This is my second attempt at a reply. I decided to take a second look at my first attempt after reading tiny-tim's reply
ttzhou said:
Homework Statement
Suppose that there is a negligibly thin tree in the forest of infinite length that begun tipping over. Negating frictional effects from the pivoting, does the tree ever hit the ground?
Homework Equations
My approach was to solve the problem for a tree of length l and see what happens in the limit as l \rightarrow \infty
<br />
\tau = I\alpha<br />
<br />
\tau = Mg\cos{\theta}(l/2)\<br />
<br />
I = \frac{1}{3} Ml^2\<br />
The Attempt at a Solution
<br />
I\alpha = Mg\cos{\theta} (l/2)<br />
<br />
\alpha = \frac{3gl}{2} \cos{\theta}<br />
Not that it matters much (since you approached the problem in a different way below), but I think you have your l in the wrong place in the above equation.
Now, I know how to approach and get a function for \omega by using energy conservation; however, out of curiosity, would I be able to solve this DE purely mathematically?
In any case, \omega = \sqrt{\frac{3g(1-\sin{\theta})}{l}}
I interpret this to mean that if I take the limit as the length goes to infinity, the tree simply has no angular speed and thus cannot fall over at all. However, this seems unsatisfactory as an answer
Well, for what it's worth, your approach seems pretty good to me.

Your formula for
ω looks correct to me, assuming a uniform gravitational acceleration,
g. It's the same as what I came up with.
I'm guessing your approach is adequate for the correct answer. I mean sure, you could replace the uniform gravitational acceleration with Newton's law of universal gravitation, but that wouldn't make the problem any easier. And really, what would it mean for such a "tree" to fall down if it's already infinitely longer than the Earth's diameter? I mean, that's just getting silly. So I don't see anything wrong with your answer the way it is now.
- is it possible to actually derive an explicit function for \theta(t)?
I think so, but it wouldn't be a walk in the park.
Using the conservation laws that you used to find
ω, you've reduced the original second order nonlinear ordinary differential equation into a first order one (but still nonlinear). So at least there's that.
Tiny-tim's advice might help quite a bit. There is a trig identity that makes it simpler -- an identity that even WolframAlpha doesn't catch on its own.
That said, "simpler" is a relative term. I'm still not making much headway myself on an a
simple solution for
θ as a function of
t.
