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While studying the dynamics of a meteorite entering the atmosfphere, the book "Impact Cratering - A geological Process" by H.J. Melosh considers the forces of drag, lift and gravity and compares their sum to $m\vec{a}$. This is okay if the mass of the meteorite is constant, but then he writes that, due to the process of ablation, th mass changes following this equation: $$\frac{dm}{dt}=-\frac{C_H\rho Av}{2\xi}(v^2-v_{cr}^2)$$ where $v=|\vec{v}|$ and the other terms are constants depending on the shape and material of the meteorite and the density of the atmosphere.

My question is: if the mass changes during the motion, shouldn't we add a term $$\vec{v}\frac{dm}{dt}$$ to Newton's second law? And, if not, how do I know in which cases I must not consider that term even if mass is changing? (Why is ablation different from other ways the mass of an object changes?)

Rhino
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The equation $\vec{F}=\frac{d\vec{p}}{dt}$ cannot just blindly be applied to systems in which mass is entering or leaving the system. You have to consider how mass enters or leaves a system. For example, if the mass is being ejected in the opposite direction of $\vec{p}$ (a rocket) this will increase $\vec{p}$, while if the mass is being isotropically ejected this will decrease $\vec{p}$ (since the mass of the body decreases, but the speed does not). The equation $\vec{F}=m\frac{d\vec{v}}{dt}+\frac{dm}{dt}\vec{v}$ is simply not a true equation, and should not be applied. I would go so far as to call it a dangerous equation, because there are specific cases in which it is true and this often misleads students (and even occasional textbook authors!) to think it is a general rule.

The general rule for a variable mass system is

$$ \vec{F}+\vec{v}_{rel}\frac{dm}{dt}=m\frac{d\vec{v}}{dt} $$ where $\vec{v}_{rel}$ is the relative velocity between the mass that is lost and the object you care about. Notice that if $\vec{v}_{rel}$ is opposite $\vec{v}$, it tends to increase $\vec{v}$, as in the case of a rocket. If $\vec{v}_{rel}=-\vec{v}$, we get the "dangerous" equation, which only holds in this case. Finally, in the case of meteor ablation, we have $\vec{v}_{rel}=0$, because the pieces falling off the meteor have the same initial speed as the meteor. Thus, we can ignore the $\frac{dm}{dt}$ term entirely.

Jahan Claes
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I think you are right, but we should think about it like this:

$$\frac{d\vec{p}}{dt}=\vec{F}\rightarrow \frac{d(m\vec{v})}{dt}=\frac{dm}{dt}\vec{v}+m\frac{d\vec{v}}{dt}=\vec{F}$$

Assuming those forces do not depend on the mass, you should actually be subtracting that from the acceleration:

$$\frac{d\vec{v}}{dt}=\frac{F}{m(t)}-\frac{1}{m}\frac{dm}{dt}\vec{v}$$

But just to be clear, that $\vec{F}$ (which is net force, of course), is probably velocity-dependent as well (since the drag force is). So we are now solving some complicated differential equation, which is a polynomial in $\vec{v}$.

EDIT: To try and clarify and summarize what's wrong with this (my) answer. The relationship between Newton's laws and momentum relies on interactions transferring momentum. This makes sense in the case of objects either collecting mass (via interactions) or ejecting mass (via interactions). However, in the case of a meteorite, the prevailing model uses interactions that do not transfer momentum, at least not in the direction of motion. The model of a meteorite traveling through the atmosphere is to treat the solid rock as a collection of smaller rocks, traveling together but not interacting. The interaction of the atmosphere pulls rocks away from the clump (possibly transferring momentum in the longitudinal direction), but the rest of the meteorite "doesn't know anything about it". As long as this happens roughly evenly across the body of the asteroid, it's path remains approximately 1-dimensional.

In this way, $\vec{F}=\frac{d\vec{p}}{dt}$ can be applied consistently, as long as one carefully specifies how momentum is being transferred.

EDIT EDIT: Another answer with more detail on this consistency, and an article from EJP.

levitopher
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