Translations:Transportstrecke/18/en: Unterschied zwischen den Versionen
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produces the outflow at the end of the pipe. | |||
This approximation method derived from Kalinin-Miljukov is identical to the linear storage cascade used for calculating runoff concentration. This means the flow ina transport reach can be simulated using a linear storage cascade consisting of <math>n</math> storages with the retention constant <math>K^*</math>. |
Aktuelle Version vom 25. November 2020, 18:34 Uhr
with:
[math]\displaystyle{ Q_z }[/math]: | Inflow to calculation section |
[math]\displaystyle{ Q_a }[/math]: | Outflow from calculation section |
[math]\displaystyle{ i }[/math]: | Current calculation time step |
[math]\displaystyle{ i-1 }[/math]: | Previous calculation time step |
[math]\displaystyle{ dt }[/math]: | Calculation time interval |
[math]\displaystyle{ C_1=1- e^{-dt/K^*} }[/math] | |
[math]\displaystyle{ C_2=1- \frac{K^*}{dt}/C_1 }[/math] |
produces the outflow at the end of the pipe. This approximation method derived from Kalinin-Miljukov is identical to the linear storage cascade used for calculating runoff concentration. This means the flow ina transport reach can be simulated using a linear storage cascade consisting of [math]\displaystyle{ n }[/math] storages with the retention constant [math]\displaystyle{ K^* }[/math].