The water velocity at any point in a stream or river is related to the logarithm of the depth at that point. For the Hoback River near Bondurant, Wyoming,
where is the velocity of the water, in feet per second, and is the vertical distance from the stream bed, in feet, at that point. For Pole Creek near Pinedale, Wyoming,
Both streams are feet deep at the locations mentioned. (Source: Leopold, Luna, Wolman, and Gordon, 1992)
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Complete the table of values for each stream.
Distance from bed (feet) |
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Velocity, Hoback River, (ft/sec) |
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Velocity, Pole Creek (ft/sec) |
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If you double the distance from the bed, by how much does the velocity increase in each stream?
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Plot both functions on the same graph.
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The average velocity of the entire stream can be closely approximated as follows: Measure the velocity at 20% of the total depth of the stream from the surface and at 80% of the total depth, then average these two values. Find the average velocity for the Hoback River and for Pole Creek.