Sliding on a Rough Quarter-Pipe - On Ice!

A particle P P of mass m m slides on the surface of a rough quarter-pipe of mass M > m M > m . The cross-sectional profile of the quarter-pipe is a quadrant of a circle of radius a a , and the coefficient of (kinetic) friction between the particle and the quarter-pipe is 0 < μ < 1 0 < \mu < 1 . The quarter-pipe is standing on a large horizontal layer of ice, which may be treated as a smooth surface. The particle starts at rest at the point A A at the top of the quarter-pipe, which is also stationary, and begins to slide down its surface. The quarter-pipe will also begin to slide on the ice.

In the case that m = 1 m = 1 kg and M = 10 M = 10 kg, there is a value μ 0 \mu_0 such that the particle will reach the bottom of the quarter-pipe at the point B B (and then continue sliding on the ice) if μ < μ 0 \mu < \mu_0 , but such that the particle will be brought to rest at some point on the quarter-pipe (and never reach the ice) if μ > μ 0 \mu > \mu_0 . Give the value of 1 0 6 μ 0 \lfloor 10^6\mu_0\rfloor .


The answer is 597149.

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1 solution

Mark Hennings
Jul 18, 2020

At time t t , let X X be the distance travelled by the quarter-pipe, and let θ \theta be the angle P C A PCA , where C C is the centre of the circle of the quarter-pipe surface. The the position vector of the particle (relative to O O , the initial position of the bottom-left corner of the quarter-pipe) is r = ( X + a a cos θ a a sin θ ) \mathbf{r} \; = \; \left(\begin{array}{c} -X + a - a\cos\theta \\ a - a\sin\theta \end{array}\right) While it is sliding, the particle is subject to a normal reaction force m R mR and a friction force μ m R \mu mR , as well as the force of gravity. Thus

m X ¨ ( 1 0 ) + m a θ ¨ ( sin θ cos θ ) + m a θ ˙ 2 ( cos θ sin θ ) = m R ( cos θ sin θ ) + μ m R ( sin θ cos θ ) + m g ( 0 1 ) -m\ddot{X}\left(\begin{array}{c} 1 \\ 0 \end{array}\right) + ma\ddot{\theta}\left(\begin{array}{c} \sin\theta \\ -\cos\theta \end{array}\right) + ma\dot{\theta}^2\left(\begin{array}{c}\cos\theta \\ \sin\theta \end{array}\right) \; = \; mR\left(\begin{array}{c} \cos\theta \\ \sin\theta \end{array}\right) + \mu mR\left(\begin{array}{c}-\sin\theta \\ \cos\theta \end{array}\right) + mg\left(\begin{array}{c}0 \\ -1 \end{array}\right) and hence X ¨ cos θ + a θ ˙ 2 = R g sin θ X ¨ sin θ + a θ ¨ = μ R + g cos θ \begin{aligned} -\ddot{X}\cos\theta + a\dot{\theta}^2 & = \; R - g\sin\theta \\ -\ddot{X}\sin\theta + a\ddot{\theta} & = \; -\mu R + g\cos\theta \end{aligned} The only external forces acting on the quarter-pipe and the particle are gravity and the normal reaction from the ice, all of which are vertical. Thus the horizontal component of the center of mass of the particle/quarter-pipe system stays constant throughout the motion. Hence M X + m ( X + a a cos θ ) -MX + m(-X + a - a\cos\theta) is constant, and so ( M + m ) X ˙ = m a θ ˙ sin θ (M+m)\dot{X} \; = \; ma\dot\theta\sin\theta Eliminating both R R and X X from these equations, we obtain the formidable differential equation ( 2 M + m + m cos 2 θ μ m sin 2 θ ) θ ¨ + ( μ ( 2 M + m ) m sin 2 θ μ m cos 2 θ ) θ ˙ 2 = 2 ( M + m ) g a ( cos θ μ sin θ ) \big(2M + m + m\cos2\theta - \mu m\sin2\theta\big)\ddot{\theta} + \big(\mu(2M+m) - m\sin2\theta - \mu m \cos2\theta\big)\dot{\theta}^2 \; = \; \frac{2(M+m)g}{a}(\cos\theta - \mu\sin\theta) Remarkably, we can find the first integral of this differential equation. To find the required integrating factor, we need to perform the integral 2 ( μ ( 2 M + m ) m sin 2 θ μ m cos 2 θ ) 2 M + m + m cos 2 θ μ m sin 2 θ d θ = ln ( 2 M + m + m cos 2 θ μ m sin 2 θ ) + 2 μ ( 2 M + m ) 2 M + m + m cos 2 θ μ m sin 2 θ d θ \int \frac{2\big(\mu(2M+m) - m\sin2\theta - \mu m \cos2\theta\big)}{2M + m + m\cos2\theta - \mu m\sin2\theta}\,d\theta \;=\; \ln\big(2M+m+m\cos2\theta-\mu m\sin2\theta\big) + \int \frac{2\mu(2M+m)}{2M+m+m\cos2\theta-\mu m\sin2\theta}\,d\theta This can be handled using a t = tan θ t = \tan\theta substitution. Omitting the details, if we define the function F ( θ ) = e x p [ 2 μ ( 2 M + m ) 4 M 2 + 4 M m μ 2 m 2 tan 1 ( 2 M tan θ μ m 4 M 2 + 4 M m μ 2 m 2 ) ] F(\theta) \; = \; \mathrm{exp}\,\left[\frac{2\mu(2M+m)}{\sqrt{4M^2 + 4Mm - \mu^2m^2}}\tan^{-1}\left(\frac{2M\tan\theta - \mu m}{\sqrt{4M^2 + 4Mm - \mu^2m^2}}\right)\right] then d d θ [ [ 2 M + m + m cos 2 θ μ m sin 2 θ ] F ( θ ) ] = 2 [ μ ( 2 M + m ) m sin 2 θ μ m cos 2 θ ] F ( θ ) \frac{d}{d\theta}\Big[\left[2M+m + m\cos2\theta - \mu m \sin2\theta\right]F(\theta)\Big] \; = \; 2\big[\mu(2M+m) - m\sin2\theta - \mu m\cos2\theta\big]F(\theta) so the differential equation becomes d d θ [ 1 2 ( 2 M + m + m cos 2 θ μ m sin 2 θ ) F ( θ ) θ ˙ 2 ] = 2 ( M + m ) g a ( cos θ g sin θ ) F ( θ ) ( 2 M + m + m cos 2 θ μ m sin 2 θ ) F ( θ ) θ ˙ 2 = 4 ( M + m ) g a G ( θ ) \begin{aligned} \frac{d}{d\theta}\Big[\tfrac12\big(2M+m + m\cos2\theta - \mu m \sin2\theta\big)F(\theta)\dot{\theta}^2\Big] & = \; \frac{2(M+m)g}{a}(\cos\theta - g\sin\theta)F(\theta) \\ \big(2M+m + m\cos2\theta - \mu m \sin2\theta)F(\theta)\dot{\theta}^2 & = \; \frac{4(M+m)g}{a} G(\theta) \end{aligned} where G ( θ ) = 0 θ ( cos φ μ sin φ ) F ( φ ) d φ G(\theta) \; = \; \int_0^\theta (\cos\varphi - \mu \sin\varphi)F(\varphi)\,d\varphi Now m cos 2 θ μ m sin 2 θ m 1 + μ 2 < m 2 < 2 M + m \big|m\cos2\theta - \mu m \sin2\theta\big| \; \le \; m\sqrt{1 + \mu^2} \; < \; m\sqrt{2} \; < \; 2M+m and hence 2 M + m + m cos 2 θ μ m sin 2 θ > 0 2M+m + m\cos2\theta - \mu m\sin2\theta > 0 for all 0 < θ < 1 2 π 0 < \theta < \tfrac12\pi . We can also show that R = 2 M ( a θ ˙ 2 + g sin θ ) 2 M + m + m cos 2 θ μ m sin 2 θ > 0 R \; = \; \frac{2M(a\dot{\theta}^2 + g\sin\theta)}{2M + m + m\cos2\theta - \mu m\sin2\theta} \; > \; 0

Thus the particle never leaves the surface of the quarter-pipe before reaching B B , and so either the particle reaches the bottom B B of the quarter-pipe, where θ = 1 2 π \theta = \tfrac12\pi , or else the particle comes to rest at some point with a value of θ \theta less than 1 2 π \tfrac12\pi . The function G ( θ ) G(\theta) is increasing for 0 < θ < cot 1 μ 0 < \theta < \cot^{-1}\mu , and decreasing for cot 1 μ < θ < 1 2 π \cot^{-1}\mu < \theta < \tfrac12\pi . Thus the particle will have come to rest before reaching B B if G ( 1 2 π ) < 0 G(\tfrac12\pi) < 0 , and will pass B B and move onto the ice if G ( 1 2 π ) > 0 G(\tfrac12\pi) > 0 . Thus the critical value μ 0 \mu_0 is the one for which G ( 1 2 π ) = 0 G(\tfrac12\pi) = 0 . When M = 10 M = 10 , m = 1 m = 1 , plotting G ( 1 2 π ) G(\tfrac12\pi) against μ \mu shows that there is unique value μ 0 \mu_0 for which G ( 1 2 π ) = 0 G(\tfrac12\pi) = 0 . Numerical calculations show that μ 0 = 0.5971498673... \mu_0 = 0.5971498673... , and hence 1 0 6 μ 0 = 597149 \lfloor 10^6 \mu_0 \rfloor \; = \; \boxed{597149} .

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