1974
DOI: 10.1016/s0006-3495(74)85962-x
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Mechanism of Osmotic Flow in Porous Membranes

Abstract: A model for osmotic flow in porous membranes is developed from classical transport and thermodynamic relations. Mathematical expressions for the reflection coefficient as a function of solute dimension and shape, and more generally pore/bulk distribution coefficient, are derived for long cylindrical pores of circular cross section. For a rigid, spherical macromolecule the osmotic reflection coefficient equals (1 - Phi)(2), where Phi is the solute distribution coefficient; this result differs significantly from… Show more

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Cited by 176 publications
(173 citation statements)
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“…The predicted values of ω and σ s exhibited reasonable agreement with experimental observations (Sugihara-Seki 2006). Zhang, Curry & Weinbaum (2006) studied osmotic flow through the EGL model using a method developed by Anderson & Malone (1974) for osmotic flow in porous membranes. From considerations of classical transport and thermodynamics, Anderson & Malone (1974) showed that the presence of an exclusion region of solute near the pore walls produces a radial discontinuity in hydrostatic pressure and solute concentration, which generates the driving force for the osmotic flow.…”
Section: Introductionsupporting
confidence: 72%
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“…The predicted values of ω and σ s exhibited reasonable agreement with experimental observations (Sugihara-Seki 2006). Zhang, Curry & Weinbaum (2006) studied osmotic flow through the EGL model using a method developed by Anderson & Malone (1974) for osmotic flow in porous membranes. From considerations of classical transport and thermodynamics, Anderson & Malone (1974) showed that the presence of an exclusion region of solute near the pore walls produces a radial discontinuity in hydrostatic pressure and solute concentration, which generates the driving force for the osmotic flow.…”
Section: Introductionsupporting
confidence: 72%
“…Zhang, Curry & Weinbaum (2006) studied osmotic flow through the EGL model using a method developed by Anderson & Malone (1974) for osmotic flow in porous membranes. From considerations of classical transport and thermodynamics, Anderson & Malone (1974) showed that the presence of an exclusion region of solute near the pore walls produces a radial discontinuity in hydrostatic pressure and solute concentration, which generates the driving force for the osmotic flow. Zhang et al (2006) applied this formulation to the osmotic flow across the EGL model consisting of hexagonally arranged cylinders.…”
Section: Introductionmentioning
confidence: 99%
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“…The results of capillary E from Table 2 are compared, in Fig. 5, with theoretical curves consistent with the equations of Curry (1974) and Anderson & Malone (1974). A curve drawn for a pore radius of 1-1 or 1P2 nm fits the data for sodium chloride and urea but is inconsistent with the data for sucrose which is fitted by a theoretical curve for a pore radius of 2-4 nm.…”
Section: Discussionmentioning
confidence: 91%
“…to= PC (1-P)+a-P. Bean, 1972;Curry, 1974;Anderson & Malone, 1974 The data in Tables 1 and 2 Tables 1 and 2 These calculations suggest that about 10 % of the average filtration coefficient is represented by the exclusive water pathway (the cells), the remainder being accounted for by the shared pathway (the pore system). They also offer evidence for the hypothesis that variations in permeability properties between different capillaries arise from variations in the number rather than the dimensions of the 'pores'.…”
Section: Discussionmentioning
confidence: 99%