The MBR Book: Principles and Applications of Membrane
The MBR Book: Principles and Applications of Membrane
The MBR Book: Principles and Applications of Membrane
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92 <strong>The</strong> <strong>MBR</strong> <strong>Book</strong><br />
In a more recent study, the contribution <strong>of</strong> conditioning fouling to overall resistance<br />
was found to become negligible once filtration takes place (Choi et al., 2005a). By<br />
applying a vacuum (rather than suction) pump coupled with air backflushing, Ma et al.<br />
(2005) were able to reduce colloidal adsorption onto the membrane (Ma et al., 2005).<br />
<strong>The</strong>se studies suggest that colloid adsorption onto new or cleaned membranes coupled<br />
with initial pore blocking may be expected in <strong>MBR</strong>s (Jiang et al., 2005). <strong>The</strong> intensity<br />
<strong>of</strong> this effect depends on membrane pore size distribution, surface chemistry <strong>and</strong><br />
especially hydrophobicity (Ognier et al., 2002a). In a test cell equipped with direct<br />
observation through a membrane operating with crossflow <strong>and</strong> zero flux, flocculant<br />
material was visually observed to temporarily l<strong>and</strong> on the membrane (Zhang et al.,<br />
2006). This was defined as a r<strong>and</strong>om interaction process rather than a conventional<br />
cake formation phenomenon. While some flocs were seen to roll <strong>and</strong> slide across the<br />
membrane, biological aggregates typically detached <strong>and</strong> left a residual footprint <strong>of</strong><br />
smaller flocs or EPS material. Biomass approaching the membrane surface was then<br />
able to attach more easily to the membrane surface to colonise it <strong>and</strong> contribute to<br />
Stage 2.<br />
2.3.8.2 Stage 2: Slow fouling<br />
Even when operated below the critical flux for the biomass, temporary attachment <strong>of</strong><br />
the floc can contribute to the second fouling stage. After Stage 1, the membrane surface<br />
is expected to be mostly covered by SMP, promoting attachment <strong>of</strong> biomass particulate<br />
<strong>and</strong> colloidal material. Because <strong>of</strong> the low critical flux measured for SMP<br />
solutions, further adsorption <strong>and</strong> deposition <strong>of</strong> organics on the membrane surface<br />
may also occur during Stage 2. Since adsorption can take place across the whole<br />
surface <strong>and</strong> not just on the membrane pore, biological flocs may initiate cake formation<br />
without directly affecting the flux in this initial stage. Over time, however, complete<br />
or partial pore blocking takes place. <strong>The</strong> rate <strong>of</strong> EPS deposition, <strong>and</strong> resulting<br />
TMP rise, would then be expected to increase with flux leading to a shorter Stage 2.<br />
Such fouling would prevail even under favourable hydrodynamic conditions providing<br />
adequate surface shear over the membrane surface. However, since uneven<br />
distribution <strong>of</strong> air <strong>and</strong> liquid flow is to be expected in i<strong>MBR</strong>s, correspondingly inhomogeneous<br />
fouling must take place.<br />
2.3.8.3 Stage 3: TMP jump<br />
With regions <strong>of</strong> the membrane more fouled than others, permeability is significantly<br />
less in those specific locations. As a result, permeation is promoted in less fouled<br />
areas <strong>of</strong> the membrane, exceeding a critical flux in these localities. Under such conditions,<br />
the fouling rate rapidly increases, roughly exponentially with flux according<br />
to data <strong>of</strong> Le-Clech et al. (2003b) (Fig. 2.33). <strong>The</strong> sudden rise in TMP or “jump” is a<br />
consequence <strong>of</strong> constant flux operation, <strong>and</strong> several mechanisms can be postulated<br />
for the rapid increase in TMP under a given condition. As with classical filtration<br />
mechanisms (Fig. 2.9), it is likely that more than one mechanism will apply when an<br />
<strong>MBR</strong> reaches the TMP jump condition, <strong>and</strong> a number <strong>of</strong> models can be considered:<br />
(i) Inhomogeneous fouling (area loss) model: This model was proposed to explain the<br />
observed TMP pr<strong>of</strong>iles in nominally sub-critical filtration <strong>of</strong> upflow anaerobic