1998
DOI: 10.1016/s1383-5866(97)00065-8
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Modelling reverse osmosis by irreversible thermodynamics

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Cited by 36 publications
(19 citation statements)
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“…Furthermore, the three transport parameters of this model, which is known as the hydraulic water permeability constant , the reflection coefficient of the solute and the solute permeability coefficient are independent of each other and can simply represent the original phenomenological coefficients. They can be expressed as less independent of concentration (Van Gauwbergen and Baeyens, 1998;Jonsson, 1980;Kedem and Katchalsky, 1958;Soltanieh and Gill, 1981).…”
Section: The Kedem and Katchalsky Modelmentioning
confidence: 99%
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“…Furthermore, the three transport parameters of this model, which is known as the hydraulic water permeability constant , the reflection coefficient of the solute and the solute permeability coefficient are independent of each other and can simply represent the original phenomenological coefficients. They can be expressed as less independent of concentration (Van Gauwbergen and Baeyens, 1998;Jonsson, 1980;Kedem and Katchalsky, 1958;Soltanieh and Gill, 1981).…”
Section: The Kedem and Katchalsky Modelmentioning
confidence: 99%
“…Scenario B. Lastly, for desalination of the concentrated salt water, the procedure can be reversed by applying higher pressure than the solution osmotic pressure, which forces water to pass over the membrane towards the low concentration solution side accompanied by salt rejection, i.e. Scenario C. Usually, this process can happen under ambient temperature and without any phase change (Jain and Gupta, 2004;Van Gauwbergen and Baeyens, 1998). Reverse osmosis can therefore be counted as a prominent separation process in industrial applications due to its power to separate impurities effectively and commensurate with environmental demands.…”
Section: Introductionmentioning
confidence: 99%
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“…These models can be divided into three main groups: the irreversible thermodynamic models, where the local fluxes of solute and solvent are related to the chemical potential differences across the membrane [12][13][14]; the porous flow model, which assumes that water both diffuses and advects through the membrane pores [1,15,16]; and the solution-diffusion model, which assumes that both water and solutes diffuse between the interstitial spaces of the membrane polymer chains [11,17,18].…”
Section: Introductionmentioning
confidence: 99%
“…The validity of the Spiegler and Kedem model has been assessed later by Van Gauwbergen and Baeyens [16]. They concluded that this model can be utilized effectively for high volume flow rates and high concentration gradients.…”
mentioning
confidence: 99%