How do I take in account the motion of the hemisphere??
How are the motions of the hemisphere and the sliding mass related? What does Newton's 3rd law tell you? How can you revise the conservation of energy expression?

Analyze the forces from the accelerating frame of the hemisphere.
 
  • #12
I did so but m and M continue to not appear:confused:
 
  • #13
benf.stokes said:
I did so but m and M continue to not appear
Show what you did. (What you wrote in post #1 assumes the hemisphere to be stationary.)
 
  • #14
[tex]\mbox{Let the aceleration of the hemisphere be equal to A and the radius of the hemisphere R. Then the transversal force is equal to:}[/tex]

[tex]m\cdot g\cdot \sin\theta+mA \left( \cos \right) \,\theta=ma[/tex]

[tex]{\it Ft}=m{\frac {d}{dt}}v \left( t \right) ={\frac {mv \left( t<br /> \right) {\it dv}}{{\it ds}}}={\frac {mv \left( t \right) {\it dv}}{Rd<br /> \theta }}[/tex]

Or

[tex]\left( g \left( \sin \right) \,\theta+A \left( \cos \right) \,\theta<br /> \right) Rd\theta =v{\it dv}[/tex]

[tex]\mbox{Integrating both sides yields:}[/tex]

[tex]\int_0^\theta \! g\cdot R\cdot \sin(\theta) \, d\theta + \int_0^\theta \! A\cdot R\cdot \cos(\theta) \, d\theta = \int_0^v \! v \, dv[/tex]

Or

[tex]{v}^{2}=2\,gR \left( 1- \left( \cos \right) \,\theta \right) +AR<br /> \left( \sin \right) \,\theta[/tex]

[tex]\mbox{Using the centripetal aceleration condition:}[/tex]

[tex]mg \left( \cos \right) \,\theta+mA \left( \sin \right) \,\theta-N={<br /> \frac {m{v}^{2}}{R}}[/tex]

[tex]\mbox{When the body loses contact with the surface N = 0 and so the previous equation becomes:}[/tex]

[tex]{v}^{2}=R \left( g \left( \cos \right) \,\theta+A \left( \sin \right) <br /> \,\theta \right)[/tex]

[tex]\mbox{Solving both equations in order to v^2 gives:}[/tex]

[tex]R \left( g\cos \left( \theta \right) +A\sin \left( \theta \right) <br /> \right) =2\,gR \left( 1-\cos \left( \theta \right) \right) +AR\sin<br /> \left( \theta \right)[/tex]

[tex]\mbox{Having reduced this to a problem of math I still don't have m or M appearing here}[/tex]

Thanks for the help
 
Last edited:
  • #15
benf.stokes said:
[tex]\mbox{Let the aceleration of the hemisphere be equal to A and the radius of the hemisphere R. Then the transversal force is equal to:}[/tex]

[tex]m\cdot g\cdot \sin\theta+mA \left( \cos \right) \,\theta=ma[/tex]
OK. But realize that A and the horizontal acceleration of the sliding body are not independent.

[tex]{\it Ft}=m{\frac {d}{dt}}v \left( t \right) ={\frac {mv \left( t<br /> \right) {\it dv}}{{\it ds}}}={\frac {mv \left( t \right) {\it dv}}{Rd<br /> \theta }}[/tex]

Or

[tex]\left( g \left( \sin \right) \,\theta+A \left( \cos \right) \,\theta<br /> \right) Rd\theta =v{\it dv}[/tex]

[tex]\mbox{Integrating both sides yields:}[/tex]

[tex]\int_0^\theta \! g\cdot R\cdot \sin(\theta) \, d\theta + \int_0^\theta \! A\cdot R\cdot \cos(\theta) \, d\theta = \int_0^v \! v \, dv[/tex]

Or

[tex]{v}^{2}=2\,gR \left( 1- \left( \cos \right) \,\theta \right) +AR<br /> \left( \sin \right) \,\theta[/tex]
A is not a constant. It varies as the body slides down.

I would approach the problem by first figuring out the sliding body's velocity (in the accelerating frame of the hemisphere) as a function of theta using conservation of energy. Don't neglect the relationship between the speeds of hemisphere and sliding body. (That's where m and M come in.)

It seems like a nasty bit of algebra.
 
  • #16
I have come to a full stop on this question.Intuition sort of tells me that the hemisphere should accelerate in the horizontal plane but when I sketch force diagrams which ignore friction I can see no resultant horizontal force that will cause this acceleration.The weight of the small mass acts vertically on the hemisphere and has no horizontal component.What,if anything,am I overlooking?:frown:
 
  • #17
Dadface said:
I have come to a full stop on this question.Intuition sort of tells me that the hemisphere should accelerate in the horizontal plane but when I sketch force diagrams which ignore friction I can see no resultant horizontal force that will cause this acceleration.The weight of the small mass acts vertically on the hemisphere and has no horizontal component.What,if anything,am I overlooking?:frown:
The hemisphere and mass exert a normal force on each other. That normal force has a horizontal component which accelerates the hemisphere. (Just to nitpick, the weight of the small mass acts vertically on the small mass, not the hemisphere.)
 
  • #18
Doc Al said:
The hemisphere and mass exert a normal force on each other. That normal force has a horizontal component which accelerates the hemisphere. (Just to nitpick, the weight of the small mass acts vertically on the small mass, not the hemisphere.)

Yes ,when I sketch the force diagrams and consider the effects more carefully I see it.Thanks Doc Al,I was having one of my dumb periods.:biggrin:
 

Similar threads

  • · Replies 5 ·
Replies
5
Views
2K
  • · Replies 38 ·
2
Replies
38
Views
4K
  • · Replies 3 ·
Replies
3
Views
1K
  • · Replies 30 ·
2
Replies
30
Views
2K
  • · Replies 10 ·
Replies
10
Views
2K
  • · Replies 10 ·
Replies
10
Views
2K
  • · Replies 10 ·
Replies
10
Views
2K
  • · Replies 7 ·
Replies
7
Views
2K
Replies
12
Views
2K