# Osm.Uncoupled2

Uncoupled, independent fluxes of water and of 2 solutes, across a membrane separating 2 stirred tanks equipped with columns above each to provide observable column heights as measures of their pressures.

Model number: 0274

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## Description

This model is the same as Osm.Uncoupled1.proj except for using column heights instead of elasticity. It also allows temperature changes. Uncoupled, independent fluxes of water and of 2 solutes, A and B, across a membrane separating 2 stirred tanks. Solute activities are assumed unity so concentrations = thermodynamic activity. The model describes a situation similar to that for the simplest expressions of Kedem and Katchalsky (1958) but omits all interactions between solutes and between water and any solute. One can think of the solutes passing though the membrane by passive permeation with permeability coefficients PermA and Perm B, and the water passing through aqueous pores with filtration coefficient or hydraulic conductivity, Lp. The aqueous pores do not permit solute passage. Lp is the same as the traditional filtration coefficient Kf. Lp translates to a conventional permeability for water filtration, Pf cm/s, Pf = Lp*RT/Vw where RT = 19.347*10^6 mmHg*cm^3*mol^(-1) at 37C, Vw is the partial molar volume of water, 18 ml/mol or the concentration of water in water is 55.55 M The driving forces are the pressure difference for water flux and the concentration for the solute fluxes. The pressure difference across the membrane is the hydrostatic pressure difference minus the osmotic pressure difference. The osmotic pressure is given by Van't Hoff's Eq: p_osm = a.C.RT, where p_osm is the osmotic pressure, mmHg, "a" is the activity coefficient, assumed in this model to equal unity, C is concentration, M, and RT is the Gas Constant times Temperature Kelvin. In this model the solute doesn't permeate the aqueous pore so there is no consideration of a reflection coefficient, or rather it is assumed to be unity. Thus solute concentration in the pore water is zero, and there is no solute advection.. The system is composed of two volumes of pressure-dependent size, yet stirred instantaneously continually. The slope of the pressure/volume relationship is linear and defined by the height of a column of fluid above the rigid chambers The narrow columns of fluid have heights h1 and h2. The pressure is rho*grav*h1 in chamber 1, where rho is fluid density, grav is acceleration due to gravity; The fluid in the columns is considered to be instantaneously mixed with that in the chamber from which it rises. Fluid or volume flux, Jv, from side 1 to side 2 causes a difference in the column heighta between the two sides by Base*(h2-h1) = Jv, where Base = area of the base of the column, and the pressure difference rises to rho* grav*(h2-h1) cm H2O, where rho is the fluid density. g/ml, in the narrow colums.. The model OsmUncoupledA.proj uses an analogous linear chamber elastance, Elast mmHg/ml, gives an equivalent measure for flexible chambers, assuming a linear relationship between the pressure change and the volume change. (1 mmHg = 13.59 cm H2O.) Notes: Situation 1:= Model default par. . PermA = 0, PermB > 0.1. See Notes. Situation 2 = Model par2 PermB > 0.

**Figure:**Top shows concentration of solute A and solute B as a function of time (A1, B1: conc in volume 1, A2, B2 conc in volume 2). Note change in volume 1 (V1) from initial volume of 1 ml. Y is volume 1 calculated from the membrane permeability while V1 is calculated from Hydraulic conductivity. Bottom figure shows hydrostatic pressure in V1 and volume 2 (V2) as a function of time. Permeability of A into V2 is one tenth the permeability of B and A2

_{init}and B1

_{init}are 0 mM for both figures.

## Equations

The equations for this model may be viewed by running the JSim model applet and clicking on the Source tab at the bottom left of JSim's Run Time graphical user interface. The equations are written in JSim's Mathematical Modeling Language (MML). See the Introduction to MML and the MML Reference Manual. Additional documentation for MML can be found by using the search option at the Physiome home page.

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## References

Katchalsky A and Curran PF. Nonequilibrium Thermodynamics in Biophysics. Cambridge, MA: Harvard University Press, 1965. Kedem O and Katchalsky A. Thermodynamic analysis of the permeability of biological membranes to non-electrolytes. Biochim Biophys Acta 27: 229-246, 1958. Stein WD. The Movement of Molecules across Cell Membranes. New York: Academic Press, 1967. Stein WD. Transport and Diffusion across Cell Membranes. Orlando, Florida: Academic Press Inc., 1986.

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## Model History

Get Model history in CVS.## Acknowledgements

Please cite **www.physiome.org** in any publication for which this software is used and send one reprint to the address given below:

The National Simulation Resource, Director J. B. Bassingthwaighte, Department of Bioengineering, University of Washington, Seattle WA 98195-5061.

[This page was last modified 29Jan20, 1:02 pm.]

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