Na+, K+ and Cl- in Xylem Sap Flowing to Shoots of NaCl-Treated Barley

Munns, R. 1985. Na⁺, K⁺ and Cl^– in xylem sap flowing toshoots of NaCl-treated barley.—J. exp. Bot. 36: 1032–1042. Na⁺, Cl^– and K⁺ concentrations were measured in xylemsap obtained by applying pressure to the roots of decapitatedbarley plants grown at external [NaCl] of 0, 25, 50, 100, 150and 200 mol m^–3. For any given NaCl treatment, ion concentrationsin the xylem sap were hyperbolically related to the flux ofwater. Ion concentrations in sap collected at very low volumefluxes (without applied pressure) were 5–10 times higherthan in sap collected at moderate fluxes (under pressure). Fora given moderate volume flux, Na+ concentration in the xylemsap, [Na⁺]_x, was only 4.0 mol m^–3 at external [NaCl] of25–150 mol m^–3, and increased to 7.0 mol m^–3at 200 mol m^–3. [Cl-]x showed a similar pattern. Thisshows there would be little difference in the rate of uptaketo the shoot of plants at 25–150 mol m^–3 externalNaCl and indicates little change even at 200 mol m^-3 NaCl becausetranspiration rates would be much lower. Thus the reduced growthof the shoot of plants at high NaCl concentrations is not dueto higher uptake rates of Na⁺ or Cl^–. The fluxes of Na⁺, Cl^– and K^– increased non-linearlywith increasing volume flux indicating little movement of saltin the apoplast. The flux of K⁺ increased even when [K⁺]_x wasgreater than external [K⁺], indicating that membrane transportprocesses modify the K⁺ concentration in the transpiration streamas it flows through the root system. Key words: -Xylem sap, Na⁺, K⁺, Cl^– fluxes, salinity, barley     

Ion and Glycerol Concentrations in 12 Isolates of Dunaliella

Ginzburg, M., and Ginzburg, B. Z., 1985. Ion and glycerol concentrationsin 12 isolates of Dunaliella.—J. exp. Bot. 36: 1064–1074. Twelve isolates of Dunaliella with average cell volumes rangingfrom 50 to 1400x10^–18 m³ were grown in batch culture at0.5 M or 2.0 M NaCl. Glycerol and ions (Na⁺, K⁺, Mg²⁺, CI^–,phosphate) were measured in log-phase cultures. The contentsof Mg²⁺, K⁺ and phosphate per cell were found to be a functionof cell-volume. Cell glycerol, Na⁺ and Cl^– were functionsof cell-volume and of the NaCl concentration in the medium.Solute concentrations were calculated from the measured cell-volumesand from the ³H₂O content of pellets corrected for intercellularspace using Blue Dextran. Cell glycerol was found to accountfor about one-half of the expected osmolarity, the remainderbeing largely accounted for by Na⁺ and CI^–. Key words: —Dunaliella, isolates, glycerol, ion concentrations     

Interaction of Salinity and Anaerobiosis in Barley and Rice

Barley and rice at the early tillering stage were exposed simultaneouslyto anaerobiosis and high [NaCl]. Barley was grown at 0.5, 70,and 125 mol m^–3 NaCl, and rice at 2, 20, 40, and 80 molm^–3 NaCl. Surprisingly, anaerobiosis only slightly aggravatedthe adverse effects of high [NaCl] on root and shoot growthof both species. For rice and barley grown under aerobic conditions, high [NaCl]increased [Na⁺] and [Cl^–] and decreased [K+] in both rootsand shoots. However, the changes in ion concentrations in theshoots were smaller for rice than for barley. For roots of barley, anaerobiosis decreased [Na⁺], [Cl^–],and [K⁺] at both low and high [NaCl], possibly as a result ofinhibition of active ion accumulation. For barley shoots, anaerobiosisincreased [Na⁺] and [Cl^–], but only at high salinity;in contrast, [K⁺] was reduced by anaerobiosis at both low andhigh [NaCl]. These results indicate that anaerobiosis slightlyincreased the permeability of the barley root system to Na+and Cl^–. For rice, the most important interaction between salinity andanaerobiosis occurred in the shoots, where anaerobiosis increased[Na⁺] and decreased [K⁺], particularly at 40 and 80 mol m^–3NaCl, while there was no interaction between anaerobiosis andsalinity for Cl^– uptake. It is therefore suggested thatanaerobic treatment of rice decreased the selectivity for K⁺over Na⁺ of cation transport to the shoots, at least for plantsgrown at high salinities.     

Effects of Anoxia on Solute Loss from Beetroot Storage Tissue

Beetroot storage tissue that had been aged in an aerated solutionwas particularly suited for studies of solute losses duringanoxia;retention of betacyanin being a good indicator of tonoplastintegrity. During anoxia, loss of K⁺ was nearly always greater than thatof Na⁺ while Cl^– loss was intermediate. Supply of glucoseduringageing increased the tolerance of beetroot tissue to anoxia.In these tolerant tissues, there were three phases of soluteloss.During the first phase, losses of K⁺ and amino acids wererapid, presumably due to membrane depolarization from –156to –95 mV. In contrast, losses of Na⁺ and Cl^– wereslow. During the second phase, K⁺ loss had decreased to a lowrate, while losses of Na⁺ and Cl⁺ remained slow. Furthermore,the membrane potential remained at –95 to –90mV,which was consistent with the diffusion potential estimatedfrom the modified Goldman equation. In the third and final phase,loss of K⁺ Na⁺ Cl⁺,sugars, and amino acids began to increase,soon followed by loss of betacyanin. Tissues that had lost their betacyanin during anoxia were irreversiblyinjured, as shown by rapid uptake of Evans Blue and afailureto take up K⁺ , Na⁺ and Cl⁺ during re–aeration. In contrast,tissues which had retained their betacyanin did not take upEvansBlue, but took up substantial amounts of K⁺ , Na⁺ , and Cl^–after re–aeration. After return to air for 1.5 h, tissuethat hadretained its betacyanin had a membrane potential of– 154 mV. Key words: Anoxia, beetroot, solute, membrane potential     

The intercellular distribution of vacuolar solutes in the epidermis and mesophyll of barley leaves changes in response to NaCl

Concentrations of inorganic and organic solutes were measuredin sap extracted from individual mesophyll and epidermal cellsof the third leaf of barley. During the development of the thirdleaf plants were grown in various salt solutions (NaCl; 2, 50,100, and 150 mM, KCI; 100 mM or KNO₃; 100 mM). Leaves were analysed2–4 d after full expansion. Cell-sap was extracted usinga modified pressure probe and analysed for its osmolality, concentrationsof P, Na⁺ K⁺ Ca²⁺, and Cl^– and, in some cases, of nitrate,hexoses and total amino acids. Salt treatment caused differentialchanges in the concentrations of solutes in mesophyll and epidermalcells, but did not affect the basic pattern of solute compartmentationbetween these tissues. Calcium was found at osmotically significantconcentrations only in the epidermis, whereas P and organicsolutes were almost exclusively found in the mesophyll. Chlorideand Na⁺ accumulated preferentially in the epidermis, althoughmesophyll concentrations also increased considerably. At 150mM external NaCl, mesophyll cells contained 302 mM Na and 167mM Cl^–, compared to 29 mM Na⁺ and 16 mM Cl^– in thecontrol. Mesophyll Cl^– levels were even higher in the100 mM KCl treatment (216 mM) where mesophyll and epidermalK⁺ accumulated to 424 and 491 mM, respectively. These huge increasesin mesophyll Na⁺ Cl^– and K⁺ were not associated with abreakdown in leaf performance since net rates of photosynthesisdecreased only by less than 20%. Under control (2 mM NaCl) conditions,solutes followed patterned gradients between the various epidermalcell types. The extent of these gradients changed with leafage. During 50 mM NaCl treatment, gradients in Cl^–, nitrateand malate concentrations progressively disappeared, with malateconcentrations approaching zero. Potassium and Na⁺ exhibitedaltered distribution profiles, whereas Ca²⁺ distribution wasunaffected. NaCl-dependent increases in osmolalities differedbetween cells. Exposure of plants to 150 mM NaCl caused qualitativelysimilar changes in both epidermal solute and osmolality profiles,although absolute values differed from those at 50 mM NaCl.In particular, epidermal Cl^– and Na⁺ increased to about500 mM and K⁺ disappeared (<<5 mM) from the vacuole ofcertain epidermal cell types completely. Key words: Barley leaf epidermis, mesophyll, salt stress, single-cell analysis, vacuolar solutes     

Influence of Age of Culture and Light Intensity on Solute Concentrations in Two Dunaliella Strains

Two strains of Dunaliella, one halotolerant and one halophilic,were grown in batch culture at NaCl concentrations varying from500 mol m^–3 to 3000 mol m^–3. Measurements were madeof the following solutes: glycerol, Na⁺, K⁺, Mg²⁺, Cl^–,phosphate in the cells of logarithmic and of stationary-phasecultures. The method used was to separate the cells from thebulk of the medium by differential density centrifugation. Soluteconcentrations were calculated using Blue Dextran as a markerfor extracellular space. It was found that in log-phase cells,glycerol accounted for one-half to two-thirds of the total cellsolute concentration, the remainder being largely accountedfor by Na⁺ and Cl^–. In the stationary phase glycerol felland Na⁺, plus Cl^–, rose. Light intensity was found toaffect cell volume and solute content. The means whereby soluteconcentrations are controlled is discussed. Key words: Osmoregulation, Ion concentrations, Dunaliella     

Measurements of Ion Concentrations and Fluxes in Dunaliella parva

Measurements of K⁺, Na⁺, and Cl^– were made on a halotolerantstrain of Dunaliella growing at 500 mM NaCl, 25 ?C, and a relativelylow light intensity (6000 Lx). Much effort was spent in searchingfor a means of measuring the extracellular volume of fluid trappedbetween the cells of centrifuged pellets. All of the sugarstried as markers were rejected because they were found to bedigested in the cell suspension. The most suitable marker wasfound to be [¹⁴C]polyethylene glycol² (mol. wt. 4000); althoughthis substance was apparently adsorbed to the cell exterior,it was found possible to correct for adsorption and then obtaina reasonable figure for the trapped fluid. The final concentrationsof cell K⁺ and Na⁺ were 128 ? 53 mM and 131 ? 117 mM respectively.Cl^– balanced the sum of K⁺ Na⁺. Influxes of ²²Na⁺, ⁴²K⁺,and ³⁶C1^– were measured in cells in which the ions werein the steady state. Averages of 610 and 6.6 nmol m^–2s^–1 were obtained for Na⁺ and K⁺ respectively. Cl^–influx was divided into 2 phases with values of 1540 and 178mmol m^–2 s^–1. The faster influx was considered tobe across the outer cell membrane. The membrane responsiblefor the slower influx has not been identified. By comparingvalues of the potential difference calculated from the Nernstand Goldman equations, it was concluded that Na⁺ and K⁺ areprobably controlled by active mechanisms, whereas cell Cl^–is likely to be at thermodynamic equilibrium with the medium.     

Effect of NaCI Salinity on Flows and Partitioning of C, N, and Mineral Ions in Whole Plants of White Lupin, Lupinus albusL.

Plants of Lupinus albus L., cv. Ultra, were grown hydroponicallywith NO₃^–-nutrition for 51 d under control (0.05 mol m^–3Na⁺ and 10 mol m^–3 Cl^–) and saline (40 mol m^–3NaCI) conditions. Plants were harvested 41 and 51 d after germinationand analysed for content and net increment of C, N and the mineralcations K⁺, Na⁺, Mg²⁺, and Ca²⁺ and the anions Cl^–, NOJ,malate, phosphate, and SO₄^2–. Roots, stem interaodes,petioles and leaflets were analysed separately. During the studyperiod net photosynthesis, respiratory losses of CO₂ from shootand root and the composition of the spontaneously bleeding phloemsap and the root pressure xylem exudate were also determined.Using molar ratios of C over N in the transport fluids, incrementsof C and N, and photosynthetic gains as well as respiratorylosses of C, the net flows of C and N in the xylem and phloemwere then calculated as in earlier studies (Pate, Layzell andMcNeill, 1979a). Knowing the carbon flows, the ratios of ionto carbon in the phloem sap, and ion increments in individualorgans, net flows of K⁺, Na⁺, and Cl^– over the study periodwere also calculated. Salt stress led to a general decrease of all partial componentsof C and N partitioning indicating that inhibitions were notdue to specific effects of NaCI salinity on photosynthesis oron NO₃ uptake. However, there were differences between variouslyaged organs, and net phloem export of nitrogenous compoundsfrom ageing leaves was substantially enhanced under saline conditions.In addition, NO₃^–reduction in the roots was specificallyinhibited. Uptake and xylem transport of K⁺ was more severelyinhibited than photosynthetic carbon gain or NO₃^– uptakeby the root. K⁺ transport in the phloem was even more severelyrestricted under saline conditions. Na⁺ and Cl^– flowsand uptake, on the other hand, were substantially increasedin the presence of salt and, in particular, there were thenmassive flows of Na^– in the phloem. The results are discussedin relation to the causes of salt sensitivity of Lupinus albus.The data suggest that both a restriction of K⁺ supply and astrongly increased phloem translocation of Na⁺ contribute tothe adverse effects of salt in this species. Restriction ofK⁺ supply occurs by diminished K⁺ uptake and even more by reducedK⁺ cycling within the plant. Key words: Lupinus albus, salt stress, phloem transport, xylem transport, partitioning, carbon, nitrogen, K⁺, Na⁺, CI^–     

The Ionic Relations of Acetabularia mediterranea

The concentrations of K⁺, Na⁺, and Cl^– in the cytoplasmand the vacuole of Acetabularia mediterranea have been measured,as have the vacuolar concentrations of SO₄^–– andoxalate. The electrical potential difference between externalsolution, and vacuole and cytoplasm has been measured. The resultsindicate that Cl^– and SO₄^–– are probably transportedactively into the cell, and that active transport of Na⁺ isoutwards. The results for K⁺ are equivocal. The fluxes of K⁺,Na⁺, Cl^–, and S0₄^–– into the cell and theeffluxes of Na⁺ and Cl^– have been determined. The Cl^–fluxes are extremely large. In all cases the plasmalemma isthe rate-limiting membrane for ion movement. A technique isdescribed for the preparation of large, completely viable cellfragments containing only cytoplasm, with no vacuole.     

Biophysical and Biochemical Regulation of Cytoplasmic pH in Chara corallina during Acid Loads

The contribution of membrane transport to regulation of cytoplasmicpH in Chara corallina has been measured during proton-loadingby uptake of butyric acid. In the short-term (i.e. up to 20min) uptake of butyric acid is not affected by removal of externalK⁺, Na⁺ or Cl^– but over longer periods uptake is decreased(by 20–50% in different experiments) in the absence ofexternal Na⁺ or, sometimes, K⁺. Influxes of both Na⁺ and K⁺increase temporarily after addition of butyrate, Na⁺ immediatelyand K⁺ after a lag. Effects on Cl^– influx are small butCl^– efflux increases enormously after a short lag. Anapproximate comparison of internal butyrate with changes inthe concentration of K⁺, Na⁺, and Cl^– suggests that initially(i.e. for a few min) cytoplasmic pH is determined by bufferingand possibly by some decarboxylation of organic acids (biochemicalpH regulation), and that biophysical pH regulation involvingefflux of H⁺ balanced by influxes of K⁺, Na⁺ and especiallyefflux of Cl^– progressively becomes dominant. When butyric acid is washed out of the cells, cytoplasmic pHis restored completely or partially (depending on the butyrateconcentration used) and this is independent of the presenceor absence of external Cl^–. Where Cl^– is present,its influx is relatively small. It is suggested that cytoplasmicpH is then controlled biochemically, involving the synthesisof an (unidentified) organic acid and the accumulation of acidicanions in place of butyurate lost from the cell. During thesecond application of butyrate, net Cl^– efflux is small:it is suggested that control of cytoplasmic pH then involvesdecarboxylation of the organic acid anions. The questions of the source of Cl^– lost from the cell(cytoplasm or vacuole) and of possible cytoplasmic swellingassociated with the accumulation of butyrate are discussed. Key words: Chara corallina, butyric acid, cytoplasmic pH, membrane transport     

Effects of Sodium Chloride Stress on Callus Cultures of Cicer arietinum L. cv. BG-203: Growth and Ion Accumulation

Growth and ion accumulation were measured in callus culturesof Cicer arietinum L. cv. BG-203, grown on media supplementedwith 0–200 mol m^–3 NaCl. Fresh and dry weights decreasedat concentrations ranging from 100–200 mol m^–3,the reduction being greater during the third and fourth weeksof culture. Slight stimulation of growth was observed at 25and 50 mol m^–3 NaCl. There was also a decrease in tissuewater content (fresh weight: dry weight) at 100–200 molm^–3 NaCl. The concentration of Na⁺ and Cl^– in thetissue increased with increasing salinity of the medium. Mostof the accumulation of these ions occurred by the first weekwhile significant growth inhibition became apparent by onlythe third week of culture. Tissue K⁺ and Mg²⁺ decreased withincreasing salinization, the decrease being greater in K⁺ levels.Levels of Ca²⁺, however, were maintained throughout the experimentalrange. Key words: Cicer arietinum, NaCl stress, Callus cultures, Ion accumulation     

Electrophysiological Measurements on the Root of Atriplex hastata

The ion contents and membrane potentials of the cells of young,hydroponically cultured seedlings of Atriplex hastata L. var.salina, Wallr. have been measured at several different NaClconcentrations. The total tissue concentrations of Na⁺ and Cl^–increase as external NaCl increases, but there is always a markedexcess of internal Na⁺ over Cl^–; this is balanced by endogenousorganic anion formation with a concomitant extrusion of H⁺ tothe bathing solution. Membrane potentials of the root cells remain essentially invariantwith changes in external NaCl at approx. –130 mV; thereis no evidence of a radial gradient of potential across theroot. The potential seems to contain a cyanide-sensitive electrogeniccomponent, also invariant with NaCl concentration, of about–70 mV, and a diffusion component. The electrogenic componentseems likely to be a H⁺ efflux, probably through a H⁺ uniportATPase.     

IONIC COMPOSITION AND ELECTRIC RESPONSE OF LAMPROTHAMNIUM SUCCINCTUM

The concentrations of K⁺, Na⁺ and Cl^– in the cytoplasmof Lamprothamnium succinctum, a brackish water Characeae, areabout 137, 47 and 86 mM respectively. The concentration of K⁺in the cytoplasm is of the same order as that in the cell sap,while the concentrations of Na⁺ and Cl^– are much lowerthan those in the cell sap (i.e., 140 mM Na⁺, 370 mM Cl^–).In the brackish water, in which the plant grows, the internodesis never excitable electrically. However, it acquires excitabilitywhen it is kept in a mannitol-pond water. The action potentialthus elicited is accompanied by a temporary cessation or slowdown of the cytoplasmic streaming. ¹This work was supported by Research Grants from the Ministryof Education of Japan     

Effects of Na2SO4, K2SO4 and KCl on Growth and Ion Uptake of Callus Cultures of Vaccinium corymbosum L. cv. Blue Crop

Non-selected and Na₂SO-, K₂SO₄- or KCl-selected callus culturesof Vaccinium corymbosum L. cv. Blue Crop were grown on mediasupplemented with 0, 25 and 50 mM Na₂SO₄ (non-selected and Na₂SO(-selectedonly), 0, 25 and 50mMK₂SO₄ (non-selected and K₂SO₄-selectedonly) or 0, 50 and 100 mM KCl (non-selected and KCl-selectedonly). On all media, growth of selected callus (on a fresh-weightor dry-weight basis) was greater than that of non-selected callus,and selected callus grew optimally on the level and type ofsalt on which it was selected. Selected callus was friable andmaintained a higher f. wt:d. wt ratio. Tissue water potentialin selected callus was more negative than in non-selected callus. Flame photometry and chloridometry showed Na⁺, K⁺ and Cl^–accumulated in callus to concentrations equal to or greaterthan the initial concentration in the medium. Turbidometry showedthat tissue SO₄^2- concentration was lower than the concentrationin the medium. In most cases selected callus accumulated moreNa⁺, K^sup, SO₄^2– or Cl^– than non-selected callus.Vacuolar ion concentration was measured by electronprobe X-raymicroanalysis, and on most media selected callus had highervacuolar ion concentrations than non-selected callus. SO₄^2–and Cl^– were accumulated in the vacuoles at concentrationshigher than the external medium, but vacuolar Na⁺ concentrationdid not reach external concentration on Na₂SO₄ and on potassiumsalts was maintained between 12 and 17 mM. Vacuolar K⁺ concentration(approx. 142–191 mM on no salt) decreased on Na₂SO₄ andincreased on K₂SO₄ and KCl. There was no precise correlation between total or specific ionaccumulation (Na⁺, K⁺, SO₄^2– and Cl^– and fresh-weightyield. Results suggest that selection results in adaptationin response to decreased water potential of the medium. Vaccinium corymbosum, blueberry, electronprobe X-ray microanalysis, callus, in vitro selection, salt tolerance, KCl, K₂SO₄, Na₂SO₄     

The Effect of Salinity on Germination and Its Correlation with K+, Na+, Cl- Accumulation in Germinating Seeds of Triticum aestivum L. cv. Akbar

NaCl salinity stress consistantly decreased the rate of germinationof wheat. GA alone or in combination with kinetin alleviatedthe inhibitory effect of salinity on germination. However, kinetinfurther decreased the rate of germination under NaCl salinitystress. NaCl salinity increased accumulation of Na⁺ and Cl^–while it decreased K⁺ accumulation in germinating seeds. GAcaused an increase in K⁺ accumulation and a decrease in Cl^–accumulation in the germinating seeds while kinetin increasedCl^– accumulation in salinity stressed plants. The co-relationbetween the effect of salinity on germination and that on accumulationof ions is discussed. (Received February 12, 1992; Accepted August 4, 1992)     

Determination of Volume of Dunaliella Cells by Lithium Dilution Measurements and Derivation of Internal Solute Concentrations

A method has been developed to measure the cell volume of theunicellular green alga Dunaliella parva 19/9 using Li⁺ measurementsonly. Concentrations of internal solutes can also be calculatedif they are assayed in the same samples as Li⁺. We found thatD. parva cells grown in 0.4 kmol m^–3 NaCl have an averageaqueous cell volume of 65.1 ?2.9 µm³, a K⁺ concentrationof 126?6 mol m^–3, a Na⁺ concentration of 11?11 mol m^–3and a glycerol concentration of 615?27 mol m–3 (n= 12).Algae grown in 1.5 kmol m^–3 NaCl have an average aqueouscell volume of 131 ?7.5 µm³, a K⁺ concentration of 109?4mol m^–3, a Na⁺ concentration of 10?39 mol m^–3 anda glycerol concentration of 1 425?59 mol m^–3 (n = 12).These results indicate that D. parva cells adapted to high salinitieshave larger cell volumes than those adapted to lower salinities.However, there is no evidence for a significant difference ininternal Na⁺ concentration, despite the almost 4-fold differencein the concentration of external NaCl. The intracellular glycerolconcentration alone accounts for 65% and 54%, respectively,of the osmotic balance in low and high salt grown cells. Key words: Dunaliella, cell volume, intracellular solutes     

Osmotic and Ionic Regulation in Chara L-cell Fragments

Ion absorption from rather complicated artificial pond water(APW) by cell fragments having a lower osmotic pressure thanthe intact internodal cell (L-cell fragments) was studied. L-cellfragments were prepared by taking advantage of trans cellularosmosis and ligating the cell with thread. The results wereas follows: (1) L-cell fragments absorbed more K⁺ than Na⁺ fromaKCL + NaCl mixture in the presence of Ca²⁺, Mg²⁺ and SO₂₄ inthe light; (2) the influx of KCI was larger than that of KNO₃;(3) the amount of positive charge carried by K⁺, Na⁺ and Mg²⁺across the cell membrane balanced well with the amount of negativecharge carried by Cl^– in Cl^–-containing and NO₃^–-free APW; (4) no conclusion could be made as to whether ornot the rule of electro neutrality held for the K⁺, Na⁺, Ca²⁺and NO₃^– fluxes across the cell membrane, because dilutedKNO₃ is unstable; (5) L-cell fragments in KCl-containing APWsurvived longer than those in KNO₃-containing and Cl^–-free APW; (6) after incubation in KNO₃-containing and Cl^–-freeAPW, L-cell fragments absorbed a great amount of KCI immediatelyafter being transferred to KCl-containing and NO₃^– -freeAPW; and (7) lowering the turgor pressure of the intact cellby raising the external osmotic pressure did not induce ionflux into the cell. Thus, we concluded that the L-cell fragmentsabsorbed ions from the external solution not because of theirlower turgor pressure, but because of the diluted ion concentrationof the cytoplasm and the vacuole. The electroneutrality ruleheld, at least, for K⁺, Na⁺, Mg²⁺ and Cl^– influxes acrossthe cell membrane inthe KCl-containing and NO₃^–-free APW.These results were analyzed on the basis of an extended poremodel which presumed the existence of ATP-dependent processesin the membrane, and suggested that K⁺, Na⁺ and Mg₂₊ inflowsinto an L-cell fragment are likely to be induced by active Cl^–inflow. (Received May 18, 1987; Accepted September 29, 1987)     

Diurnal K+ and Anion Transport in Phaseolus Pulvinus

Diurnal movement of Phaseolus leaf is caused by deformationof the laminar pulvinus located at the joint of the leaf bladeand the petiole. The plants were cultured in solutions withvarious ion compositions, and changes of K⁺, Na⁺, Ca²⁺, Mg²⁺,Cl^–, NO₃– and P₁ concentrations both in the upperand lower parts of the laminar pulvinus were measured. Culturein 10 mM KCl solution caused an increase in K⁺ and Cl^–concentrations both in the upper and lower parts without anysignificant change in the concentration of NO₃^–; culturein 10 mM KNO₃ solution caused an increase in K⁺ and NO₃^–concentration without any significant change in the concentrationof Cl^–; and culture in 10 mM KH₂PO₄ solution caused anincrease in K⁺ and P₁ concentrations without any significantchange in the concentrations of NO₃- and Cl^–. K⁺ moved from the upper to lower parts or from the lower toupper parts diurnally in all plants cultured in any solutionmentioned above. The main inorganic anion that accompanied thisK⁺ movement was Cl^– in KCl solution, and NO₃^– inKNO₃ solution. When the seedlings were cultured in distilledwater or in KH₂PO₄ solution, neither Cl^– NO₃^– norP₁ accompanied this K⁺ movement. In these cases, mainly H⁺ and/ororganic anions are supposed to move in exchange for and/or incombination with K⁺ movement. (Received November 8, 1982; Accepted June 13, 1983)     

The Effects of Salinity upon Ion Content and Ion Transport of the Marine RedAlga Porphyra purpurea(Roth) C.Ag.

Ion contents and concentrations (K⁺, Na⁺, Cl^–, Ca²⁺, Mg²⁺,SO^2–₄, NO^–₃, HPOJ^2–₄, amino and organic acids)of P. purpurea have been studied in relation to salinity variation.Cells were shown to accumulate large amounts of K⁺ and Cl^–against their respective gradients of electrochemical potentialin all dilute and concentrated seawater media. Active influxof SOJ^2–₄, NO^–₃, and HPOJ^2–₄ is also suggested,while Na⁺ is actively excluded from cells under hyposaline andhypersaline conditions. The relative proportions of individualcomponents of the internal osmotic potential were found to changeaccording to the external salt concentration. KCL forms themajor fraction of _j} in concentrated seawater media while K⁺-aminoacids form the major fraction in dilute seawaters. Other intracellularsolutes comprise less than 15% oft_j, in all media. Unidirectional fluxes of K⁺ and Cl^– were studied by radioisotopicmeans. Fluxes of K⁺ and Cl^– are reduced in hyposalinemedia, as is absolute KCL content per cell. Intracelhilar KCLcontent was also found to be markedly dependent upon externalK⁺ concentration, rather than water potential. Changes in KC1levels induced by salinity variation occur over a 6 h period.     

NaCl Uptake in Roots of Zea mays Seedlings: Comparison of Root Pressure Probe and EDX Data

The extent by which salinity affects plant growth depends partlyon the ability of the plant to exclude NaCl. To study the uptakeof NaCl into excised roots of Zea mays L. cv. ‘Tanker’,two different techniques were applied. A root pressure probewas used to record steady state as well as transient valuesof root (xylem) pressure upon exposure of the root to mediacontaining NaCl and KCl as osmotic solutes. In treatments withNaCl, pressure/time responses of the root indicated a significantuptake of NaCl into the xylem. NaCl induced kinetics were completelyreversible when the NaCl solution was replaced by an isosmoticKCl solution. This indicated a passive movement of Na⁺-saltsacross the root cylinder. Root samples were taken at differenttimes of exposure to NaCl and prepared for X-ray microanalysis(EDX analysis). Radial profiles of ion concentrations (Na⁺,K⁺, Cl^–) were measured in cell vacuoles and xylem vesselsalong the root axis. Na⁺ appeared rapidly in mature xylem (earlymetaxylem) and living xylem (late metaxylem) before it was detectablein vacuoles of the root cortex. EDX results confirmed that thekinetics observed by the pressure probe technique correspondedmainly to an influx of Na⁺-salts into early metaxylem. In latemetaxylem, the uptake of Na⁺ was associated with a decline ofK⁺. The Na⁺/K⁺ exchange indicated a mechanism to reduce sodiumfrom the transpiration stream. Ion localization, ion transport, maize, root pressure, salinity, water relations, X-ray microanalysis, Zea mays