Allosteric and Non-Allosteric Regulation of Rubidium Influx in Barley Roots

Uptake of Rb⁺ was investigated in 6–8-day-old intact barley plants (Hordeum vulgare cv. Kristina), which had been cultivated or pretreated in nutrient solutions with various K⁺ concentrations. The relationship between Rb⁺ influx and the K⁺ concentration of roots appeared to be sigmoidal for plants grown in solutions containing K⁺, indicating regulation of Rb⁺ uptake by allosteric inhibition of the uptake mechanism. Pretreatment of the roots in K⁺-free solutions changed the pattern of uptake and caused the Rb⁺ influx to become linearly related to the chemical Rb⁺ potential of the uptake solution. Pretreatment in K⁺-free solutions probably abolishes the allosteric inhibition of a carrier system.     

Control of K+ (Rb+) influx and transport with changed internal K+ concentration and age in two varieties of barley

The influx of Rb⁺ into the roots of two barley varieties (Hordeum vulgare L. cv. Salve and cv. Ingrid) from a K⁺-free ⁸⁶Rb-labelled nutrient solution with 2.0 mM Rb⁺, was checked at intervals from day 6 to day 18. The control plants were continuously grown in complete nutrient solution containing 5.0 mM K⁺, while two other groups of plants were grown in K⁺-free nutrient solution starting on day 6 and between day 6 and day 9, respectively. The pattern of Rb⁺ influx was similar for both varieties, although their efficiencies in absorbing Rb⁺ were different. The relationship between Rb⁺ influx and K⁺ concentration of the root could be interpreted in terms of negative feedback through allosteric control of uptake across the plasmalemma of the root cells. Hill plots were bimodal, but in the opposite direction. The Hill coefficients, reflecting the minimum number of interacting allosteric binding sites for K⁺ (Rb⁺), were low (≤–3.0). It is discussed whether the threshold value, that is the breaking point in the Hill plot, is indicative of a changed efficiency of transporting units for K⁺ (Rb⁺) transport to the xylem. Moreover, feedback regulation might be involved in transport of K⁺ between root and shoot. The variation in K⁺ concentrations in the roots and shoots of control plants were cyclic but in phase opposition despite an exponential growth. The average K⁺ concentration varied only slightly with age.     

Varietal variation in uptake and utilization of potassium (rubidium) in high-salt seedlings of barley

Seedlings of eleven varieties of barley (Hordeum vulgare L.) showed differences in utilization of K⁺ from a full nutrient solution containing 3.0 mM K⁺. The K⁺ content of both roots and shoots was proportional to the fresh weights and dry weights after a week in the nutrient solution. The K⁺ use-efficiency ratio, which indicates the efficiency of nutrient utilization (mg dry weight produced per mg K⁺ absorbed), differed significantly among the varieties. There was no correlation between influx of Rb⁺ and the content of K⁺. It is suggested that there are wide varietal differences in such genetically-determined properties as ion influx and efflux and net ion transport to the shoot. Further-more, the influx of Rb⁺ was closely linked to transpiration, probably due to a variety-specific non-metabolic part of Rb⁺ influx. Varietal differences in influx of Rb⁺ were more pronounced in high-K⁺ roots than in low-K⁺ roots with maximum rate of Rb⁺ uptake, but the rank of varieties was the same in each case. – Criteria for the selection of K⁺ use-efficient varieties of barley are discussed.     

K+(Rb+) and Ca2+ fluxes in young winter wheat plants exposed to sub-zero temperatures

Ice crystal formation temperature was determined in the region of the crown in one group of 7-day-old intact unhardened high-salt plants of winter wheat (Triticum aestivum L. cv. Weibulls Starke II) with TA (Thermal Analysis) and DTA (Differential Thermal Analysis) methods. After exposure of another group of plants, grown for the first 7 days in the same way as the first group, to various sub-zero temperatures (-1 to 5°C), influx in roots of Rb⁺(⁸⁶Rb⁺) and Ca²⁺(⁴⁵Ca²⁺) and contents of K⁺ and Ca²⁺ were determined at intervals during 7 days of recovery. Ice crystal formation in the crown tissue was probably extracellular and took place at about -4°C. There was a large loss of K⁺ from the roots after treatment at sub-zero temperatures. This loss increased as the temperature of the sub-zero treatment decreased. During recovery, roots of plants exposed to -1, -2 and -3°C gradually reabsorbed K⁺. Reabsorption of K⁺ in roots of plants exposed to -4°C was greatly impaired. Rb⁺ influx decreased and Ca²⁺ influx increased after sub-zero temperature treatments of the plants. Active Rb⁺ influx mechanisms and active extrusion of Ca²⁺ were impaired or irreversibly damaged by the exposure. While Rb⁺ influx mechanisms were apparently repaired during recovery in plants exposed to temperatures down to -3°C, Ca²⁺ extrusion mechanisms were not. The temperature for ice crystal formation in the region of the crown tissue coincides with the temperature at which the plants lost the ability to reabsorb K⁺ and to repair Rb⁺ influx mechanisms during the recovery period. Plants were lethally damaged at temperatures below ?4°C.     

Allosteric Regulation of Potassium Uptake in Plant Roots

In uptake experiments from nutrient solutions containing 2.0 mM K⁺ labelled with ⁸⁶Rb⁺, the relationship between potassium uptake efficiency and internal potassium concentration of the roots, [K⁺]_i was found to be partly sigmoidal for intact plants of spring wheat (Triticum aestivum L.), glasshouse cucumber (Cucumis sativus L.), birch (Betula verrucosa Ehrh.), lingonberry (Vaccinium vitis-idaea L.), Scots pine (Pinus silvestris L.) and Norway spruce (Picea abies (L.) Karst.), The results were interpreted in terms of sigmoidal enzyme kinetics for allosteric regulation. Hill plots of the data gave straight lines at specific [K⁺]_i intervals for the species. The slopes of the lines are the Hill coefficient, which could be regarded as a measure of the minimal number of allosteric sites. The Hill coefficient varied between - 14.4 and - 15.9. When divided by four, these values are fairly consistent with those in the literature. It is suggested that four active uptake sites interact with four groups of allosteric sites, each group containing four such sites, or that one active uptake site interacts with all the allosteric sites. Thus the results are evidence that the mechanism regulating K⁺ uptake is basically similar for the investigated plants. It is the interval of [K⁺]_i mediating highly negatively cooperative allosteric regulation that differs among species. For some of the species, n decreased from about 15 and approached unity at high [K⁺]_i values. This may indicate that only few sites are still available, making cooperativity unimportant. Alternatively high vacuolar [K⁺]_i concentrations may give rise to an incorrect evaluation of data from Hill plots, since the cytoplasmic K⁺ content likely regulates the allosteric mechanism. Moreover, it is suggested that gene-controlled carrier synthesis is responsible for the varying maximum K⁺ uptake efficiency among species.     

Influence of low temperature on regulation of Rb+ and Ca2+ influx in roots of winter wheat

Influx of Rb⁺(⁸⁶Rb⁺) and Ca²⁺(⁴⁵Ca²⁺) was determined in roots of winter wheat (Triticum aestivum L. cv. Weibulls Starke II) after 14 days at 16°C/16 h light, after 1 and 8 weeks of cold acclimation (2°C/8 h light) and at intervals after deacclimation (16°C/16 h light) for up to 14 days. The plants were cultivated at 3 ionic strengths: 100, 10 and 1% of a full strength nutrient solution, containing 3.0 mM K⁺ and 1.0 mM Ca²⁺. K⁺ concentrations in roots and shoots increased during cold treatment, while Ca²⁺ in the roots decreased. In the shoots Ca²⁺ concentrations remained the same. Influx of Rb⁺ as a function of average K⁺ concentration in the roots of 14-day-old, non-cold-treated plants was high at a certain K⁺ level in the root and decreased at higher root K⁺ levels (negative feedback). The pattern for Ca²⁺ influx versus average concentration of Ca²⁺ in the root was the reverse. Independent of duration of treatment (1–8 weeks), cold acclimation partly changed the regulation of Rb⁺ influx, so that it became less dependent upon negative feedback and more dependent on the ionic strength of the cultivation solution. After exposure to 2°C, Ca²⁺ influx increased at high Ca²⁺ concentrations in the root as compared with influx in roots of 14-day-old non-cold-treated plants. Under deacclimation, Ca²⁺ influx gradually decreased again, and reached the level observed before cold treatment within 7–14 days at 16°C; the number of days depending on the exposure time at 2°C. It is suggested that Rb⁺(K⁺) influx became adjusted to low temperature and that abscisic acid (ABA) may be involved in this mechanism. It is also suggested that extrusion of Ca²⁺ was impaired and/or Ca²⁺ channels were activated at 2°C in roots of plants grown in the full-strength solution and that extrusion was gradually restored and/or Ca²⁺ channels were closed under deacclimation conditions.     

Compartmental analysis of efflux of K+(86Rb+) and Rb+(86Rb+) from roots of intact plants of barley (Hordeum vulgare) of high and low K+ status, and after excision of the shoot

The classic compartment analysis of ion efflux from roots is often applied with the assumption that there is a system of 3 compartments in series. However, complex ion transport across the root tissues, as well as influences from the shoot, may complicate the picture. The present experiments were performed to study the immediate effects that excision of the shoot before the experiment exerts on the efflux of Rb⁺(⁸⁶Rb⁺) and of K⁺(⁸⁶Rb⁺) from 9-day-old roots of plants of barley (Hordeum vulgare L. cv. Salve). The efflux from high K⁺ and low K⁺ roots of intact and detopped plants were compared. After excision of the shoot of high K⁺ plants, a marked increase in efflux was observed after 2.5 h with a maximum at about 7 h. The increase in efflux was seen as a peak in plots of efflux versus time. Excision of the shoot from low K⁺ roots did not give rise to a consistent increase in efflux. Regular K⁺ ion efflux curves were observed from roots of intact plants of high or low K⁺ status. Furthermore, after a pulse treatment of 9-day-old roots of intact plants of high or low K⁺ status with a solution containing Rb⁺(⁸⁶Rb⁺), the Rb⁺(⁸⁶Rb⁺) transport to the shoots was not reduced during the following 3 h in unlabelled solution. It is suggested that both the peak appearing in the efflux plots and the maintained tracer transport to the shoots after transfer of the roots to an unlabelled solution indicate the existence of a K⁺/Rb⁺ transport system in the symplasm of the roots that has only a slow exchange with the bulk cytoplasm and vacuoles.     

Effects of Growth and Assay Temperatures on Unidirectional K+ Fluxes in Roots of Rye (Secale cereale)

The effects of growth and assay temperature on unidirectionalK⁺ fluxes in excised roots of rye (Secale cereale cv. Rheidol)were studied using ⁸⁶Rb⁺ as a tracer. Both K⁺ influx to thevacuole, estimated as K⁺ uptake between 3 and 12 h after transferof unlabelled roots to radioactive solution, and movement ofK⁺ to the xylem were determined directly. Other fluxes weredetermined on excised roots of plants, which had been labelledwith ⁸⁶Rb⁺ since germination, by conventional triple exponentialefflux analysis. When assayed at 20°C, roots of plants previously grown at20°C(WG roots) had lower rates of net K⁺ uptake than rootsof low temperature-acclimated plants, grown with a temperaturediferential between roots (87°C) and shoots (20°C) eithersince germination (DG roots) or for 3 d prior to experiments(DT roots). This resulted from a greater unidirectional K⁺ effluxacross the plasma membrane and a reduced K⁺ flux to the xylemin WG roots, compared to DG or DT roots, rather than a decreasein unidirectional K⁺ influx or a decrease in the net K⁺ fluxto the vacuole. Indeed, although WG roots had lower rates ofK⁺ influx and K⁺ efflux across the tonoplast at 20°C thanDG or DT roots, roots of plants from all growth temperaturetreatments showed an equivalent net K⁺ flux to the vacuole. Although all unidirectional K⁺ fluxes in roots from plants grownunder all temperature regimes were reduced by lowering the temperatureof the root, these fluxes were differentially affected in rootsof plants from contrasting growth temperature treatments. Rapidcooling to 8°C of WG roots resulted in a lower rate of K+influx and a transient increase in K⁺ efflux across both theplasma membrane and tonoplast, compared to DG and DT roots.Furthermore, since the K⁺ flux to the xylem was lower in WGroots, the net K⁺ uptake at 8°C into WG roots was considerablyreduced compared to DG and DT roots. These results suggest thatlow temperature-acclimation of K⁺ fluxes in rye roots may involvea reduction in the temperature sensitivity of K⁺ influx anda curtailment of K⁺ efflux across both the plasma membrane andtonoplast at low temperatures. Key words: K⁺influx, K⁺ efflux, low temperature, potassium, rye (Secale cereale cv. Rheidol)     

Alkali cation selectivity of the wheat root high-affinity potassium transporter HKT1

The wheat root high-affinity K⁺ transporter HKT1 functions as a sodium-coupled potassium co-uptake transporter. At toxic millimolar levels of sodium (Na⁺), HKT1 mediates low-affinity Na⁺ uptake while potassium (K⁺) uptake is blocked. In roots, low-affinity Na⁺ uptake and inhibition of K⁺ uptake contribute to Na⁺ toxicity. In the present study, the selectivity among alkali cations of HKT1 expressed in Xenopus oocytes and yeast was investigated under various ionic conditions at steady state. The data show that HKT1 is highly selective for uptake of the two physiologically significant alkali cations, K⁺ and Na⁺ over Rb⁺, Cs⁺ and Li⁺. In addition, Rb⁺ and Cs⁺, and an excess of extracellular K⁺ over Na⁺, are shown to partially reduce or block HKT1-mediated K⁺-Na⁺ uptake. Furthermore, K⁺, Rb⁺ and Cs⁺ also effectively reduce outward currents mediated by HKT1, thereby causing depolarizations. In yeast, HKT1 can produce high-affinity Rb⁺ uptake at approximately 15-fold lower rates than for K⁺. Rb⁺ influx in yeast can be mediated by the ability of the yeast plasma membrane proton pump to balance the 35-fold lower HKT1 conductance for Rb⁺. A model for HKT1 activity is presented involving a high-affinity K⁺ binding site and a high-affinity Na⁺ binding site, and competitive interactions of K⁺, Na⁺ and other alkali cations for binding to these two sites. Possible implications of the presented results for physiological K⁺ and Na⁺ uptake in plants are discussed.     

Ion fluxes and phytochrome protons in mung bean hypocotyl segments: I. Fluxes of potassium

K⁺ [⁸⁶Rb⁺] uptake by Phaseolus aureus Roxb. hypocotyl segments cut immediately below the hook is inhibited by the active form of phytochrome (Pfr). Short load-short wash experiments indicate that the inhibition of uptake occurs across the plasmalemma. A maximal inhibition of short term uptake occurs in 10 to 50 millimolar KCI. Low temperature had only a small effect on influx and the inhibition of influx from 50 millimolar KCI. A consideration of the electrochemical gradient for K⁺ suggests that passive K⁺ fluxes may predominate under these conditions. Red light induces small depolarizations of membrane potential in subhook cells. Far red light antagonizes this effect. Pfr inhibits efflux of K⁺[⁸⁶Rb⁺] from subhook segments. This effect is also relatively insensitive to low temperature. This inhibition of efflux may reflect inhibition of a K⁺ -K⁺ exchange process, or reduced passive permeability of the plasmalemma to K⁺. In contrast, Pfr enhances short term uptake of K⁺[⁸⁶Rb⁺] in apical hypocotyl hook segments of Phaseolus aureus Roxb. Short load-short wash experiments indicate that fluxes across the plasmalemma are modified by Pfr. A maximal enhancement of short term influx occurs in 50 millimolar KCI. Influx and the red light enhancement of influx from 50 millimolar KCI are relatively insensitive to low temperature. Pfr also enhances efflux of K⁺[⁸⁶Rb⁺] from preloaded apical hook segments. This increased influx may reflect enhancement of a K⁺ -K⁺ exchange process or increased passive permeability of the plasmalemma to K⁺.     

Modulation of K+ translocation by AKT1 and AtHAK5 in Arabidopsis plants

Root cells take up K⁺ from the soil solution, and a fraction of the absorbed K⁺ is translocated to the shoot after being loaded into xylem vessels. K⁺ uptake and translocation are spatially separated processes. K⁺ uptake occurs in the cortex and epidermis whereas K⁺ translocation starts at the stele. Both uptake and translocation processes are expected to be linked, but the connection between them is not well characterized. Here, we studied K⁺ uptake and translocation using Rb⁺ as a tracer in wild‐type Arabidopsis thaliana and in T‐DNA insertion mutants in the K⁺ uptake or translocation systems. The relative amount of translocated Rb⁺ to the shoot was positively correlated with net Rb⁺ uptake rates, and the akt1 athak5 T‐DNA mutant plants were more efficient in their allocation of Rb⁺ to shoots. Moreover, a mutation of SKOR and a reduced plant transpiration prevented the full upregulation of AtHAK5 gene expression and Rb⁺ uptake in K⁺‐starved plants. Lastly, Rb⁺ was found to be retrieved from root xylem vessels, with AKT1 playing a significant role in K⁺‐sufficient plants. Overall, our results suggest that K⁺ uptake and translocation are tightly coordinated via signals that regulate the expression of K⁺ transport systems.     

Changes in Rb+ and Ca2+ influx in winter wheat roots before, during and after exposure to low temperature and short days

Influx of Rb⁺(⁸⁶Rb⁺) and Ca²⁺ (⁴⁵Ca²⁺) in roots of intact winter wheat (Triticum aestivum L. cv. Weibulls Starke II) was determined at intervals before, during and after exposure to cold acclimation conditions (2°C and 8 h light period). The plants were grown in nutrient medium of two ionic strengths. During the initial two weeks of growth at 16°C and 16 h light period, Rb⁺ influx into roots decreased with increasing age, probably as a consequence of a decreasing proportion of metabolically active roots. The presence of 10^?4M 2,4-dinitrophenol (DNP) reduced Rb⁺ influx to a low and constant level, indicating that metabolic influx was the dominant process. In contrast, Ca²⁺ influx in plants grown in full strength nutrient solution was higher in the presence than in the absence of DNP. This effect may have been due to an active extrusion mechanism mediating re-export of absorbed Ca²⁺(⁴⁵Ca²⁺) during the uptake experiment. With the metabolic uncoupler inhibiting such extrusion the Ca²⁺(⁴⁵Ca²⁺) influx mesured would increase. During cold treatment, Rb⁺ influx remained at a low level, and was further decreased when DNP was present in the uptake solution. This effect may have been due to inhibition of residual active influx of Rb⁺ at 2°C by the uncoupler and/or to a decrease in membrane permeability. In contrast to Rb⁺, Ca²⁺ influx increased during cold treatment, which could again be explained as inhibition of re-export. The presence of DNP reduced Ca²⁺ influx at 2°C, indicating decreased membrane permeability by DNP at low temperature. After transfer of plants from cold acclimation conditions to 16°C, Rb⁺ and Ca²⁺ influx increased in plants grown at both ionic strengths. Influx levels were independent of the length of the cold acclimation period (1, 6 and 8 weeks), but the patterns were different for the two ions. After each of the cold acclimation periods, Rb⁺ influx increased during the first week and decreased or remained at the same level during the second week, while Ca²⁺ influx always decreased during the second week of post-cold treatment.     

Potassium Transport in Corn Roots : II. The Significance of the Root Periphery

The relative transport capabilities of the cells of the root periphery and cortex were investigated using a variety of experimental techniques. Brief (30 seconds to 1 minute) exposures with the penetrating sulfhydryl reagent, N-ethyl maleimide (NEM), and the impermeant reagent, p-chloromercuribenzene sulfonic acid (PCMBS), dramatically reduced ⁸⁶Rb⁺ (0.2 millimolar RbCl) uptake into 2 centimeter corn (Zea mays [A632 × (C3640 × Oh43)]) root segments. Autoradiographic localization studies with [³H]NEM and [²⁰³Hg]PCMBS demonstrated that, during short term exposures with either reagent, sulfhydryl binding occurred almost exclusively in the cells of the root periphery.

Corn root cortical protoplasts were isolated, and exhibited significant K⁺(⁸⁶Rb⁺) influx. The kinetics for K⁺ uptake were studied; the influx isotherms were smooth, nonsaturating curves that approached linearity at higher K⁺(Rb⁺) concentrations (above 1 millimolar K⁺). These kinetics were identical in shape to the complex kinetics previously observed for K⁺ uptake in corn roots (Kochian, Lucas 1982 Plant Physiol 70: 1723-1731), and could be resolved into a saturable and a first order kinetic component.

The existence of a hypodermal apoplastic barrier was investigated. The apoplastic, cell wall binding dye, Calcofluor White M2R, appeared to be excluded from the cortex by the hypodermis. However, experiments with damaged roots indicated that this result may be an artifact resulting from the binding of dye to the epidermal cell walls. Furthermore, [²⁰³Hg] PCMBS autoradiography demonstrated that the hypodermis was not a barrier to apoplastic movement of PCMBS.

These results suggest that although cortical cells possess the capacity to absorb ions, K⁺ influx at low concentrations is limited to the root periphery. Cortical cell uptake appears to be repressed under these conditions. At higher concentrations, cortical cells may function to absorb K⁺. Such a model may involve regulation of cortical cell ion transport capacity.

     

Cloning and functional characterization of the high-affinity K<Superscript>+</Superscript> transporter HAK1 of pepper

High-affinity K⁺ uptake in plants plays a crucial role in K⁺ nutrition and different systems have been postulated to contribute to the high-affinity K⁺ uptake. The results presented here with pepper (Capsicum annum) demonstrate that a HAK1-type transporter greatly contributes to the high-affinity K⁺ uptake observed in roots. Pepper plants starved of K⁺ for 3 d showed high-affinity K⁺ uptake (K _m of 6 M K⁺) that was very sensitive to NH and their roots expressed a high-affinity K⁺ transporter, CaHAK1, which clusters in group I of the KT/HAK/KUP family of transporters. When expressed in yeast (Saccharomyces cerevisiae), CaHAK1 mediated high-affinity K⁺ and Rb⁺ uptake with K _m values of 3.3 and 1.9 M, respectively. Rb⁺ uptake was competitively inhibited by micromolar concentrations of NH and Cs⁺, and by millimolar concentrations of Na⁺.     

Potassium Transport in Corn Roots : III. Perturbation by Exogenous NADH and Ferricyanide

It has recently been reported that plasmalemma electron transport may be involved in the generation of H⁺ gradients and the uptake of ions into root tissue. We report here on the influence of extracellular NADH and ferricyanide on K⁺ (⁸⁶Rb⁺) influx, K⁺ (⁸⁶Rb⁺) efflux, net apparent H⁺ efflux, and O₂ consumption in 2-centimeter corn (Zea mays [A632 × Oh43]) root segments and intact corn roots. In freshly excised root segments, NADH had no effect on O₂ consumption and K⁺ uptake. However, after the root segments were given a 4-hour wash in aerated salt solution, NADH elicited a moderate stimulation in O₂ consumption but caused a dramatic inhibition of K⁺ influx. Moreover, net apparent H⁺ efflux was significantly inhibited following NADH exposure in 4-hour washed root segments.

Exogenous ferricyanide inhibited K⁺ influx in a similar fashion to that caused by NADH, but caused a moderate stimulation of net H⁺ efflux. Additionally, both reagents substantially altered K⁺ efflux at both the plasmalemma and tonoplast.

These complex results do not lend themselves to straightforward interpretation and are in contradiction with previously published results. They suggest that the interaction between cell surface redox reactions and membrane transport are more complex than previously considered. Indeed, more than one electron transport system may operate in the plasmalemma to influence, or regulate, a number of transport functions and other cellular processes. The results presented here suggest that plasmalemma redox reactions may be involved in the regulation of ion uptake and the `wound response' exhibited by corn roots.

     

Effects of cadmium and lead on the accumulation of Ca2+ and K+ and on the influx and translocation of K+ in wheat of low and high K+ status

The effects of cadmium and lead on the internal concentrations of Ca²⁺ and K⁺, as well as on the uptake and translocation of K(⁸⁶Rb⁺) were studied in winter wheat (Triticum aestivum L. a. MV-8) grown hydroponically at 2 levels of K⁺ (100 uM and 10 mM). Cd²⁺ and Pb²⁺ were applied in the nutrient solution in the range of 0.3 to 1000 u.M. Growth was more severely inhibited by Cd²⁺ and in the high-K⁺ plants as compared to Pb^z+ and low-K⁺ plants. Ions of both heavy metals accumulated in the roots and shoots, but the K⁺ status influenced their levels. Ca²⁺ accumulation was increased by low concentrations of Cd²⁺ mainly in low-K⁺ shoots, whereas it was less influenced by Pb²⁺. The distribution of Cd²⁺ and Ca²⁺ in the plant and in the growth media indicated high selectivity for Cd²⁺ in the root uptake, while Ca²⁺ was preferred in the radial and/or xylem transport. Cd²⁺ strongly inhibited net K⁺ accumulation in high-K⁺ plants but caused stimulation at low K⁺ supply. In contrast, the metabolis-dependent influx of K⁺(⁸⁶Rb⁺) was inhibited in low-K⁺ plants, while the passive influx in high-K⁺ plants was stimulated. Translocation of K⁺ from the roots to the shoots was inhibited by Cd²⁺ but less influenced in Pb²⁺-treated plants. It is concluded that the effects of heavy metals depend upon the K⁺-status of the plants.     

High salinity tolerance in the stl2 mutation of Ceratopteris richardii is associated with enhanced K+ influx and loss

The roles of K⁺ uptake and loss in the salinity response of the wild type and the salt-tolerant mutant stl2 of Ceratopteris richardii were studied by measuring Rb⁺ influx and loss and the effects of Na⁺, Mg²⁺, Ca²⁺ and K⁺-transport inhibitors. In addition, electrophysiological responses were measured for both K⁺ and Rb⁺ and for the effects of Na⁺ and NH₄⁺ on subsequent K⁺-induced depolarizations. stl2 had a 26–40% higher uptake rate for Rb⁺ than the wild type at 0.5–10 mol m^?3 RbCl. Similarly, membrane depolarizations induced by both RbCl and KCl were consistently greater in stl2. In the presence of 0–180 mol m^?3 NaCl, stl2 maintained a consistently greater Rb⁺ influx than the wild type. stl2 retained a greater capacity for subsequent KCl-induced depolarization following exposure to NaCl. Five mol m^?3 Mg²⁺ decreased Rb⁺ uptake in stl2; however, additional Mg²⁺ up to 40 mol m^?3 did not affect Rb⁺ uptake further. Ca²⁺ supplementation resulted in a very minor decrease of Rb⁺ uptake that was similar in the two genotypes. Tetraethylammonium chloride and CsCl gave similar inhibition of Rb⁺ uptake in both genotypes, but NH₄Cl gave substantially greater inhibition in the wild type than in stl2. NH₄Cl resulted in a greater membrane depolarization in the wild type and the capacity for subsequent depolarization by KCl was markedly reduced. stl2 exhibited a higher Independent loss of Rb⁺ than the wild type, but, in the absence of external K⁺, loss of Rb⁺ was equivalent in the two genotypes. Since constitutive K⁺ contents are nearly identical, we conclude that high K⁺ influx and loss exact a metabolic cost that is reflected in the inhibition of gametophytic growth. Growth inhibition can be alleviated by reduced supplemental K⁺ or by treatments that slightly reduce K⁺ influx, such as moderate concentrations of Na⁺ or Mg²⁺. We propose that high throughput of K⁺ allows maintenance of cytosolic K⁺ under salt stress and that a high uptake rate for K⁺ results in a reduced capacity for the entrance and accumulation of alternative cations such as Na⁺ in the cytosol.     

Acclimation of potassium influx in rye (Secale cereale) to low root temperatures

The influx of K⁺(⁸⁶Rb⁺) into intact roots of rye (Secale cereale L. cv. Rheidal) exposed to a differential temperature (DT) between the root (8° C) and shoot (20° C) is initially reduced compared with warm-grown (WG) controls with both shoot and root maintained at 20° C. Over a period of 3 d, however, K⁺-influx rates into DT plants are restored to levels similar to or greater than those of the WG controls, the absolute rates of K⁺ influx being strongly dependent upon the shoot/root ratio. Acclimation in DT plants results in a reduction of K⁺ influx into the apical (0–2 cm) region of the seminal root which is associated with a compensatory increase in K⁺ influx into the more mature, basal regions of the root. Values of V _max and apparent K _m for K⁺ influx into DT plants were similar to those for WG plants at assay temperatures of 8° C and 20° C except for an increase in the apparent K _m at 8° C. The influx of K⁺ from solutions containing 0.6 mol·m^-3 K⁺ into both WG and DT plants was found to be linearly related to assay temperature over the range 2–27° C, and the temperature sensitivity of K⁺ influx to be dependent upon shoot/root ratio. At high shoot/root ratios, the ratio of K⁺ influx at 20° C:K⁺ influx at 8° C for WG plants approached a minimum value of 1.9 whereas that for DT plants approached unity indicating that K⁺ influx into DT plants has a large temperature-insensitive component. Additionally, when plants were grown in solutions of low potassium concentration, K⁺ influx into DT plants was consistently greater than that into WG plants, in spite of having a greater root potassium concentration ([K⁺]int). This result indicates some change in the regulation of K⁺ influx by [K⁺]int in plants exposed to low root temperatures. We suggest that K⁺ influx into rye seedlings exposed to low root temperatures is regulated by the increased demand placed on the root system by a proportionally larger shoot and that the acclimation of K⁺ influx to low temperatures may be the result of an increased hydraulic conductivity of the root system.Abbreviations DT differential temperature pretreatment - [K⁺]int root potassium concentration - [K⁺]ext potassium concentration of nutrient medium - WG warm-grown pretreatment     

Conditions controlling relative uptake of potassium and rubidium by plants from soils

Earlier studies have demonstrated close inverse relationships between Rb⁺ concentrations in plants and pH or base (including K⁺) saturation of soils. This study aims at elucidating conditions in soils influencing plant uptake of Rb⁺. Growth experiments with Carex pilulifera L. were performed, modifying the acidity and K⁺ supply of acid soils and solutions. We were unable to assess any reduction in Rb⁺ uptake by adding precipitated CaCO₃ to acid soil unless pH was raised to near neutrality. Though not fully compensating the loss of soil solution K⁺and exchangeable K⁺ from uptake by the growing plants, soil treated with 0.5 mM K⁺ (as KCl) reduced the Rb⁺ concentration in the shoots by 40% without measurably changing soil pH. Experiments varying the pH and K⁺ concentration of a nutrient solution (20% Hoagland), spiked with 6 uM Rb⁺, clearly demonstrated that plant uptake of Rb⁺ and K⁺ was unaffected by acidity in the pH range 3.6–5.0 tested, whereas Rb⁺ uptake was reduced by ca. 50%, when K⁺ concentration was increased from 1.2 to 3.6 mM. The sensitivity of this reaction indicates that shortage or low availability of K⁺ controls Rb⁺ uptake from acid soils, being probably more important than soil acidity per se. Secondary effects of high soil acidity, such as leaching losses of K⁺, might also be of importance in accounting for the high uptake of Rb⁺ from such soils. It is suggested that leaf analysis of Rb⁺ may be used as a method to assess early stages of K⁺ deficiency in plants on acid soils.     

Effects of switches in nutrient levels during the life cycle of spring wheat

Accumulation of cations in roots and shoots and influx of K⁺(⁸⁶Rb⁺) and Ca²⁺(⁴⁵Ca²⁺) into the roots were investigated in spring wheat (Triticum aestivum L. cv. Svenno). Plants were sampled at four main developmental stages: tillering, shooting, heading and grain filling. The effects of switches between a high and a low supply of nutrients were characterized. Growth of the shoots and roots was affected by the switches. A high supply of nutrients at the seedling stage and towards tillering supported a high growth rate, while a further high supply of nutrients increased vegetative growth and delayed grain filling. An early high supply of nutrients followed by a low supply at shooting, heading and grain filling accelerated root growth and growth of the main culm. Switches of the mineral supply gave only small changes in concentration of Mg in the plants. Generally, the K⁺(⁸⁶Rb⁺) influx into the roots decreased during ontogenesis, while Ca²⁺(⁴⁵Ca²⁺) influx increased more or less independent of the switches between nutrients levels.