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In the process of developing a mathematical model of water flow and sediment transport it was required to go over a large number of hydraulic and sediment data. While preparing these measurements for the model's needs, we found a great number of data that varied notably in comparison to the data around it suggesting they could be measurement mistakes. Accordingly, this issue was further investigated aiming to eliminate the existing measuring lapses. This paper deals with the approach ofdoi:10.14415/zbornikgfs34.03 fatcat:zad2t4admfc47dshcdyyndn4g4