Conservation of Momentum for Asteroid in Dust Cloud

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SUMMARY

The discussion focuses on the conservation of momentum for a spherical asteroid of mass m_0 moving through a dust cloud with uniform density ρ_d. The participants derive expressions for the asteroid's velocity v(t) and the force exerted on it by the dust. The correct expression for the velocity, as provided by the textbook, is v(t) = v_0 m_0 / [m_0^{4/3} + (4ρ_dπv_0 m_0 / (3(m/r^3)^{2/3}))t]^{3/4}. The confusion arises from the relationship between the asteroid's mass and the dust it collects, as well as the assumption that the asteroid's radius remains constant.

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Homework Statement



A spherical asteroid of mass m_0 is moving freely in interstellar space (no external forces) with velocity v_0 . It runs into a dust cloud whose uniform density is \rho_d Assume that every particle of dust that hits the asteroid sticks to it and that the asteroid remains spherical at all times. (a) Obtain an expression for the velocity of the asteroid as a function of time. (b) Obtain an expression for the force exerted on the asteroid by the dust as a function of time.

Homework Equations



p_f = p_i
F_{ext} = 0 which implies that m\frac{dv}{dt} + v\frac{dm}{dt}

The Attempt at a Solution


What I did initially was create an expression for m(t) which I got as:
m(t) = \frac{4}{3} \pi r^3(t) \rho_d + m_0

and I took the first derivative with respect to time. Since \rho_d is constant for the cloud, the only thing that was time dependent was r(t). Well, I got this

4 \pi r^2(t) \rho_d \frac{dr}{dt}.

I figured that, to within a proportionality constant r' = x' = v{t}

which also gave that

r = r_0 + d

where d is the total distance traveled in the cloud and is equivalent to v(t)*t .

So I plugged this all into my equation and I got that

\left[\frac{4}{3} \pi r^3(t) \rho_d + m_0 \right] \frac{dv}{dt} = V(t) \left[ 4 \pi r^2(t) \rho_d \frac{dr}{dt} \right]

which simplified down to

\left[\frac{4}{3} \pi r^3(t) \rho_d + m_0 \right] \frac{dv}{dt} = V(t) \left[ 4 \pi r^2(t) \rho_d v(t) \right]

Solving this out gives us that

v(t) = \frac{ \left( 4d^3\rho_d\pi + 3m_0 \right )t }{ 12 d^2 \rho_d \pi }.

This seems fair enough but the correct answer (as given by the book) is apparently

\frac{v_0 m_0}{ \left[ m_0^{4/3} + \frac{4\rho_d\pi v_0 m_0}{3 \left( \frac{m}{r^3} \right )^{2/3} }t \right]^{3/4} }.

I am utterly baffled as to how they solved this or got the power of \frac{3}{4} in the denominator. Any help would be very much appreciated.
 
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I've no idea how you got <br /> m(t) = \frac{4}{3} \pi r^3(t) \rho_d + m_0<br />

since how much mass the asteroid picks up depends on v and v isn't constant. You also don't
want the volume of the asteroid, but the largest crosssectional area.

\frac {dm}{dt} isn't too hard to find however.

apparently r is meant to be a constant, and the asteroid never becomes bigger no matter how
much mass is picked up. The density of the compacted dust isn't given and r is clearly meant
to be a constant.

still working on it.
 
I don't understand the book answer at all. There's still an m in there, should that be m_0?

m \frac {dv} {dt} + v \frac {dm}{dt} = 0 doesn't get you any further than m v = m_0 v_0


if the asteroid travels a distance x through the cloud it will have swept up a volume \pi r^2 x with mass \pi \rho r^2 x

let \pi r^2 \rho = C

m = m_0 + C x

v = \frac {dx}{dt} = \frac {v_0 m_0} {m} = \frac {v_0 m_0} {m_0 + C x}

this differential equation gives

m_0 v_0 t = (1/2) C x^2 + m_0 x after separation of variables.

solving the quadratic for x gives x = \frac {2 m_0} {C} (\sqrt {1 + \frac {2 c v_0 t}{m_0}}-1)

(the solution with the negative square root has x<0)

substituting this in the equation for v gives

v = \frac {v_0} { \sqrt { 1 + \frac {2 v_0 C t} {m_0}}}
 

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