Abstract:
The mean (average) flow velocity is an important hydraulic parameter for river engineers. It is calculated by using the stream flow rate (discharge) and the sectional flow area. Several techniques are available to estimate the sectional average or mean flow velocity. Rectently introduced entropy theory technique is a reliable as well as a quick approach compared to the traditional techniques like the velocity-area method. The entropy theory technique can estimate the discharge by measuring the single point velocity measurement only. The estimated parameters are well compared with the observed ones. The obtained results were compared in terms of correlation coefficient and error percentage. The error percentage is well within the acceptable limits.
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