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Membrane and Desalination Technologies - TCE Moodle Website

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<strong>Membrane</strong> Systems Planning <strong>and</strong> Design 359<br />

Because the TCF is a dimensionless ratio, the values for viscosity can be expressed in any<br />

convenient <strong>and</strong> consistent units. Thus, the temperature-normalized flux can be expressed in<br />

simplified terms, as shown in Eq. (12):<br />

J20 ¼ JTðTCFÞ; (12Þ<br />

where J20 is the normalized flux at 20 C, gal/ft 2 /d, JT is the actual flux at temperature T,gal/ft 2 /d,<br />

<strong>and</strong> TCF is the temperature correction factor, dimensionless.<br />

Generally, in order to identify changes in productivity (as measured by flux) that are<br />

specifically attributable to membrane fouling, it is desirable to normalize the flux for pressure<br />

as well as temperature, as shown in Eq. (13). Note that the temperature- <strong>and</strong> pressurenormalized<br />

flux is often referred to as either the specific flux or permeability.<br />

M ¼ J20<br />

; (13Þ<br />

TMP<br />

where M is the temperature- <strong>and</strong> pressure-normalized flux, gal/ft 2 /d/psi, J20 is the normalized<br />

flux at 20 C, gal/ft 2 /d, <strong>and</strong> TMP is the trans-membrane pressure, psi.<br />

4.3. NF <strong>and</strong> RO Processes<br />

As with the microporous MF, UF, <strong>and</strong> MCF membranes, the driving force for the transport<br />

of water across a semi-permeable membrane – such as that utilized by NF <strong>and</strong> RO processes –<br />

is a pressure gradient across the membrane. However, because NF <strong>and</strong> RO processes reject<br />

dissolved salts, the resulting osmotic pressure gradient, which acts against the transport of<br />

water from the feed to the filtrate side of the membrane, must also be taken into account.<br />

Typically, the osmotic pressure gradient is approximated from the concentration of total<br />

dissolved solids (TDS) on the feed <strong>and</strong> filtrate sides of the membrane. The corrected driving<br />

force across semi-permeable membrane is termed the net driving pressure (NDP) <strong>and</strong> can be<br />

calculated using Eq. (14) (5):<br />

where:<br />

NDP ¼ Pf þ Pc<br />

2<br />

0:01<br />

NDP = net driving pressure, psi<br />

P f = feed pressure, psi<br />

Pc = concentrate pressure, psi<br />

TDSf = feed TDS concentration, mg/L<br />

TDSc = concentrate TDS concentration, mg/L<br />

TDSp = filtrate TDS concentration, mg/L<br />

Pp = filtrate pressure (i.e., backpressure), psi<br />

TDS þ TDSc<br />

2<br />

TDSp Pp; (14Þ<br />

Equation (14) can be considered as three distinct components. The first term represents the<br />

average pressure on the feed side of the membrane; the second term represents the average<br />

osmotic backpressure; <strong>and</strong> the third term represents the filtrate backpressure. The conversion<br />

factor of 0.01 in the osmotic pressure term comes from a widely used rule of thumb for fresh

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