A civil and environmental water resources engineer at the UNLV Howard R. Hughes College of Engineering is designing a pressurized subsurface drainage culvert to convey stormwater and treated municipal effluent under Tropicana Avenue in Las Vegas.
The culvert is constructed as a circular reinforced concrete conduit of internal radius R=0.5 meters. Due to viscous fluid friction and boundary layer adhesion along the conduit wall, the stormwater exhibits a fully developed axisymmetric parabolic velocity profile, modeled in Cartesian coordinates as:
v(x,y)=4(0.25−(x2+y2))[meters per second, m/s]
where x2+y2≤(0.5)2.
Step-by-Step Solution:
Convert Domain Boundaries to Polar Coordinates: State the Circle Boundary Equation in Polar Form:
x2+y2≤R2⟹r2≤(0.5)2⟹0≤r≤0.5 m
Because the conduit cross-section is a complete circle enclosing the origin, the angular sweep encompasses the full circumference:
0≤θ≤2π rad
Thus, the domain is the polar rectangle D={(r,θ)∣0≤r≤0.5,0≤θ≤2π}.
Transform Velocity Profile and Area Element: Apply the Polar Coordinate Substitution Rule:
x2+y2=r2
Substitute into the Cartesian velocity distribution:
v(r)=4(0.25−r2)=1−4r2 m/s
State the Polar Area Element Formula with Jacobian:
dA=rdrdθ
Formulate the double integral for total volumetric discharge Q:
Quantitative Interpretation: The total volumetric flow rate through the circular conduit is exactly 8π m3/s≈0.393 m3/s (approximately 393 liters per second).
Engineering Application: In civil flood-control engineering, evaluating volumetric discharge across circular pipe cross-sections is fundamental to Hagen-Poiseuille pipe flow analysis and stormwater master planning. By converting Cartesian coordinate profiles into polar form, engineers eliminate cumbersome radical boundaries (y=±R2−x2) and verify whether gravity drainage or lift pump stations can handle peak convective desert storm runoffs without exceeding culvert hydraulic capacity.