The effect of hypophysectomy and prolactin therapy on water balance of the brown trout Salmo trutta.

A technique for the hypophysectomy of the brown trout is described which might be applicable to other salmonids. Hypophysectomy produced a decrease in water turnover which was corrected by prolactin therapy. Hypophysectomy resulted in a decrease in the next flux of osmotic water. Both osmotic and diffusional water permeabilities were evenly decreased after hypophysectomy, such that the ratio of the osmotic and diffusional permeability coefficients (Pos/Pd) retained a value of approximately unity. The data suggest that calcium and prolactin have opposing actions on water balance and that their modes of action are likely to separate.     

Barriers to water flow in vasopressin-treated toad urinary bladder

Summary Unstirred layers of water complicate the measurement of water permeability across epithelia. In the toad urinary bladder, the hormone vasopressin increases the osmotic water permeability of the granular epithelial cell's luminal membrane, and also leads to the appearance of aggregates of particles within this membrane. The aggregates appear to be markers for luminal membrane osmotic water permeability. This report analyzes the relationship between transbladder osmotic water flow and aggregate frequency, and demonstrates that flow across the bladder is significantly attenuated by unstirred layers of water or by structural barriers other than the luminal membrane when the luminal membrane is made permeable by vasopressin. This analysis in addition yields unique values for the permeabilities of both the luminal membrane and the barriers to water flow which lie in series with it.     

Salt-water coupling in leaky epithelia

Summary The theory of quasi-isotonic transport by cellular osmosis (the standing-gradient theory) has been challenged on the grounds that the osmotic permeabilities of the mucosal and interspace membranes are too low; if they were as high as the theory requires then the osmotic permeability of the whole epithelium would be 2–3 orders of magnitude higher than observed. This objection has basically been accepted for it is now claimed that these enormous permeabilities do exist, but are masked by unstirred-layer effects; I show that this is incorrect because unstirredlayer corrections are small and that the situation has not changed since 1975.The view that the route of fluid transport is junctional is replacing the cellular theory, and trans-junctional water flows seem to account for major fractions of the flow in various epithelia. I argue on grounds of general theory that these are unlikely to be osmotic flows because the junctional pores cannot satisfy both the osmotic and diffusive properties required of them, but the basic osmotic theory is also rather vague here.Non-osmotic theories, if junctional flow is accepted, must be either electro-kinetic or peristaltic.     

An analogue computer simulation of cloacal resorption of salt and water from ureteral urine in birds

The transmural flow of NaCl and water occurring during the retrograde flow of ureteral urine into the coprodeum and large intestine of birds has been simulated by analogue computation. The purpose was to estimate whether a fraction of the urine (water) which in the dehydrated state is hyperosmotic to plasma can, in spite of this, be absorbed from the narrow space between the epithelium and the central faeces core. The values of urine flow, urine osmolality, osmotic permeability, net NaCl absorption rate, and solute-linked water flow determined by in vivo perfusion studies in the domestic fowl were used in the calculation. The cloacal sojourn of ureteral urine was found to result in a net water gain but at the expense of a hyperosmotic NaCl absorption. The model was further used to evaluate the quantitative influence of the system's parameters upon the fractional water absorption. This was found very sensitive to the urine osmolality, moderately sensitive to the urine flow and NaCl absorption rate and almost unaffected by the osmotic permeability of the coprodeum and large intestine within a reasonable physiological range. The change of the epithelial transport parameters from the normally hydrated to the dehydrated state resulted in a marked increase in water absorption.     

Water permeabilities and salt reflection coefficients of luminal, basolateral and intracellular membrane vesicles isolated from rabbit kidney proximal tubule

The mechanisms of water transport across the rabbit renal proximal convoluted tubule were approached by measuring osmotic permeabilities and solute reflection coefficients of the brush-border and the basolateral membranes. Plasma and intracellular membrane vesicles were isolated from rabbit renal cortex by centrifugation on a Percoll gradient. Three major turbidity bands were obtained: a fraction of purified basolateral membranes (BLMV), the two others being brush-border (BBMV) and endoplasmic reticulum (ERMV) membrane vesicles. The osmotic permeability (Pf) of the three types of vesicle was measured using stop-flow techniques and their geometry was determined by quasi-elastic light scattering. Pf was equal to 123 +/- 8 microns/s (n = 10) for BBMV, 166 +/- 10 microns/s (n = 10) for BLMV and 156 +/- 9 microns/s (n = 4) for ERMV (T = 26 degrees C). A transcellular water permeability, per unit of apical surface area, of 71 microns/s was calculated considering that the luminal and the basolateral membranes act as two conductances in series. This value is in close agreement, after appropriate normalizations, with previously reported transepithelial water permeabilities obtained using in vitro microperfusion techniques thus supporting the hypothesis of a predominantly transcellular route for water flow across rabbit proximal convoluted tubule. The addition of 0.4 mM HgCl2, a sulfhydryl reagent, decreased Pf about 60% in three types of membrane providing evidence for the existence of proteic pathways. NaCl and KCl reflection coefficients were measured and found to be close to one for plasma and intracellular membranes suggesting that the water channels are not shared by salts.     

The Dependence of Calcium Transport and Leaf Tipburn in Strawberry on Relative Humidity and Nutrient Solution Concentration

Strawberry plants were grown in controlled-environment cabinetswith different day-and-night relative humidities, in nutrientsolutions of different osmotic potential and different calciumconcentrations. Leaf calcium (% d. wt.) depended strongly on leaf age and waslowest and very sensitive to environment when the leaf was emergingfrom the bud. Calcium in the emergent leaf was greatest andtipburn least when plants were grown in humid nights (VPD usually< 100 Pa) and weak nutrient solutions (osmotic potentialabout –25 kPa). Such plants guttated freely. In contrastplants grown in dry nights (VPD, c. 600 Pa) never guttated,had small concentrations of calcium in emergent leaves and sufferedtipburn. The behaviour of plants transferred between humiditytreatments rapidly reflected the new conditions. Increasingthe osmotic potential of the nutrient increased tipburn anddecreased calcium in emergent leaves even though the nutrientcontained more calcium. When the calcium concentration in the emergent leaf exceeded0.07 per cent of d. wt, tipburn was never seen; below 0.05 percent tipburn was usually severe. These results suggest that pre-emerged, and therefore non-transpiring,leaves depend for their calcium on water flow arising from rootpressure at night. After leaf emergence, calcium intake intoleaves was promoted by dry days, indicating that calcium wasthen supplied by transpirational water flow. Humid nights, drydays and weak nutrient solutions minimize the risk of leaf tipburnin strawberry. Fragaria ananassa Duch., strawberry, tipburn, calcium transport, relative humidity, nutrient supply, guttation     

Mechanism and Control of Fluid Secretion

Fluid secretion and reabsorption by a variety of plant and animal tissues appear to be accomplished by osmotic coupling between solute transport and water movement. The local osmosis model suggests that active accumulation of solutes within narrow folds at the cell surface may produce the local gradients that generate water flow. Both micropuncture techniques and electron-probe X-ray microanalysis have established that local osmotic gradients occur in absorptive epithelia, but they have not as yet been detected in secretory tissues.Hormonal control of secretion involves stimulation of solute pumps and adjustments of permeability to non-transported solutes. Since hormone receptors and pumps are often located on opposite surfaces of the cell, intracellular second messengers convey the secretory signal through cytoplasm. Much has been learned by study of insect tissues that are anatomically simple and that function for long periods in vitro. Aspects of hormone-receptor interaction have been explored, including the action of halluninogenic molecules. In insect salivary glands cyclic AMP appears to stimulate cation transport, while calcium increases anion permeability. The various second messengers probably interact with each other in complex feedback loops that stabilize the system and make it quickly responsive to hormone. Cyclic AMP may stimulate release of calcium from mitochondria. Unresolved is the way second messengers alter properties of the cell surface.     

Adaptive responses of aglomerular toadfish to dilute sea water

Plasma and urine of toadfish (Opsanus tau) in sea water and 10% sea water were analyzed to assess responses of an aglomerular fish to hypoosmotic challenge. Following transfer to 10% sea water, plasma osmotic pressure decreased slowly from 318 to 241 mmol · kg H₂O⁻¹, over a period of 10–15 days. Urine osmotic pressure decreased in parallel from 299 to 207 mmol · kg H₂O⁻¹, leaving urine/plasma ratios of osmotic pressure essentially unchanged. In contrast, the volume and composition of urine changed rapidly following transfer to 10% sea water. Urine flow rate increased 110% from 3.0 to 6.3 μl · 100g⁻¹ · h⁻¹ and Na⁺ excretion increased 346%, while excretion of Mg²⁻ and SO₄ ²⁻ decreased 81% and 90%, respectively. Excretion rates for Cl⁻ were low in seawater toadfish and decreased further in 10% sea water. An unknown sulfur-containing anion, present in the urine of seawater toadfish, contributed significantly to the composition and ionic balance in urine of toadfish in 10% sea water. These results suggest that the inability to produce strongly dilute urine obliges toadfish to lose salt in order to excrete water, in hypoosmotic media. The decrease in plasma osmotic pressure may be both a strategy to reduce osmotic and ionic gradients in dilute media and a consequence of the kidney's inability to excrete water without salt. Accepted: 22 August 1996     

The relationship between membrane fluidity and permeabilities to water,solutes, ammonia,and protons

Several barrier epithelia such as renal collecting duct, urinary bladder, and gastric mucosa maintain high osmotic pH and solute gradients between body compartments and the blood by means of apical membranes of exceptionally low permeabilities. Although the mechanisms underlying these low permeabilities have been only poorly defined, low fluidity of the apical membrane has been postulated. The solubility diffusion model predicts that lower membrane fluidity will reduce permeability by reducing the ability of permeant molecules to diffuse through the lipid bilayer. However, little data compare membrane fluidity with permeability properties, and it is unclear whether fluidity determines permeability to all, or only some substances. We therefore studied the permeabilities of a series of artificial large unilamellar vesicles (LUV) of eight different compositions, exhibiting a range of fluidities encountered in biological membranes. Cholesterol and sphingomyelin content and acyl chain saturation were varied to create a range of fluidities. LUV anisotropy was measured as steady state fluorescence polarization of the lipophilic probe DPH. LUV permeabilities were determined by monitoring concentration-dependent or pH-sensitive quenching of entrapped carboxyfluorescein on a stopped- flow fluorimeter. The relation between DPH anisotropy and permeability to water, urea, acetamide, and NH3 was well fit in each instance by single exponential functions (r > 0.96), with lower fluidity corresponding to lower permeability. By contrast, proton permeability correlated only weakly with fluidity. We conclude that membrane fluidity determines permeability to most nonionic substances and that transmembrane proton flux occurs in a manner distinct from flux of other substances.     

Osmotic permeabilities across corneal endothelium and antidiuretic hormone-stimulated toad urinary bladder structures

Osmotic permeabilities of several epithelial structures have been determined with novel optical procedures based on specular microscopy. The osmotic permeabilities of several tissue layers were determined by continuously monitoring the position of the apical tissue borders while an osmotic flow was imposed across those layers. The values found were (in μm/s; mean ± SE): corneal epithelium, 137 ± 30 (n = 5); antidiuretic hormone stimulated toad bladder, 429 ± 64 (n = 6); and corneal endothelium, 711 ± 34 (n = 7). In addition, the osmotically-induced transient change in thickness of the corneal endothelial cells was determined with the help of a computer, and the apparent osmotic permeability measured for the apical membrane was 1420 ± 160 μm/s (n = 5). It is concluded that the osmotic permeability across the endothelial layer is sizably larger than had been previously detected and that osmotic flows across such layer largely traverse the cellular membranes. With osmotic permeability values (per unit of cell membrane area) as large as presently reported, isotonic fluid transport by epithelia can be explained simply on the basis of local osmotic gradients.     

Effect of monensin on osmotic water flow across the toad bladder and its stimulation by vasopressin and cyclic AMP

The effects of the sodium ionophore monensin on osmotic water flow across the urinary bladder of the toad Bufo marinus were studied. Monensin alone did not alter osmotic water flow; however, the ionophore inhibited the hydrosmotic response to vasopressin and cyclic AMP in a dose-dependent manner. The inhibitory effects of monensin were apparent when the ionophore was added to th serosal bathing solution but not when it was added to the mucosal bathing solution. The inhibitory effect of serosal monensin required the presence of sodium in the serosal bathing solution but not the presence of calcium in the bathing solutions. Thus, it appears that intracellular sodium concentration is a regulator of the magnitude of the hydrosmotic response to vasopressin and cyclic AMP.     

Changes in body fluids of the frog Leptodactylus fuscus during estivation (Anura, Leptodactylidae)

The frog, L. fuscus, becomes dormant during the dry season in southeastern Brazil. Plasma and urine were obtained and analyzed for K+, Na+, and osmotic concentrations in active and estivating frogs. Soil water potential from the estivation sites was compared with the osmotic concentrations of the frog. Plasma and urine osmotic concentrations (286.2 +/- 13.8 and 242.3 +/- 17.2 mOsm1(-1), respectively) were higher in the estivating than in active frogs (240.3 +/- 12.8 and 112.7 +/- 15.6 mOsm1(-1); plasma and urine), and the same holds true for plasma K+ content. The Na+ concentration was the same for active and estivating frogs. Soil water potential corresponded to osmotic pressure of 110 mOsm1(-1), showing that L. fuscus may uptake water from the soil during the estivation.     

Comparative effect of metals on antidiuretic hormone induced transport in toad bladder: specificity of mercuric inhibition of water channels

We previously reported that HgCl₂ inhibits water and urea flux in tissues fixed with glutaraldehyde after antidiuretic hormone (ADH) stimulation and suggested that the ADH-induced water channel may share characteristics of the red blood cell and proximal tubule water transport pathway. To determine the specificity of mercury's action, we examined the effect of numerous other metals. In tissues fixed after ADH stimulation, water flow and urea and sucrose permeabilities are maintained from mucosal bath pH 2.5 through pH 12. Several metals including Ba, Co, Fe, Sr and Zn did not alter flux. Al, Cd, La, Li, Pb and U inhibited urea permeability but not water flow. At pH 2.8, Cu inhibited water flow by 30% and urea permeability by 50%. At pH 4.9–7.4, Cu inhibited urea permeability but not water flow. At pH 3.0, Pt inhibited flow in ADH-pretreated tissues. The inhibitory effect was not present at pH>3.0. At pH<3.0, Au inhibited flow by 90% in tissues fixed after pretreatment with ADH but increased the permeability of tissues fixed in the absence of ADH. Ag inhibited flow by 70% but also increased sucrose, urea, and basal permeabilities. This suggests that Ag and Au disrupt epithelial integrity. These results indicate that at physiologic pH, the ADH-induced water channel is specifically blocked by Hg but not by other metals. This specificity may reflect the presence of a large number of sulfhydryl groups in the water channel.     

Combined transport of water and ions through membrane channels

The coupling of ion and water flow through membrane channels is under dispute. Among all human aquaporins only aquaporin-6 exhibits ion channel activity. Whether aquaporin-6 functions also as a water channel cannot yet be determined with confidence. Similarly, a comparison of single-channel water permeabilities from ion channels and aquaporins suggests that ion channels may play a secondary role as water channels. However, the fraction of absorbed fluid that crosses epithelial ion channels still remains to be determined.     

Effects of epinephrine on branchial and renal calcium handling in the rainbow trout

Acute exposure of rainbow trout (Salmo gairdneri) to low external calcium (25 microM) caused an immediate but transient increase in plasma epinephrine concentration that may have been related to a concomitant depression of blood pH. Intra-arterial infusion of epinephrine at normal ambient calcium levels (0.35 mM) for 4 h caused circulating levels of epinephrine to rise from 2.9 X 10(-9) to 8.0 X 10(-8) M but did not affect norepinephrine levels, or branchial unidirectional calcium fluxes. Active (ATP-dependent) calcium transport across basolateral plasma membranes prepared from gill epithelial cells was not affected by pretreatment of fish with epinephrine or by direct application of epinephrine or cAMP, in vitro. Epinephrine infusion elevated urine flow rate, decreased urine pH, and increased urine phosphate levels significantly. Net renal calcium efflux increased significantly as a result of the increased urine flow rate. It is concluded that epinephrine does not stimulate branchial calcium uptake or renal conservation of calcium in rainbow trout at normal external calcium levels and therefore we cautiously suggest that epinephrine is unlikely to be involved in calcium balance during periods of exposure to low external calcium. Instead, epinephrine may play a role in compensating the acid-base disturbances and the increased branchial water influx that are associated with exposure to low ambient calcium.     

Water permeability in the human amnion: pH regulation of the paracellular pathway

Human amnion was mounted, immediately after delivery, as a diaphragm between two lucite chambers and the net transepithelial water movement (Jw) was recorded minute by minute. When Jw was plotted against the applied transepithelial hydrostatic pressure (fetal side positive), in the absence of any other gradient, a linear relationship was observed (Phydr = 0.32 +/- 0.05 cm/s, n = 10). A linear relationship was also found when Jw was measured in the presence of an osmotic gradient, generated by adding (to the maternal side) different concentrations of poly(ethylene glycol) (Mr approximately equal to 3600; reflexion coefficient (sigma) = 1; Posm = 0.015 +/- 0.001 cm/s, n = 10). When sucrose, a paracellular marker, was used as the osmotic probe, the observed sigma was 0.5. Medium acidification in the presence of bicarbonate reduced in the same proportion both the hydrostatic and osmotic permeabilities. The effect was fully reversible, but was not observed when bicarbonate was replaced by Tris. To test the comparative role of transcellular versus paracellular paths, Jw and the [14C]sucrose permeability (Psuc) were simultaneously recorded minute by minute, in the presence of an osmotic or an hydrostatic gradient. In both cases, the percentage reductions in Jw and Psuc induced by medium acidification were similar. Quantification of theoretical and observed values for Jw and Psuc strongly suggests that effects of pH on both the osmotic and hydrostatic flux reflect a modification of the paracellular path.     

Effect of monensin on osmotic water flow across the toad bladder and its stimulation by vasopressin and cyclic AMP

Summary The effects of the sodium ionophore monensin on osmotic water flow across the urinary bladder of the toadBufo marinus were studied. Monensin alone did not alter osmotic water flow; however, the ionophore inhibited the hydrosmotic response to vasopressin and cyclic AMP in a dose-dependent manner. The inhibitory effects of monensin were apparent when the ionophore was added to the serosal bathing solution but not when it was added to the mucosal bathing solution. The inhibitory effect of serosal monensin required the presence of sodium in the serosal bathing solution but not the presence of calcium in the bathing solutions. Thus, it appears that intracellular sodium concentration is a regulator of the magnitude of the hydrosmotic response to vasopressin and cyclic AMP.     

Stability and reaction characteristics of reverse-phase evaporation vesicles (REVs) as enzyme containers

The ion-dependent enzymes, activities of which are affected by ions, were entrapped in the inside aqueous phase of reverse-phase evaporation vesicles (REVs) to protect the enzyme activities from inhibitory cations. Their activities were still preserved in the presence of the inhibitory cations because the permeabilities of the inhibitory cations through the lipid membranes of REVs were much lower than those of substrates and products. The REVs were relatively stable in hypertonic condition, while they were unstable in hypotonic condition. Changes in osmotic pressure difference largely affected solute permeabilities of REVs. The shrinking and swelling of REVs resulting from osmotic pressure differences led to these changes in stabilities and solute permeabilities. Although the entrapment of the enzyme into REVs showed good protective effects against divalent cations, it was not effective against univalent cations. The measurements of cation permeabilities revealed that the enzyme trapped in the bilayer regions of REVs acts as a selective channel for the univalent cations. The REVs containing the enzyme could be used without any activity losses in a hollow fiber module.     

Permeability studies on red cell membranes of dog, cat, and beef

Water permeability coefficients of dog, cat, and beef red cell membranes have been measured under an osmotic pressure gradient. The measurements employed a rapid reaction stop flow apparatus with which cell shrinking was measured under a relative osmotic pressure gradient of 1.25 to 1.64 times the isosmolar concentration. For the dog red cell the osmotic permeability coefficient is 0.36 cm⁴/(sec, osmol). The water permeability coefficient for the dog red cell under a diffusion gradient was also measured (rate constant = 0.10/msec). The ratio between the two permeabilities was used to calculate an equivalent pore radius of 5.9 A. This value agrees welt with an equivalent pore radius of 6.2 A obtained from reflection coefficients of nonelectrolyte water-soluble molecules, and is consistent with data on the permeability of the dog red cell membrane to glucose. These data provide evidence supporting the existence of equivalent pores in single biological membranes.     

Effect of norepinephrine and vasopressin on renal kallikrein excretion in rats

The purpose of this study was to investigate the effect of norepinephrine and vasopressin on urinary kallikrein excretion in the rat. Two studies were undertaken: (a) acute experiments in which the rats were infused with 30% dextrose in water with the addition of norepinephrine or vasopressin, (b) chronic experiments in which the drugs were infused during seven days through an osmotic minipump. In acute experiments, urinary kallikrein excretion increased without modification in urinary flow and glomerular filtration rate. In chronic experiments, urinary kallikrein excretion was not modified in norepinephrine-treated rats and decreased in vasopressin-infused animals. This decrease followed the modifications of the urine flow. In chronic experiments the dextrose infusion increased urinary kallikrein excretion. In all the groups studied a positive correlation between urine flow and urinary kallikrein excretion was observed. It is concluded that norepinephrine and vasopressin are important stimulators of the urinary kallikrein excretion only in those circumstances where it is necessary to eliminate an excess of water.