Augmented water binding and low cellular water content in erythrocytes of camel and camelids.

We investigated a link between hemoglobin primary structure, hemoglobin hydrophobicity-hydrophilicity, and erythrocyte water content in various mammalian species. Some hemoglobin molecules, particularly those of the camel and camelids, contain more charged amino acid residues and are more hydrophilic than the hemoglobins of human and a number of other mammalian species. To test the in vivo significance of these alterations of hemoglobin primary structure, we determined the osmotically unresponsive erythrocyte water fractions in mannit solutions of various osmolarities at 4 degreesC. Among the species investigated, the size of the osmotically unresponsive erythrocyte water fraction relates in a positive linear way to hemoglobin hydrophilicity. The extreme low total erythrocyte water content of camel erythrocytes (1.1-1.3 g water/g dry mass) may be explained by a comparatively high osmotically unresponsive erythrocyte water fraction. It is proposed that alterations of hemoglobin sequences of camel and camelids may be the part of a natural selection process aimed at protecting these animals against osmotic dehydration in arid environments.     

A non-ideal replacement for the Boyle van't Hoff equation

A non-ideal osmotic equilibrium equation is proposed as a replacement for the Boyle van’t Hoff equation to describe the equilibrium volume of a living cell as a function of external osmolality. Contrary to common understanding, the Boyle van’t Hoff equation is only thermodynamically correct for ideal, dilute solutions. However, the Boyle van’t Hoff equation is commonly used to determine the osmotically inactive fraction of the cell. This involves extrapolating to infinite osmolality, which violates the ideal, dilute solution constraint. It has been noted that the osmotically inactive fractions obtained from the Boyle van’t Hoff equation for human erythrocytes are markedly larger than measured values of the dry volume fraction of the cell. Using the new osmotic equilibrium equation to analyze experimental osmotic equilibrium data reduces the inferred osmotically inactive fraction of human erythrocytes by approximately 20%.     

The erythrocyte membrane site for the effect of temperature on osmotic fragility

The osmotic fragility of human erythrocytes is well known to decrease as the temperature is elevated. The cellular site for the temperature effect was studied by assessing possibles roles of hemoglobin and of membrane lipids and by taking advantage of the unique response of camel erythrocytes to temperature. It is concluded that the erythrocyte membrane is the site for the temperature effect on osmotic fragility. The human erythrocyte is likely to rupture in protein-lipid boundary regions in the membrane, from which cholesterol is apparently excluded.     

Steady-state volumes and metabolism-independent osmotic adaptation in mammalian erythrocytes

Erythrocytes of various mammalian species -- including human -- maintain osmotic balance with the blood plasma (osmotic activity 270-310 mosmol). However, their intracellular levels of osmotically active ions (potassium, sodium, chloride, and hydrogencarbonate), water content and osmotic resistance deviate significantly. In the present report we study the relationship among intracellular water, potassium and sodium levels of the erythrocytes of various mammalian species and in the developing calf. In addition, the osmotic resistance, K(+) (Rb(+)) uptake and the DPH fluorescence anisotropy of various erythrocytes and erythrocyte ghost membranes were correlated. The results show no statistically significant relationship between erythrocyte water content and [K(+)+Na(+)] levels or K(+)/Na(+) ratios. The reversal of erythrocyte K(+)/Na(+) ratios coincides with the decrease of steady-state ATP levels in the developing calf. The mobility of lipids within the hydrophobic inner layer of the plasma membrane relates closely to passive K(+) (Rb(+)) uptake, and plays a significant role in regulatory volume changes.     

Osmotic properties of bovine erythrocytes aged in vivo

The osmotic properties of bovine erythrocytes aged in vivo were studied by the modified microhematocrit method. The osmotic fragility of older red cells decreases due to their larger relative osmotically non-active volume. Relative critical cell volume of bovine erythrocytes does not alter significantly with cell age. The age dependent change in the osmotic fragility of human red blood cells, the reverse of that found for bovine erythrocytes, is due to a different alteration of the critical cell volume during intravascular erythrocyte aging.     

Comparison of erythrocyte osmotic fragility among ectotherms and endotherms at three temperatures

1. Comparison of erythrocyte osmotic fragility (EOF) between various ectotherms and endotherms was investigated at 5, 25, and 38 degrees C. 2. We hypothesized that ectotherms might possess erythrocytes whose osmotic fragility would be less affected by temperature than those of endotherms. 3. Ectotherm erythrocytes were much more osmotically resistant than those of endotherms. 4. The EOF of ectotherms and endotherms showed similar responses to temperature. 5. It does not appear that the osmotic fragility of erythrocytes from ectotherms in this study are adapted to be less affected by temperature than those of endotherms. The highly osmotic resistant erythrocytes of ectotherms may alleviate the need for further adaptation for osmotic resistance.     

The osmotic sensitivity of rat growth plate chondrocytes in situ; clarifying the mechanisms of hypertrophy

Bone elongation is predominantly driven by the volume expansion of growth plate chondrocytes. This mechanism was initially believed to be "hypertrophy", describing a proportional increase of cell water and organelles. However, morphometrical analysis subsequently assumed the increase to be "swelling", resulting in a disproportionate increase of cell water (osmotically active fraction). Histological approaches were performed on fixed tissue, and for the "swelling" assumption to be valid, the osmotic sensitivity of living cells before and during volume increase should differ. To test this, analysis of images acquired by 2-photon laser scanning microscopy (2PLSM) were used to determine the osmotic sensitivity, and osmotically active/inactive proportions of in situ chondrocytes from 15 living rat growth plates exposed to varying media osmolarities ( approximately 0-580 mOsm). The dimensions of cell volume swelling in hypotonic media were different to the preferential lengthening seen in vivo, confirming the complexity of directional cell volume increase. Boyle-van't Hoff analysis of cell volume over the range of media osmolarity indicated no significant difference (Student's t-test) in the osmotically inactive fraction, 39.5 +/- 2.9% and 47.0 +/- 4.3% (n = 13) for proliferative and hypertrophic zones, respectively, or the sensitivity of volume to changes in media osmolarity (proliferative 15.5 +/- 0.8 and hypertrophic zone 15.5 +/- 1.2%volume . Osm). The osmotic fractions did not change as chondrocytes progress from proliferative to hypertrophic regions of the growth plate. Our data suggest cell volume increase by hypertrophy may play a greater role in cell enlargement than swelling, and should be re-evaluated as a mechanism responsible for growth plate chondrocyte volume increase and hence bone elongation.     

Water of hydration in the intra- and extra-cellular environment of human erythrocytes

The proton nuclear magnetic resonance (NMR) titration method (which requires measurement of the relaxation rate at multiple measured levels of dehydration) was applied to the analysis of human erythrocytes, a hemoglobin solution, plasma, and serum. The results allowed identification of bulk water and four motionally perturbed water of hydration subfractions. Based on previous NMR studies of homopolypeptides we designated these subfractions as superbound, irrotationally bound, rotationally bound, and structured. The total water of hydration (sum of both structured and bound water subfractions) in plasma, serum, and hemoglobin ranged from 2.78 to 3.77 g H2O/g dry mass and the sum of the three bound water subfractions ranged from 1.23 to 1.72 g H2O/g dry mass. The total water of hydration on hemoglobin, as determined by (i) spin-lattice (T1) and spin-spin (T2) NMR data, (ii) quench ice-crystal imprint size, (iii) calculations based on osmotic pressure data, and (iv) two other methods, ranged from 2.26 to 3.45 g H2O/g dry mass. In contrast, the estimates of total water of hydration in the intact erythrocytes ranged from 0.34 to 1.44 g H2O/g dry mass, as determined by osmotic activity and spin-lattice titration, respectively. Studies on the magnetic-field dependence of the spin-lattice relaxation rate (1/T1 rho) of solvent water nuclei in protein solutions and in intact and disrupted erythrocytes indicated that hemoglobin aggregation exists in the intact erythrocytes and that erythrocyte disruption decreases the extent of hemoglobin aggregation. Together, the present and past data indicate that the extent of water of hydration associated with hemoglobin depends on the amount of salt present and the degree of aggregation of the hemoglobin molecules.     

On the osmotically unresponsive water compartment in cells

Differences in colligative properties (freezing point, boiling point, vapor pressure and osmotic behavior) between water in living cells and pure bulk water were investigated by re-evaluating reports of the osmotic behavior of mammalian cells. In five different animal cells, osmotically unresponsive water (OUW) values ranged from 1.1 to 2.2 g per g dry mass. Detailed analysis of human red blood cell (RBC) data indicates a major role for hemoglobin OUW-values, aggregation and packing in cell volume regulation that can be explained for the first time in relevant molecular terms.     

The entrance of water into beef and dog red cells

The rate constants for diffusion of THO across the red cell membrane of beef and dog, and the rate of entrance of water into the erythrocytes of these species under an osmotic pressure gradient have been measured. For water entrance into the erythrocyte by diffusion the rate constants are 0.10 ± 0.02 msec.^-1 (beef) and 0.14 ± 0.03 msec.^-1 (dog); the permeability coefficients for water entrance under a pressure gradient of 1 osmol./cm³ are 0.28 See PDF for Equation These values permit the calculation of an equivalent pore radius for the erythrocyte membrane of 4.1 A for beef and 7.4 A for dog. In the beef red cell the change in THO diffusion due to osmotically produced cell volume shifts has been studied. The resistance to THO diffusion increases as the cell volume increases. At the maximum volume, (1.06 times normal), THO diffusion is decreased to 0.84 times the normal rate. This change in diffusion is attributed to swelling of the cellular membrane.     

THE OSMOTIC PROPERTIES OF LIVING CELLS (EGGS OF ARBACIA PUNCTULATA)

We have attempted to answer the question: How nearly ideal, as an osmometer, is the unfertilized Arbacia egg? The following conclusion have been reached: 1. Volumes can be measured accurately over a wide range of pressures since the cell is in general spherical and does not suffer deformation from its own weight or other factors. 2. The product of volume and pressure is approximately constant, if allowance be made for osmotically inactive cell contents. It is computed that from 7 to 14 per cent of cell volume is occupied by osmotically inactive material. 3. Evidence is presented that no appreciable escape of cell contents occurs while the cell is in hypotonic sea water; that, therefore, the semipermeability of the membrane is approximately perfect, so long as injury to the cell is avoided. 4. In comparison with osmotic pressure the influence of other forces, such as elasticity or surface tension, on cell volume must in these experiments be slight.     

Water diffusion permeability of human erythrocytes studied by a pulsed gradient NMR technique

Water diffusion permeability of human erythrocytes has been measured by NMR using a pulsed magnetic field gradient technique. The measurement of exchange rates was based on restricted diffusion of water molecules within red blood cells. This method avoids addition of paramagnetic ions, such as Mn²⁺ and is used in vivo.The mean lifetime of water inside human erythrocytes was found to be 17 ms at 24°C. A sulfhydryl reagent, known to inhibit water osmotic permeability, reduced significantly water diffusion across the red cell membrane.     

Water diffusion permeability of human erythrocytes studied by a pulsed gradient NMR technique.

Water diffusion permeability of human erythrocytes has been measured by NMR using a pulsed magnetic field gradient technique. The measurement of exchange rates was based on restricted diffusion of water molecules within red blood cells. This method avoids addition of paramagnetic ions, such as Mn2+, and is used in vivo. The mean lifetime of water insed human erythrocytes was found to be 17 ms at 24 degrees C. A sulfhydryl reagent, known to inhibit water osmotic permeability, reduced significantly water diffusion across the red cell membrane.     

A model to explain the osmotic pressure behavior of hemoglobin and serum albumin

Previously published osmotic pressure data on hemoglobin and bovine serum albumin were used to determine the osmotically unresponsive solvent volume per unit dry mass of protein. A model is presented that accounts for the osmotic pressure of globular proteins based on a surface-associated osmotically unresponsive solvent volume. The model also accounts for changes in the osmotically unresponsive solvent volume owing to changes in pH, cosolute salt concentration, protein conformation, and protein aggregation.     

Adaptation mechanisms of respiratory blood function in Teleostei

Analysis of osmotic resistance of erythrocytes identified the similarity between marine and freshwater Teleostei and inclination of erythrocytes from freshwater fish to intravascular haemolysis. Structural resistance of hemoglobin was significantly higher in marine species and resistance to dehydration was significantly higher in freshwater fish. The resistance of erythrocytes and hemoglobin in freshwater fish widely varyies depending on species’ inhabitation conditions. Several strategies for stabilization of respiratory function in the blood of Teleostei were formulated as following: (1) a strategy of compensatory type in the fish ontogenesis, (2) formation of different quality resistance to haemolysis of young and mature erythrocytes; (3) variability resistance of hemoglobin to dehydration and (4) transformation of homeostasis of an organism in extreme conditions.     

Osmotic factors of dehardening in cornus Florida L

The killing temperature for cortical cells from the flowering dogwood changes abruptly from −25 C to −15 C during dehardening. Cell sap concentration, minimum critical cell volume, and osmotically inactive cell volume show a progressive change during dehardening, but only cell sap concentration is correlated directly with the killing temperature, showing the same step change. There is a limit to the extent to which hardy dogwood cells can be osmotically reduced in volume. Beyond this limiting volume, the extracellular osmotically can be increased without further volume reduction. Ultimately the cell succumbs, presumably to an osmotic pressure gradient. Nonhardy cells do not exhibit this resistance to shrinkage. The ability to resist volume reduction is probably a crucial factor in the freezing resistance of dogwood cortical cells.     

Effects of red blood cell potassium and hypertonicity on the growth of Plasmodium falciparum in culture

Malarial parasites reproduce asexually inside the erythrocytes of their vertebrate host. Relatively little is known about the interaction between host cell and parasite metabolism. In the present study the effect of host cell cation composition and osmotic shrinkage on in vitro growth and propagation of Plasmodium falciparum in human erythrocytes was investigated. It is shown that throughout the parasite cell cycle, infected cells lose potassium and gain sodium. Compartment analysis of infected cells revealed that host cell cytosol is poor in potassium and rich in sodium while in the parasite this relationship is reversed, indicating that the parasite is able to regulate its ionic composition independently. Parasites proceeded normally through their cell cycle in the presence of the sodium-pump inhibitor ouabain, although host cells lost up to 75-80% of their normal potassium content. Potassium-depleted erythrocytes harboring trophozoites and schizonts also display normal rates of protein synthesis as measured by isoleucine incorporation. Parasite growth was inhibited when infected cells were osmotically shrunken in hypertonic media, but this was not due to parasite dehydration. It is suggested that increased viscosity of host cell cytosol and/or hemoglobin gelation, are responsible for the effect, probably through interference with parasite feeding. The relevance of these results to understanding of the cellular mechanism involved in the inhibiton of parasite growth in deoxygenated sickle-trait erythrocytes is discussed.     

Curves of osmotic fragility calculated from the isotonic areas and volumes of individual human erythrocytes

Theoretical osmotic fragility curves were calculated and drawn by computer using the van't Hoff equation and the isotonic areas and volumes of 1000 individual erythrocytes. We studied the influence on the calculated curves of theoretically altering the fraction of the volume which was osmotically active from 50 to 70%, and of altering the permissible stretch before hemolysis from zero to 10%. With the two assumptions–that the membrane does not stretch before hemolysis, and that the osmotically active fraction of the cell volume is 0.58–it was possible to duplicate the general shape of the standard fragility curve; the exact NaCl concentration, however, at which there was 50% hemolysis was approximately 0.1 gm/100 ml higher than found in vitro. The calculated osmotic fragility curves can be made quantitatively similar to in vitro ones if the following statements are true: the osmotically active volume is 58%, the permissible stretch of the membrane without lysis is 6%, the cell membrane resists a slight osmotic pressure gradient of approximately 0.1 atmospheres, and hemolysis is an all or nothing phenomenon. This set of values for the relevant factors is sufficient but not unique in causing the superposition of the calculated and experimental curves. The frequency distribution of the cells according to the hemolytic salt concentrations (the sodium chloride concentration at which an individual cell just hemolyzes) was skewed positively and was leptokurtic for each of the seven normal subjects studied.     

Factors Affecting Polyamine Accumulation in Barley (Hordeum vulgare L.) Leaf Sections during Osmotic Stress

Turner, L. B. and Stewart, G. R. 1988. Factors affecting polyamineaccumulation in barley (Hordeum vulgare L.) leaf sections duringosmotic stress.-J. exp. Bot. 39: 311–316. Polyamine concentrations in peeled leaf sections of Hordeumvulgare were unaffected by decreases in leaf water potentialif osmotic adjustment took place and leaf turgor was maintained.Putrescine accumulation occurred concomitantly with a decreasein leaf turgor. Increases in the order of 3-to 4-fold were observed.An apparently greater putrescine accumulation (7-fold) occurredwhen leaf sections were osmotically stressed in the presenceof exogenous phosphate ions. This was the result of water lossfrom the tissue and the large decline which occurred in theputrescine levels of control tissue sections incubated withphosphate ions. Putrescine accumulation was at its maximum after4 h osmotic stress. In contrast, proline accumulation took placebetween 4 h and 24 h after the imposition of osmotic stress. Key words: Hordeum vulgare, osmotic stress, polyamine