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Answer: Fluid leaving a hemispherical vessel

Thursday, 20 of December , 2007 at 11:56 pm

Question: A hemispherical vessel of radius R has a small rounded orifice of area A_0 at the bottom. If A_h \gg A_0, how much time does it require to lower the level from h_1 to h_2?

Answer: First, lets assume fluid is incompressible and has a inviscid, steady, barotropic flow. If this is the case, the rate fluid leaves the vessel will be equal to the rate the fluid drops in the vessel. Therefore,

A_h \frac{\partial h}{\partial t} = A_0 u
\therefore \frac{\partial h}{\partial t} = \frac{A_0}{A_h} u

where \frac{\partial h}{\partial t} is the rate the water level drops and u is the rate the water leaves the orifice.

Now, if we use Bernoulli’s equation, we will get:

\frac{1}{2} (\frac{\partial h}{\partial t})^2 + \frac{P_{atm}}{\rho_0} + gh = \frac{1}{2}u^2 + \frac{P_{atm}}{\rho_0}
\frac{1}{2} (\frac{A_0}{A_h})^2 u^2 + gh = \frac{1}{2}u^2

Since A_h \gg A_0, \therefore (\frac{A_0}{A_h})^2 \approx 0. Using this approximation, we find that

u = \sqrt{2gh}

Next, we will need to find A_h.

According to Pythagoras ,

R^2 = r^2 + (R-h)^2
r = (R^2 - R^2 - h^2 +2hR)^{\frac{1}{2}} = (2hR - h^2)^{\frac{1}{2}}

Therefore,

A_h = \pi r^2 = \pi (2hR-h^2)

Now using the fact that A_h \frac{\partial h}{\partial t} = A_0 u, we have

\pi(2hR - h^2)\frac{\partial h}{\partial t} = A_0  \sqrt{2gh}
\int_{h_1}^{h_2} \pi (2 h^{\frac{1}{2}}R - h^{\frac{3}{2}})dh = \int_0^t A_0 \sqrt{2g}dt
\pi(\frac{4}{3}Rh^{\frac{3}{2}} - \frac{2}{5}h^{\frac{5}{2}}) \arrowvert_{h_1}^{h_2} = A_0 \sqrt{2g}t
t = \frac{2\pi}{A_0 \sqrt{2g}}(\frac{2}{3}R(h_1^{\frac{3}{2}}-h_2^{\frac{3}{2}}) - \frac{1}{5}(h_1^{\frac{5}{2}} - h_2^{\frac{5}{2}}))

Category: Answers, Fluid Dynamics

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