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超顺磁性FeO@CA纳米颗粒及其作为正向渗透中汲取剂的潜力。

Superparamagnetic FeO@CA Nanoparticles and Their Potential as Draw Solution Agents in Forward Osmosis.

作者信息

Petrinic Irena, Stergar Janja, Bukšek Hermina, Drofenik Miha, Gyergyek Sašo, Hélix-Nielsen Claus, Ban Irena

机构信息

Faculty of Chemistry and Chemical Engineering, University of Maribor, Smetanova 17, SI-2000 Maribor, Slovenia.

Institute of Biomedical Sciences, Faculty of Medicine, University of Maribor, Taborska Ulica 8, SI-2000 Maribor, Slovenia.

出版信息

Nanomaterials (Basel). 2021 Nov 4;11(11):2965. doi: 10.3390/nano11112965.

Abstract

In this study, citric acid (CA)-coated magnetite FeO magnetic nanoparticles (FeO@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% / colloidal solutions of FeO@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. FeO@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 FeO@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 FeO@CA and 2.5 GMH for NaCl. These differences are ascribed to a more pronounced internal dilutive concentration polarization with FeO@CA as DS compared to NaCl as DS. This research demonstrated that the proposed FeO@CA can be used as a potential low reverse solute flux DS for FO processes.

摘要

在本研究中,通过共沉淀法合成了用于正向渗透(FO)中作为汲取溶液(DS)剂的柠檬酸(CA)包覆磁铁矿Fe₃O₄磁性纳米颗粒(Fe₃O₄@CA MNPs),并通过傅里叶变换红外光谱(FTIR)、热重分析(TGA)、动态光散射(DLS)、透射电子显微镜(TEM)和磁性测量对其进行了表征。制备的3.7% Fe₃O₄@CA MNPs胶体溶液在纯化后表现出18.7巴的渗透压且无聚集现象,并且具有44 emu/g的足够磁化强度,以便通过外部磁场实现DS再生。Fe₃O₄@CA悬浮液被用作FO错流过滤中的DS,以去离子(DI)水作为进料溶液(FS),FO膜的活性层面向FS,以NaCl作为参考DS。相同的跨膜总体渗透压分别导致NaCl和MNPs的水通量不同。因此,Fe₃O₄@CA的初始水通量为9.2 LMH,而以0.45 M NaCl作为DS时为14.1 LMH。Fe₃O₄@CA的反向溶质通量为0.08 GMH,NaCl为2.5 GMH。这些差异归因于与以NaCl作为DS相比,以Fe₃O₄@CA作为DS时更明显的内部稀释浓度极化。本研究表明,所提出的Fe₃O₄@CA可作为FO过程中潜在的低反向溶质通量DS。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/570e/8625881/1c26a5c0cc74/nanomaterials-11-02965-g001.jpg

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