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Hydraulic Conduit Laminar Volumetric Flow Rate (Civil & Environmental Engineering) Solution

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 metersR = 0.5\text{ 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]v(x, y) = 4\left(0.25 - (x^2 + y^2)\right) \quad [\text{meters per second, m/s}]
where x2+y2≤(0.5)2x^2 + y^2 \le (0.5)^2.

Step-by-Step Solution:

  1. 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 mx^2 + y^2 \le R^2 \implies r^2 \le (0.5)^2 \implies 0 \le r \le 0.5\text{ m}
    Because the conduit cross-section is a complete circle enclosing the origin, the angular sweep encompasses the full circumference:
    0≤θ≤2π rad0 \le \theta \le 2\pi\text{ rad}
    Thus, the domain is the polar rectangle D={(r,θ)∣0≤r≤0.5, 0≤θ≤2π}D = \{(r, \theta) \mid 0 \le r \le 0.5, \, 0 \le \theta \le 2\pi\}.

  2. Transform Velocity Profile and Area Element:
    Apply the Polar Coordinate Substitution Rule:

    x2+y2=r2x^2 + y^2 = r^2
    Substitute into the Cartesian velocity distribution:
    v(r)=4(0.25−r2)=1−4r2 m/sv(r) = 4\left(0.25 - r^2\right) = 1 - 4r^2\text{ m/s}
    State the Polar Area Element Formula with Jacobian:
    dA=r dr dθdA = r \, dr \, d\theta
    Formulate the double integral for total volumetric discharge QQ:
    Q=∬Dv dA=∫02π∫00.5(1−4r2) r dr dθ=∫02π∫00.5(r−4r3) dr dθQ = \iint_D v \, dA = \int_{0}^{2\pi} \int_{0}^{0.5} (1 - 4r^2) \, r \, dr \, d\theta = \int_{0}^{2\pi} \int_{0}^{0.5} (r - 4r^3) \, dr \, d\theta

  3. Evaluate the Double Integral:
    Apply Fubini's Separability Theorem in Polar Coordinates (defined in Separability in Polar Integrals):

    Q=(∫02πdθ)(∫00.5(r−4r3) dr)Q = \left( \int_{0}^{2\pi} d\theta \right) \left( \int_{0}^{0.5} (r - 4r^3) \, dr \right)

    Evaluate the radial integral:

    ∫00.5(r−4r3) dr=[r22−r4]00.5=((0.5)22−(0.5)4)−0\int_{0}^{0.5} (r - 4r^3) \, dr = \left[ \frac{r^2}{2} - r^4 \right]_{0}^{0.5} = \left( \frac{(0.5)^2}{2} - (0.5)^4 \right) - 0
    =0.252−0.0625=0.125−0.0625=0.0625=116 m3/s= \frac{0.25}{2} - 0.0625 = 0.125 - 0.0625 = 0.0625 = \frac{1}{16}\text{ m}^3/\text{s}

    Evaluate the angular integral:

    ∫02πdθ=[θ]02π=2π rad\int_{0}^{2\pi} d\theta = [\theta]_{0}^{2\pi} = 2\pi\text{ rad}

    Multiply the evaluated components:

    Q=2π×116=π8 m3/s≈0.3927 m3/sQ = 2\pi \times \frac{1}{16} = \frac{\pi}{8}\text{ m}^3/\text{s} \approx 0.3927\text{ m}^3/\text{s}

Meaning of the Answer & Real-Life Application:

  • Quantitative Interpretation: The total volumetric flow rate through the circular conduit is exactly π8 m3/s≈0.393 m3/s\frac{\pi}{8}\text{ m}^3/\text{s} \approx 0.393\text{ m}^3/\text{s} (approximately 393 liters per second393\text{ 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−x2y = \pm\sqrt{R^2 - x^2}) and verify whether gravity drainage or lift pump stations can handle peak convective desert storm runoffs without exceeding culvert hydraulic capacity.