In collaboration with Iranian Watershed Management Association

Document Type : Research Paper

Authors

1 Scientific Board, Faculty of Natural Resources, Kordestan University, Iran‎

2 MSc, Faculty of Natural Resources, Tehran University, Iran‎

3 Assistant Professor, Faculty of Natural Resources, Tehran University, Iran‎

4 BSc, Sabzevar Environmental Office, Iran

Abstract

Effective discharge (Qeff) that transports the most of suspended sediment in rivers and controls the bed conditions is an important criterion for evaluating the quality of water. Qeff usually has 1.5 years recurrence interval on the yearly maximum flood data series. For examining similarity between Qeff and Q1.5 in ten stations of Daryacheh Namak Drainage Basin, at first the probability density function (pdf) of daily flows and sediment rating curves was plotted, after that probability density function of suspended sediment was constructed by multiplying the coefficient of sediment rating curves with pdf of daily flows. Then its recurrence interval was estimated by Vibul's method. The results showed that there are not any similarities between Qeff and Q1.5, and the ratio of Qeff to Q1.5 ranged from 1.03 to 16.8. Therefore more research is required to reach more certain result.

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