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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

y_max=2,84 (g’q)^1/3 Г ^-1/2

S=0,31 g’^1/3 y_max q^-2/3

B=max[L_tsin θ; 0,93L_t F^-1/3]

e=SQ/BU_a

where Г=-(g/ρ)dρ_a/dy is the stratification coefficient (s^-2) and y_max is the thickness of the mixing layer (m).

2.2.2 Separated ports.- In such a case, we have the next equations

y_max=3,98 (g’Q_b)^1/4 Г ^-3/8

S=0,071 g’^1/3 y^5/3_max Q_b^-2/3

B=max[L_tsin θ; 0,93L_t F^-1/3]

e=SQ/BU_a

2.2.3 Single port.-

y_max=3,98 (g’Q)^1/4 Г ^-3/8

S=0,071 g’^1/3 y^5/3_max Q^-2/3

e=0,13 y_max

B=SQ/eU_a

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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