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从水相到反渗透膜的聚酰胺活性层中分配碱金属盐和硼酸。

Partitioning of Alkali Metal Salts and Boric Acid from Aqueous Phase into the Polyamide Active Layers of Reverse Osmosis Membranes.

机构信息

Department of Environmental Sciences and Engineering, Gillings School of Global Public Health, University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599-7431, United States.

Department of Applied Physical Sciences, University of North Carolina at Chapel Hill , Chapel Hill, North Carolina 27599-3216, United States.

出版信息

Environ Sci Technol. 2017 Feb 21;51(4):2295-2303. doi: 10.1021/acs.est.6b04323. Epub 2017 Feb 1.

Abstract

The partition coefficient of solutes into the polyamide active layer of reverse osmosis (RO) membranes is one of the three membrane properties (together with solute diffusion coefficient and active layer thickness) that determine solute permeation. However, no well-established method exists to measure solute partition coefficients into polyamide active layers. Further, the few studies that measured partition coefficients for inorganic salts report values significantly higher than one (∼3-8), which is contrary to expectations from Donnan theory and the observed high rejection of salts. As such, we developed a benchtop method to determine solute partition coefficients into the polyamide active layers of RO membranes. The method uses a quartz crystal microbalance (QCM) to measure the change in the mass of the active layer caused by the uptake of the partitioned solutes. The method was evaluated using several inorganic salts (alkali metal salts of chloride) and a weak acid of common concern in water desalination (boric acid). All partition coefficients were found to be lower than 1, in general agreement with expectations from Donnan theory. Results reported in this study advance the fundamental understanding of contaminant transport through RO membranes, and can be used in future studies to decouple the contributions of contaminant partitioning and diffusion to contaminant permeation.

摘要

溶质在反渗透(RO)膜聚酰胺活性层中的分配系数是决定溶质渗透的三个膜性质之一(与溶质扩散系数和活性层厚度一起)。然而,目前还没有成熟的方法来测量溶质在聚酰胺活性层中的分配系数。此外,少数测量无机盐分配系数的研究报告的值明显高于 1(~3-8),这与 Donnan 理论的预期和对盐的高排斥率观察结果相悖。因此,我们开发了一种在台式条件下测定 RO 膜聚酰胺活性层中溶质分配系数的方法。该方法使用石英晶体微天平(QCM)测量由于被分配的溶质吸收而引起的活性层质量的变化。该方法使用几种无机盐(氯化物的碱金属盐)和一种在海水淡化中常见的弱酸(硼酸)进行了评估。总的来说,所有的分配系数都低于 1,这与 Donnan 理论的预期基本一致。本研究的结果推进了对 RO 膜中污染物传输的基本认识,并可用于未来的研究中,以分离污染物分配和扩散对污染物渗透的贡献。

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