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The Rubble-Pile Spin Limit

Circular motion and gravitation

Many asteroids larger than a few hundred metres are 'rubble piles': loose collections of boulders and gravel held together almost entirely by their own gravity, with negligible cohesion. Model such an asteroid as a uniform sphere of density ρ\rho and radius RR, rotating with period TT about an axis through its centre. Assume the shape stays spherical. Use ρ=2.00×103 kg m−3\rho = 2.00 \times 10^{3}\ \text{kg m}^{-3} where a value is needed.
Data: G = 6.67 × 10⁻¹¹ N m² kg⁻²

(a)

show that2 marks
Using the fact that a uniform spherical shell exerts no net gravitational force on a mass inside it, show that the gravitational field strength at distance rr from the centre (r≤Rr \le R) is g(r)=43πGρrg(r) = \tfrac{4}{3}\pi G\rho r.

(b)

show that2 marks
By considering the forces acting on a loose boulder resting on the surface at the equator, show that the shortest rotation period the asteroid can have without the boulder lifting off is Tc=3πGρT_c = \sqrt{\dfrac{3\pi}{G\rho}}, and calculate TcT_c in hours.

(c)

calculate2 marks
An asteroid of this density rotates with period 3.50 h3.50\ \text{h}. Calculate the ratio of the apparent weight of a boulder at the equator to its apparent weight at a pole.

(d)

discuss2 marks
Surveys find that almost no asteroids larger than about 300 m rotate faster than about 2.2 h, while many smaller asteroids spin in minutes. Use parts (a) and (b) to explain why the critical period does not depend on the asteroid's size, why at TcT_c the whole body (not just its surface) is on the verge of flying apart, and why small asteroids can beat the limit. Comment on one assumption of the model.

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The Rubble-Pile Spin Limit — Scholarship Physics | Xametric