Ball rolling down an incline gaining mass

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Homework Help Overview

The problem involves a snowball of initial mass m sliding down an incline at an angle φ, while accumulating additional mass Δm = αx as it travels a distance x. The discussion centers on deriving the differential equation of translational motion for the snowball, while ignoring rotation and friction.

Discussion Character

  • Mixed

Approaches and Questions Raised

  • Participants explore the application of conservation of momentum and the implications of variable mass in the context of the problem. There are questions regarding the treatment of mass changes and the physical validity of certain equations used in the derivation.

Discussion Status

Several participants have provided insights and cautions regarding the assumptions made in the derivation. There is an ongoing examination of the definitions and implications of the equations being used, particularly concerning the momentum of the system versus the snowball alone. Some participants have acknowledged the need for clarity in the treatment of mass and velocity in the context of the problem.

Contextual Notes

There are discussions about the initial conditions of the snow and the implications of mass accumulation on the dynamics of the snowball. Participants also note the complexities involved in variable-mass dynamics and the potential for errors in applying certain principles without careful consideration of the system as a whole.

Physgeek64
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Homework Statement


A snowball, initially of mass m, slides down a slope inclined at an angle φ with respect to the horizontal. As it moves, the mass of additional snow Δm = αx that it accumulates is proportional to the distance traveled x. Write the differential equation
of translational motion for the snowball, ignoring rotation and friction

Homework Equations



Conservation of momentum mv_before =mv_after [\itex]<br /> <br /> <h2>The Attempt at a Solution</h2><br /> <br /> ##dp= (m+dm)(v+dv)-mv##<br /> ##dp= mdv +vdm ##<br /> \frac{dp}{dt}= m\frac{dv}{dt}+v\frac{dm}{dt}<br /> mg sin(φ) = m\frac{dv}{dt}+vαx<br /> <br /> But this doesn&#039;t seem right to me<br /> <br /> Many thanks :)
 
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What happended to ##dm\over dt## ? Ah, sorry ##v\alpha x## is that term ?
So what is it that makes you feel uneasy ?
What makes me feel uneasy is ##dm = \alpha \, x## but effectively you replaced it with ##\alpha\, dx##.
Or did you ? because I don't see ##dm\over dt##, only ##dm##
 
BvU said:
What happended to ##dm\over dt## ? Ah, sorry ##v\alpha x## is that term ?
So what is it that makes you feel uneasy ?
What makes me feel uneasy is ##dm = \alpha \, x## but effectively you replaced it with ##\alpha\, dx##.
Or did you ? because I don't see ##dm\over dt##, only ##dm##

Ah yes, sorry I forgot to update this thread

So dm= ##\alpha\, x##
so \frac {dm}{dt}=\alpha\ \frac {dx}{dt}

and the rest follows from there. I think I have done it now :) Thank you though
 
Just a word of caution using Fdt=dp=vdm+mdv. In the sense in which that equation follows directly from dp=d(mv), it treats mass as though it can appear out of nowhere, which is not physically possible. The equation does work in practice, but only where the mass being added arrives with no initial velocity of its own. Similarly, if losing mass, it only works if the shed mass retains no velocity. E.g. for water leaking from a moving cart, vdm is negative, but no force is required to prevent it getting faster.
 
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haruspex said:
Just a word of caution using Fdt=dp=vdm+mdv. In the sense in which that equation follows directly from dp=d(mv), it treats mass as though it can appear out of nowhere, which is not physically possible. The equation does work in practice, but only where the mass being added arrives with no initial velocity of its own. Similarly, if losing mass, it only works if the shed mass retains no velocity. E.g. for water leaking from a moving cart, vdm is negative, but no force is required to prevent it getting faster.

Is that not the case here? I'm assuming the snow is initially at rest on the plane? Had it not been, I would have to take this into account.

Thank you for your input :)
 
Physgeek64 said:
Is that not the case here? I'm assuming the snow is initially at rest on the plane? Had it not been, I would have to take this into account.

Thank you for your input :)

As the ball slides down the ramp, the snow it picks up goes from an initial velocity of 0 to the velocity of the ball.

Variable-mass dynamics can be quite tricky, and until fairly recently, several of the published accounts have been found to be erroneous in some respects. See, eg.,
http://adsabs.harvard.edu/full/1992CeMDA..53..227P
for a post-1990 account. In particular, blind use of dp/dt = m dv/dt + v dm/dt = F can lead to serious errors.
 
Last edited:
Physgeek64 said:
Is that not the case here? I'm assuming the snow is initially at rest on the plane? Had it not been, I would have to take this into account.

Thank you for your input :)
Yes, it works in this case, but as Ray confirms it is not really simply a result of applying the product rule of calculus to p=mv.
 
haruspex said:
Yes, it works in this case, but as Ray confirms it is not really simply a result of applying the product rule of calculus to p=mv.
I didn't did I? I thought I derived it from the conservation of momentum? I may be wrong :)
 
Physgeek64 said:
I didn't did I? I thought I derived it from the conservation of momentum? I may be wrong :)
You wrote, and used, dp=vdm+mdv. Consider a cart containing water rolling smoothly on a horizontal track. Water leaks out at some steady rate ρ. dm=-ρdt, but no horizontal forces act on the cart, so you might write dp=mdv-vρdt=0, and conclude that the cart is accelerating.
The problem lies in the definition of m. If you define it as the mass of the cart and contents at time t, that is not a closed system. The cart does not merely become less massive; that mass goes somewhere and may carry momentum away with it.
Similarly in your snowball problem, if you define m as the mass of the snowball at time t then the accumulating mass has to come in from somewhere, and potentially arrives with its own initial momentum. In this case you get away with it because the additional snow had been at rest.
 
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haruspex said:
You wrote, and used, dp=vdm+mdv. Consider a cart containing water rolling smoothly on a horizontal track. Water leaks out at some steady rate ρ. dm=-ρdt, but no horizontal forces act on the cart, so you might write dp=mdv-vρdt=0, and conclude that the cart is accelerating.
The problem lies in the definition of m. If you define it as the mass of the cart and contents at time t, that is not a closed system. The cart does not merely become less massive; that mass goes somewhere and may carry momentum away with it.
Similarly in your snowball problem, if you define m as the mass of the snowball at time t then the accumulating mass has to come in from somewhere, and potentially arrives with its own initial momentum. In this case you get away with it because the additional snow had been at rest.

Sorry to be a pain, but I only got that expression from considering dp=(m+dm)(v+dv)-mv-dm(u), (i.e. the total change in momentum) where u is the initial speed of 'dm'. But since u=0 and dmdv is almost zero this simply reduced to the usual formula of dp=vdm+mdv . I'm struggling to see how this is different from what you are saying?
 
  • #11
Physgeek64 said:
Sorry to be a pain, but I only got that expression from considering dp=(m+dm)(v+dv)-mv-dm(u), (i.e. the total change in momentum) where u is the initial speed of 'dm'. But since u=0 and dmdv is almost zero this simply reduced to the usual formula of dp=vdm+mdv . I'm struggling to see how this is different from what you are saying?
But that is not what you originally posted. You just wrote dp=(m+dm)(v+dv)-mv. That is a correct equation if p represents just the momentum of the snowball. But you did not define p. Is it intended as just that, or is it the momentum of the system? Since m is just the mass of the snowball, the obvious guess is that p is intended as the momentum of just that. If you are then going to write dp =ΣF.dt then it had better be the total system that F acts on in time dt.
To appreciate the subtlety, consider the reference frame of a skier going down the mountain at constant speed w. This changes v to v' =v-w everywhere, giving you dp=mdv+v'dm, yet the force is the same. With your updated formula, the -dm(u) term is +dm(w)=dm(v-v'), giving the right dp for the system.
 
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haruspex said:
But that is not what you originally posted. You just wrote dp=(m+dm)(v+dv)-mv. That is a correct equation if p represents just the momentum of the snowball. But you did not define p. Is it intended as just that, or is it the momentum of the system? Since m is just the mass of the snowball, the obvious guess is that p is intended as the momentum of just that. If you are then going to write dp =ΣF.dt then it had better be the total system that F acts on in time dt.
To appreciate the subtlety, consider the reference frame of a skier going down the mountain at constant speed w. This changes v to v' =v-w everywhere, giving you dp=mdv+v'dm, yet the force is the same. With your updated formula, the -dm(u) term is +dm(w)=dm(v-v'), giving the right dp for the system.

I thought it was since the first line of my working was : dp= (m+dm)(v+dv)-mv, i.e the change in momentum and the u=0 was implied, (and yes, p=momentum of the system, not the snowball- I should have explicitly said this, sorry). Maybe I should have made this more clear. But its an interesting point, and also highlights the importance of clarifying notation. Thanks, I appreciate the help :)
 
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