A hemispherical bowl of radius R is filled with water
A hemispherical bowl of radius $R$ is filled with water at the constant rate of $a$ litres per second. Find the rate at which the depth increases at depth $h$, and show that it is inversely proportional to the area of the free surface.
Explanation of Method
The rate of rise is the inflow divided by the free surface area.
Step 1: The cross-section at height $z$
Put the origin at the lowest point of the bowl, $z$ upward; the centre of the sphere is then at $z = R$, and the wall satisfies
\[ x^{2}+y^{2}+\bigl(z-R\bigr)^{2} = R^{2} \;\Longrightarrow\; x^{2}+y^{2} = 2Rz-z^{2}. \]
So the horizontal cross-section at height $z$ is a disc of area $\pi\bigl(2Rz-z^{2}\bigr)$.
Step 2: Volume filled to depth $h$
\[ V(h) = \int_{0}^{h}\pi\bigl(2Rz-z^{2}\bigr)dz = \pi\left[Rz^{2}-\frac{z^{3}}{3}\right]_{0}^{h} = \pi\left(Rh^{2}-\frac{h^{3}}{3}\right). \]
Step 3: Differentiate with respect to time
Both $V$ and $h$ change with $t$: \[\frac{dV}{dt} = \pi\bigl(2Rh-h^{2}\bigr)\frac{dh}{dt}. \tag{1}\]
The bracket is precisely the cross-sectional area at the top of the water — which is no accident, since the volume added in time $dt$ is a thin layer of that area.
Step 4: Solve for the rate of rise
The inflow is $\dfrac{dV}{dt} = a\cdot10^{-3}\ \text{m}^{3}\text{/s}$, so
\[ \frac{dh}{dt} = \frac{a\cdot10^{-3}}{\pi h\bigl(2R-h\bigr)}. \]
Step 5: The free surface area
At depth $h$ the water surface is a disc of radius $\sqrt{2Rh-h^{2}}$, of area
\[ S(h) = \pi\bigl(2Rh-h^{2}\bigr) = \pi h\bigl(2R-h\bigr), \]
so the answer takes the compact form below and the inverse proportionality is immediate.
Step 6: Verification
\[\text{Full bowl: } V(R) = \pi\left(R^{3}-\frac{R^{3}}{3}\right) = \frac{2\pi R^{3}}{3}, \text{ a hemisphere} \;\;\checkmark\]
\[h\to0:\ \frac{dh}{dt}\to\infty \text{ (the bottom is a point); } h = R:\ \frac{dh}{dt} = \frac{a\cdot10^{-3}}{\pi R^{2}}, \text{ the slowest rise} \;\;\checkmark\]
\[R = 0.5\ \text{m},\ a = 1,\ h = 0.25:\ \frac{dh}{dt} = \frac{10^{-3}}{\pi\cdot0.25\cdot0.75} \approx 1.70\ \frac{\text{mm}}{\text{s}} \;\;\checkmark\]
Result
Final answer:
\[\boxed{\,\frac{dh}{dt} = \frac{a\cdot10^{-3}}{\pi h\bigl(2R-h\bigr)} = \frac{a\cdot10^{-3}}{S(h)}\,}\]
Remark
Remark. The relation $\dfrac{dh}{dt} = \dfrac{\text{inflow}}{\text{surface area}}$ holds for a vessel of any shape, since the added volume is always a layer of thickness $dh$ spread over the free surface. In a hemisphere the surface widens all the way to the rim, so the water rises ever more slowly — the opposite of a cone standing on its point.