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当测站积累了足够的用公式法推求的天然漂浮物层平均流速系数的资料后,就可以分析出适用于本站的各类天然漂浮物的层流速系数.如果本站有足够多的多点法的流速仪流理测验资料,那么就可以利用多点法流速资料分别计算出不同相对水深的层于均流速,再分析出不同的相对水深的层平均流速系数,作为本站天然深浮物的层平均流速系数.
When the station has accumulated enough data to calculate the average velocity coefficient of the natural floating layer using the formula method, it can analyze the layer velocity coefficient of various natural floating materials applicable to this station. If the site has enough multi-point flowmeter flow test data, then you can use the multi-point flow rate data were calculated for different relative depth of the layer of the average flow rate, and then analyzed the different relative depth of the layer average velocity Coefficient, as the site of natural deep buoy layer average velocity coefficient.