Differential Equation Application

Join the discussion
Registration is free. Ask a follow-up in this thread, or start your own.
27 replies · 5K views
james brug
Messages
34
Reaction score
0
I'm having trouble understanding this post: https://www.physicsforums.com/showthread.php?t=81157

Specifically, part (a)

(1) [tex]\frac{dV}{dt} = k - \alpha \pi \left( \frac{3a}{\pi h} \right) ^{2/3} V ^{2/3}[/tex]

Leaving out k, and considering a cone with no water coming in:

(2) [tex]\frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi h} \right) ^{2/3} V ^{2/3}[/tex]

How would I solve this for an equation to determine the volume in terms of time t? How do I interpret V in terms of t?

(3) [tex]\frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi h} \right) ^{2/3} {\left(\frac{1}{3}\pi r^2 h\right)} ^{2/3}[/tex]

I can't just solve eq. 3, that doesn't seem to make sense.
 
Physics news on Phys.org
Start by finding the relationship between r and h for the cone, this will allow you to express V and dV/dt in terms of a single time dependent variable (h or r, whichever you choose).
 
To make things a little clearer, say I change the h in thiago_j's posting to b, so that (3) looks like

(4) [tex]\frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi b} \right) ^{2/3} {\left(\frac{1}{3}\pi r^2 h\right)} ^{2/3}[/tex].


[tex]\frac{a}{b}=\frac{r}{h}[/tex], so [tex]r=\frac{h a}{b}[/tex] ? Is this the relationship you are talking about? I don't understand.
 
Yes, the opening angle of the cone [itex]\theta[/itex] is constant, so if the full height of the cone is [itex]b[/itex], and the radius of the opening at the top is [itex]a[/itex], then [itex]tan(\theta /2)=a/b=r(t)/h(t) \Rightarrow r(t)= h(t)\frac{a}{b}[/itex].

So substitute this result into your equation 4 and into the equation for the Volume to obtain V(h). Then use the chain rule: [tex]\frac{dV}{dt}=\frac{dV}{dh} \frac{dh}{dt}[/tex] to obtain a differential equation involving only h(t) and then solve.
 
[tex]\frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi b} \right) ^{2/3} {\frac{2}{3}\left(\frac{\pi}{3} h(t)^3 \left(\frac{a}{b}\right)^2 \right)} ^{-1/3} 3 h(t)^2[/tex] ?

I'm still not getting how this works.
 
james brug said:
[tex]\frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi b} \right) ^{2/3} {\frac{2}{3}\left(\frac{\pi}{3} h(t)^3 \left(\frac{a}{b}\right)^2 \right)} ^{-1/3} 3 h(t)^2[/tex] ?

I'm still not getting how this works.

No, a straight substitution into your equation (4) gives:

[tex] \frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi b} \right) ^{2/3} {\left(\frac{1}{3}\pi h(t)^3(\frac{a}{b})^2 \right)} ^{2/3} [/tex]

But you can also express [itex]V[/itex] as a function of h(t) because you know that the volume of the water at time [itex]t[/itex] is [itex]V=\frac{1}{3} \pi r(t)^3 h(t)=\frac{1}{3} \pi (\frac{a}{b})^3 h(t)^4[/itex]...use the chain rule on this last expression to find another expression for [itex]\frac{dV}{dt}[/itex] in terms of [itex]\frac{dh}{dt}[/itex]
 
gabbagabbahey said:
But you can also express [itex]V[/itex] as a function of h(t) because you know that the volume of the water at time [itex]t[/itex] is [itex]V=\frac{1}{3} \pi r(t)^3 h(t)=\frac{1}{3} \pi (\frac{a}{b})^3 h(t)^4[/itex]
How did you get [tex]r(t)^3[/tex]?
...use the chain rule on this last expression to find another expression for [itex]\frac{dV}{dt}[/itex] in terms of [itex]\frac{dh}{dt}[/itex]
[tex]\frac{4 \pi}{3} \left(\frac{a}{b} \right)^3 h(t)^3 \frac{dh}{dt}[/tex] ?
 
james brug said:
How did you get [tex]r(t)^3[/tex]?

[tex]\frac{4 \pi}{3} \left(\frac{a}{b} \right)^3 h(t)^3 \frac{dh}{dt}[/tex] ?

Errg, sorry typo it should be r^2 and so [itex]V=\frac{1}{3} \pi r(t)^3\2 h(t)=\frac{1}{3} \pi (\frac{a}{b})^2 h(t)^3[/itex]

And so the chain rule gives:

[tex]\frac{dV}{dt} =\pi \left(\frac{a}{b} \right)^2 h(t)^2 \frac{dh}{dt}[/tex]

Now equate that with the other expresion for dV/dt and you will have a separable differential equation for h(t) which you can easily solve...After that, you can simply plug it into the expression for V annd obtain an expression for V(t)
 
Now equate that with the other expresion for dV/dt


I don't know what you mean by that.
 
Well, you have 2 equations for dV/dt now:

[tex]\frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi b} \right) ^{2/3} {\left(\frac{1}{3}\pi h(t)^3(\frac{a}{b})^2 \right)} ^{2/3}[/tex]

and

[tex]\frac{dV}{dt} =\pi \left(\frac{a}{b} \right)^2 h(t)^2 \frac{dh}{dt}[/tex]

surely you can deduce that

[tex]\pi \left(\frac{a}{b} \right)^2 h(t)^2 \frac{dh}{dt}=- \alpha \pi \left( \frac{3a}{\pi b} \right) ^{2/3} {\left(\frac{1}{3}\pi h(t)^3(\frac{a}{b})^2 \right)} ^{2/3}[/tex]

right?
 
It wasn't clear to me how those two equations were equivalent. Even then, with this, [tex]\frac{dh}{dt}=\frac{- \alpha \left( \frac{3a}{\pi b} \right) ^{2/3} {\left(\frac{1}{3}\pi h(t)^3\left(\frac{a}{b}\right)^2 \right)} ^{2/3} }{ \left(\frac{a}{b} \right)^2 h(t)^2}[/tex]

Do I get [tex]h(t)=\alpha t +c[/tex] ?

After that, you can simply plug it into the expression for V annd obtain an expression for V(t)


So, if [tex]V=\frac{1}{3} \pi r(t)^2 h(t)[/tex], then [tex]V=\frac{1}{3} \pi \left({\frac{a}{b}}\right)^2 h(t)^3[/tex] , then [tex]V=\frac{1}{3} \pi \left({\frac{a }{b}}\right)^2 \left(\alpha t + c \right)^3[/tex] ?
 
james brug said:
It wasn't clear to me how those two equations were equivalent. Even then, with this, [tex]\frac{dh}{dt}=\frac{- \alpha \left( \frac{3a}{\pi b} \right) ^{2/3} {\left(\frac{1}{3}\pi h(t)^3\left(\frac{a}{b}\right)^2 \right)} ^{2/3} }{ \left(\frac{a}{b} \right)^2 h(t)^2}[/tex]

Do I get [tex]h(t)=\alpha t +c[/tex] ?




So, if [tex]V=\frac{1}{3} \pi r(t)^2 h(t)[/tex], then [tex]V=\frac{1}{3} \pi \left({\frac{a}{b}}\right)^2 h(t)^3[/tex] , then [tex]V=\frac{1}{3} \pi \left({\frac{a }{b}}\right)^2 \left(\alpha t + c \right)^3[/tex] ?

Close, you should [itex]h(t)=-\alpha t +c[/itex]...in other words your missing a negative sign in front of your alpha...you can check that your solution (with -alpha) for V satisfies the DE in your first post (equation 2).
 
[tex]h(t)=\alpha t +c[/tex] is what Maxima gives me for the equation

[tex]\frac{dh}{dt}=\frac{- \alpha \left( \frac{3a}{\pi b} \right) ^{2/3} {\left(\frac{1}{3}\pi h(t)^3\left(\frac{a}{b}\right)^2 \right)} ^{2/3} }{ \left(\frac{a}{b} \right)^2 h(t)^2}[/tex]. But that equation simplifies to [tex]\frac{dh}{dt}=- \alpha[/tex] which of course would give [tex]h(t)=-\alpha t +c[/tex]. Perhaps Maxima was absorbing the minus sign into c?


...you can check that your solution (with -alpha) for V satisfies the DE in your first post (equation 2)


(5) [tex]\frac{dV}{dt}=-\alpha \pi \left(\frac{3a}{\pi b}\right)^{2/3}\left(\frac{\pi}{3} \left({\frac{a }{b}}\right)^2 \left(\alpha t + c \right)^3 \right)^{2/3}[/tex]

So how does this bring me any closer to determining V at a time t?
I am told alpha is the proportionality constant, but I still don't understand its function. Couldn't a/b be a kind of proportionality constant? What do I do with alpha?
 
You leave alpha as it is; it is just some constant which you may or may not know... a/b is also a constant which you can easily measure, since [itex]a[/itex] is the radius of the conical depression, and [itex]b[/itex] is its depth/height.

Given that [itex]h(t)=-\alpha t +c[/itex], V at tme t is just

[tex]V(t)=\frac{1}{3} \pi \left({\frac{a }{b}}\right)^2 \left(-\alpha t + c \right)^3[/tex]

And that IS your solution!...you simply plug in the values of a,b and alpha and you can calculate V at a time t!

You can check to see that it is correct by differentiating it and making sure that it satisfies your original ODE:

[tex]\frac{dV}{dt} = - \alpha \pi \left( \frac{3a}{\pi h} \right) ^{2/3} V ^{2/3}[/tex]

If it does (and it does!), then your solution is obviously correct.
 
How do I know where alpha comes from, from where its derived?


And I'm still not clear on how these two equations relate to each other,

(6) [tex]\frac{dV}{dt} = \underbrace{- \alpha \pi \left( \frac{3a}{\pi b} \right) ^{2/3}}_{u1} \underbrace{{\left(\frac{1}{3}\pi h(t)^3(\frac{a}{b})^2 \right)} ^{2/3}}_{u2}[/tex]

(7) [tex]\frac{dV}{dt} =\underbrace{\pi \left(\frac{a}{b} \right)^2 h(t)^2}_{u3} \frac{dh}{dt}[/tex]

So, u3 is dV/dh, correct? And u2 is V^(2/3) in terms of h(t).

What would u1 be?
 
Yes, [itex]u_3[/itex] is dV/dh and [itex]u_2[/itex] is V^(2/3) in terms of h(t).

The quantity [tex]\pi \left( \frac{3a}{\pi b} \right) ^{2/3}\left(\frac{1}{3}\pi h(t)^3(\frac{a}{b})^2 \right) ^{2/3}}[/tex] is the surface area of puddle at a time [itex]t[/itex]

The proportionality constant [itex]\alpha[/itex] is a quantity that can be experimentally measured, by measuring the height of the water at a few different times, or theoretically derived based on knowledge of how water evaporates.
 
Is there an easy way to find t, if [tex]V(0)=t_{0}[/tex] and [tex]V(t)=t_0/2[/tex] ?

[tex]V(t)=\frac{1}{3} \pi \left({\frac{a }{b}}\right)^2 \left(-t + c \right)^3[/tex]

[tex]c=\left(\frac{t_0}{\frac{\pi}{3} \left(\frac{a}{b}\right)^2}\right)^{1/3}[/tex]

if [tex]t_0/2=\frac{1}{3} \pi \left({\frac{a }{b}}\right)^2 \left(-t + \left(\frac{t_0}{\frac{\pi}{3} \left(\frac{a}{b}\right)^2}\right)^{1/3} \right)^3[/tex] then [tex]t=\frac{-b^{2/9} \left(3t_0\right)^{1/9} \left( b^{4/9} \cdot 2^{2/3} \left( 3t_0 \right)^{2/9} -2a^{4/9} \cdot \pi^{2/9} \right) }{2a^{2/3} \cdot \pi^{1/3}}[/tex]

but when I check it against real values, I don't get the same answers. I have the strong suspicion this is wrong.
 
What happened to [itex]\alpha[/itex]?

The easiest way is probably to just use:

[tex]\frac{V(t)}{V(0)}=\frac{\frac{t_0}{2}}{t_0}=\frac{1}{2}=\frac{(-\alpha t+c)^3}{c^3} \Rightarrow (\frac{-\alpha t}{c}+1)=\frac{1}{\sqrt[3]{2}}[/tex]
 
Last edited:
gabbagabbahey said:
What happened to [itex]\alpha[/itex]?

It's not strictly necessary is it?

The easiest way is probably to just use:

[tex]\frac{V(t)}{V(0)}=\frac{\frac{t_0}{2}}{t_0}=\frac{ 1}{2}=\frac{(-\alpha t+c)^3}{c^3} \Rightarrow (\frac{-\alpha t}{c}+1)=\sqrt[3]{2}[/tex]

So a and b don't matter?
 
Last edited:
Yes, it is...is the proportionality constant so it determines how quiickly water evaproates after all, the original DE is essentially:

[tex]\frac{dV}{dt}=-\alpha( \text{Surface Area})[/tex]

Which means setting [itex]\alpha=1[/itex] makes the puddle evaporate very quickly...but if you just want to check your solution for various values, I suppose you can set it equal to one. But your solution for [itex]t[/itex] was incorrect regardless (although you got [itex]c[/itex] right).
 
It should have been [itex]\frac{1}{\sqrt[3]{2}}[/itex]...I've edited that post.

And a and b do matter, but they are contained in your expression for c.
 
gabbagabbahey said:
The easiest way is probably to just use:...

Is the way I was trying to do it hard?

I tried again and I get:
[tex]t=\frac{-b^{2/3} \left(2^{2/3}-2\right) \left( 3 t_0 \right) }{2a^{2/3} \cdot \pi^{1/3}}[/tex]
 
The way you are trying to do it is unnecessarily complicated, and you are making mistakes because of it.

I get (setting alpha=1):

[tex](\frac{-t}{c}+1)=\frac{1}{\sqrt[3]{2}} \Rightarrow t=(1-\frac{1}{\sqrt[3]{2}})c=(1-\frac{1}{\sqrt[3]{2}})\left(\frac{t_0}{\frac{\pi}{3} \left(\frac{a}{b}\right)^2}\right)^{1/3}[/tex]
 
Arrghh... if [tex]V(t)=t_0/2[/tex] , then what is the time period in between then and when [tex]V=0[/tex] ?
 
[tex]V(T)=0 \Rightarrow \frac{1}{3} \pi \left({\frac{a }{b}}\right)^2 \left(-T + c \right)^3=0 \Rightarrow T=c=\left(\frac{t_0}{\frac{\pi}{3} \left(\frac{a}{b}\right)^2}\right)^{1/3}[/tex]

And so computing the time period between [itex]t[/itex] and [itex]T[/itex] should be simple. It's just [tex]T-t=\frac{1}{\sqrt[3]{2}}\left(\frac{t_0}{\frac{\pi}{3} \left(\frac{a}{b}\right)^2}\right)^{1/3}[/tex].
 
Let's say I hadn't posted post #17 of this thread. Is the method you used in post #25 the most direct method? If I had only posted #24, is that what you would have said?
 
If you hadn't posted #17, I would have had to use your method, but you would have to know what [itex]t[/itex] was, because based only on #24 you would end up with [itex]T-t[/itex] being a function of [itex]t[/itex] (since c would be expressed in terms of [itex]t_0[/itex] and [itex]t[/itex])
 
Suppose that were the case--how would I do that? t is the number of units of time that have elapsed when half the water has evaporated, so I'm not quite sure what you mean.