Osmotic water permeability of plasma and vacuolar membranes in protoplasts II. Theoretical basis

Water permeability of the plasma membrane (PM) and the vacuolar membrane (VM) is important for intracellular and transcellular water movement in plants, because mature plant cells have large central vacuoles. We have developed a new method for measuring the osmotic water permeability of the PM and VM (P _f1 and P _f2, respectively) in individual plant cells. Here, the theoretical basis and procedure of the method are discussed. Protoplasts isolated from higher plant tissues are used to measure P _f1 and P _f2. Because of the semi-permeability (selective permeability) of cellular membranes, protoplasts swell or shrink under hypotonic or hypertonic conditions. A theoretical three-compartment model is presented for simulating time-dependent volume changes in the vacuolar and cytoplasmic spaces in a protoplast during osmotic excursions. The model describes the theoretical relationships between P _f1, P _f2 and the bulk osmotic water permeability of protoplasts (P _f(bulk)). The procedure for measuring the osmotic water permeability is: (1) P _f(bulk) is calculated from the time when half of the total change in protoplast volume is completed, by assuming that the protoplast has a single barrier to water movement across it (two-compartment model); (2) P _f2 of vacuoles isolated from protoplasts is obtained in the same manner; and (3) P _f1 is determined from P _f(bulk) and P _f2 according to the three-compartment model. The theoretical relationship between P _fl (m s⁻¹) and L _Pl (hydraulic conductivity, l=1, 2) (m s⁻¹ Pa⁻¹) is also discussed. Electronic supplementary material Supplementary material is available in the online version of this article at and is accessible for authorised users. Tsuneo Kuwagata and Mari Murai-Hatano contributed equally to the paper.     

Osmotic water permeability of plasma and vacuolar membranes in protoplasts I. High osmotic water permeability in radish ( Raphanus sativus ) root cells as measured by a new method

Intra- and transcellular water movements in plants are regulated by the water permeability of the plasma membrane (PM) and vacuolar membrane (VM) in plant cells. In the present study, we investigated the osmotic water permeability of both PM (P _f1) and VM (P _f2), as well as the bulk osmotic water permeability of a protoplast (P _f(bulk)) isolated from radish (Raphanus sativus) roots. The values of P _f(bulk) and P _f2 were determined from the swelling/shrinking rate of protoplasts and isolated vacuoles under hypo- or hypertonic conditions. In order to minimize the effect of unstirred layer, we monitored dropping or rising protoplasts (vacuoles) in sorbitol solutions as they swelled or shrunk. P _f1 was calculated from P _f(bulk) and P _f2 by using the ‘three-compartment model’, which describes the theoretical relationship between P _f1, P _f2 and P _f(bulk) (Kuwagata and Murai-Hatano in J Plant Res, 2007). The time-dependent changes in the volume of protoplasts and isolated vacuoles fitted well to the theoretical curves, and solute permeation of PM and VM was able to be neglected for measuring the osmotic water permeability. High osmotic water permeability of more than 500 μm s⁻¹, indicating high activity of aquaporins (water channels), was observed in both PM and VM in radish root cells. This method has the advantage that P _f1 and P _f2 can be measured accurately in individual higher plant cells. Electronic supplementary material Supplementary material is available in the online version of this article at and is accessible for authorized users. It includes four appendices, four tables and two figures. Mari Murai-Hatano and Tsuneo Kuwagata contributed equally to the paper. An erratum to this article is available at .     

Behavior of the Plasma Membrane of Isolated Protoplasts during a Freeze-Thaw Cycle

Cryomicroscopy of protoplasts isolated from nonacclimated (NA) rye leaves (Secale cereale L. cv Puma) revealed that the predominant form of injury following cooling to the minimum temperature for 50% survival (LT₅₀) (−5°C) was expansion-induced lysis of the plasma membrane during warming and thawing of the suspending medium when the decreasing osmolality resulted in osmotic expansion of the protoplasts. When cooled to temperatures below the LT₅₀, the predominant form of injury was loss of osmotic responsiveness following cooling so that the protoplasts were osmotically inactive during warming. Only a low incidence (<10%) of expansion-induced lysis was observed in protoplasts isolated from acclimated (ACC) leaves, and the predominant form of injury following cooling to the LT₅₀ (−25°C) was loss of osmotic responsiveness. The tolerable surface area increment (TSAI) which resulted in lysis of 50% of a population (TSAI₅₀) of NA protoplasts osmotically expanded from isotonic solutions was 1122 ± 172 square micrometers. Similar values were obtained when the protoplasts were osmotically expanded from hypertonic solutions. The TSAI determined from cryomicroscopic measurements of individual NA protoplasts was similar to the TSAI₅₀ values obtained from osmotic manipulation. The TSAI₅₀ of ACC protoplasts expanded from isotonic solutions (2145 ± 235 square micrometers) was approximately double that of NA protoplasts and increased following osmotic contraction. Osmotic contractions were readily reversible upon return to isotonic solutions. During freeze-induced dehydration, endocytotic vesicles formed in NA protoplasts whereas exocytotic extrusions formed on the surface of ACC protoplasts. During osmotic expansion following thawing of the suspending medium, the endocytotic vesicles remained in the cytoplasm of NA protoplasts and the protoplasts lysed before their original volume and surface area were regained. In contrast, the exocytotic extrusions were drawn back into the surface of ACC protoplasts as the protoplasts regained their original volume and surface area.     

Osmotic water permeability of isolated protoplasts. Modifications during development

A transference chamber was developed to measure the osmotic water permeability coefficient (P_os) in protoplasts 40 to 120 μm in diameter. The protoplast was held by a micropipette and submitted to a steep osmotic gradient created in the transference chamber. P_os was derived from the changes in protoplast dimensions, as measured using a light microscope. Permeabilities were in the range 1 to 1000 μm s⁻¹ for the various types of protoplasts tested. The precision for P_os was ≤40%, and within this limit, no asymmetry in the water fluxes was observed. Measurements on protoplasts isolated from 2- to 5-d-old roots revealed a dramatic increase in P_os during root development. A shift in P_os from 10 to 500 μm s⁻¹ occurred within less than 48 h. This phenomenon was found in maize (Zea mays), wheat (Triticum aestivum), and rape (Brassica napus) roots. These results show that early developmental processes modify water-transport properties of the plasma membrane, and that the transference chamber is adapted to the study of water-transport mechanisms in native membranes.     

Cryopreservation of rye protoplasts by vitrification

A procedure has been developed for the vitrification of mesophyll protoplasts isolated from leaves of nonacclimated (NA) and cold-acclimated (ACC) winter rye seedlings (Secale cereale L. cv Puma). The procedure involves (a) equilibration (loading) of the protoplasts with an intermediate concentration (1.5, 1.75, or 2.0 molar) of ethylene glycol (EG) at 20°C; (b) dehydration of the protoplasts in a concentrated vitrification solution made of 7 molar EG + 0.88 molar sorbitol + 6% (w/v) bovine serum albumin (BSA) at 0°C; (c) placing the protoplasts into polypropylene straws and quenching in liquid nitrogen (LN₂); and (d) recovery of the protoplasts from LN₂ and removal (unloading) of the vitrification solution. For NA protoplasts, 47 + 1% survival was obtained following recovery from LN₂ if the protoplasts were first loaded with 1.75 molar EG prior to the dehydration step. However, to achieve this level of survival, NA protoplasts had to be unloaded in a hypertonic (2.0 osmolal [osm]) sorbitol solution. If they were unloaded in an isotonic solution (0.53 osm), survival was 3±2%. In contrast, survival of ACC protoplasts following recovery from LN₂ was 34 ± 10% when the protoplasts were loaded in a 2.0 molar EG solution and unloaded in an isotonic sorbitol solution (1.03 osm). If ACC protoplasts were unloaded in an hypertonic sorbitol solution (1.5 osm), survival was 51 ± 9%. These results indicate that the osmotic excursions incurred during the procedure are a major factor affecting survival.     

The Mechanics of Injury to Isolated Protoplasts following Osmotic Contraction and Expansion

Micro-osmotic manipulation was used to determine the influence of osmotic contraction on the expansion potential of individual protoplasts isolated from rye (Secale cereale L. cv Puma) leaves. For protoplasts isolated from leaves of nonacclimated plants (NA protoplasts), osmotic contraction in sufficiently hypertonic solutions (>1.53 osmolal) predisposed the protoplasts to lysis during osmotic expansion when they were returned to isotonic conditions (0.53 osmolal). In contrast, for protoplasts isolated from leaves of cold acclimated plants (ACC protoplasts), osmotic contraction in either 2.6 or 4.0 osmolal solutions was readily reversible. Following osmotic contraction, the resting tension (γ_r) of NA protoplasts was similar to that determined for protoplasts in isotonic solutions (i.e. 110 ± 22 micronewtons per meter). In contrast, γ_r of ACC protoplasts decreased from 164 ± 27 micronewtons per meter in isotonic solutions to values close to zero in hypertonic solutions. Following expansion in hypotonic solutions, γ_r's of both NA and ACC protoplasts were similar for area expansions over the range of 1.3 to 1.6. Following osmotic contraction and reexpansion of NA protoplasts, hysteresis was observed in the relationship between γ_r and surface area—with higher values of γ_r at a given surface area. In contrast, no hysteresis was observed in this relationship for ACC protoplasts. Direct measurements of plasma membrane tension (γ) during osmotic expansion of NA protoplasts from hypertonic solutions (1.53 osmolal) revealed that γ increased rapidly after small increments in surface area, and lysis occurred over a range of 1.2 to 8 millinewtons per meter. During osmotic expansion of ACC protoplasts from hypertonic solutions (2.6 osmolal), there was little increase in γ until after the isotonic surface area was exceeded. These results are discussed in relation to the differences in the behavior of the plasma membrane of NA and ACC protoplasts during osmotic contraction (i.e. endocytotic vesiculation versus exocytotic extrusion) and provide a mechanistic interpretation to account for the differential sensitivity of NA and ACC protoplasts to osmotic expansion from hypertonic solutions.     

Quantitative examination of a perfusion microscope for the study of osmotic response of cells

The perfusion microscope was developed for the study of the osmotic response of cells. In this microscope, the cells are immobilized in a transparent chamber mounted on the stage and exposed to a variety of milieus by perfusing the chamber with solutions of different concentrations. The concentration of the supplied solution is controlled using two variable-speed syringe pumps, which supply an isotonic solution and a hypertonic solution. Before using this system to characterize the osmotic response of cells, the change in the concentration of NaCl solution flowing through the chamber is examined quantitatively using a laser interferometer and an image processing technique. The NaCl concentration is increased from an isotonic condition to a hypertonic condition abruptly or gradually at a given constant rate, and decreased from a hypertonic condition to an isotonic condition. It is confirmed that the concentration is nearly uniform in the cross direction at the middle of the chamber, and the change in the NaCl concentration is reproducible. The average rate of increase or decrease in the measured concentration agrees fairly well with the given rate when the concentration is changed gradually at a constant rate. The rate of the abrupt change is also determined to be the highest limit achieved by the present method. As the first application of using the perfusion microscope for biological studies, the volume change of cells after exposure to a hypertonic solution is measured. Then, the hydraulic conductivity of the cell membrane is determinedfrom the comparison of the volume change between the experiment and the theoretical estimation for the measured change in the NaCl concentration of the perfused solution.     

Plasma Membrane Water Permeability of Cultured Cells and Epithelia Measured by Light Microscopy with Spatial Filtering

A method was developed to measure the osmotic water permeability (P_f) of plasma membranes in cell layers and applied to cells and epithelia expressing molecular water channels. It was found that the integrated intensity of monochromatic light in a phase contrast or dark field microscope was dependent on relative cell volume. For cells of different size and shape (Sf9, MDCK, CHO, A549, tracheal epithelia, BHK), increased cell volume was associated with decreased signal intensity; generally the signal decreased 10–20% for a twofold increase in cell volume. A theory relating signal intensity to relative cell volume was developed based on spatial filtering and changes in optical path length associated with cell volume changes. Theory predictions were confirmed by signal measurements of cell layers bathed in solutions of various osmolarities and refractive indices. The excellent signal-to-noise ratio of the transmitted light detection permitted measurement of cell volume changes of <1%. The method was applied to characterize transfected cells and tissues that natively express water channels. P_f in control Chinese hamster ovary cells was low (0.0012 cm/s at 23°C) and increased more than fourfold upon stable transfection with aquaporins 1, 2, 4, or 5. P_f in apical and basolateral membranes in polarized epithelial cells grown on porous supports was measured. P_f ^bl and P_f ^ap were 0.0011 and 0.0024 cm/s (MDCK cells), and 0.0039 and 0.0052 cm/s (human tracheal cells) at 23°C. In intact toad urinary bladder, basolateral P_f was 0.036 cm/s and apical membrane P_f after vasopressin stimulation was 0.025 cm/s at 23°C. The results establish light microscopy with spatial filtering as a technically simple and quantitative method to measure water permeability in cell layers and provide the first measurement of the apical and basolateral membrane permeabilities of several important epithelial cell types.     

Effect of dDAVP on basolateral cell surface water permeability in the outer medullary collecting duct

We report a novel approach for assessing the volume of living cells which allows quantitative, high-resolution characterization of dynamic changes in cell volume while retaining the cell functionality. The aim of this study was to evaluate the short-term effect of vasopressin on basolateral cell surface water permeability in the outer medullary collecting duct (OMCD). The permeability of the basolateral cell membrane was determined in the tubules where the apical membrane was blocked with oil injected into the lumen. The apparent coefficient of water permeability (P _f) was evaluated by measuring the cell swelling after the step from hypertonic to isotonic medium (600 mosm to 300 mosm). Desmopressin (dDAVP) induced an increase of the basolateral P _f from 113.7±8.5 μm/s in control cells to 186.6±11.4 μm/s in micro-dissected fragments of the OMCD incubated in vitro (10⁻⁷ M dDAVP, 30 min at 37 °C) (P<0.05). Mercury caused pronounced inhibition of basolateral water permeability (26.0±6.9 μm/s; P<0.05). The effect of mercury (1.0 mM HgCl₂) was reversible: after washing the fragments with PBS for 20 min, P _f values were restored to the control levels (125.0±9.5 μm/s). The results of the study indicate the existence of a mechanism controlling the osmotic water permeability of the basolateral cell membrane in the OMCD epithelium.     

Osmosis in Cortical Collecting Tubules : A Theoretical and Experimental Analysis of the Osmotic Transient Phenomenon

This paper reports a theoretical analysis of osmotic transients and an experimental evaluation both of rapid time resolution of lumen to bath osmosis and of bidirectional steady-state osmosis in isolated rabbit cortical collecting tubules exposed to antidiuretic hormone (ADH). For the case of a membrane in series with unstirred layers, there may be considerable differences between initial and steady-state osmotic flows (i.e., the osmotic transient phenomenon), because the solute concentrations at the interfaces between membrane and unstirred layers may vary with time. A numerical solution of the equation of continuity provided a means for computing these time-dependent values, and, accordingly, the variation of osmotic flow with time for a given set of parameters including: P_f (cm s^–1), the osmotic water permeability coefficient, the bulk phase solute concentrations, the unstirred layer thickness on either side of the membrane, and the fractional areas available for volume flow in the unstirred layers. The analyses provide a quantitative frame of reference for evaluating osmotic transients observed in epithelia in series with asymmetrical unstirred layers and indicate that, for such epithelia, P_f determinations from steady-state osmotic flows may result in gross underestimates of osmotic water permeability. In earlier studies, we suggested that the discrepancy between the ADH-dependent values of P_f and P_DDw (cm s^–1, diffusional water permeability coefficient) was the consequence of cellular constraints to diffusion. In the present experiments, no transients were detectable 20–30 s after initiating ADH-dependent lumen to bath osmosis; and steady-state ADH-dependent osmotic flows from bath to lumen and lumen to bath were linear and symmetrical. An evaluation of these data in terms of the analytical model indicates: First, cellular constraints to diffusion in cortical collecting tubules could be rationalized in terms of a 25-fold reduction in the area of the cell layer available for water transport, possibly due in part to transcellular shunting of osmotic flow; and second, such cellular constraints resulted in relatively small, approximately 15%, underestimates of P_f.     

Pre-steady-state analysis of the turn-on and turn-off of water permeability in the kidney collecting tubule

Summary Water transport across the mammalian collecting tubule is regulated by vasopressin-dependent water channel insertion into and retrieval from the cell apical membrane. The time course of osmotic water permeability (P _f ) following addition and removal of vasopressin (VP) and 8-Br-cAMP was measured continuously by quantitative fluorescence microscopy using an impermeant fluorophore perfused in the lumen. Cortical collecting tubules were subjected to a 120 mOsm bath-to-lumen osmotic gradient at 37°C with 10–15 nl/min lumen perfusion and 10–20 ml/min bath exchange rate. With addition of VP (250 U/ml), there was a 23±3 sec (sem,n=16) lag in whichP _f did not change, followed by a rise inP _f (initial rate 1.4±0.2×10^–4 cm/sec²) to a maximum of 265±10×10^–4 cm/sec. With addition of 8-Br-cAMP (0.01–1mm) there was an 11±2 sec lag. For [8-Br-cAMP]=0.01, 0.1 and 1mm, the initial rate ofP _f increase following the lag was (units 10^–4 cm/sec²): 1.1±0.1, 1.2±0.1 and 1.7±0.3. MaximumP _f was (units 10^–4 cm/sec): 64±4, 199±9 and 285±11. With removal of VP,P _f decreased to baseline (12×10^–4 cm/sec) with aT _1/2 of 18 min; removal of 0.1 and 1mm 8-Br-cAMP gaveT _1/2 of 4 and 8.5 min. These results demonstrate (i) a brief lag in theP _f response, longer for stimulation by VP than by 8-Br-cAMP, representing the transient build-up of biochemical intermediates proximal to the water channel insertion step, (ii) similar initialdP _f /dt (water channel insertion) over a wide range of [8-Br-cAMP] and steady-stateP _f values, and (iii) more rapidP _f decrease with removal of 8-Br-cAMP than with VP. These pre-steady-state results define the detailed kinetics of the turn-on and turn-off of tubuleP _f and provide kinetic evidence that the rate-limiting step for turn-on ofP _f is not the step at which VP regulates steady-stateP _f . If water channel insertion is assumed to be the rate-limiting step in the turn-on ofP _f , these results raise the possibility that water channels must be activated following insertion into the apical membrane.     

Development of a microfluidic device for determination of cell osmotic behavior and membrane transport properties

An understanding of cell osmotic behavior and membrane transport properties is indispensable for cryobiology research and development of cell-type-specific, optimal cryopreservation conditions. A microfluidic perfusion system is developed here to measure the kinetic changes of cell volume under various extracellular conditions, in order to determine cell osmotic behavior and membrane transport properties. The system is fabricated using soft lithography and is comprised of microfluidic channels and a perfusion chamber for trapping cells. During experiments, rat basophilic leukemia (RBL-1 line) cells were injected into the inlet of the device, allowed to flow downstream, and were trapped within a perfusion chamber. The fluid continues to flow to the outlet due to suction produced by a Hamilton Syringe. Two sets of experiments have been performed: the cells were perfused by (1) hypertonic solutions with different concentrations of non-permeating solutes and (2) solutions containing a permeating cryoprotective agent (CPA), dimethylsulfoxide (Me₂SO), plus non-permeating solute (sodium chloride (NaCl)), respectively. From experiment (1), cell osmotically inactive volume (V_b) and the permeability coefficient of water (L_p) for RBL cells are determined to be 41% [n = 18, correlation coefficient (r²) of 0.903] of original/isotonic volume, and 0.32 ± 0.05 μm/min/atm (n = 8, r² > 0.963), respectively, for room temperature (22 °C). From experiment (2), the permeability coefficient of water (L_p) and of Me₂SO (P_s) for RBL cells are 0.38 ± 0.09 μm/min/atm and (0.49 ± 0.13) × 10⁻³ cm/min (n = 5, r² > 0.86), respectively. We conclude that this device enables us to: (1) readily monitor the changes of extracellular conditions by perfusing single or a group of cells with prepared media; (2) confine cells (or a cell) within a monolayer chamber, which prevents imaging ambiguity, such as cells overlapping or moving out of the focus plane; (3) study individual cell osmotic response and determine cell membrane transport properties; and (4) reduce labor requirements for its disposability and ensure low manufacturing costs.     

Serial permeability barriers to water transport in human placental vesicles

Summary Microvillous vesicles were prepared from term human placenta by shearing, differential centrifugation and Mg²⁺ precipitation. Vesicles were purified further on a sucrose density gradient producing two bands with densities of 1.16 to 1.18 g/ml (C1) and 1.13 to 1.15 g/ml (C2). The C2 fraction, which had a 24-fold enrichment of alkaline phosphatase and a three-fold reduction in Na⁺, K⁺-ATPase activity compared to homogenates, was used to measure osmotic water (P _f ) permeability.P _f was measured from the time course of scattered light intensity following exposure of vesicles to specified gradients of impermeant solutes.P _f decreased from 3.0×10^–3 to 0.6×10^–3 cm/sec with increasing gradient size (65 to 730mm; 23°C). Four possible causes of this behavior were examined theoretically and experimentally: an unstirred layer, saturation of water transport, large changes in the vesicle surface area with changes in volume and a structural restriction to vesicle volume change. The measured dependence ofP _f on gradient size and the effect of the channel-forming ionophore gramicidin onP _f fit best to the theoretical dependences predicted by a structural restriction mechanism. This finding was supported by experiments involving the effects onP _f of increased solution viscosity, initial vesicle volume, the magnitude of transmembrane volume flow, and the effects of gradient size on activation energy (E _a) forP _f . The decreasedP _f resulting from a structural restriction limiting vesicle volume change was modeled mathematically as a second barrier in series with the vesicle membrane.E _a measured using a 250-mm inwardly directed sucrose gradient was 5.4±0.6 kcal/mol (T>27°C) and 10.0±0.6 kcal/mol (T<27°C).E _a above 27°C is in the range normally associated with transmembrane passage of water via aqueous channels. Water transport was not inhibited byp-chloromercuribenzenesulfonate.     

Water transport in invertebrate peripheral nerve fibers

Osmotic and diffusion permeabilities (P_f and P_d) of invertebrate nerve fibers to tritiated water were measured to determine what water flux studies could reveal about "the nerve membrane" and to directly test the possibility of active transport of water into or out of invertebrate nerve fibers. P_f/P_d ratios for lobster walking leg nerve fibers were found to be about 20 ± 7 at 14°C. P_d measurements were made for squid giant axons at 25°C. and found to yield a value of 4 x 10^–4 cm.^–1 sec.^–1. When combined with the data of D. K. Hill for P_f, a P_f/P_d ratio of 21 ± 5 is obtained. These P_f/P_d ratios correspond to "effective pore radii" of about 16 ± 4 angstrom units, according to theories developed by Koefoed-Johnsen and Ussing and independently by Pappenheimer and his colleagues. Variations of water flux ratios with temperatures were studied and apparent activation energies calculated for both diffusion experiments and osmotic filtration experiments using the Arrhenius equation, and found to be close to 3 to 5 cal. per mole of water transferred. Cyanide (5 x 10^–3 molar) and iodoacetate (1 x 10^–3 molar) poisoned lobster leg nerve fibers showed no appreciable change in diffusion or osmotic filtration water effluxes. Caution in interpreting these proposed channels as simple pores was emphasized, but the possibility that such channels exist and are related to ionic flow is not incompatible with electrophysiological data.     

Osmosis in Cortical Collecting Tubules : ADH-Independent Osmotic Flow Rectification

The present experiments were designed to evaluate the effects of varying the osmolality of luminal solutions on the antidiuretic hormone (ADH)-independent water and solute permeability properties of isolated rabbit cortical collecting tubules. In the absence of ADH, the osmotic water permeability coefficient (cm s^–1) P_f^l→b, computed from volume flows from hypotonic lumen to isotonic bath, was 20 ± 4 x 10^–4 (SEM); the value of P_f^b→l in the absence of ADH, computed from volume flows from isotonic bath to hypertonic lumen, was 88 ± 15 x 10^–4 cm s^–1. We also measured apparent urea permeability coefficients (cm s^–1) from ¹⁴C-urea fluxes from lumen to bath (P_DDurea^l→b) and from bath to lumen (P_DDurea^b→l). For hypotonic luminal solutions and isotonic bathing solutions, P_DDurea^l→b was 0.045 ± 0.004 x 10^–4 and was unaffected by ADH. The ADH-independent values of P_DDurea^l→b and P_urea^b→l were, respectively, 0.216 ± 0.022 x 10^–4 cm s^–1 and 0.033 ± 0.002 x 10^–4 cm s^–1 for isotonic bathing solutions and luminal solutions made hypertonic with urea, i.e., there was an absolute increase in urea permeability and asymmetry of urea fluxes. Significantly, P_DDurea^l→b did not rise when luminal hypertonicity was produced by sucrose; and, bathing fluid hypertonicity did not alter tubular permeability to water or to urea. We interpret these data to indicate that luminal hypertonicity increased the leakiness of tight junctions to water and urea but not sucrose. Since the value of P_f^b→l in the absence of ADH, when tight junctions were open to urea, was approximately half of the value of P_f^l→b in the presence of ADH, when tight junctions were closed to urea, we conclude that tight junctions are negligible paracellular shunts for lumen to bath osmosis with ADH. These findings, together with those in the preceding paper, are discussed in terms of a solubility-diffusion model for water permeation in which ADH increases water solubility in luminal plasma membranes.     

Effects of anions and/or cell volume on the permeance of an apical water pathway induced by Hg in toad skin epithelium

Hg compounds block membrane transport units behaving as water channels. Here we show that Hg induces an apical water pathway in toad skins pretreated with 10^–3 M CH₃ClHg or HgCl₂, added to the outer bathing medium. Washing with SO₄-Ringer caused a several-fold increase in net water flow (J _w ) and osmotic permeability coefficient (P _f ) that was reversed by re-exposure to Cl- or NO₃-Ringer and mimicked by gluconate-Ringer. These P _f changes could be elicited repeatedly and were present if, and only if, anion replacements took place in the inner bathing solution. Such inner polarity was related to the anion permeability of the epidermal basolateral membrane: impermeant anions (SO₄, gluconate) increased P _f ; permeant anions (Cl, NO₃) did not change basal P _f but reversed the high P _f induced by impermeant anions. Hg induced the appearance of aggregates that persisted despite repeated washings of the skins during 4–5 h, and whether P _f was high (SO₄-Ringer) or low (Cl-Ringer) before skin fixation.The Hg-induced apical water pathway in toad skin appears to be a unique model for studying the interplay between cell volume, cell ionic composition and water permeability.We thank P. Brawand and P. Fruleux for technical assistance. This work has been supported by grants from the Swiss National Science Foundation (Nos. 31-30030.90 to A.G. and R.C.dS., and 32-34090.92 to P.M.)     

Volume flows across gallbladder epithelium induced by small hydrostatic and osmotic gradients

Summary The hydraulic conductivity of rabbit gallbladder epithelium has been studied using a continuous volumetric method based on capacitance measurements. The time resolution for measuring osmotic flows is in the range of seconds. Volume flows have been induced by osmotic gradients between 0 and 100 mosmol. In this range the flow-force relation is linear and theP _f value is 9.3×10^–3 cm/sec. After correction for solute polarization effects, theP _f value amounts to 0.05 cm/sec. The observed flow is constant between 5 sec up to 20 min after a sudden increase in the osmolarity of the mucosal solution. The wet weight of the gallbladder tissue decreases by 22% and increases by 30% during osmotic flows from serosa to mucosa and from mucosa to serosa, respectively. Volume flows induced by hydrostatic pressure gradients on the mucosal surface are linearly related to the driving forces between 0 and 40 mbar. TheP _f value is 0.15 cm/sec. The volume flows are constant between 2 sec and 15 min after pressure application. The flow-force relation for pressure gradients on the serosal surface is markedly nonlinear for gradients greater than 5 mbar. Below 5 mbar theP _f value is 4.5 cm/sec. From electrical measurements, e.g., resistance and streaming potentials, and from flux studies with inulin and polyethylene glycol 4000, it is concluded that hydrostatic and osmotic gradients are not comparable when they are applied to gallbladder epithelium. They induce volume flows across different pathways, e.g., osmosis predominantly across the cellular route and pressure filtration predominantly across paracellular routes.     

Water permeability differs between growing and non-growing barley leaf tissues

A pressure probe technique and an osmotic swelling assay were used to compare water transport properties between growing and non-growing tissues of leaf three of barley. The epidermis was analysed in planta by pressure probe, whereas (predominantly) mesophyll protoplasts were analysed by osmotic swelling. Hydraulic conductivity (Lp) and, by implication, water permeability (Pf) of epidermal cells was 31% higher in the leaf elongation zone (Lp=0.5+/-0.2 microm s-1 MPa-1; Pf=65+/-25 microm s-1; means+/-SD of n=17 cells) than in the, non-growing, emerged leaf zone (Lp=0.4+/-0.1 microm s-1 MPa-1; Pf=50+/-15 microm s-1; n=24; P<0.05). Similarly, water permeability of mesophyll protoplasts was by 55% higher in the elongation compared with emerged leaf zone (Pf=13+/-1 microm s-1 compared with 8+/-1 microm s-1; n=57 and 36 protoplasts, respectively; P<0.01). Within the leaf elongation zone, a small population of larger-sized protoplasts could be distinguished. These protoplasts, which originated most likely from parenchymateous bundle sheath or midrib parenchyma cells, had a three-fold higher water permeability (P<0.001) as mesophyll protoplasts. The effect on Lp and Pf of known aquaporin inhibitors was tested with the pressure probe (Au+, Ag+, Hg2+, phloretin) and the osmotic swelling assay (phloretin). Only phloretin, when applied to protoplasts in the swelling assay caused an average decrease in Pf, but the effect varied between isolations. Technical approaches and cell-type and growth-specific differences in water transport properties are discussed.