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Topographic Retention Basin Drainage (Environmental & Civil Engineering) Solution

An environmental and water resources engineer studies a high-resolution topographic survey contour map of an alluvial valley in the Las Vegas wash basin to design a regional stormwater detention basin. The contour lines represent lines of constant ground surface elevation E(x,y)E(x, y) marked in meters (m\text{m}) above sea level.

At a prospective retention inlet located at survey coordinate point P(x0,y0)P(x_0, y_0):

  • The contour lines run perfectly horizontal (straight east-to-west, parallel to the xx-axis).
  • Moving vertically northward (in the positive yy-direction) from point PP, the contour elevation labels decrease steadily: 105 m→100 m→95 m105\text{ m} \to 100\text{ m} \to 95\text{ m}.
  • The contour lines representing 5 m5\text{ m} elevation drops are spaced tightly at Δy=10 m\Delta y = 10\text{ m} intervals on the ground.
  1. State the visual rules for determining the sign of partial derivatives ∂E∂x\frac{\partial E}{\partial x} and ∂E∂y\frac{\partial E}{\partial y} from a contour plot.
  2. Determine the signs and instantaneous numerical values (or approximations) of ∂E∂x\frac{\partial E}{\partial x} and ∂E∂y\frac{\partial E}{\partial y} at point PP.
  3. Explain why the horizontal orientation of the contour line forces ∂E∂x=0\frac{\partial E}{\partial x} = 0.
  4. In hydrological engineering, stormwater runoff velocity VV is proportional to the hydraulic ground gradient S=(∂E/∂x)2+(∂E/∂y)2S = \sqrt{(\partial E/\partial x)^2 + (\partial E/\partial y)^2}. Calculate SS at point PP and state the direction in which surface water will flow.

Step-by-Step Solution:

  1. State the Visual Step-and-Observe Rules:

    • For ∂E∂x\frac{\partial E}{\partial x}: Step to the right (east, +x+x) holding yy constant. Crossing into higher contours means ∂E∂x>0\frac{\partial E}{\partial x} > 0; crossing into lower contours means ∂E∂x<0\frac{\partial E}{\partial x} < 0; traveling tangent along a contour means ∂E∂x=0\frac{\partial E}{\partial x} = 0.
    • For ∂E∂y\frac{\partial E}{\partial y}: Step upward (north, +y+y) holding xx constant. Crossing into higher contours means ∂E∂y>0\frac{\partial E}{\partial y} > 0; crossing into lower contours means ∂E∂y<0\frac{\partial E}{\partial y} < 0. (Defined in Visual Estimation of Partial Derivatives from Contour Maps.)
  2. Evaluate the Signs and Magnitudes:

    • East-West Derivative ∂E∂x\frac{\partial E}{\partial x}: Moving along the +x+x axis travels directly along the horizontal contour line. Because elevation does not change along the contour, the instantaneous rate of change is zero:
      ∂E∂x=0\frac{\partial E}{\partial x} = 0
    • North-South Derivative ∂E∂y\frac{\partial E}{\partial y}: Moving along the +y+y axis crosses from 100 m100\text{ m} to 95 m95\text{ m} over a distance of Δy=10 m\Delta y = 10\text{ m}.
      ΔE=95−100=−5 m\Delta E = 95 - 100 = -5\text{ m}
      ∂E∂y≈ΔEΔy=−5 m10 m=−0.50 m/m=−50%\frac{\partial E}{\partial y} \approx \frac{\Delta E}{\Delta y} = \frac{-5\text{ m}}{10\text{ m}} = -0.50\text{ m/m} = -50\%
      Thus, ∂E∂y\frac{\partial E}{\partial y} is negative, with a magnitude of 0.50 m/m0.50\text{ m/m}.
  3. Geometric Reason for Vanishing East-West Derivative:

    • A contour line E(x,y)=cE(x, y) = c represents an isoline of constant height. Because the contour runs east-west, the tangent vector to the contour is T⃗=⟨1,0⟩=i^\vec{T} = \langle 1, 0 \rangle = \hat{i}.
    • Differentiating in the direction of the contour tangent measures zero change in elevation. Hence, the ground is completely level along the east-west axis at point PP.
  4. Calculate Hydraulic Gradient and Flow Direction:

    • State the Hydraulic Ground Gradient Formula:
      S=(∂E∂x)2+(∂E∂y)2=02+(−0.50)2=0.25=0.50 m/mS = \sqrt{\left(\frac{\partial E}{\partial x}\right)^2 + \left(\frac{\partial E}{\partial y}\right)^2} = \sqrt{0^2 + (-0.50)^2} = \sqrt{0.25} = 0.50\text{ m/m}
    • Flow Direction: Under gravity, water flows down the steepest descent gradient (−∇E-\nabla E):
      −∇E=−⟨∂E∂x,∂E∂y⟩=−⟨0,−0.50⟩=⟨0,0.50⟩-\nabla E = -\left\langle \frac{\partial E}{\partial x}, \frac{\partial E}{\partial y} \right\rangle = -\langle 0, -0.50 \rangle = \langle 0, 0.50 \rangle
    • Surface runoff flows due north (straight down the fall line into the detention inlet) at a steep 50%50\% drop.