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Superparamagnetic Fe(3)O(4)@CA Nanoparticles and Their Potential as Draw Solution Agents in Forward Osmosis
In this study, citric acid (CA)-coated magnetite Fe(3)O(4) magnetic nanoparticles (Fe(3)O(4)@CA MNPs) for use as draw solution (DS) agents in forward osmosis (FO) were synthesized by co-precipitation and characterized by Fourier transform infrared spectroscopy (FTIR), thermogravimetric analysis (TGA...
Autores principales: | , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
MDPI
2021
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8625881/ https://www.ncbi.nlm.nih.gov/pubmed/34835728 http://dx.doi.org/10.3390/nano11112965 |
Sumario: | In this study, citric acid (CA)-coated magnetite Fe(3)O(4) magnetic nanoparticles (Fe(3)O(4)@CA MNPs) for use as draw solution (DS) agents in forward osmosis (FO) were synthesized by co-precipitation and characterized by Fourier transform infrared spectroscopy (FTIR), thermogravimetric analysis (TGA), dynamic light scattering (DLS), transmission electron microscopy (TEM) and magnetic measurements. Prepared 3.7% w/w colloidal solutions of Fe(3)O(4)@CA MNPs exhibited an osmotic pressure of 18.7 bar after purification without aggregation and a sufficient magnetization of 44 emu/g to allow DS regeneration by an external magnetic field. Fe(3)O(4)@CA suspensions were used as DS in FO cross-flow filtration with deionized (DI) water as FS and with the active layer of the FO membrane facing the FS and NaCl as a reference DS. The same transmembrane bulk osmotic pressure resulted in different water fluxes for NaCl and MNPs, respectively. Thus the initial water flux with Fe(3)O(4)@CA was 9.2 LMH whereas for 0.45 M NaCl as DS it was 14.1 LMH. The reverse solute flux was 0.08 GMH for Fe(3)O(4)@CA and 2.5 GMH for NaCl. These differences are ascribed to a more pronounced internal dilutive concentration polarization with Fe(3)O(4)@CA as DS compared to NaCl as DS. This research demonstrated that the proposed Fe(3)O(4)@CA can be used as a potential low reverse solute flux DS for FO processes. |
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