Bernoulli's Equation — Question 4

Section 14-9 · Physics pages 2218–2219

Question 4 A finite reservoir has a moving free surface Use a quasi-steady, lossless model for water draining from a vertical tank of constant area A through an outlet of area a at its bottom elevation. The free surface and jet are both at atmospheric pressure. Treat their velocities as uniform and let h be their height difference. Define r = a/A < 1. vo vs Instantaneous tank geometry in the specified quasi-steady approximation. (a) Using continuity and Bernoulli at an instant, derive the outlet speed including free-surface motion. (b) For r = 0.20 and g = 10 m/s2, estimate the time to drain from h = 1.0 to 0.25 m. Explain why the limit r →1 signals failure of the approximation.
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Question 4 - Solution A finite reservoir has a moving free surface vo vs (a) Derivation and calculation With r = a/A, continuity gives Avs = avo, so vs = rvo. Instantaneous quasi-steady Bernoulli gives gh + 1 2v2 s = 1 2v2 o ⇒gh = 1 2(1 −r2)v2 o. vo = √ 2gh 1 −r2 , dh dt = −r √ 2gh 1 −r2 . (b) Result and interpretation ∆t = √ 1 −r2 r √ 2 g( √ hi − √ hf). ∆t = √ .96 .20 √2 10(1 −.50) = 1.09545 s . r →1−: vo →∞, ∆t →0. These singular predictions flag failure of the quasi-steady approximation; unsteady dynamics must then be retained. Physical check For r ≪1, the outlet-speed expression approaches √2gh for a large reservoir.

Question 4

A finite reservoir has a moving free surface

Use a quasi-steady, lossless model for water draining from a vertical tank of constant area AA through an outlet of area aa at its bottom elevation. The free surface and jet are both at atmospheric pressure. Treat their velocities as uniform and let hh be their height difference. Define r=a/A<1r=a/A<1.

Diagram shown in the original SVG worksheet.

  1. Using continuity and Bernoulli at an instant, derive the outlet speed including free-surface motion.

  2. For r=0.20r=0.20 and g=10m/s2g=10\,\mathrm{m/s^2}, estimate the time to drain from h=1.0h=1.0 to 0.25m0.25\,\mathrm{m}. Explain why the limit r→1r\to1 signals failure of the approximation.

Question 4 - Solution

A finite reservoir has a moving free surface

Diagram shown in the original SVG worksheet.

(a) Derivation and calculation

With r=a/Ar=a/A, continuity gives Avs=avoAv_s=av_o, so vs=rvov_s=rv_o. Instantaneous quasi-steady Bernoulli givesgh+12vs2=12vo2⇒gh=12(1−r2)vo2.gh+\tfrac12v_s^2=\tfrac12v_o^2\Rightarrow gh=\tfrac12(1-r^2)v_o^2.vo=2gh1−r2,dhdt=−r2gh1−r2.\boxed{v_o=\sqrt{\frac{2gh}{1-r^2}}},\qquad\frac{dh}{dt}=-r\sqrt{\frac{2gh}{1-r^2}}.

(b) Result and interpretation

Δt=1−r2r2g(hi−hf).\Delta t=\frac{\sqrt{1-r^2}}r\sqrt{\frac2g}(\sqrt{h_i}-\sqrt{h_f}).Δt=.96.20210(1−.50)=1.09545s.\boxed{\Delta t=\frac{\sqrt{.96}}{.20}\sqrt{\frac2{10}}(1-.50)=1.09545\,\mathrm s}.r→1−:vo→∞,Δt→0.r\to1^-:\quad v_o\to\infty,\quad\Delta t\to0.These singular predictions flag failure of the quasi-steady approximation; unsteady dynamics must then be retained.

Physical check

For r≪1r\ll1, the outlet-speed expression approaches 2gh\sqrt{2gh} for a large reservoir.