Balancing Hemispheres

Two rigid hemispheres A A and B B with uniform volume density ρ \rho have radii a a and b , b, respectively. Hemisphere B B has its flat face glued to a plane. Hemisphere A A is then balanced on top of hemisphere B B such that their curved surfaces are in contact.

Naturally, A A is in equilibrium when its flat face lies parallel to the flat face of B B . However, if given a small nudge, A A rolls without slipping on the curved surface of B B and will either oscillate about the equilibrium position or fall.

The constraint on a a such that A A can oscillate is given to be a < k b , a<kb, where k k is some positive real number.

Find the value of k k .

For this problem, assume gravity points down, perpendicular to the plane of B B 's flat face.


The answer is 0.600.

This section requires Javascript.
You are seeing this because something didn't load right. We suggest you, (a) try refreshing the page, (b) enabling javascript if it is disabled on your browser and, finally, (c) loading the non-javascript version of this page . We're sorry about the hassle.

1 solution

Brandon Monsen
Oct 21, 2017

Let θ \theta be the angle formed with the axis of hemisphere B B and the center of the flat surface of hemisphere A A . Since all forces which do work in this scenario (gravity) are conservative, we will analyze this problem using conservation of energy, and determine for which a give a gravitational potential energy well about θ = 0 \theta=0 .

Let the U ( θ ) = 0 U(\theta)=0 line be the plane of hemisphere B B 's flat surface, and let the center of mass position of each hemisphere with respect to its flat face be a a' and b b' respectively. For example, hemisphere B B is flat on the ground with its curved surface up, the center of mass position would be at b b' above the plane.

For hemisphere A A , we need some more variables - Let ϕ \phi be the angle formed by the axis of hemisphere A A , and the line connecting the centers of both hemisphere's flat surfaces. Then ϕ + θ \phi + \theta gives the angle formed by the axis of hemisphere A A and the vertical. Here, it is important to note that due to the no-slip condition, the arcs traced out by θ \theta and ϕ \phi are the same, and so a ϕ = b θ ϕ = b a θ a\phi = b\theta \Rightarrow \phi = \frac{b}{a}\theta . Then θ + ϕ = ( 1 + b a ) θ \theta + \phi = (1+\frac{b}{a})\theta . Let k = 1 + b a θ + ϕ = k θ k = 1+\frac{b}{a} \rightarrow \theta + \phi = k\theta .

We can then find the gravitational potential energy of the system to be

U ( θ ) = ρ V b g b + ρ V a g [ ( a + b ) cos ( θ ) a cos ( θ + ϕ ) ] = ρ V b g b + ρ V a g [ ( a + b ) cos ( θ ) a cos ( k θ ) ] U(\theta) = \rho V_{b} g b' + \rho V_{a} g \left[(a+b)\cos(\theta) - a'\cos(\theta+\phi) \right] = \rho V_{b} g b' + \rho V_{a} g \left[(a+b)\cos(\theta) - a'\cos(k\theta) \right]

Let ρ V a g = c ˉ \rho V_{a} g = \bar{c} . Then

U ( θ ) = c ˉ [ a k sin ( k θ ) ( a + b ) sin ( θ ) ] U ( θ ) = c ˉ [ a k 2 cos ( k θ ) ( a + b ) cos ( θ ) ] U' (\theta) = \bar{c} \left[ a'k \sin(k\theta) - (a+b)\sin(\theta) \right] \Rightarrow U''(\theta) = \bar{c} \left[ a'k^{2} \cos(k\theta) - (a+b) \cos(\theta) \right]

For stable equilibrium to hold, U > 0 U''>0 . We then plug in our equilibrium theta and find our constraint on a a

U ( 0 ) = c ˉ [ a k 2 ( a + b ) ] > 0 a + b < a k 2 U''(0) = \bar{c} \left[ ak^{2}- (a+b) \right] >0 \Rightarrow a+b<a'k^{2}

We then use the fact that the center of mass position of a hemisphere lies on the axis a distance 3 8 r \frac{3}{8}r from the flat face.

a + b < 3 8 a ( 1 + b a ) 2 a 2 ( a + b ) < 3 8 a ( a + b ) 2 a < 3 8 a + 3 8 b a < 3 5 b a+b< \frac{3}{8}a \left( 1 + \frac{b}{a} \right)^{2} \Rightarrow a^{2}(a+b) < \frac{3}{8}a(a+b)^{2} \Rightarrow a<\frac{3}{8}a + \frac{3}{8}b \Rightarrow a<\frac{3}{5}b

And so our answer is 3 5 = . 600 \frac{3}{5} = \boxed{.600}

Nice problem, I knew we have to apply U ( 0 ) > 0 U''(0)>0 but could not do the angle parts.

Keep posting more! :D

Harsh Shrivastava - 3 years, 6 months ago

0 pending reports

×

Problem Loading...

Note Loading...

Set Loading...