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. 2022 Jan 17;24(1):138. doi: 10.3390/e24010138

Modelling of the Electrical Membrane Potential for Concentration Polarization Conditions

Kornelia M Batko 1,*, Izabella Ślęzak-Prochazka 2, Andrzej Ślęzak 3, Wioletta M Bajdur 4,*, Radomir Ščurek 5
Editor: Luis L Bonilla
PMCID: PMC8774907  PMID: 35052163

Abstract

Based on Kedem–Katchalsky formalism, the model equation of the membrane potential (Δψs) generated in a membrane system was derived for the conditions of concentration polarization. In this system, a horizontally oriented electro-neutral biomembrane separates solutions of the same electrolytes at different concentrations. The consequence of concentration polarization is the creation, on both sides of the membrane, of concentration boundary layers. The basic equation of this model includes the unknown ratio of solution concentrations (Ci/Ce) at the membrane/concentration boundary layers. We present the calculation procedure (Ci/Ce) based on novel equations derived in the paper containing the transport parameters of the membrane (Lp, σ, and ω), solutions (ρ, ν), concentration boundary layer thicknesses (δl, δh), concentration Raileigh number (RC), concentration polarization factor (ζs), volume flux (Jv), mechanical pressure difference (ΔP), and ratio of known solution concentrations (Ch/Cl). From the resulting equation, Δψs was calculated for various combinations of the solution concentration ratio (Ch/Cl), the Rayleigh concentration number (RC), the concentration polarization coefficient (ζs), and the hydrostatic pressure difference (ΔP). Calculations were performed for a case where an aqueous NaCl solution with a fixed concentration of 1 mol m−3 (Cl) was on one side of the membrane and on the other side an aqueous NaCl solution with a concentration between 1 and 15 mol m−3 (Ch). It is shown that (Δψs) depends on the value of one of the factors (i.e., ΔP, Ch/Cl, RC and ζs) at a fixed value of the other three.

Keywords: membrane transport, membrane potential, concentration polarization, Kedem–Katchalsky equations, polymeric membrane, concentration Rayleigh number

1. Introduction

Both biological and synthetic membranes are sensitive to changes in the physicochemical properties of the environment [1,2,3,4]. Therefore, membrane transport of its solution components can be governed by local fields (such as concentration, temperature, electric potential, or pressure fields) and global fields (such as gravitational or electromagnetic fields) [1,5]. Under real-world conditions (no external mixing of membrane-separated solutions), concentration polarization plays an important role, involving the formation of concentration boundary layers in solution regions immediately adjacent to the membrane [6,7,8,9]. In electrochemistry, the term concentration polarization is used to describe a set of phenomena accompanying the formation of concentration gradients in electrolyte solutions adjacent to a semipermeable solid/liquid interfacial surface during the flow of an electric current and the appearance of a boundary current [10,11,12,13,14].

The term concentration polarization is also used to describe the phenomena accompanying the formation of concentration boundary layers (CBLs) in both electrolyte and non-electrolyte solutions [3,4,7,8,9,15,16,17]. The effect of concentration polarization is to reduce membrane transport [7,8,9,16,17]. These layers are formed on both sides of electrically neutral selective membranes oriented horizontally, and the concentration (density) gradients in them are sensitive to the gravitational field [1,7,15,16,17]. The effect of this field is natural convection, which modifies the concentration fields in the membrane regions [7,15]. Its consequence is a partial restoration of concentration gradients across the membrane and increased membrane transport [3,16,17]. One of the effects of changing the concentration field are gravitational effects in passive osmotic and diffusive transport [1,18,19] and the gravielectric effect [16]. Theoretical modeling of the concentration polarization phenomenon is usually based on the Kedem–Katchalsky and Nernst-Planck equations [14,20,21,22,23].

The gravielectric effect in an electrochemical cell is a consequence of diffusion, concentration polarization, and the action of gravity [16]. In this study, we used a system in which two solutions with different NaCl or KCl solutions were separated by a synthetic membrane. The solutions were connected to Ag/AgCl electrodes using original bridges [16] or immersed directly into the solutions [24,25,26]. Furthermore, mathematical models of this effect were developed using the Kedem–Katchalsky equations [24,25,26]. In the first case, the dependence of the measured difference of electric potentials on the distance of electrodes from the membrane was eliminated. In the second case, the dependence was obvious. These studies showed, among other things, that the reversal of the mechanical pressure gradient with respect to the concentration (density) gradient has a significant effect on the value of the membrane potential difference [26].

The decrease in fluxes and thermodynamic forces due to the concentration polarization commonly found in nature, contributes to slowing down the source of entropy. This is an anti-entropic process.

The aim of this paper was to develop model equations of the membrane potential difference (Δψs) for concentration polarization conditions based on Kedem–Katchalsky formalism. The basic equation of this model includes the unknown ratio of solution concentrations (Ci/Ce) at the membrane/concentration boundary layers. We present the calculation procedure (Ci/Ce) based on the novel equations derived in the paper containing the transport parameters of the membrane (Lp, σ, and ω), solutions (ρ, ν), concentration boundary layer thicknesses (δl, δh), concentration Raileigh number (RC), concentration polarization factor (ζs), volume flux (Jv), mechanical pressure difference (ΔP), and ratio of known solution concentrations (Ch/Cl). We used the obtained equation to calculate the characteristics Δψs=f(Ch/Cl), Δψs=fΔP, and Δψs=fRC. The characteristics Δψs=f(Ch/Cl) were calculated for different fixed values of ΔP, ζs, and RC. In contrast, the characteristics Δψs=fRC were calculated for different fixed values of ΔP, ζs, and (Ch/Cl), while the characteristics Δψs=fΔP were calculated for different fixed values of RC, ζs, and (Ch/Cl).

2. Materials and Mathematical Modeling

2.1. Membrane System

In this paper, the considerations were based on the membrane system schematically shown in Figure 1. In this system, two mechanically unstirred solutions of the same electrolyte were separated by a hemodialyzer biomembrane (i.e., Nephrophan) made of regenerated cellulose (M), oriented in the horizontal plane. Nephrophan (Orwo VEB Filmfabrik, Wolfen, Germany) is a microporous, highly hydrophilic, isotropic, homogeneous, symmetric, and electro-neutral membrane [27]. The transport properties of a δ thick membrane are determined by the following coefficients: hydraulic conductivity (Lp), reflection (σ), solute permeability (ω), electrical conductivity (κ), and transfer number (τ). At the initial time (t=0), the concentrations of these solutions were Ch and Cl (Ch > Cl). For t>0, water and solute diffusing through the membrane form on both sides of the membrane concentration boundary layers lh and ll with thicknesses of δh and δl, respectively. These layers can be perceived as membranes with diffusion coefficients Dh and Dl, reflection coefficients σh = σl = 0, transfer numbers τh and τl, and electrical conductivity coefficients κh and κl. The membrane together with the concentration boundary layers form the lh/M/ll complex. The transport properties of this complex are determined by the following coefficients: reflection (σ), solute permeability (ω), electrical conductivity (κ), and the transfer number (τj). The process of creating concentration boundary layers causes the concentration of the solution on the M/ll border to increase from Cl to Ce (Ce > Cl) and on the lh/M border to decrease from Ch to Ci (Ch > Ci).

Figure 1.

Figure 1

Membrane system (M—membrane; ll and lh—concentration boundary layers; Cl, Ce, Ci, and Ch—solution concentrations; Jv—volume flux; Jl, Jm, and Jh—solute fluxes; Il, Is, Im, and Ih—ionic currents; δl and δh—concentration boundary layers thicknesses; δm—membrane thickness.

The solute flux and ionic current through the ll layer are denoted by Jl and Il, respectively, through the M membrane by Jm and Im and through the lh layer by Jh and Ih. The volume, solute, and ion current fluxes through the lh/M/ll complex are denoted by Jv, Js, and Is, respectively. It is worth noting that it is possible to select the concentrations of the solutions in such a way that the concentration gradient and the density gradient are parallel or antiparallel to the gravity vector. Interferometric studies have shown that the formation of the layers lh and ll ends when natural convection occurs, and the membrane system reaches a steady state.

2.2. Equations for Fluxes and Concentration Polarization Conditions

For electrically neutral membranes, the results of membrane transport studies of electrolyte solutions can be interpreted based on Kedem–Katchalsky formalism [22,23,27]. In this formalism, the membrane is treated as a “black box”, and its properties are described by the relationship between the thermodynamic forces (which cause the permeation of solution components through the membrane) and the thermodynamic fluxes that result from these forces. For binary electrolyte solutions, the Kedem–Katchalsky equations are of the form [23,24]:

Jv=LpγσRTChCl + PEκImΔP (1)
Js=ωRTChCl + C¯1σJv+τjzjϰjFIm (2)
Im=PEJv+τjκzjϰjFΔμm+κE (3)
Δψm=ImκRTFΔτlnChCl (4)

where Jv—volume flux; Js—solute flux; Im—ion current; Lp, σ, and PE, and  ω—coefficients of hydraulic conductivity, reflection, electroosmotic permeability, and solute permeability, respectively; γ—van’t Hoff coefficient; RT—the product of the gas constant and the absolute temperature; Ch and Cl—solution concentrations (Ch > Cl); κ—electrical conductivity; τj, zj, and ϰj—transfer number, valence, and ion number, respectively; C¯=ChCllnChCl11  0.5 Ch+Cl—average concentration of the solution (C¯ 0.5 Ch+Cl  is only valid when the Ch and Cl values are not very different); Δψm—potential difference measured with two reversible electrodes; Δτ=τaτc, τa, and τc—transfer numbers of anions (a) and cations (c) in the membrane, respectively; τa+τc=1.

Equations (1)–(4) are correct for sufficiently dilute and homogeneous solutions [23,24]. As already mentioned, when the solutions are not mechanically mixed, CBLs form on both sides of the membrane [4,6,15,16,17,18]. These layers can be thought of as pseudomembranes connected in series with the material membrane. The consequence of the formation of these layers is a decrease in membrane transport, which is manifested by a decrease in volume flux, solute flux, membrane potential, and ionic current [1,4,6,15,16,17].

Based on the classical [22,23] and modified [28,29] form of Equation (2) and the amperostatic condition Il=Ih=Is=0, we can write:

Jl=DlδlCeCl + 12Ce+ClJv (5)
Js=ωζsRTChCl + 12Ch+Cl1σJv (6)
Jh=DhδhChCi + 12Ch+CiJv (7)
Jv=LpΔPLpζsσRTChCl (8)

where ζs—the concentration polarization coefficient, Jvp=LpΔP—the hydraulic volume flux, and Jvo=LpζsσRTChCl—osmotic volume flux.

In the steady state, the condition is fulfilled by:

Jl=Jh=Js (9)

Equations (5)–(7) and (9) are used to calculate the solution stabilities at the boundaries M/ll (Ce) and lh/M (Ci), assuming that σh = σl = 0:

Ce=DlCl+δlζsωRTChCl + 12JvCh1ζsσ)ClζsσDl+12Jvδl1 (10)
Ci=δhζsωRTChCl + 12JvCl1ζsσ)ChζsσDhCh12JvδhDh1 (11)

For isoosmotic conditions (Jv=0, ζsσRTChCl = ΔP), Equations (10) and (11) simplify to the form:

Ce=Cl+δlζsωRTChClDl (12)
Ci=ChδhζsωRTChClDh (13)

For Jvo = 0, Jv=Jvp=LpΔP and therefore Equations (10) and (11) will take the form

Ce=DlCl+δlζsωRTChCl + 12LpΔPCh1ζσ)ClζσDl+12LpΔPδl1 (14)
Ci=δhζsωRTChCl + 12LpΔPCl1ζσ)ChζσDhCh12LpΔPδhDh1 (15)

2.3. Equations for the Concentration Rayleigh Number

The process of creating concentration boundary layers is controlled by the Rayleigh concentration number (RC) [15]. For the membrane system in question, containing concentration boundary layers ll and lh with thicknesses δl and δh, the expressions for the concentration Rayleigh numbers take the forms:

RCl=gαlβl(δl)4Dlνl1 (16)
RCh=gαhβh(δh)4Dhνh1 (17)

where g is acceleration due to the fact of gravity, ρl and ρh are the mass density of solutions (ρh > ρl), νl  and νh are the kinematic viscosity of the solutions (νh > νl), δl and δh are the layer ll and lh thicknesses, Dl and Dh are the diffusion coefficients in the layers ll and lh, νl and νh are the kinematic viscosity coefficients (νh > νl), αl=ρl/Cl/ρl and αh=ρh/Ch/ρh represent the change in density of a solution due to the change in the solution concentration, and βl=Cl/z and βh=Ch/z represent the density gradient along the vertical axis. When the density of the solution above the membrane is greater than the density of the solution below the membrane, convective instabilities appear in the membrane regions when the values of RCl and RCh exceed their critical values. For membrane transport processes, the critical value of the RC = 1100.6 [30]. In the linear case, that is, when αlβl = ρeρl(ρlδl)1 and αhβh = ρhρi(ρhδh)1, Equations (16) and (17) can be written in the form [31]:

RCl=gρeρl(δl)3ρlDlνl1 (18)
RCh=gρhρi(δh)3(ρhDhνh)1 (19)

where ρe and ρi are the solution densities at the boundaries of M/ll and M/lh (ρi > ρe), and ρl and ρh are the solution densities beyond ll and lh (ρh > ρl).

In order to estimate ρeρl and ρhρi at steady state, we carried out the following considerations. Assuming that for small concentrations of solutions the density–concentration dependence is linear, we can write:

ρ=ρo+ρCC (20)

where ρ and ρo are the densities of the solution and solvent, respectively, and (ρ/C) = const. For binary solutions, the above equation takes the form:

ρeρl=ρCCeCl (21)
ρhρi=ρCChCi (22)

Considering Equations (10) and (11) in Equations (21) and (22) and then in Equations (18) and (19), we obtain concentration Rayleigh numbers (RCl, RCh) for isothermal processes of passive membrane transport

RCl=gρCδl4ζsωClRTChCl1+12JvCh1ζsσ  Cl1+ζsσρlDlνlDl+12Jvδl1 (23)
RCh=gρCδh4ζsωChRT1ClCh12JvCh1+ζsσ  Cl1ζsσρhDhνhDh12Jvδh1 (24)

For isoosmotic conditions (Jv=0, ζsσRTChCl = ΔP), Equations (23) and (24) simplify to the form [15]:

RCl=gRTωClζsρCChCl1δl4Dl2νlρl1 (25)
RCh=gRTωChζsρC1ClChδh4Dh2νhρh1 (26)

For Jvo = 0 and Jv=Jvp=LpΔP; therefore, Equations (23) and (24) take the form:

RCl=gρCδl4ζsωClRTChCl1+12LpΔPCh1ζsσ  Cl1+ζsσρlDlνlDl+12LpΔPδl1 (27)
RCh=gρCδh4ζsωChRT1ClCh12LpΔPCh1+ζsσ  Cl1ζsσρhDhνhDh12LpΔPδh1 (28)

2.4. Membrane Potential Equations for Concentration Polarization Conditions

Using the procedure presented in the previous paper [4], for the situation presented in Figure 1, Equation (4) can be written in the following forms:

Δψl=IlκlRTFτlaτlclnCeCl (29)
Δψm=ImκRTFτaτclnCiCe (30)
Δψh=IhκhRTFτhaτhclnChCi (31)

In the steady state, the following conditions are fulfilled:

Δψs=Δψl+Δψm+Δψh (32)
Il=Im=Ih=Is=const (33)

Based on Equations (29) and (30) and the condition τl = τh = τ0, we obtain:

Δψs=IsκsRTFΔτ0lnChCl+ΔτΔτ0lnCiCe (34)

where Δτ0=τ0aτ0c, Δτ=τaτc, and κs=κlκκhκκh+κlκh+κlκ1.

In order to represent the Ci/Ce ratio in a form suitable for calculation, we form the quotient of the left and right sides of Equations (10) and (11). After performing the appropriate algebraic transformations, we obtain:

CiCe=ChClα0+α1Jv+α2Jv2β0+β1Jv+β2Jv2 (35)

where

α0=DlDhδhζsωRT1ClCh
α1=12δlDhδhζsωRT1ClChDlδhClCh1ζsσ+ζsσ
α2=14δlδhζsσClCh1ζsσ
β0=DhDlδlζsωRTChCl1
β1=12DhδlChCl1ζsσ+ζsσ  δhDl+δhζsωRTChCl1
β2=14δlδhζsσ  ChCl1ζsσ

For the denominator of this equation to be greater than zero, the following condition must be fulfilled: β0+β1Jv+β2Jv2 > 0. For Jv = 0, Equation (35) takes the form:

CiCe=ChClDlDhδhζsωRT1ClChDhDlδlζsωRTChCl1 (36)

For the denominator of this equation to be greater than zero, the following condition must be fulfilled:

ChClDlδlζsωT>1

If we neglect the osmotic effects (Jvo=LpζsσRTChCl << Jv=LpΔP), we obtain from Equation (35):

CiCe=ChClα0+γ1ΔP+γ2ΔP2β0+ε1ΔP+ε2ΔP2 (37)
γ1=12LpδlDhδhζsωRT1ClCh  DlδhClCh1ζsσ+ζsσ
γ2=14Lp2δlδhζsσClCh1ζsσ
ε1=12LpDhδlChCl1ζsσ+ζsσ  δhDl+δhζsωRTChCl1
ε2=14Lp2δlδhζsσChCl1ζsσ

2.5. Equations for the Thickness of the Concentration Boundary Layers

The equations for δl and δh can be obtained by transforming Equations (27) and (28) into the forms:

a1δl4a2δla3=0 (38)
b1δh4+b2δhb3=0 (39)

where a1=gρCζsωClRTChCl1 + 12JvCh1ζsσCl1+ζsσ, a2=12JvRClDlρlνl, a3=RClDl2ρlνl, b1=gρCζsωChRT1ClCh12JvCh1+ζsσ  Cl1ζsσ, b2=12JvRChDhρlνh, and b3=RChDh2ρhνh. If we neglect the osmotic effects (Jvo << Jv, LpζsσRTChCl << LpΔP), considering the equation Jv = LpΔP in Equations (38) and (39) we obtain:

e1δl4+e2δle3=0 (40)
f1δh4f2δhf3=0 (41)

where e1=gρCζsωClRTChCl1+12LpΔPCh1ζsσ  Cl1+ζsσ, e2=12LpΔPRClDlρlνl, e3=RClDl2ρlνl, f1=gρCζsωChRT1ClCh12LpΔPCh1+ζsσ  Cl1ζsσ, f2=12LpΔPRChDhρhνh, and f3=RChDh2ρhνh. To obtain the equations describing δl and δh for isoosmotic conditions (Jv=0, ζsσRTChCl = ΔP), it is sufficient to transform Equations (25) and (26) into the forms:

δl=RClνlρlDl2gRTωζsClρCChCl1114 (42)
δh=RChνhρhDh2gRTωζsChρC1ClCh114 (43)

Expressions (35), (36) and (38)–(41) constitute the equations describing the membrane potential generated in a membrane system containing an isotropic, symmetric, and electron neutral polymer membrane for the conditions of concentration polarization.

3. Results of Calculations and Discussion

Calculations of the membrane potential (Δψs) were made based on Equations (34), (35), (40) and (41) for a membrane system characterized as follows. The membrane was positioned on a horizontal plane and separated by two aqueous NaCl solutions with concentrations of Cl = 1 mol m−3 and Ch = nΔC, where ΔC = 1.25 mol m−3 and n = 1, 2, …, 8. For the density (ρh, ρl) and kinematic viscosity (νh, νl) the following relationships were satisfied: ρh = ρl + nΔρ and νh = νl + nΔν, where ρl = 997.4 kg m−3, Δρ = 0.03.4 kg m−3, νl = 997.7 × 10−9 m2s−1, Δν = −0.03 × 10−9 m2s−1, and n = 1, 2, …, 8. The concentration gradient density calculated on the basis of the above data was (ρ/C) = 0.026 kg mol−1. It was assumed that the diffusion coefficient of NaCl in the range of tested solution concentrations was constant (Dl = Dh=D) and, therefore, the table value D = 1.57 × 10−9 m2s−1 was used for the calculations. For the calculations, the transport parameters of the Nephrophan membranes used as an element of the hemodialyzer were used [32] for NaCl with the following values: Lp = 5 × 10−12 m3N−1s−1, σ = 0.06, ω = 1.43 × 10−9 mol N−1s−1, Δτ = 0.39, and Δτ0 = 0.216 [16]. The values of the ζ coefficient assume values in the range 0.01ζs0.5. Moreover, the constants R = 8.31 J mol−1K−1, g = 9.81 m s−1, and F = 9.65 × 105 C mol−1 were used for the calculations. The calculations were made using the MATLAB software package. All calculations were made for isothermal conditions (T = 295 K). The characteristics Δψs=f(Ch/Cl) for different set values of ΔP, ζs, and RC are shown in Figure 2. The characteristics Δψs=fRC for different set values of ΔP, ζs, and (Ch/Cl) are shown in Figure 3. Figure 4 shows the characteristics of Δψs=fΔP for different fixed values of RC, ζs, and (Ch/Cl).

Figure 2.

Figure 2

The families of the characteristics Δψs=f(Ch/Cl) for different fixed values of ΔP, ζs, and RC. (a) characteristics of Δψs=f(Ch/Cl) for the same ΔP = −100 kPa value and ζs = 0.22 of different set values of RC. (b) characteristics of Δψs=f(Ch/Cl) for the same ΔP = +100 kPa value and ζs = 0.049 of different set values of RC. (c) characteristics of Δψs=f(Ch/Cl) for the same ΔP = −100 kPa value and ζs = 0.049 of different set values of RC; characteristics of Δψs=f(Ch/Cl) for the same ΔP = −100 kPa value and ζs = 0.07 of different set values of RC (d) characteristics of Δψs=f(Ch/Cl) for the same ΔP = −100 kPa value and ζs = 0.3 of different set values of RC; characteristics of Δψs=f(Ch/Cl) for the same ΔP = +100 kPa value and ζs = 0.22 of different set values of RC.

Figure 3.

Figure 3

The families of the characteristics Δψs=fΔP for different fixed values of Ch/Cl, ζs, and RC. (a) characteristics of Δψs=fΔP for the same RC = 244.5968 value and ζs = 0.049 of different set values of  Ch/Cl). (b) characteristics of Δψs=fΔP for the same RC = 244.5968 value and ζs = 0.049 of different set values of  Ch/Cl = 20. (c) characteristics of Δψs=fΔP for the same RC = 4423.6023 value and ζs = 0.03 of different set values of  Ch/Cl = 3.75. (d) characteristics of Δψs=fΔP for the same value ζs = 0.3 and Ch/Cl = 20 of different set values of  RC.

Figure 4.

Figure 4

The families of the characteristics Δψs=fRC for different fixed values of ΔP, ζs and Ch/Cl. (a) characteristics of Δψs=fRC for the same ΔP = −100 kPa value and ζs = 0.049 of different set values of Ch/Cl. (b) characteristics of Δψs=fRC for the same ΔP = +100 kPa value and Ch/Cl = 20 of different set values of ζs. (c) characteristics of Δψs=fRC for the same ΔP = −100 kPa value and Ch/Cl = 20 of different set values of ζs. (d) characteristics of (RC)lim=fζs for the different set values of ΔP.

3.1. Concentration Dependence of Membrane Potential

Figure 2a shows the characteristics of Δψs=f(Ch/Cl) for the same ΔP value and ζs of different set values of RC. This figure shows that the curves (1)–(5) start from a point with the coordinates Ch/Cl = 1 and Δψs = 0. Curve (1) shows that Δψs is positive over the entire range of the Ch/Cl values. Curve (2) shows that Δψs fulfilled the following conditions: Ch/Cl = 3.85, Δψs = 0; Ch/Cl < 3.85, Δψs < 0. For curves (3)–(5), Δψs < 0.

Figure 2b shows that the change of the sign of ΔP and the value of ζs and the change of the set values of RC caused a change in the nature of the curves, illustrating the dependence Δψs=f(Ch/Cl). This figure shows that the curves (1)–(5) started from different positive values of Δψs. The curves (1)–(3) show that Δψs was positive for the entire range of Ch/Cl values. The course of the curves (4) and (5) shows that Δψs fulfilled the following conditions: Ch/Cl ≈ 2.65, Δψs = 0; Ch/Cl < 2.65, Δψs < 0; Ch/Cl > 2.65, Δψs > 0. For curves (3)–(5), Δψs < 0.

Figure 2c shows two families of the characteristics Δψs=f(Ch/Cl). The first is illustrated by the curves (1)–(3), the second by the curves (4)–(6). The course of the curves (1)–(3) shows that with the increase in the value of Ch/Cl, the value of Δψs increased nonlinearly. The shape of the curves for the same Ch/Cl values depended on the RC value. Curve (1), in the tested interval Ch/Cl, was a characteristic of the saturation type. The change in the type of the mentioned characteristic from (1) to (2) and (3), controlled by the RC value, occurred for Ch/Cl ≥ 18.

The average slope of the characteristics Δψs=f(Ch/Cl)ΔP, ζs, RC can be calculated from the expression αs=Δψs/Ch/ClΔP,ζsRc. For 1 ≤ Ch/Cl < 18, the value of αs was constant and approximately αs = 1.65 mV (for curve (1)), αs = 3.5 mV (for curve (4)), and αs = 4 mV (for curve (3)). For Ch/Cl ≥ 18, the value of αs was constant and amounted to approximately αs = 2 mV (for curve 1), αs = 20 mV (for curve (2)), and αs = 85 mV (for curve (3)). This means that for RC > 200, there was an almost abrupt increase in the value of αs. The comparison of curves (1) and 3 for Ch/Cl > 18 shows that the value of the αs coefficient for curve (3) was 42.5 times greater than the value of the αs coefficient for curve (1). In turn, curves (4)–(6) show that that with the increase in the value of Δψs, Ch/Cl decreased nonlinearly, and for Ch/Cl = 3.48, it reached the minimum value of Δψs = 0.225 V. For Ch/Cl > 3.48, Δψs increased. Similarly, as in the previous case, it was possible to calculate the average slope of the characteristics Δψs=f(Ch/Cl)ΔP, ζs, RC. For 1 ≤ Ch/Cl > 3.48, the value of αs for curves (4)–(6) was constant and amounted to approximately αs = 1.11 mV. For Ch/Cl < 3.48, the value of αs was constant and approximately αs = −167 mV (for curve (3)), αs = −44 mV (for curve 2), and αs = −7.1 mV (for curve (1)). The comparison of curves (1) and (3) for Ch/Cl < 3.48 shows that the value of the αs coefficient for curve (3) was 23.5 times greater than the value of the αs coefficient for curve (1).

Figure 2d shows two groups of characteristics for +ΔP (curves (1a)–(5a)) and –ΔP (curves (1b)–(5b)). These characteristics differed from the characteristics shown in Figure 2a–c because curves (1a),(2a), (3a), (4a), (1b), (2b), (3b) and (4b), illustrating the dependencies Δψs=f(Ch/Cl), had minima Δψs, for which the value decreased as the RC value increased. The curves (5a) and (5b) did not have minima, because for RC = 4423.6023 (curves (5b)) and RC = 0.6023 (curves (5a)). This is because Equation (31) has no solutions in the set of real numbers.

3.2. Hydrostatic Pressure Dependencies of Membrane Potential

Figure 3 shows the characteristics Δψs=f±ΔP calculated for the set values of ζs = 0.049, RC = 244.5968, Ch/Cl = 8.75 (curves (1a,b) and (3a,b) in Figure 3a), and Ch/Cl  = 15 (curves (2a,b) and 4a,b in Figure 3a)). These figures show that in the tested interval (i.e., ζs, RC and Ch/Cl), Equation (31) had two solutions. Let us consider the curves (2a,b) shown in Figure 3a, illustrating two solutions for Equation (31) in the set of real numbers. The coordinates of the point determining the minimum of curve (1a) are as follows: Δψs = 0.103 V and ΔP = 0.478 MPa. In turn, the coordinates of the point determining the maximum of curve (1b) are as follows: Δψs = −0.064 V and ΔP = 1.275 MPa. The coordinates of the point determining the minimum of the curve (2a) are Δψs = 0.1 V and ΔP = 0.5 MPa. In turn, the coordinates of the point determining the maximum of curve 2b are as follows: Δψs = −0.086 V and ΔP = 1.55 MPa. This means that the change from Ch/Cl = 8.75 to Ch/Cl = 15 shifts curve (2a) in relation to curve (1a) towards higher values of ΔP and lower values of Δψs. In turn, the change from Ch/Cl = 8.75 to Ch/Cl = 15 shifts curve (2b) in relation to curve (1b) towards lower values of ΔP and higher values of Δψs. Moreover, curves (1a) and (2a) are symmetrical to curves (3a) and (4a) as are curves (1b) and (2b) to curves (3b) and (4b).

Curve (1a), as depicted in Figure 3b, shows that the range of changes Δψs falls on a relatively narrow range ΔP that meets the condition −78 ≤ ΔP ≤ 700 kPa. In the case of the curve (1b) presented in this figure, it follows that the range of changes Δψs is within the wide range ΔP, which satisfies the condition −780 kPa ≤ ΔP ≤ 11.7 MPa. Curve (1a) had Δψs had a minimum at the coordinate Δψs = −0.012 V and ΔP = 0.545 MPa. In turn, curve (1b) had a maximum at the coordinates Δψs = −0.034 V and ΔP = 1.052 MPa.

Figure 3c shows the characteristics Δψs=fΔP calculated for the set values ζs = 0.3, RC = 4423.6023, and Ch/Cl = 3.75 (curves (1a,b) in Figure 3c). This figure shows that in the tested interval (i.e., ζs, RC and Ch/Cl), Equation (31) had two solutions. The first is illustrated by curve (1a), and the second is shown by curve (1b). The curves presented in Figure 3c show that the curve (1a) was asymmetric in relation to curve (1b). Curve (1a) presented in Figure 3c shows that the range of changes Δψs was within the ΔP interval, which satisfies the condition −300 ≤ ΔP ≤ −170 kPa. In this range ΔP, the value of Δψs decreased nonlinearly from Δψs = 0.05 V to Δψs = −0.3 V. In turn, in the case of curve (1b), the range of changes Δψs was within the range ΔP, satisfying the condition −100 ≤ ΔP ≤ +300 kPa. In this case, the value of Δψs decreases nonlinearly from Δψs = −0.3 to Δψs = +0.107 V.

Curve 1a, as depicted in Figure 3d, shows that the range of changes Δψs was in the ΔP interval, which satisfies the condition −0.45 ≤ ΔP ≤ +0.514 MPa. This curve had a minimum at the point with the coordinates Δψs = −0.04 V and ΔP = 0.3 MPa. Moreover, this curve shows that with the increase in ΔP, the value of Δψs decreased nonlinearly until reaching the minimum value and then increased nonlinearly. On the other hand, in the case of curve (1b), the range of changes of Δψs was within the ΔP range, which satisfies the condition of 0.78 ≤ ΔP ≤ +2.54 MPa. This curve had a maximum at the coordinates Δψs = −0.08 V and ΔP = 1.12 MPa. Moreover, this curve shows that with the increase in ΔP, the value of Δψs increased nonlinearly until reaching the maximum value and then decreased nonlinearly.

The curves 2a,b shown in Figure 3d illustrate the dependence Δψs=fΔP, calculated based on Equation (31) for the determined values ζs = 0.3, RC = 10, and Ch/Cl = 20. This figure shows that in the examined interval (i.e.,  ζs, RC and Ch/Cl), Equation (31) had two solutions, which are graphically illustrated by the curves (2a,b). Curve (2a) shows that the range of changes Δψs was in the ΔP range, which satisfies the condition of −280 kPa ≤ ΔP ≤ +2.33 MPa. This curve had a minimum at the point with coordinates Δψs = −0.015 V and (ΔP = 1.85 MPa). Moreover, this curve shows that with the increase in ΔP, the value of Δψs decreased nonlinearly until reaching the minimum value and then increased nonlinearly. On the other hand, in the case of curve (1b), the range of changes of Δψs was within the ΔP range, which satisfies the condition of 2.6 ≤ ΔP ≤ 6.0 MPa. This curve had a maximum at the coordinates Δψs = −0.032 V and ΔP = 3.5 MPa. Moreover, this curve shows that with the increase in ΔP, the value of Δψs increased nonlinearly until reaching the maximum value and then decreased nonlinearly.

3.3. Rayleigh Number Dependencies of Membrane Potential

Figure 4 shows the characteristics of Δψs=fRC  for various fixed values of ΔP, ζs, and Ch/Cl . Figure 4a shows Δψs=fRC for the same value ΔP = +100 kPa and ζs = 0.049 for different set values of Ch/Cl. The calculation results illustrated by the curve presented in Figure 4a show that the value of Δψs increased nonlinearly with the increase in the RC value. This means that this increase was different in different RC ranges. For 0 < RC < 6333.3, the tangent of the slope of the tangent to the curve segment was approximately constant and amounted to ΔΔψs/ΔRC = 6.8 μV. In turn, for 6333.3 ≤ RC ≤ 6729.2, the tangent of the slope of the tangent to the curve segment was approximately constant and amounted to ΔΔψs = 0.27 mV. Hence, it follows that the ratio of the tangent slopes of the tangents to the discussed sections of curve (1), as shown in Figure 4a, was approximately 400. This means that after crossing the point with the coordinates Δψs = 0.04 V and RC = 6333.3, the kinetics of membrane transport change abruptly. It should be noted that for the tested RC range, all Δψs values were positive.

Curves (2–4), depicted in Figure 4a, show that an increase in the value of Ch/Cl while maintaining the values of ΔP and ζs, changes the course of the characteristic Δψs=fRC from nonlinearly increasing (curve in Figure 3a) to nonlinearly decreasing (curves 2, 3, and 4 in Figure 4a). Moreover, for the tested RC range, the Δψs values were both positive and negative. It should also be noted that in the case of curve (2), in the range of small RC values, as the RC value increased, Δψs initially decreased quickly and then, after reaching the minimum value, (Δψs)min = −0.002 V for RC = 1800, slowly grew. Curves (3) and (4) are nonlinearly decreased, but in the case of curve (4), the decrease in the value of the potential Δψs caused by the increase in the value of RC was significantly faster than in the case of curve (3).

Figure 4b shows the characteristics Δψs=fRC calculated for the set values ΔP = +100 kPa, Ch/Cl = 20, and ζs = 0.049 (curve (1)) and ζs = 0.049 (curve (2)). The course of these curves shows that an increase in the RC value causes a nonlinear decrease in the value of Δψs. Moreover, Δψs takes both positive and negative values. This decrease in value is greatest for 0 < RC < 265 and it decreases for higher values of RC. It should be noted that an increase in the value of ζs shifts the curves towards smaller values of Δψs.

Figure 4c shows the characteristics Δψs=fRC calculated for the set values ΔP = −100 kPa, Ch/Cl = 20, and ζs = 0.049 (curve 1), ζs = 0.055 (curve (2)), and ζs = 0.058 (curve 3). The course of these curves shows that an increase in the RC value caused a nonlinear increase in the value of Δψs and that Δψs  was positive. Moreover, it should be noted that an increase in the value of ζs shifted the abovementioned curves towards higher values of RC. Within curves 1–3, three segments can be distinguished: the first—linear, the second—nonlinear, and the third—linear. The tangents to the linear segments of these curves intersected at the following coordinates: Δψs = 0.078 V and RC = 228.57 (curve (1)); Δψs = 0.077 V and RC = 779.22 (curve (2)); Δψs = 0.077 V and RC = 1641.56 (curve (3)). This means that after crossing this point, the kinetics of membrane transport changes abruptly. The tangents of the angles of inclination of the first linear sections of curves (1–3) were, respectively, Δ(Δψs)/ΔRC = 0.19, 0.056, and 0.026 mV. This means that the value of this tangent decreased with the increasing value of RC. In turn, the tangents of the angles of inclination of the second linear sections of curves (1–3) were, respectively, Δ(Δψs)/ΔRC = 20, 19, and 17 mV. In addition, in this case, the value of this tangent decreased with an increasing RC value. These data also show that the tangent ratio of the angles of inclination for the second and first sections of the curves 1–3 were 105.339 and 654, respectively. This means that the value of this ratio decreased with an increasing value of RC.

Figure 4d shows the characteristics (RC)lim=f(ζs)ΔP, calculated for the different set values of ΔP. The curves in this figure are of a similar shape. The values of (RC)lim illustrated by curve (1) were independent of ζs for 0 ≤ ζs ≤ 0.05. For ζs > 0.05, the value of (RC)lim increased until the maximum value was reached at the point with coordinates (RC)lim = 0.83 and ζs = 0.122. After reaching the maximum value, the value of (RC)lim decreased nonlinearly until reaching (RC)lim = 0, for ζs > 0.6. The values of (RC)lim illustrated by curve (2) increased until the maximum value was reached at the point with coordinates (RC)lim = 0.2 and ζs = 0.206. After reaching the maximum value, the value of (RC)lim decreased nonlinearly until reaching (RC)lim = 0, for ζs > 0.6.

In summary, the results of calculations based on Equations (34), (35), (40) and (41), presented in Figure 2, Figure 3 and Figure 4, show that the membrane potential for concentration polarization conditions depends on the value of one of the four factors—ΔP, (Ch/Cl ), RC, and ζs—at fixed values of the other three.

3.4. Discussion

Equations (1)–(3) show that for Im = 0, four processes were involved in the creation of the characteristics shown in Figure 1, Figure 2, Figure 3 and Figure 4: hydraulic flow, osmosis, diffusion, and advection. In the studied range of Ch and Cl, the role of the osmotic agent in the creation of Δψs was negligibly small. To demonstrate this, let us consider the equation Jvo=LpζsσRTChCl, describing the osmotic flux. Considering in this equation, the data Lp = 5 × 10−12 m3N−1s−1, σ = 0.06, RT = 2.45 × 103 J mol−1, and ΔC = 12.5 mol m−3, we obtain Jvo = 0.9 × 10−8 m s−1. For isoosmotic conditions, Jvo = Jvp=LpΔP. This condition corresponds to ΔPp = 1.8 kPa. For ΔP >> ΔPp and Jvo << Jvp. This means that the influence of osmosis on the creation of Δψs was negligibly small and the mechanical pressure was large. In order to show what the contribution of the diffusion and advection factor in the creation of Δψs, let us consider Equations (1) and (2). If we consider Equation (1) in Equation (2) we obtain:

Js=JsdJsao+Jsap=ωLpσC¯1σRTChCl+C¯1σLpΔP (44)

where Jsd—diffusion flux, Jsao—advective (osmotic) flux, and Jsap—advective (hydraulic) flux.

By substituting appropriate values into Equation (44), it can be shown that Jsd >> Jsao, because Jsd = 4 × 10−5 mol m−2s−1, Jsao = 3 × 10−9 mol m−2s−1, and ωLpσC¯1σ. This means that the effect of osmosis on diffusion and, therefore, on the creation of Δψs was negligibly small. In turn, Jsap= C¯1σLpΔP. Given the relevant data, one can show that if Jsap = Jsd = 4 × 10−5 mol m−2s−1, then ΔPap = 1.9 × 106 kPa. For ΔP >> ΔPap, the effect of pressure advection on diffusion and, thus, on the creation of Δψs was large. From the above discussion, it is clear that due to the organic range of (Ch/Cl) and the unlimited range of ΔP, only molecular diffusion and hydraulic advection are involved in the creation of Δψs.

4. Conclusions

This paper presented an equation describing the membrane potential generated in a membrane system (containing an isotropic, symmetric, and electronically inert polymer membrane) for concentration polarization conditions. This equation for currentless conditions (Is = 0) has the form:

Δψs=RTFΔτ0lnChCl + ΔτΔτ0lnCiCe (45)
CiCe=ChClα0+α1Jv+α2Jv2β0+β1Jv+β2Jv2 (46)

where

α0=DlDhδhζωRT1ClCh
α1=12δlDhδhζωRT1ClChDlδhClCh1ζσ+ζσ
α2=14δlδhζσClCh1ζσ
β0=DhDlδlζωRTChCl1
β1=12DhδlChCl1ζσ+ζσδhDl+δhζωRTChCl1
β2=14δlδhζσChCl1ζσ
Δτ0=τ0aτ0c, Δτm=τmaτmc
δl=RClνlρlDl2gRTωζClρCChCl1114
δh=RChνhρhDh2gRTωmζsChρC1ClCh114

This is an equation that is the sum of two logarithmic expressions. The second component is particularly complex, because it contains components with different powers, ranging from fractional to quadratic. The above equation certainly has many different solutions, depending on the parameters regarding the transport properties of the membrane and the physicochemical and hydrodynamic properties of the solutions it separates. Figure 2, Figure 3 and Figure 4 show examples of solutions in the form of the dependence: Δψs=f(Ch/Cl) for different fixed values of ΔP, ζs, and RC; Δψs=fRC for different fixed values of ΔP, ζs, and (Ch/Cl); Δψs=fΔP for different fixed values of RC, ζs, and (Ch/Cl). Certainly, the curves presented in Figure 2, Figure 3 and Figure 4 do not exhaust all types of solutions to Equation (21).

It can be seen from the relationships in these figures that changing the values of ΔP, ζs, RC, and/or (Ch/Cl) causes a change in the type of characteristic. This means that Δψs is sensitive to a factor (e.g., environmental forces), the source of which is the thermodynamic environment of the membrane. Biological membranes, which are the microscale equivalent of our skin, behave in a similar but more complex way [2]. The membrane has embedded switches that respond to physical signals from the environment, relaying information to intracellular protein pathways. Almost every environmental signal recognized by a cell has a different switch in the cell membrane. What these switches have in common is a similar design and method of operation.

Undoubtedly, synthetic membranes used as an active dressing component in the treatment of hard-to-heal wounds, such as extensive burns or venous leg ulcers, are a skin substitute [32]. In this process, the membrane serves as a barrier that creates an appropriate microenvironment between the wound and the membrane surface. The physiological environment thus created contributes to faster wound healing, which has both medical and economic dimensions.

Acknowledgments

We would like to thank those who have touched our science paths.

List of Symbols

Jv volume flux (m s−1)
Jl, Jm, Jh solute fluxes; (mol m−2s−1)
Il, Is, Im, Ih ionic currents (A)
Lp hydraulic conductivity coefficient (m−3N−1s−1)
σ reflection coefficient
PE electroosmotic permeability coefficient (NA−1)
ω solute permeability coefficient (mol N−1s−1)
γ van’t Hoff coefficient
R gas constant (J mol−1K−1)
T absolute temperature (K)
κ electrical conductivity (Ω−1m−2)
τj transfer number
zj valence
ϰj ion number
C¯ average concentration of the solution (mol m−3)
Δψm potential difference measured with two reversible electrodes (V)
τa, τc transfer number of anions (a) and cations (c) in the membrane
t time (s)
lh and ll concentration boundary layers
δl, δh thickness of the concentration boundary layers (m)
δm membrane thickness (m)
ΔP mechanical pressure difference (Pa)
CBLs concentration boundary layers
g acceleration due to the fact of gravity (m s−2)
Dl, Dh diffusion coefficients (m2s−1)
νl, νh the kinematic viscosity coefficients (m2s−1)
Ce, Ci solution concentrations at the boundaries of M/ll and M/lh (mol m−3)
ρe, ρi solution densities at the boundaries of M/ll and M/lh (kg m−3)
Cl, Ch solution concentrations beyond ll and lh (mol m−3)
ρl, ρh solution densities beyond ll and lh (kg m−3)

Author Contributions

Conceptualization, K.M.B. and A.Ś.; methodology, K.M.B., A.Ś. and I.Ś.-P.; software, K.M.B.; formal analysis: K.M.B., A.Ś., I.Ś.-P. and W.M.B.; investigation, K.M.B., A.Ś. and I.Ś.-P.; resources, K.M.B., A.Ś., I.Ś.-P. and W.M.B.; data curation, K.M.B. and A.Ś.; writing—original draft preparation, K.M.B., A.Ś., I.Ś.-P., R.Ś. and W.M.B., writing—review and editing, K.M.B., A.Ś., I.Ś.-P., W.M.B. and R.Ś.; visualization, K.M.B. and A.Ś.; supervision, A.Ś.; funding acquisition, R.Ś. and W.M.B. All authors have read and agreed to the published version of the manuscript.

Funding

The scientific research was funded by the statute subvention of Czestochowa University of Technology.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

The data sets for this study are available upon request from the corresponding author.

Conflicts of Interest

The authors declare no conflict of interest.

Footnotes

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Availability Statement

The data sets for this study are available upon request from the corresponding author.


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