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CANARINA:
DESCAR:
INPUT DATA:
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Algorithms IV · software · environmental audit reports
2.2 Water is not stratified
In this case, the picnocline or thermocline has been formed. We will distinguish the following cases:
2.2.1 Multiport diffuser.- In such a case, we have the next equations
ymax=2,84 (g’q)1/3 Г -1/2 S=0,31 g’1/3 ymax q-2/3 B=max[Ltsin θ; 0,93Lt F-1/3] e=SQ/BUa
where Г=-(g/ρ)dρa/dy is the stratification coefficient (s-2) and ymax is the thickness of the mixing layer (m).
2.2.2 Separated ports.- In such a case, we have the next equations
ymax=3,98 (g’Qb)1/4 Г -3/8 S=0,071 g’1/3 y5/3max Qb-2/3 B=max[Ltsin θ; 0,93Lt F-1/3] e=SQ/BUa
2.2.3 Single port.-
ymax=3,98 (g’Q)1/4 Г -3/8 S=0,071 g’1/3 y5/3max Q-2/3 e=0,13 ymax B=SQ/eUa
For a profile of velocities different from the previous ones, it will be required a more complex method of numeric integration to solve the problem.
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