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Membrane technology  65

            effective threshold chemicals, including phosphonates. have become available.
            Polycarboxylic acids,  such  as  polyacrylates  and  polymalonates,  operate  by
            blocking crystal growth sites preventing the growth of nuclei into crystals whiIst
            chelating chemicals react with potentially insoluble cations like calcium to form
            a soluble complex. Dosage rates are typically of  the order of  5-10  mg 1-1  and,
            whilst some indication of  the efficacy of these reagents may arise from the scale
            inhibition mechanism, it is generally the case that only pilot trials yield reliable
            information as to their suitability for a particular duty.
              Where scale-inhibiting chemicals are unable to cope with the concentrations
            involved, and where  chemical dosing is  to be  avoided for  some reason, then
            pretreatment of  the water is necessary to remove the scale-forming salts. This
            may be by  sodium cycle ion exchange softening, ion exchange dealkalisation,
            lime or lime-soda softening or even a nanofiltration process  if divalent ions are to
            be selectively removed. Some scalants are particularly recalcitrant. Dissolved (or
            “active”) silica,  evaluated  using  ASTM  D4993,  is  not  readily  removed  by
            pretreatment  and  there  are  proprietary  reagents  that  have  been  developed
            specifically to  inhibit  its precipitation.  However, modern  RO membranes  are
            reasonably tolerant, and raw environmental waters rarely require more than
            filtration and dosing as pretreatment for membrane permeation.

            Mircroorganisms and nutrients
            Bacteria are ubiquitous  and thrive in the high surface area environment of  a
            reverse  osmosis  membrane  element,  where  they  form  biofilms.  They  are
            naturally  transported  towards the membrane surface under the force of  the
            permeate flow, and are supplied with nutrients both from the feedwater and,
            under some circumstances, the pretreatment chemicals. Reports of  the latter, as
            discussed  by  Flemming  (1992), include  flocculants  (Graham  et  al.,  1989),
            phosphorus-containing  scale  inhibition  chemicals  (Ahmed  and  Alansari,
            1989), sodium  thiosulphate,  as  used  for  quenching  chlorine  (Winters  and
            Isquith, 1979), and even chlorine itself, which was found to degrade organic
            matter sufficiently for it to become biologically assimilable (Applegate et  al.,
            1986). Although  they  can  form  substantial  biofilm  layers  in  potable  and
            wastewater applications, bacteria require only an extremely low nutrient load to
            survive in biofilms and can exist even in ultrapure water systems, where their
            management  becomes  particularly  vexing,  Biofilm  formation  is  thus
            unavoidable in most membrane operations, and it is likely that all membrane
            fouling is associated with biofilm formation, although the biofilm itself is not
            necessarily onerous.
              Biofilm formation results from the rapid formation of an organic film, normally
            within the first few minutes of  operation, followed by  microbial adhesion and
            further entrapment of  dissolved and suspended solid matter which co-deposits
            with the microorganisms. The conditioning film can be existing organic matter
            from the feedwater, such as NOM, or microbial products, namely extracellular
            polymeric substances (EPS). The rate of  microbial deposition and the overall
            biofilm thickness depend on hydrodynamics, with biofilm thickness apparently
            decreasing  with  increasing  turbulence  (Ridgeway, 1988). Other  key  factors
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