Membrane scaling and flux decline during fertiliser-drawn forward osmosis desalination of brackish groundwater

IWA publisher
Publication Type:
Journal Article
Water Research, 2014, 57 pp. 172 - 182
Issue Date:
Full metadata record
Files in This Item:
Filename Description Size
2013006592 am.pdfAccepted Manuscript335.13 kB
Adobe PDF
2013006592 figures.pdfAccepted Manuscript980.47 kB
Adobe PDF
2013006592 tables.pdfAccepted Manuscript212.75 kB
Adobe PDF
Fertiliser-drawn forward osmosis (FDFO) desalination has been recently studied as one feasible application of forward osmosis (FO) for irrigation. In this study, the potential of membrane scaling in the FDFO process has been investigated during the desalination of brackish groundwater (BGW). While most fertilisers containing monovalent ions did not result in any scaling when used as an FO draw solution (DS), diammonium phosphate (DAP or (NH4)2HPO4) resulted in significant scaling, which contributed to severe flux decline. Membrane autopsy using scanning electron microscopy (SEM), energy-dispersive x-ray spectroscopy (EDS), and x-ray diffraction (XRD) analysis indicated that the reverse diffusion of DAP from the DS to the feed solution was primarily responsible for scale formation during the FDFO process. Physical cleaning of the membrane with deionised water at varying crossflow velocities was employed to evaluate the reversibility of membrane scaling and the extent of flux recovery. For the membrane scaled using DAP as DS, 80–90% of the original flux was recovered when the crossflow velocity for physical cleaning was the same as the crossflow velocity during FDFO desalination. However, when a higher crossflow velocity or Reynolds number was used, the flux was recovered almost completely, irrespective of the DS concentration used. This study underscores the importance of selecting a suitable fertiliser for FDFO desalination of brackish groundwater to avoid membrane scaling and severe flux decline.
Please use this identifier to cite or link to this item: