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Kissimmee River outlets flow into Lake Okeechobee, which sits 18 feet above sea level.
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The modeled peak outlet flow is 0.85·106 m3 s−1.
Three runs, with different outlet flow ranges, were carried out.
Figure 5 shows the average outlet flow of the anisotropic model.
Open image in new window Fig. 5 Outlet flow drawing of different fracture angles.
The outlet flow rate of the dispersed organic phase has been measured vs time until steady-state is reached (outlet flow rate equals inlet flow rate).
The feasible combinations of inlet and outlet flow rates are identified.
The system is also equipped with data logging for three variables; namely, inlet pressure, outlet pressure, and outlet flow.
Detailed flow measurement and computation were performed for outlet flow field for investigating the responsible flow mechanisms.
This change also causes a dramatic increase in the outlet flow of the hot water from the unit.
The lab scale experimental goal is to achieve an outlet flow of 650 °C at 5 bar absolute operating pressure.
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