Animated Solution for Mathematics - Differential Equations: A hemispherical tank of radius 2 metres is initially full of water and has an outlet of 12 cm2 cross-sectional area at the bottom. The outlet is opened at some instant. The flow through the outlet is according to the law v(t)=0.62gh(t), where v(t) and h(t) are respectively the velocity of the flow through the outlet and the height of water level above the outlet at time t, and g is the acceleration due to gravity. Find the time it takes to empty the tank.
Visualized Solution
Visualizing the System
Hemispherical tank radius: R=2 m
Outlet area: a=12 cm2=12×10−4 m2
Initial height: h(0)=2 m
Flow velocity law: v(t)=0.62gh(t)
The Principle of Continuity
Rate of change of volume = − Rate of outflow
dtdV=−a⋅v(t)
Substituting v(t): dtdV=−a⋅0.62gh
Geometry of the Water Surface
Let r be the radius of the water surface at height h.
From the right triangle: r2+(R−h)2=R2
Expanding: r2=2Rh−h2
Given R=2: r2=4h−h2
Relating dV and dh
Cross-sectional area: A(h)=πr2=π(4h−h2)
Infinitesimal volume: dV=A(h)dh
Rate of change: dtdV=π(4h−h2)dtdh
Equating the Rates
Equating both expressions for dtdV:
π(4h−h2)dtdh=−a⋅0.62gh
Substitute a=12×10−4:
π(4h−h2)dtdh=−12×10−4×0.62gh
Simplify constants: 12×10−4×0.6=7.2×10−4
Separating the Variables
Divide by h and multiply by dt:
π(h4h−hh2)dh=−7.2×10−42gdt
Simplify the powers of h:
π(4h1/2−h3/2)dh=−7.2×10−42gdt
Setting Up the Integral
Integrate both sides to find total time T.
Initial state: at t=0, h=2
Final state: at t=T, h=0
π∫20(4h1/2−h3/2)dh=−7.2×10−42g∫0Tdt
Executing the Integration
Integrate the left side:
∫h1/2dh=32h3/2 and ∫h3/2dh=52h5/2
π[4⋅32h3/2−52h5/2]20=−7.2×10−42g[t]0T
Substitute limits (upper limit gives 0):
π(0−(38(2)3/2−52(2)5/2))=−7.2×10−42gT
Evaluating the Limits
Simplify the terms with base 2:
(2)3/2=22 and (2)5/2=42
−π(38(22)−52(42))=−7.2×10−42gT
Cancel the negative signs and factor out 2:
π2(316−58)=7.2×10−42gT
Solving for Time T
Cancel 2 from both sides.
Simplify the fraction: 316−58=1580−24=1556
π(1556)=7.2×10−4gT
Isolate T: T=15×7.2×10−4g56π
Final Answer
Multiply the denominator: 15×7.2=108
T=108×10−4g56π
Simplify the fraction: 10856=2714
Move 10−4 to numerator: 104
Final Answer: T=27g14π×104 units
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The Sigma Insight: Variable Separable Method
Solution Diagram
Analyzing the Geometry of the Surface
Our first challenge is to understand the shape of the water surface. Because the tank is a hemisphere, the surface is a circle, but its radius r is not constant.
If you look at a vertical cross-section of the tank, you can form a right-angled triangle. The hypotenuse is the tank's radius R=2, one leg is the vertical distance from the center of the sphere to the water surface, which is R−h, and the other leg is the surface radius r.
By the Pythagorean theorem, we have r2+(R−h)2=R2. Substituting R=2, this simplifies to:
r2=4h−h2
The area of the water surface at any height h is given by:
A(h)=πr2=π(4h−h2)
The Continuity Equation
The principle of continuity states that the rate at which the volume of water in the tank changes must equal the rate at which it leaves through the outlet. Mathematically, this is expressed as:
dtdV=−a⋅v(t)
We know the outlet area a=12×10−4 m2 and the velocity law v(t)=0.62gh. Combining these, we get:
dtdV=−a⋅0.62gh
Since the change in volume for an infinitesimal drop in height dh is dV=A(h)dh, we can write:
dtdV=π(4h−h2)dtdh
The Calculus of Emptying
Equating the two expressions for dtdV gives us our differential equation:
π(4h−h2)dtdh=−7.2×10−42gh
By separating the variables, we divide both sides by h and move dt to the right:
π(4h1/2−h3/2)dh=−7.2×10−42gdt
Now, we integrate the left side from the initial height h=2 to the final height h=0, and the right side from time t=0 to t=T:
π∫20(4h1/2−h3/2)dh=∫0T−7.2×10−42gdt
Final Calculation
The integration yields the following expression:
π[38h3/2−52h5/2]20=−7.2×10−42gT
Evaluating the limits, the upper limit at h=0 vanishes. The lower limit at h=2 provides a negative value that cancels the negative sign on the right side:
π2(316−58)=7.2×10−42gT
The 2 terms cancel out, leading to the final result for the time T: