A simple technique of measuring high membrane permeabilities of human erythrocytes

Concentration dependence of the cell membrane permeability to cryoprotectant and water and implications for design of methods for post-thaw washing of human erythrocytes

For more than fifty years the human red blood cell (RBC) has been a widely studied model for transmembrane mass transport. Existing literature spans myriad experimental designs with varying results and physiologic interpretations. In this review, we examine the kinetics and mechanisms of membrane transport in the context of RBC cryopreservation. We include a discussion of the pathways for water and glycerol permeation through the cell membrane and the implications for mathematical modeling of the membrane transport process. In particular, we examine the concentration dependence of water and glycerol transport and provide equations for estimating permeability parameters as a function of concentration based on a synthesis of literature data. This concentration-dependent transport model may allow for design of improved methods for post-thaw removal of glycerol from cryopreserved blood. More broadly, the consideration of the concentration dependence of membrane permeability parameters may be important for other cell types as well, especially for design of methods for equilibration with the highly concentrated solutions used for vitrification.

The effects of the extracellular manganese concentration and variation of the interpulse delay time in the CPMG sequence on water exchange time across erythrocyte membranes

There has been broad disagreement in the literature regarding the dependence of water exchange times (Te) across erythrocyte membranes studied by the 1H-NMR Carr-Purcell-Meiboom-Gill (CPMG) pulse sequence on extracellular Mn2+ concentration. While some workers saw no change in Te with Mn2+, others reported a 35-50% decrease in Te with this extracellular paramagnetic relaxation agent. We present 1H-NMR evidence that a 30-50% change in Te can be produced by interdependence of the interpulse delay time of the CPMG pulse sequence and the external Mn2+ concentration. Such a large dependency is interpreted in terms of the diffusional effect as a major source. However, it is shown experimentally that if a large number of refocusing pi pulses are used, the observed transverse relaxation times are unaffected by Mn2+. Under these conditions excellent agreement of Te obtained in our study (13.0 +/- 0.64 ms (N = 36) at 21 degrees C) and that of 12.8 +/- 3.6 ms at 20-23 degrees C reported by the radiotracer method was found. Our findings suggest new and important implications for evaluating the previous reports of the 1H-NMR CPMG method concerning the [Mn2+] effect in the decrease of Te, and provide conditions where studies of water transport across erythrocyte membranes using this magnetic resonance method can be used with confidence.

On measuring the diffusional water permeability of human red blood cells and ghosts by nuclear magnetic resonance

The characteristics of water diffusional permeability (P) of human red blood cells were studied on isolated erythrocytes and ghosts by a doping nuclear magnetic resonance technique. In contrast to all previous investigations, systematic measurements were performed on blood samples obtained from a large group of donors. The mean values of P ranged from 2.2 X 10(-3) cm.s-1 at 5 degrees C to 8.1 X 10(-3) cm.s-1 at 42 degrees C. The reasons for some of the discrepancies in the permeability coefficients reported by various authors were found. In order to estimate the basal permeability, the maximal inhibition of water diffusion was induced by exposure of red blood cells to p-chloromercuribenzenesulfonate (PCMBS) under various conditions (concentration, duration, temperature). The lowest values of P were around 1.3 X 10(-3) cm.s-1 at 20 degrees C, 1.6 X 10(-3) cm.s-1 at 25 degrees C, 1.9 X 10(-3) cm.s-1 at 30 degrees C and 3.2 X 10(-3) cm.s-1 at 37 degrees C. The results reported here represent the largest series of determinations of water diffusional permeability of human red blood cells (without or with exposure to mercurials) available in the literature, and consequently the best estimates of the characteristics of this transport process. The values of P can be taken as references for the studies of water permeability in various cells or in pathological conditions.

A review of water diffusion measurement by NMR in human red blood cells

This review of water transport measurement in normal human erythrocytes attempts to harmonize discordant results obtained under diverse study conditions with two different techniques: nuclear magnetic resonance (NMR) and radioactive tracer (THO) diffusion. Natural aggregation of red cells into rouleaux appeared to cause most of the variation among results from NMR experiments. The remainder of the discrepancy was attributed to the use of inappropriate mathematical approximations of the two-site exchange equations, differences in blood storage time, and failure to adjust NMR calculations for the nonwater protons. Differences in hematocrit, frequency-magnetic field strength, or NMR pulse technique played no apparent role in the disparity among NMR reports. When these confounding factors were removed, diffusion results obtained by NMR or by influx or bulk diffusion of radioactive tracer agreed within a relatively narrow range of values. These techniques place the mean lifetime of water inside fresh normal human erythrocytes at room temperature (20-25 degrees C) between the extremes of 9.8 and 14 ms, where the uncorrected range was previously 9.8-21.7 ms. This new range of water exchange times corresponds to a range of diffusional permeability between 3.3 and 4.7 x 10(-3) cm/s.

Measurement of rapid membrane permeation in cell suspensions by application of a generalized capillary method

An improved version of the capillary technique for the determination of diffusion coefficients has been developed as a simple method of measuring membrane permeabilities of single cells suspended at relative densities between 0.70 and 0.97. A new, generalized theoretical formulation to describe the diffusion process of a solute in a composite system was derived using a series-parallel-pathway model with explicit consideration of the diffusion pathways inside and between the cells. This renders the technique insensitive to unstirred layer effects. Any single cell population of known size distribution may be investigated. High permeabilities (above 5.10(-3) cm/s) can be measured with the greatest precision, but lower permeabilities, down to a limit of about 5.10(-4) cm/s, may also be determined by the method. Measurements in erythrocyte suspensions have been made using non-electrolytes such as hexanol, water and ethylene glycol as test solutes. The permeabilities obtained agree with the values obtained by much more sophisticated equipment. Cell shape was shown to be without significant influence on the permeability data obtained. The procedure may become of particular interest for measurement of suspensions of membrane vesicles.

Determination of cell membrane permeability in concentrated cell ensembles

The method of volume averaging is used to analyze the process of diffusion in concentrated cell ensembles in which significant resistance to mass transfer is caused by the cellular membrane. A general closure scheme is given that allows for direct theoretical prediction of effective diffusivities for any cellular geometry. Numerical results are presented for the classical parallelepiped arrangement used to model cellular systems, and these results are used in conjunction with experimental studies of concentrated cell ensembles to determine membrane permeabilities for solute diffusion in several cellular systems. Membrane permeabilities are compared with predictions from other models of diffusion in cellular systems.

Water exchange through erythrocyte membranes: nuclear magnetic resonance studies on resealed ghosts compared to human erythrocytes

The water diffusion across human erythrocyte membrane has been studied on intact cells and resealed ghosts by a doping NMR technique. Although the water exchange time of ghosts was longer than that of erythrocytes, no significant differences in their diffusional permeability were noticed for temperatures in the range 2-43 degrees C. Contrary to what was previously noticed in erythrocytes, no significant increase in the water exchange time of ghosts in the acid range of pH occurred.

On the water and proton permeabilities across membranes from erythrocyte ghosts

The diffusional permeability of water across membranes from bovine and human erythrocyte ghosts was measured by a recently developed method which is based on the different indices of refraction of H2O and 2H2O. Resealed erythrocyte ghosts were prepared by a gel-filtration technique. Pd (2H2O/H2O) values of 1.2 X 10(-3) cm/s (human) and 1.7 X 10(-3) cm/s (bovine) were calculated at 20 degrees C. The activation energies of the water exchange were 23.5 kJ/mol (human) and 25.4 kJ/mol (bovine). Treatment of the ghosts with p-chloromercuribenzenesulfonic acid (PCMBS) led to a 60-70% inhibition of the diffusional water exchange. The pH equilibration across membranes of erythrocyte ghosts was measured by intracellular carboxyfluorescein. The rates of proton flux after pH-jumps (pH 7.3 to pH 6.1) were about 100-fold lower than those of the water exchange and dependent on the kind of anions present (Cl-, NO-3, SO2-4). The activation energies of proton flux were 60-70 kJ/mol. 4,4'-Diisothiocyanatostilbene-2,2'-disulfonic acid (DIDS) inhibited the exchange by 97-98% and lowered the activation energy. The inhibitor of water exchange, PCMBS, increased the proton-permeation rate by a factor of 4-5. It is assumed that the rate-limiting step for the proton permeation is determined by the anion exchange. Under this condition our results are not in accord with one channel as a common pathway for both the passive water and anion transport.

Binding of DTNB to band 3 in the human red cell membrane

Inhibition of red cell water transport by the sulfhydryl reagent 5,5'-dithiobis(2-nitrobenzoic acid) (DTNB) has been reported by Naccache and Sha'afi ((1974) J. Cell Physiol. 84, 449-456) but other investigators have not been able to confirm this observation. Brown et al. ((1975) Nature 254, 523-525) have shown that, under appropriate conditions, DTNB binds only to band 3 in the red cell membrane. We have made a detailed investigation of DTNB binding to red cell membranes that had been treated with the sulfhydryl reagent N-ethylmaleimide (NEM), and our results confirm the observation of Brown et al. Since this covalent binding site does not react with either N-ethylmaleimide or the sulfhydryl reagent pCMBS (p-chloromercuribenzenesulfonate), its presence has not previously been reported. This covalent site does not inhibit water transport nor does it affect any transport process we have studied. There is an additional low-affinity (non-covalent) DTNB site that Reithmeier ((1983) Biochim. Biophys. Acta 732, 122-125) has shown to inhibit anion transport. In N-ethylmaleimide-treated red cells, we have found that this binding site inhibits water transport and that the inhibition can be partially reversed by the specific stilbene anion exchange transport inhibitor 4,4'-diisothiocyanostilbene-2,2'-disulfonate (DIDS), thus linking water transport to anion exchange. DTNB binding to this low-affinity site also inhibits ethylene glycol and methyl urea transport with the same KI as that for water inhibition, thus linking these transport systems to that for water and anions. These results support the view that band 3 is a principal constituent of the red cell aqueous channel, through which urea and ethylene glycol also enter the cell.

Role of membrane proteins and lipids in water diffusion across red cell membranes

When human red cells are treated with the mercurial sulfhydryl reagent, p-chloromercuribenzene sulfonate, osmotic water permeability is suppressed and only diffusional water permeability remains (Macey, R.I. and Farmer, R.E.L. (1970) Biochim. Biophys. Acta 211, 104-106). It has been suggested that the route for the remaining water permeation is by diffusion through the membrane lipids. However, after making allowance for the relative lipid area of the membrane, the water diffusion coefficient through lipid bilayers which contain cholesterol is too small by a factor of two or more. We have measured the permeability coefficient of normal human red cells by proton T1 NMR and obtained a value of 4.0 X 10(-3) cm X s-1, in good agreement with published values. In order to study permeation-through red cell lipids we have perturbed extracted red cell lipids with the lipophilic anesthetic, halothane, and found that halothane increases water permeability. The same concentration of halothane has no effect on the water permeability of human red cells, after maximal pCMBS inhibition. In order to compare halothane mobility in extracted red cell membrane lipids with that in red cell ghost membranes, we have studied halothane quenching of N-phenyl-1-naphthylamine by equilibrium fluorescence and fluorescence lifetime methods. Since halothane mobility is similar in these two preparations, we have concluded that the primary route of water diffusion in pCMBS-treated red cells is not through membrane lipids, but rather through a membrane protein channel.

Water permeability through biological membranes by isotopic effects of fluorescence and light scattering

A light-scattering technique used to measure the water permeability across closed biomembranes is described, which is based on the different indices of refraction of D2O and H2O. This transient technique is compared with a similar method using D2O-sensitive fluorophores in the intravesicular space. The results of both techniques are equivalent although the signal-to-noise ratio favors the light-scattering or turbidity experiment. The light-scattering method is only applicable to larger particles (no point-scatterers) and is easily extended to biological objects. Data on the H2O/D2O exchange across membranes of ghosts from human erythrocytes suggest two mechanisms: the D2O and H2O permeation through the membrane and a slower D2O-induced conformational change of membraneous proteins.

Transport of water and urea in red blood cells

Evidence for water channels in red blood cells is reviewed. In an entropically driven reaction, organic mercurials decrease water permeability, elevate the activation energy, and reduce the ratio of osmotic to diffusional water permeabilities to unity so that water transport properties of red blood cells are hardly distinguishable from lipid bilayers. It is concluded that mercurials close the water channels. A variety of kinetic, pharmacological, and comparative evidence converges on the conclusion that urea and other solutes are excluded from water channels. Urea apparently permeates the red cell membrane via a facilitated diffusion system, which plays an important role when red blood cells traverse the renal medulla; rapid urea transport helps preserve the osmotic stability and deformability of the cell, and it helps prevent dissipation of extracellular osmotic gradients. Water apparently traverses the channel via a single-file mechanism; the very low channel permeability of H+ is explained if the channel contains fixed charge, or alternatively, if the mobile water molecules within the channel do not form a continuum. An alternative unitary pore hypothesis for simultaneous transport of water, ions, and small solutes is also discussed.

On the exchange of H2O/D2O molecules across membranes of erythrocyte ghosts from patients with Huntington's disease and from normal individuals

A recently developed technique is used to study the permeation of water through membranes of human erythrocyte ghosts. The method, based on the difference of the indices of refraction of H2O and D2O, is briefly described. Comparative measurements on erythrocyte ghosts from normal donors and from patients with Huntington's disease were performed. The calculated permeability coefficients for the two groups were almost identical and did not allow differentiation between the controls and patients with Huntington's disease.

Formation of aqueous pores in the human erythrocyte membrane after oxidative cross-linking of spectrin by diamide

Oxidation of erythrocyte membrane SH-groups by diamide and tetrathionate induces cross-linking of spectrin (Haest, C.W.M., Kamp, D., Plasa, G. and Deuticke, B. (1977) Biochim. Biophys. Acta 469, 226-230). This cross-linking was now shown to go along with a concentration- and time-dependent enhancement of membrane permeability for hydrophilic nonelectrolytes and ions. The enhancement is specific for oxidative SH-group modifications, is reversible by reduction of the induced disulfides, can be suppressed by a very brief pre-treatment of the cells with low concentrations of N-ethylmaleimide and is strongly temperature-dependent. The pathway of the induced permeability discriminates nonelectrolytes on the basis of molecular size and exhibits a very low activation energy (Ea 3-8 kcal/mol). These findings are reconcilable with the formation of a somewhat inhomogeneous population of aqueous pores with radii probably less than or equal to 0.65 nm. Estimated pore numbers vary with the size of the probe molecule. Assuming a diffusion coefficient as in bulk water within the pore, at least 20 pores per cell have to be postulated; more realistic lower diffusion coefficients increase that number. Alterations of the lipid domain by changes of cholesterol contents and insertion of hexanol or nonionic detergents alter the number or size of the pores. Since aggregation of skeletal and intrinsic membrane proteins also occurs after the SH-oxidation, in parallel to the formation of membrane leaks, one may consider (a) defects in the disturbed bilayer interface, (b) a mismatch between lipid and intrinsic proteins or (c) channels in between aggregated intrinsic proteins as structures forming the pores induced by diamide treatment.

Urea and ethylene glycol-facilitated transport systems in the human red cell membrane. Saturation, competition, and asymmetry

The equilibrium exchange of [14C]urea and ethylene glycol was measured using a new type of fast flow system. Approximately equal volumes of saline and air were mixed to form a segmented fluid stream into which 14C-loaded red cells are injected. The stream flows through three filter chambers which allow sampling of the 14C in the extracellular fluid at three time points. The chambers are designed so that they do not disrupt the segmented bubble pattern. The alternating air and saline segments prevent laminar dispersion in the flowing stream and ensure good mixing at the injection and sampling sites. The equilibrium exchange of both urea and ethylene glycol showed saturation kinetics. The maximum permeability (Po) measured in the limit of zero solute concentration is 1.6 X 10(-3) cm/s for urea and 4.8 X 10(-4) cm/s for ethylene glycol (T = 23 degrees C). The apparent dissociation constant (Km) was 218 mM for urea and 175 mM for ethylene glycol. The Po for thiourea is 2.3 X 10(-6) cm/s and the Km is 19 mM. Urea and thiourea inhibit the transport of each other and the inhibition constant (KI) is approximately equal to the Km for both compounds. 53 other analogues of urea were screened for their inhibition of urea or thiourea transport. Several analogues [e.g., 1-(3,4-dichloro-phenyl)-2-thiourea] had a KI in the range of 0.03 mM. The affinity of the inhibitor increased as it was made more hydrophobic. The urea analogues did not significantly inhibit the ethylene glycol or osmotic permeability. Glycerol inhibited ethylene glycol permeability with a KI of 1,200 mM.