Enrichment of lithium from salt lake brine by forward osmosis

Forward osmosis (FO) is a concentration process based on the natural phenomena of osmosis. It is considered a breakthrough technology that can be potentially used for concentrating solutions and suspensions. The diluted nature of brine restricts the treatment technologies that can be applied. Then,...

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Main Authors: Jinli Li, Min Wang, Youjing Zhao, Hongjun Yang, Yuan Zhong
Format: Article
Language:English
Published: The Royal Society 2018-01-01
Series:Royal Society Open Science
Subjects:
Online Access:https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.180965
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author Jinli Li
Min Wang
Youjing Zhao
Hongjun Yang
Yuan Zhong
author_facet Jinli Li
Min Wang
Youjing Zhao
Hongjun Yang
Yuan Zhong
author_sort Jinli Li
collection DOAJ
description Forward osmosis (FO) is a concentration process based on the natural phenomena of osmosis. It is considered a breakthrough technology that can be potentially used for concentrating solutions and suspensions. The diluted nature of brine restricts the treatment technologies that can be applied. Then, brine concentration by FO could represent a new emerging technology enabling the application of a wider range of treatment alternatives. The performance of concentrated brine depending upon FO membranes was studied at normal temperature and pressure in this research. Cellulose triacetates on radio-frequency-weldable non-woven support (CTA-NW) and a thin-film composite with embedded polyester screen support (TFC-ES) were compared; and their orientations were considered. The brine was from Chaerhan Salt Lake after extracting potassium as the feed solution, NaCl solution or MgCl2 solution as the draw solution. The results indicated that CTA-NW exhibited better concentration performance than TFC-ES, while the water fluxes of the two membranes were exactly the opposite. In the case of CTA-NW in active layer facing feed solution orientation with MgCl2 as the draw solution, the concentration factor of Li+ was nearly 3.0. Quantitative structure–activity relationship of FO membranes and concentration characteristics was correlated, based on results of SEM, FTIR and contact angles studies. The concentration performance could be mainly attributed to the porosity and the thickness of FO membranes; while the water flux was dependent on the hydrophily of FO membrane surface.
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spelling doaj.art-d99323b3d7474ba8baf0785eaa323d632022-12-22T00:00:58ZengThe Royal SocietyRoyal Society Open Science2054-57032018-01-0151010.1098/rsos.180965180965Enrichment of lithium from salt lake brine by forward osmosisJinli LiMin WangYoujing ZhaoHongjun YangYuan ZhongForward osmosis (FO) is a concentration process based on the natural phenomena of osmosis. It is considered a breakthrough technology that can be potentially used for concentrating solutions and suspensions. The diluted nature of brine restricts the treatment technologies that can be applied. Then, brine concentration by FO could represent a new emerging technology enabling the application of a wider range of treatment alternatives. The performance of concentrated brine depending upon FO membranes was studied at normal temperature and pressure in this research. Cellulose triacetates on radio-frequency-weldable non-woven support (CTA-NW) and a thin-film composite with embedded polyester screen support (TFC-ES) were compared; and their orientations were considered. The brine was from Chaerhan Salt Lake after extracting potassium as the feed solution, NaCl solution or MgCl2 solution as the draw solution. The results indicated that CTA-NW exhibited better concentration performance than TFC-ES, while the water fluxes of the two membranes were exactly the opposite. In the case of CTA-NW in active layer facing feed solution orientation with MgCl2 as the draw solution, the concentration factor of Li+ was nearly 3.0. Quantitative structure–activity relationship of FO membranes and concentration characteristics was correlated, based on results of SEM, FTIR and contact angles studies. The concentration performance could be mainly attributed to the porosity and the thickness of FO membranes; while the water flux was dependent on the hydrophily of FO membrane surface.https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.180965forward osmosisenrichmentsalt lake brinelithium
spellingShingle Jinli Li
Min Wang
Youjing Zhao
Hongjun Yang
Yuan Zhong
Enrichment of lithium from salt lake brine by forward osmosis
Royal Society Open Science
forward osmosis
enrichment
salt lake brine
lithium
title Enrichment of lithium from salt lake brine by forward osmosis
title_full Enrichment of lithium from salt lake brine by forward osmosis
title_fullStr Enrichment of lithium from salt lake brine by forward osmosis
title_full_unstemmed Enrichment of lithium from salt lake brine by forward osmosis
title_short Enrichment of lithium from salt lake brine by forward osmosis
title_sort enrichment of lithium from salt lake brine by forward osmosis
topic forward osmosis
enrichment
salt lake brine
lithium
url https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.180965
work_keys_str_mv AT jinlili enrichmentoflithiumfromsaltlakebrinebyforwardosmosis
AT minwang enrichmentoflithiumfromsaltlakebrinebyforwardosmosis
AT youjingzhao enrichmentoflithiumfromsaltlakebrinebyforwardosmosis
AT hongjunyang enrichmentoflithiumfromsaltlakebrinebyforwardosmosis
AT yuanzhong enrichmentoflithiumfromsaltlakebrinebyforwardosmosis