Article ID Journal Published Year Pages File Type
6366578 Water Research 2014 10 Pages PDF
Abstract

•Synergistic fouling control via quorum quenching with physical cleaning was investigated.•Biofouling decreased significantly when quorum quenching was coupled with relaxation.•Quorum quenching enabled the stable operation of an MBR at the lower extreme in aeration.•Quorum quenching MBR minimized the energy consumption for filtration and aeration.•Quorum quenching activity had no influence on microbial flocs and treatment efficiency.

Membrane fouling and energy consumption are interconnected and considered as a bottleneck in membrane bioreactor (MBR) applications. This study investigated synergistic combinations of quorum quenching (QQ) and physical cleaning under different cleaning conditions and aeration intensities with respect to fouling control and energy saving. The MBR operated with periodic air backpulsing had a lower fouling tendency compared with the reactor operated with relaxation. Frequent physical cleanings mitigated the membrane fouling, but irreversible fouling inevitably occurred over time. A significant improvement in fouling control was accomplished when QQ was coupled with physical cleanings, particularly in the filtration/relaxation mode. The submerged QQ vessel helped operate the MBRs stably even at the lowest end of aeration intensity (51 s−1 in G value), without any significant loss of membrane permeability. The specific membrane filtration energy of the QQMBR remained low and independent of aeration intensities tested, whereas that of the normal MBR sharply increased with decreased aeration rates. The QQMBR with low aeration intensity (51 s−1) reduced approximately 27% of the specific aeration energy required for the MBR operated at high aeration intensity (103 s−1). QQ bacteria should hamper the formation of a biofilm on the membrane surface, but mixed liquor properties and treatment performances were not affected by the QQ activity.

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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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