Understanding the risk of scaling and fouling in hollow fiber forward osmosis membrane application

Citation data:

Process Safety and Environmental Protection, ISSN: 0957-5820, Vol: 104, Page: 452-464

Publication Year:
2016
Usage 99
Abstract Views 54
Full Text Views 28
Link-outs 11
Downloads 6
Citations 1
Citation Indexes 1
Repository URL:
http://hdl.handle.net/10754/614802
DOI:
10.1016/j.psep.2016.06.023
Author(s):
Tahir Majeed; Sherub Phuntsho; Sanghyun Jeong; Yanxia Zhao; Baoyu Gao; Ho Kyong Shon
Publisher(s):
Elsevier BV
Tags:
Environmental Science; Chemical Engineering; Engineering; Concentration polarization; Flux; Hollow fiber forward osmosis membrane; Inorganic scaling; Organic fouling
article description
Fouling studies of forward osmosis (FO) were mostly conducted based on fouling evaluation principals applied to pressure membrane processes such as reverse osmosis (RO)/nanofiltration (NF)/microfiltration (MF)/ultrafiltration (UF). For RO/NF/MF/UF processes, the single flux driving force (hydraulic pressure) remains constant, thus the fouling effect is easily evaluated by comparing flux data with the baseline. Whilst, the scenario of fouling effects for FO process is entirely different from RO/NF/MF/UF processes. Continuously changing driving force (osmotic pressure difference), the changes in concentration polarization associated with the varying draw solution/feed solution concentration and the fouling layer effects collectively influence the FO flux. Thus, usual comparison of the FO flux outcome with the baseline results cannot exactly indicate the real affect of membrane fouling, rather presents a misleading cumulative effect. This study compares the existing FO fouling technique with an alternate fouling evaluation approach using two FO set-ups. Scaling and fouling risk for hollow fiber FO was separately investigated using synthetic water samples and model organic foulants as alginate, humic acid and bovine serum albumin. Results indicated that FO flux declines up to 5% and 49% in active layer-feed solution and active layer-draw solution orientations respectively.