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"A pond forms as water collects in a conical depression of radius [tex]a[/tex] and depth [tex]h[/tex]. Suppose that water flows in at a constant rate [tex]k[/tex] and is lost through evaporation at a rate proportional to the surface area.

(a) Show that the volume [tex]V(t)[/tex] of water in the pond at time [tex]t[/tex] satisfies the differential equation

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

where [tex]\alpha[/tex] is the coefficient of evaporation.

(b) Find the equilibrium depth of water in the pond. Is the equilibrium asymptotically stable?

(c) Find a condition that must be satisfied if the pond is not to overflow."

**My work:**(a)

Consider the following

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

where [tex]r[/tex] is the radius of the pond. Thus, we have

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

[tex]r^3 = \frac{3aV}{\pi h}[/tex]

[tex]V = \frac{1}{3} \pi r^2 \left( \frac{hr}{a} \right) = \frac{1}{3} \pi r^2 L[/tex]

which satisfies the differential equation.

(b)

[tex]\frac{dV}{dt} = 0[/tex]

[tex]k - \alpha \pi r^2 = 0[/tex]

[tex]r = \sqrt{\frac{k}{\alpha \pi}}[/tex]

Then, the equilibrium depth of water in the pond is

[tex]L = \frac{h}{a} \sqrt{\frac{k}{\alpha \pi}}[/tex]

In this particular case, I don't know how to show whether or not it is asymptotically stable.

(c)

[tex]L = \frac{h}{a} \sqrt{\frac{k}{\alpha \pi}} \leq h[/tex]

Any help is highly appreciated.