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Abstract(s)
Natural surface waters in Algarve, Portugal, have important seasonal variations in natural organic matter (NOM)
content, that influences ultrafiltration (UF) performance. This paper addresses the evaluation of the pH adjustment
for seasonal control of UF fouling at a laboratory scale, using a plate and frame polysulphone membrane of 47 kDa
MWCO. Results of two types of natural water (clear water, 3-5 NTU, and turbid water, 33-34.6 NTU) and three
different water pH values (acid, neutral and basic) demonstrated that the pH adjustment could be used for seasonal
control of UF fouling: when the water has less NOM (in dry periods, clear water), the acid pH will improve the UF
performance, while during and after intense rainfall periods (turbid water with high NOM concentration) basic pH
will be advantageous, because it minimizes membrane fouling. This behaviour is explained for clear water in terms
of charge effects on membrane size. For turbid water, the electrostatic repulsion between membrane surface and
NOM and turbidity particles is reduced at pH 4.13 and protonation of the NOM functional groups decreases the
hydrodynamic radii of humic substances while increasing their hydrophobicity and their tendency to adsorb. Therefore,
a dense fouling layer develops and flux is lower at pH 4.13 than at pH 8.33. These results together with the observed
raw water feed concentrations decline and rejection decrease with WRR confirm the extensive adsorption on the
membrane enhanced by the moderate hardness cation of this water.
Description
Keywords
Ultrafiltration pH adjustment Fouling Clear water Turbid water