RATIONAL METHOD OF ESTIMATING RUNOFF
Rational Method: The rational method is used around the world for peak flow estimation of small rural drainage basins and is the most widely used method for urban drainage design.
The rational method equation is given below:
Q = kCiA
where: Q - peak flow (m3/s).
k - conversion factor equal to 0.00278 (metric). (=1/360)
C - dimensionless runoff coefficient.
i - rainfall intensity (mm/hr).
A - catchment area (ha).
The Catchment Area, A
The catchment area, A, is determined from a map which includes the drainage area of interest.
The boundaries of the drainage area using a contour map.
Once the boundaries are known, the area can be determined using the map scale.
Since the area must be in acres for use in the Rational Method equation, a useful conversion factor is 43,560 ft2/acre.
The Runoff Coefficient, C
The runoff coefficient is the fraction of rainfall striking the drainage area that becomes runoff from that drainage area. It is an empirically determined constant, dependent on the nature of the drainage area surface.
An impervious surface like a concrete parking lot will have a runoff coefficient of nearly one.
A very tight clay soil will also have a relatively high runoff coefficient.
Sandy soil would have more infiltration and a lower runoff coefficient.
In addition to the nature of the surface and the soil, the slope of the drainage area has an effect on the runoff coefficient.
A steeper slope leads to a higher runoff coefficient.
Tables showing the values for runoff coefficient for a variety of types of drainage areas in handbooks, textbooks and on the internet.
Sample values for ready reference is shown below
The Design Rainfall Intensity, i
The design rainfall intensity is the intensity of a constant intensity design storm with the specified design return period and duration equal to the time of concentration of the drainage area.
Once the design return period and duration are determined, the design rainfall intensity can be determined from an appropriate intensity-duration-frequency graph or equation for the location of the drainage area.