Osmotic Adjustment and Osmotic Constituents in Roots of Mung Bean Seedlings

Osmotic adjustment in roots of mung bean seedlings (Vigna mungo(L.) Hepper) and the effect of cotyledon excision on the osmoticadjustment were investigated. The major osmotic constituentsin roots of intact seedlings were K⁺, Cl^–, free aminoacids and sugars (glucose, fructose and sucrose). All theseintracellular concentrations distinctly increased under osmoticstress and contributed to about 80% of the intracellular osmoticpressure of the root cell sap. Cotyledon excision remarkablysuppressed both the osmotic adjustment and the elongation inroots. However, the effect of cotyledon excision on intracellularK⁺ and Cl^– concentrations in roots was quite small. Twodifferent mechanisms are likely for the osmotic adjustment inroots. One is the K⁺ and Cl^–-dependent osmotic adjustmentwhich is cotyledon-independent, and the other is the osmoticadjustment dependent on the supply of free amino acids and sugarsfrom cotyledons. (Received September 20, 1986; Accepted January 14, 1987)     

Osmotic Properties of Mitochondria

The osmotic behavior of rat liver mitochondria has been studied in a sucrose medium. The mitochondria behave like a two compartment system. One compartment is permeable to sucrose and has a volume of 1.22 µl/(mg mitochondrial dry weight) in a 272 milliosmol sucrose medium; the second, inaccessible to sucrose, has a volume of 0.555 µl/mg dry weight) under the same conditions. Part of the water in the sucrose inaccessible space is apparently not free to participate in osmotic phenomena. This volume is 0.272 µl/(mg dry weight) under the same conditions. It is suggested that the osmotically inactive water corresponds to the water of hydration of the mitochondrial macromolecules. The volume of the remainder of the water in the sucrose inaccessible space depends inversely on the osmolality of the medium, as is to be expected. The volume of water in the sucrose accessible space is constant, independent of the osmolality of the medium, as is the volume of the mitochondrial framework plus the nonvolatile solutes.     

Osmotic adjustment in Spirulina platensis

Unilateral irradiation of maize (Zea mays L.) seedlings results in a fluence-rate gradient, and hence below saturation, a gradient of the far-red-absorbing form of phytochrome (Pfr). The Pfr-gradients established by blue, red and far-red light were spectrophotometrically measured in the mesocotyl. Based on these Pfr-gradients and the fluence-response curves of phytochrome photoconversion the fluence-rate gradients were calculated. The fluence-rate gradient in the blue (460 nm) was steeper than that in the red (665 nm), which in turn was steeper than that in the far-red light (725 nm). The fluence-rate ratios front to rear were 1:0.06 (460 nm), 1:0.2 (665 nm), and 1:0.33 (725 nm). The assumption that phytochrome-mediated phototropism of maize mesocotyls is caused by local phytochrome-mediated growth inhibition was tested in the following manner. Firstly, the Pfr response curve for growth inhibition was calculated; these calculations were based on measurements of Pfr-gradients and data from red-light-induced phototropism. Secondly, the Pfr response curve for growth inhibition was used as a basis for calculating fluence-response curves for blue-and far-red-light-induced phototropism. Finally, these calculated results were compared with experimental data. It was concluded that the threshold for phytochrome-mediated phototropism of maize mesocotyls reflects the apparent photoconversion cross section of phytochrome whereas the maximal inducable curvature depends on the steepness of the light (Pfr) gradient across the mesocotyl.Abbreviations Pfr far-red-absorbing form of phytochrome - Ptot total phytochrome - Fr far-red light     

Osmotic adaption in Australian mangroves

Young and old leaves of twenty-three mangrove species from northern Queensland (Australia) were investigated for their mineral ion and organic solute content. With a few exceptions, the Na⁺ and the Cl-concentrations calculated on the basis of plant water (p.w.) were close to that of seawater and showed little age-induced changes. In some species, especially in Ceriops tagal, SO₄ ^2- accumulated with increasing leaf age. The most widely distributed organic solutes were pinitol and mannitol, which were stored up to 280 mM plant water. A negative correlation between pinitol and SO₄ ^2- was found in the case of Ceriops tagal. Other compatible solutes known for halophytes, such as proline and methylated quaternary ammonium compounds (MQAC), were present only in a few mangrove species. Proline occurred in two Xylocarpus species, while MQAC were accumulated by Avicennia eucalyptifolia, A. marina, Acanthus ilicifolius, Heritiera littoralis and Hibiscus tiliaceus. In all other species, low molecular weight carbohydrates (LMWC) were the main organic solutes.     

Osmotic responses of maize roots

Water and solute relations of excised seminal roots of young maize (Zea mays L) plants, have been measured using the root pressure probe. Upon addition of osmotic solutes to the root medium, biphasic root pressure relaxations were obtained as theoretically expected. The relaxations yielded the hydraulic conductivity Lp _r) the permeability coefficient (P _sr), and the reflection coefficient (σ _sr) of the root. Values of Lp _r in these experiments were by nearly an order of magnitude smaller than Lp _r values obtained from experiments where hydrostatic pressure gradients were used to induce water flows. The value of P _sr was determined for nine different osmotica (electrolytes and nonelectrolytes) which resulted in rather variable values (0.1·10^-8–1.7·10^-8m·s^-1). The reflection coefficient σ _sr of the same solutes ranged between 0.3 and 0.6, i.e. σ _sr was low even for solutes for which cell membranes exhibit a σ _s≈1. Deviations from the theoretically expected biphasic responses occured which may have reflected changes of either P _sr or of active pumping induced by the osmotic change. The absolute values of Lp _r, P _sr, and σ _sr have been critically examined for an underestimation by unstirred layer effecs. The data indicate a considerable apoplasmic component for radial movement of water in the presence of hydrostatic gradients and also some solute flow byppassing root protoplasts. In the presence of osmotic gradients, however, there was a substantial cell-to-cell transport of water. Cutting experiments demonstrated that the hydraulic resistance for the longitudinal movement of water was much smaller than for radial transport except for the apical ends of the segments (length=5 to 20 mm). The differences in Lp _r as well as the low σ _sr values suggest that the simple osmometer model of the root with a single osmotic barrier exhibiting nearly semipermeable properties should be extended for a composite membrane model with hydraulic and osmotic barriers arranged in series and in parallel.     

Osmotic adjustment in marine yeast

The effect of environmental salinity on cell growth, and onthe composition and accumulation of compatible solutes, or osmotica,of five yeast strains (Aureobasidium pullulans, Candida sp.,Cryptococcus albidus var. albidus, Debaryomyces hansenii andRhodotorula rubra) was compared. All these yeast were isolatedfrom manne environments, but were able to grow in the absenceof salt and should therefore be considered as halotolerant strains.According to their specific cell growth rates at different saltconcentrations, these strains vary in their capacity to osmoticallyadjust to modifications in external salinity. Candida sp. appearsto be the most sensitive since the maximum salt concentrationat which it can grow is 1.54 mol 1^-1 NaCl; however, it showedthe highest specific cell growth in the range of 0 to 1.54 mol1^-1 NaCl. Aureobasidium pullulans, on the other hand, showedthe lowest specific growth rate, but the highest halotolerancerange from 0 to 5.13 mol 1^-1 NaCl. Debaryomyces hansenii, incontrast, showed higher specific growth at this salinity rangeCryptococcus albidus var. albidus and Rhodotorula rubra showedsimilar specific cell growth rate values and halotolerance between0 and 2.45 mol 1^-1 NaCl. The protein and carbohydrate contentof the biomass of the different yeast cells, as a result ofexternal salinity vanation, remained practically constant. Themost important effects of the increase in salt concentrationin the culture medium were the reduction of cell volume andthe accumulation of low-molecular-weight metabolites (LMWM).which appear to act as osmoregulators. Glycerol was found asthe major compatible solute in the different marine yeasts studiedherein with a total contribution of 64–96% of the internalcell osmolarity. Other LMWM, like carbohydrates and amino acids,contributed to a lesser extent to compensate for the rise inosmotic pressure promoted by the salinity of the external environment.     

Osmotic relations of nerve fiber

Summary The volumetric elastic modulus of the sheath and the osmotic swelling pressure of the axoplasmic polymer network of the giant axon ofLoligo vulgaris were measured. Evidence was obtained that (1) the elastic modulus of the sheath, (2) the swelling pressure of axoplasm, and (3) theeffective osmotic pressure difference due to mobile solutes determine axonal volume. The contributions of the sheath and the axoplasm were significant because theeffective osmotic pressure due to mobile solutes was a small fraction of thetheoretical bulk osmotic pressure due to these solutes. The giant axon was converted from an imperfect to a near perfect osmometer by minimizing the contribution of the sheath and the axoplasmic gel.The early experiments were undertaken in the Stazione Zoologica, Naples, and the Democritus Nuclear Research Center, Athens, Greece; the more recent experiments were undertaken in facilities provided by Prof. N. Nikolaou, Aegina, Greece.     

Osmotic sensitivity of canine spermatozoa

The objective of this study was to determine osmotic tolerance of canine spermatozoa. The study comprised three experiments: (1) spermatozoa suspended either in an egg yolk-citrate (EYC) extender or in Kenney skim milk extender were exposed to NaCl solutions ranging from 290 to 1500 mOsm; (2) spermatozoa suspended in EYC were exposed to 550 to 1500 mOsm solutions of glucose, galactose, or fructose; and (3) spermatozoa suspended in EYC or glucose-bovine serum albumin (G-BSA) were exposed to 0.6 M (approximately 900 mOsm) or 1.2 M (approximately 1600 mOsm) solutions of glycerol, ethylene glycol (EG), or dimethyl sulfoxide (Me(2)SO). In all experiments, motility and membrane integrity of spermatozoa were assessed after they were diluted into isotonic medium at 37 degrees C. Exposure of canine spermatozoa to solutions of either NaCl or monosaccharides at osmolalities >500 mOsm caused a significant reduction of motility (P<0.01). Motility of spermatozoa was more affected by osmotic stress than their membrane integrity. Osmotic sensitivity of canine spermatozoa was dependent on the type of extender; spermatozoa suspended in the Kenney extender were more resistant to osmotic stress than those suspended in the EYC extender. Despite their sensitivity to exposure to high concentrations of nonpermeating agents, canine spermatozoa were rather resistant to exposure to glycerol and EG. However, Me(2)SO was toxic to canine spermatozoa; motility was substantially reduced after spermatozoa were exposed to 0.6 M Me(2)SO. The type of extender also affected the sensitivity of canine spermatozoa to Me(2)SO; spermatozoa suspended in the EYC extender were more resistant than those suspended in G-BSA. It was concluded that canine spermatozoa are sensitive to osmotic stress, but are tolerant to shrinking and swelling caused by exposure to permeating cryoprotectants.     

Osmotic properties of human lymphocyte

The osmotic properties of human lymphocytes isolated from 15 ml of venous blood were examined. Measurements of the permeability of the membrane to water under an osmotic gradient were also made. The Boyle-Van't Hoff relation held very well for the human lymphocyte when the cells were shrunken in hyperosmotic media to concentrations twice isosmotic. The volume of osmotically inactive material or "b" value averaged 32% of the mean corpuscular volume. These values were independent of temperature. Ponder's R ranged between 0.8 and 0.9. The average value for Lp, the hydralic coefficient was 0.46 mu/min atm +/- 0.02 (S.E.M.) at 25 degrees C. No significant effect of age, sex, or race was noted. The effect of temperature between 10 degrees C and 37 degrees C was measured and heats of activation between 11.1 and 17.4 kcal/mole were calculated with a mean of 14.1 kcal/mole +/- 1.6 (S.E.M.). Concanavalin A at 10 microgram/1.5 X 10(6) lymphocytes produced blastogenesis of 25% or more of the lymphocytes without clumping, agglutination, or toxicity. The mean corpuscular volume increased by 21% after 72 hours due to an increase in the "b" value which increased by 80%. The volume of free water remained constant. Histograms of the distribution of cell volumes showed that volume changes were uniform throughout the population with no evidence of agglutination of clumping. The significance of these results is discussed in the context of membrane fluidity and the state of intracellular water.     

Osmotic flow caused by polyelectrolytes

Osmotic flow of water caused by high concentrations of anionic polyelectrolytes across semipermeable membranes, permeable only to solvent and simple electrolyte, has been measured in a newly designed flow cell. The flow cell features small solution and solvent compartments and an efficient stirring mechanism. We have demonstrated that, while the osmotic pressure of the anionic polyelectrolytes is determined primarily by micro-counterions, the osmotic flow is determined by solution-dependent properties as embodied in the hydrodynamic frictional coefficient which is determined by the polymer backbone segment of the polyelectrolyte. The variation of the osmotic permeability coefficient, L(p)(o), with concentration and osmotic pressure closely correlated with the concentration dependence of this frictional coefficient. These studies confirm previous work that the kinetics of osmotic flow across a membrane impermeable to the osmotically active solute is primarily determined by the diffusive mobility of the solute.     

Osmotic control of bilayer fusion

We have used photography and capacitance measurement to monitor the steps in the interaction and eventual fusion of optically black lipid bilayers (BLMs), hydrostatically bulged to approximately hemispherical shape and pushed together mechanically. A necessary first step is drainage of aqueous solution from between the bilayers to allow close contact of the bilayers. The drainage can be controlled by varying the osmotic difference across the bilayers. If the differences are such as to remove water from between the bilayers, fusion occurs after a time that depends on the net osmotic difference and the area of contact. If there is an osmotic flow of water into the space between the bilayers, fusion never occurs. In the fusion process, a single central bilayer forms from the original apposed pair of bilayers. The central bilayer may later burst to allow mixing of the two volumes originally bounded by the separate bilayer; the topological equivalent of exocytosis.