Flow Duration Curve

Flow duration curve is a cumulative fequency curve in which dishcharge is plotted on the y-axis and percentage of time plotted on the x-axis. First, dishcharge and time is calculated. With the help of tis data, flow duration curve is plotted.

A typical flow duration curve is shown below.

Flow Duration Curve
Flow Duration Curve

It shows the percentage of time that a particular speed has been reached or exceeded over a specific period of time. It combines the flow characteristics of the magnetic through the discharge region into a single curve, regardless of the order in which it occurs. If the time period underlying the curve represents the long-term flow of a river, the curve can be used to predict future flow distributions for hydroelectricity, water supply, and other studies. and pollution. This report shows how geological differences affect low-flow endpoints of the flow-time curves of rivers in adjacent catchments.

Therefore, time curves are useful for assessing the geological features of a river basin. A method of adjusting short-term flux duration curves to represent long-term conditions is presented. Adjustments were made by comparing the observatory’s short- and long-term records.

How to Draw Flow Duration Curve

  1. Calculate the total number of collected data. Lets assume it is upto N numbers.
  2. Rank the data in data 1,2,3,….,N.
  3. Calculation frequency (f)
    f = total number of data (N) / rank (s)
  4. Compute the probability of exceeding (p)
    p = 1/f
    p = n/N
  5. Sort the discharges in descending order.
  6. Plot probability of exceedance or % of time against discharge. This curve is the FDC.

In this way you can draw the flow duration curve.

Applications of Flow Duration Curve

  • Flow duration curve is used for reliable multiple flow rate evaluation in hydraulic engineering projects.
  • Flow duration curve helps to evaluate low-level flows. FDC allows you to capture streams based on any percentage of the time.
  • Planning and designing hydroelectric projects. Fixed capacity is calculated from hydroelectric flow curves.
  • The total amount of sediment carried by a river can be determined if there is a sediment classification curve and an flow duration curve.
  • Flow duration curve also provides flow variation capability. If the curve slopes continuously; this indicates that the output of the stream is very fickle. This is a typical condition where most of the flow is surface runoff.
  • Used in the design of drainage systems.
  • As part of flood control research.
  • Used to compare Streamflow data.
  • Used to calculate the sediment load and dissolved solids load of the stream.

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