TY - JOUR
T1 - Evaluating the performance of gravity-driven membrane filtration as desalination pretreatment of shale gas flowback and produced water
AU - Chang, Haiqing
AU - Liu, Baicang
AU - Wang, Huizhong
AU - Zhang, Si Yu
AU - Chen, Sheng
AU - Tiraferri, Alberto
AU - Tang, Yue Qin
N1 - Publisher Copyright:
© 2019 Elsevier B.V.
PY - 2019/10/1
Y1 - 2019/10/1
N2 - The shale gas extraction industry generates a large quantity of highly contaminated flowback and produced water (FPW), with great impacts on human health and the environment. In this study, gravity-driven membrane (GDM) filtration was evaluated over a 612-day period as a pre-treatment of FPW for its subsequent desalination. The various investigated GDM systems showed similar contaminant removals, and their steady-state fluxes (i.e., 0.65–0.82 L/(m2·h)) were not significantly correlated to membrane configurations or to the hydrostatic pressures. The flux decline was primarily due to a reversible resistance, which accounted for a large proportion (>89%) of the total hydraulic resistance. Compared to traditional ultrafiltration, the GDM pretreatment resulted in better desalination performance for the subsequent nanofiltration or reverse osmosis step, which were characterized by higher organic removal and generally higher permeate fluxes. More than 60 bacterial genera and 8 eukaryotic genera were detected in the shale gas FPW, with the kingdoms Alveolata and Stramenopiles (within the eukaryote domains) reported for the first time. The biofouling layer of GDMs had a lower bacterial diversity but a higher eukaryotic diversity than the FPW feed water. The eukaryotic community, including Alveolata, Fungi, Stramenopiles and Metazoa, played a major role in the flux behavior.
AB - The shale gas extraction industry generates a large quantity of highly contaminated flowback and produced water (FPW), with great impacts on human health and the environment. In this study, gravity-driven membrane (GDM) filtration was evaluated over a 612-day period as a pre-treatment of FPW for its subsequent desalination. The various investigated GDM systems showed similar contaminant removals, and their steady-state fluxes (i.e., 0.65–0.82 L/(m2·h)) were not significantly correlated to membrane configurations or to the hydrostatic pressures. The flux decline was primarily due to a reversible resistance, which accounted for a large proportion (>89%) of the total hydraulic resistance. Compared to traditional ultrafiltration, the GDM pretreatment resulted in better desalination performance for the subsequent nanofiltration or reverse osmosis step, which were characterized by higher organic removal and generally higher permeate fluxes. More than 60 bacterial genera and 8 eukaryotic genera were detected in the shale gas FPW, with the kingdoms Alveolata and Stramenopiles (within the eukaryote domains) reported for the first time. The biofouling layer of GDMs had a lower bacterial diversity but a higher eukaryotic diversity than the FPW feed water. The eukaryotic community, including Alveolata, Fungi, Stramenopiles and Metazoa, played a major role in the flux behavior.
KW - Desalination pretreatment
KW - Flowback and produced water (FPW)
KW - Gravity-driven membrane (GDM)
KW - Microbial community
KW - Shale gas
UR - https://www.scopus.com/pages/publications/85067251677
U2 - 10.1016/j.memsci.2019.117187
DO - 10.1016/j.memsci.2019.117187
M3 - 文章
AN - SCOPUS:85067251677
SN - 0376-7388
VL - 587
JO - Journal of Membrane Science
JF - Journal of Membrane Science
M1 - 117187
ER -