On the application of the Spiegler-Kedem model to forward osmosis

IF 2.35
Jun Jie Wu
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引用次数: 6

Abstract

In Forward Osmosis the diffusion of the solute is counter to that of the solvent i.e. there is so-called “reverse salt diffusion”. Furthermore, the ratio of the two fluxes is generally taken to be a constant because of the assumption of ideal semi-permeability. However with the Spiegler-Kedem (S-K) model there is an allowance for a minor deviation from ideal semi-permeability and the ratio of the solute flux and solvent flux is no longer constant. The theoretical variation of the solute flux with increasing draw solution concentration is illustrated for various degrees of deviation from ideal semi-permeability. A novel variant of the S-K model is also introduced and predictions compared with those obtained using the standard form. With the acceptance that the form of “breakthrough” involving co-current flow is impossible, a limitation is imposed upon the S-K model but even with this limitation the theoretically predicted variation of solvent flux with increasing draw concentration is for certain sets of parameters of an unexpected form for minor deviation from ideal semi-permeability. That intriguing counter-intuitive outcomes can result from application of the S-K model indicates a need to rethink its formulation of the equations and the expressions for the coefficients. This will have implications for forward osmosis and possibly reverse osmosis modelling.

Abstract Image

Spiegler-Kedem模型在正向渗透中的应用
在正向渗透中,溶质的扩散与溶剂的扩散相反,即所谓的“反向盐扩散”。此外,由于假设有理想的半磁导率,两种磁导率之比通常取为常数。然而,在Spiegler-Kedem (S-K)模型中,允许与理想半渗透性有轻微偏差,溶质通量和溶剂通量的比值不再是恒定的。在与理想半渗透率偏差程度不同的情况下,溶质通量随萃取溶液浓度的增加而发生理论变化。还介绍了S-K模型的一种新变体,并与使用标准形式获得的预测结果进行了比较。由于承认涉及共电流的“突破”形式是不可能的,因此对S-K模型施加了限制,但即使有这种限制,理论上预测的溶剂通量随抽提液浓度增加的变化,对于某些参数集来说,与理想半渗透性的偏差很小,其形式出乎意料。应用S-K模型可能会产生有趣的反直觉结果,这表明需要重新考虑其方程的公式和系数的表达式。这将对正向渗透和可能的反渗透建模产生影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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