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Reverse Osmosis Permeate Flux & Recovery Calculator engineering
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Reverse Osmosis Permeate Flux & Recovery Calculator

Model industrial RO membrane flux (GFD / LMH), system recovery rate, feed and reject brine flows, and temperature correction factor (TCF).

Permeate Production & Recovery

Membrane Element Quantity & Area

Flux & Hydraulic Performance

Average Permeate Flux
-- GFD
-- LMH (L/m²/hr)
Flux Design Status
OPTIMAL
within source limits
Feed Flow Required
-- GPM
-- GPD
Concentrate Reject Flow
-- GPM
-- GPD to drain

Temperature & Membrane Area

Total Active Membrane Area: -- sq ft
Temperature Correction Factor (TCF): --
Daily Permeate Production: -- GPD
Concentration Factor: -- x

Membrane Life & Scaling Assessment

--

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Frequently Asked Questions

What is Permeate Flux in Reverse Osmosis and why is it measured in GFD?

Permeate flux is the rate of purified water flow passing through a unit area of membrane surface per day, expressed as GFD (Gallons per Square Foot per Day) or LMH (Liters per square meter per hour). It is the central parameter governing membrane longevity, fouling rate, and cleaning frequency.

Why must feed water temperature be corrected with TCF?

As water cools, its viscosity increases (water is ~40% more viscous at 50°F than at 77°F). In colder water, higher net driving pressure is required to push the same volume of water through the polyamide polymer pores. Sizing without TCF will leave a plant starved for water in winter months.

What is the relationship between recovery rate and brine concentration factor?

System recovery (Y) is the percentage of incoming feed water converted into pure permeate. The reject concentration factor equals 1 / (1 - Y). At 75% recovery, minerals in the concentrate stream are concentrated 4 times; at 85% recovery, they are concentrated 6.67 times, greatly increasing calcium sulfate and silica scaling potential.

What happens if design flux is set too high?

Excessive flux causes severe concentration polarization—an impenetrable boundary layer of concentrated salts and colloids right against the membrane surface. This causes rapid irreversible mineral scaling, biofouling, and loss of salt rejection.