Cation amelioration of aluminum toxicity in wheat

Aluminum is a major constituent of most soils and limits crop productivity in many regions. Amelioration is of theoretical as well as practical interest because understanding amelioration may contribute to an understanding of the mechanisms of toxicity. In the experiments reported here 2-day-old wheat (Triticum aestivum L. cv Tyler) seedlings with 15-millimeter roots were transferred to solutions containing 0.4 millimolar CaCl₂ at pH 4.3 variously supplemented with AlCl₃ and additional amounts of a chloride salt. Root lengths, measured after 2 days in the test solutions, were a function of both Al activity and the cation activity of the added salt. Percent inhibition = 100 {Al³⁺}/({Al³⁺} + K_m + α{C}^β) where {Al³⁺} is the activity of Al³⁺ expressed in micromolar, {C} is the activity of the added cation expressed in millimolar, and K_m (= 1.2 micromolar) is the {Al³⁺} required for 50% inhibition in the absence of added salt. For Ca²⁺, Mg²⁺, and Na⁺ the values of α were 2.4, 1.6, and 0.011, respectively, and the values for β were 1.5, 1.5, and 1.8, respectively. With regard to relative ameliorative effectiveness, Ca²⁺ > Mg²⁺ ≈ Sr²⁺ K⁺ ≈ Na⁺. Other cations were tested, but La³⁺, Sc³⁺, Li⁺, Rb⁺, and Cs⁺ were toxic at potentially ameliorative levels. The salt amelioration is not solely attributable to reductions in {Al³⁺} caused by increases in ionic strength. Competition between the cation and Al for external binding sites may account for most of the amelioration.     

Interaction of alginate single-chain polyguluronate segments with mono- and divalent metal cations: a comparative molecular dynamics study

The interaction of a set of monovalent (Na⁺, K⁺) and divalent (Mg²⁺, Ca²⁺) metal cations with single-chain polyguluronate (periodic chain based on a dodecameric repeat unit, 2₁-helical conformation) is investigated using explicit-solvent molecular dynamics simulations (at 300 K and 1 bar). A total of 14 (neutralising) combinations of the different ions are considered (single type of cation or simultaneous presence of two types of cation, either in the presence or absence of chloride anions). The main observations are: (1) the chain conformation and intramolecular hydrogen bonding is insensitive to the counter-ion environment; (2) the binding of the cations is essentially non-specific for all ions considered (counter-ion atmosphere confined within a cylinder of high ionic density, but no well-defined binding sites); (3) the density and tightness of the distributions of the different cations within the counter-ion atmosphere follow the approximate sequence Ca²⁺>Mg²⁺>K⁺～Na⁺; (4) the solvent-separated binding of the cations to the carboxylate groups of the chain is frequent, and its occurrence follows the approximate sequence K⁺>Na⁺>Ca²⁺>Mg²⁺ (contact-binding events as well as the binding of a cation to multiple carboxylate groups are very infrequent); and (5) the counter-ion atmosphere typically leads to a complete screening of the chain charge within 1.0–1.2 nm of the chain axis and, for most systems, to a charge reversal at about 1.5 nm (i.e. the effective chain charge becomes positive at this distance and as high in magnitude as one-quarter of the bare chain charge, before slowly decreasing to zero). These findings agree well (in a qualitative sense) with available experimental data and predictions from simple analytical models, and provide further insight concerning the nature of alginate–cation interactions in aqueous solution.     

Cation distribution in faujasite-type zeolites: A test of semi-empirical force fields for Na cations

(N,V,T) Monte Carlo (MC) simulations have been performed in order to test three available force fields for sodium cations in faujasite-type zeolites. A rigid framework faujasite model, using an average T atom scheme and the cation force field proposed by [Jaramillo, E. and Auerbach, S.M. J. Phys. Chem. 103 (1999) 9589] was found to reproduce quite well the experimentally observed cation location in NaY and could thus be used in future works for predicting cation distributions and possible cation migration upon adsorption in faujasites.     

Osmotic swelling of heart mitochondria in acetate and chloride salts. Evidence for two pathways for cation uptake.

Swelling of nonenergized heart mitochondria suspended in acetate salts appears to depend on the activity of an endogenous cation/H⁺ exchanger. Passive swelling in acetate shows a characteristic cation selectivity sequence of Na⁺ >Li⁺ >K⁺, Rb⁺, Cs⁺, or tetramethylammonium, a sharp optimum at pH 7.2–7.3, activation by Ca²⁺, and loss of activity on aging which can be related to loss of endogenous K⁺. The reaction is nearly insensitive to either addition of exogenous Mg²⁺ or removal of membrane Mg²⁺ with EDTA. Each of these characteristics of passive swelling in acetate salts is duplicated in chloride media when tripropyltin is added to induce Cl^?/OH^? exchange. In contrast to nonenergized mitochondria, swelling of respiring mitochondria has been postulated to depend on electrophoretic uptake of cations in response to an interior negative membrane potential. Respiration-dependent swelling in acetate shows an indistinct cation selectivity sequence with Li⁺ and Na⁺ supporting higher rates of swelling at higher efficiency than K⁺, Rb⁺, and Cs⁺. The high rates of respiration-dependent swelling in Li⁺ and Na⁺ are inhibited by low levels of exogenous Mg²⁺ (K_i of 5–10 μm), but a significant swelling with almost no cation selectivity persists in the presences of 2 mm Mg²⁺. Removal of membrane Mg²⁺ by addition of EDTA strongly activates the rate of respiration-dependent swelling and converts a sigmoid dependency of swelling rate on Li⁺ concentration to a hyperbolic one with a Km of about 14 mm Li⁺. The cation selectivity and Mg²⁺ dependence of the reaction induced in chloride salts by tripropyltin are identical to these properties in acetate. Energy-dependent swelling in acetate shows optimum activity at pH 6.5 which appears related to the availability of free acetic acid, since the corresponding reaction induced in chloride shows a broad optimum at about pH 7.5. These studies support the concept that monovalent cations enter nonenergized mitochondria by electroneutral exchange with protons but penetrate respiring mitochondria by electrophoretic movement through one or more uniport pathways. They further suggest that both a Mg²⁺-sensitive uniport with high activity for Na⁺ and Li⁺ and a Mg²⁺-insensitive pathway with little cation discrimination are available in the membrane.     

Cation/proton antiport systems in Escherichia coli.

Three distinct systems which function as proton/cation antiports have been identified in $\text{E.}\text{coli}$ by the ability of the ions to dissipate the ΔpH component of the protonmotive force in everted vesicles. System I exchanges H⁺ for K⁺, Rb⁺ or Na⁺; System II has Na⁺ and Li⁺ as substrates; and System III catalyzes proton exchange for Ca²⁺, Mn²⁺ or Sr²⁺.     

Super-high-affinity binding site for [3H]diazepam in the presence of Co2+, Ni2+, Cu2+, OR Zn2+

Chloride salts of Li⁺, Na⁺, K⁺, Mg²⁺, Ca²⁺, Cr³⁺, Mn²⁺, Fe²⁺, and Fe³⁺ had no effect on [³H]diazepam binding. Chloride salts of Co²⁺, Ni²⁺, Cu²⁺, and Zn²⁺ increased [³H]diazepam binding by 34 to 68% in a concentration-dependent fashion. Since these divalent cations potentiated the GABA-enhanced [³H]diazepam binding and the effect of each divalent cation was nearly additive with GABA, these cations probably act at a site different from the GABA recognition site in the benzodiazepine-receptor complex. Scatchard plots of [³H]diazepam binding without an effective divalent cation showed a single class of binding, with a Kd value of 5.3 mM. In the presence of 1 mM Co²⁺, Ni²⁺, Cu²⁺, or Zn²⁺, two distinct binding sites were evident with apparent Kd values of 1.0 nM and 5.7 nM. The higher-affinity binding was not detected in the absence of an effective divalent cation and is probably a novel, super-high-affinity binding site.     

Potential cation and H+ binding sites in acid sensing ion channel-1

Acid sensing ion channels (ASICs) are cation-selective membrane channels activated by H⁺ binding upon decrease in extracellular pH. It is known that Ca²⁺ plays an important modulatory role in ASIC gating, competing with the ligand (H⁺) for its binding site(s). However, the H⁺ or Ca²⁺ binding sites involved in gating and the gating mechanism are not fully known. We carried out a computational study to investigate potential cation and H⁺ binding sites for ASIC1 via all-atom molecular dynamics simulations on five systems. The systems were designed to test the candidacy of some acid sensing residues proposed from experiment and to determine yet unknown ligand binding sites. The ion binding patterns reveal sites of cation (Na⁺ and Ca²⁺) localization where they may compete with protons and influence channel gating. The highest incidence of Ca²⁺ and Na⁺ binding is observed at a highly acidic pocket on the protein surface. Also, Na⁺ ions fill in an inner chamber that contains a ring of acidic residues and that is near the channel entrance; this site could possibly be a temporary reservoir involved in ion permeation. Some acidic residues were observed to orient and move significantly close together to bind Ca²⁺, indicating the structural consequences of Ca²⁺ release from these sites. Local structural changes in the protein due to cation binding or ligand binding (protonation) are examined at the binding sites and discussed. This study provides structural and dynamic details to test hypotheses for the role of Ca²⁺ and Na⁺ ions in the channel gating mechanism.     

Chick brain glutamine synthetase and Mn2+−Mg2+ interactions

Glutamine synthetase (GS) from the chick brain was purified to apparent homogeneity by ammonium sulfate fractionation followed by affinity chromatography, electrofocusing and Sephadex G-150 chromatography. The purified enzyme showed a single band on sodium dodecyl sulfate analysis in polyacrylamide gel. By sedimentation equilibrium analysis and gel electrophoresis analysis, it was shown that the enzyme has a subunit molecular weight of 45,000 and a native molecular weight of 364,000, which is consistent with an octameric structure. Sedimentation analysis in the presence of Mg²⁺ revealed three different forms of macromolecules corresponding respectively to a monomer, a tetramer and an octamer. Among eight cations tested (Ca²⁺, Co²⁺, Fe²⁺, Li⁺, Mg²⁺, Mn²⁺, Ni²⁺, Zn²⁺) only Co²⁺, Mg²⁺ and Mn²⁺ supported GS activity; the order of activatory ability was Mg²⁺>Co²⁺>Mn²⁺. The maximum activating effect of Mn²⁺ occurs only within a very narrow range of concentration: with an excess of cation causing strong inhibition of GS activity. For each cation, maximal GS activity occurs at a defined cation/ATP ratio. A regulatory system in which Mn²⁺, modulates the Mg²⁺ dependent GS activity, is proposed; such cation interactions may be of significance in the intracellular control of glutamine synthesis.     

Modelling anion amelioration of aluminium phytotoxicity

There is good evidence for the ameliorating effect of SO₄ ^2- and F^- on the expression of Al phytotoxicity in acidic solutions. The role of OH^-, in both shifting Al speciation towards hydroxy-Al species and decreasing activities of H⁺ with increasing pH, is still controversially discussed. Grauer and Horst (1992) proposed a model based on the assumption that Al phytotoxicity is a function of the Al saturation (AlS) of exchange sites in the root apoplast and analyzed the predictions of the model in the case of cation amelioration, with special emphasis on H⁺. In this study the model is further developed by considering, in addition to Al³⁺, the complexation of Al with the anions OH^-, F^-, SO₄ ^2-, and Cl^- to form potentially toxic Al species. Association constants of these Al complexes with a ligand (L ^-) which is assumed to simulate the cation exchange sites in the root apoplast, were estimated. Affinity factors for binding to L ^- compared to Al³⁺ were derived from these estimated association constants, and values were, in a first approach, 0.79 for AlOH²⁺, 0.02 for Al(OH)₂ ⁺, and 0.13 for Al(OH)₃ ⁰ (or 0.03 choosing another hydrolysis constant). High toxicity of Al₁₃ (AlO₄Al₁₂(OH)₂₄(H₂O)₁₂ ⁷⁺) could be explained by diminished H⁺ amelioration and a high association constant to L ^-. From estimated association constants for Al-Cl complexes, low affinity factors for L ^- for these complexes were derived. Since the formation of these Al-Cl complexes is not favoured, Cl^- is predicted to have very little ameliorating effect. In the case of SO₄ ^2– and F^- complexes with Al, the derived affinity factors never exceeded 0.05 and, since formation of these complexes is favoured by high association constants, are thus in agreement with experimental results on ameliorating effects. The ranking of the anions for ameliorative effectiveness was estimated to be in the order of OH^->F^->SO₄ ^2–>Cl^-. Hydroxy amelioration in this context is restricted to the speciation effect, which is only significant above pH 4.     

Interactive effects of Al, h, and other cations on root elongation considered in terms of cell-surface electrical potential

The rhizotoxicities of Al³⁺ and of La³⁺ to wheat (Triticum aestivum L.) were similarly ameliorated by cations in the following order of effectiveness: H⁺ ≈ C³⁺ > C²⁺ > C¹⁺. Among tested cations of a given charge, ameliorative effectiveness was similar except that Ca²⁺ was slightly more effective than other divalent cations and H⁺ was much more effective than other monovalent cations. H⁺ rhizotoxicity was also ameliorated by cations in the order C³⁺ > C²⁺ > C¹⁺. These results suggest a role for cell-surface electrical potential in the rhizotoxicity of Al³⁺, La³⁺, H⁺, and other toxic cations: negatively charged cell surfaces of the root accumulate the toxic cations, and amelioration is effected by treatments that reduce the negativity of the cell-surface electrical potential by charge screening or cation binding. Membrane-surface activities of free Al³⁺ or La³⁺ computed according to a Gouy-Chapman-Stern model correlated well with growth inhibition, which correlated only poorly with Al³⁺ or La³⁺ activities in the external medium. The similar responses of Al-intoxicated and La-intoxicated roots to ameliorative treatments provide evidence that Al³⁺, rather than AlOH²⁺ or Al(OH)₂⁺, is the principal toxic species of mononuclear Al. Comparisons of the responses of Al-sensitive and Al-tolerant wheats to Al³⁺ and to La³⁺ did not support the hypothesis that varietal sensitivity to Al³⁺ is based upon differences in cell-surface electrical potential.     

Effects of diet and temperature on Morimus funereus larval hemolymph cation concentrations

The effects of diet and different constant temperatures on hemolymph cation concentrations (Na⁺, K⁺, Mg²⁺, Ca²⁺) have been studied in Morimus funereus larvae collected from natural habitat, fed natural (oak or beech bark) or artificial diet, as well as in larvae reared from hatching on an artificial diet. In the hemolymph of larvae maintained under natural conditions Mg²⁺ was dominant, whereas Na⁺ concentration was very low. In their natural diets concentrations of Na⁺ and K⁺ were very low, while those of Ca²⁺ and Mg²⁺ were high. In larvae continuously reared on an artificial diet, hemolymph Mg²⁺ concentration was significantly decreased and Na⁺ concentration increased more than fourfold compared to the results obtained in oak-fed larvae. Na⁺ and K⁺ are the dominant cations in the artificial diet. The concentrations of K⁺ and Ca²⁺ in the hemolymph of larvae fed natural or artificial diet are nearly identical, suggesting the existence of an internal regulatory mechanism in this insect for these cations. The hemolymph cation concentrations of M. funereus larvae are predominantly dependent upon the diet consumed, much less upon the environmental temperatures. The most stable concentrations of cations were observed in larvae continuously fed an artificial diet and exposed to different constant temperatures. There was much less stability in the hemolymph cation concentration in oak larvae fed either natural or artificial food after their transfer to constant temperatures. With respect to the response to the external factors studied, the most sensitive are the Na⁺ concentrations, the most stable seems to be K⁺. © 1992 Wiley-Liss, Inc.     

Molecular-dynamic simulation of DPPC bilayer in different phase state: Hydration and electric field distribution in the presence of Be<Superscript>2+</Superscript> cations

New molecular-dynamic topology of phosphatidylcholine bilayer (DPPC) in total atomic OPLS force field was developed and used to study the structural characteristics of liquid-crystalline and gel state of lipid bilayer in the absence and in the presence of Na⁺ and Be²⁺ cations adsorbed at the interface and different in their affinity. The parameters of bilayer geometry, the amount of surface water, and the electrostatic potential distribution were estimated quantitatively from the simulation in both phase states. The azimuthal angle of hydrocarbon chains was found nearly the same in the region of each monolayer in gel state. The amount of surface water decreases upon bilayer “freezing” mainly by loss of water molecules not participating in H-bonds between lipid headgroups. The cation adsorption was shown to have a small effect on these H-bonded water molecules, whereas Be²⁺ appeared to retain surface water in the bilayer upon its freezing. The electric potential distribution in the normal direction to the membrane-water interface had a similar shape in any bilayer phase state regardless of the presence of the adsorbed cations. Analysis of the microscopic nature of the electric potential revealed a mutual compensation of the contributions of the main structural components of the system (lipids, water, and ions). The boundary potential increased by 116 mV for pure DPPC, by 212 mV in the presence of Na⁺, and by 133 mV in the presence of Be²⁺ upon the phase transition of bilayer to the gel state. The boundary potential difference in the presence of Na⁺ and Be²⁺ and its change at the bilayer phase transition are in a good agreement with the experimental data published earlier [Ermakov Yu.A., 1993].     

Differential expression of P-type ATPases in intestinal epithelial cells: Identification of putative new atp1a1 splice-variant

P-type ATPases are membrane proteins that couple ATP hydrolysis with cation transport across the membrane. Ten different subtypes have been described. In mammalia, 15 genes of P-type ATPases from subtypes II-A, II-B and II-C, that transport low-atomic-weight cations (Ca²⁺, Na⁺, K⁺ and H⁺), have been reported. They include reticulum and plasma-membrane Ca²⁺-ATPases, Na⁺/K⁺-ATPase and H⁺/K⁺-ATPases. Enterocytes and colonocytes show functional differences, which seem to be partially due to the differential expression of P-type ATPases. These enzymes have 9 structural motifs, being the phosphorylation (E) and the Mg²⁺ATP-binding (H) motifs the most preserved. These structural characteristics permitted developing a Multiplex-Nested-PCR (MN-PCR) for the simultaneous identification of different P-type ATPases. Thus, using MN-PCR, seven different cDNAs were cloned from enterocytes and colonocytes, including SERCA3, SERCA2, Na⁺/K⁺-ATPase α1-isoform, H⁺/K⁺-ATPase α2-isoform, PMCA1, PMCA4 and a cDNA-fragment that seems to be a new cassette-type splice-variant of the atp1a1 gen. PMCA4 in enterocytes and H⁺/K⁺-ATPase α2-isoform in colonocytes were differentially expressed. This cell-specific expression pattern is related with the distinctive enterocyte and colonocyte functions.     

Role of structural water for prediction of cation binding sites in apoproteins

Structures of many metal-binding proteins are often obtained without structural cations in their apoprotein forms. Missing cation coordinates are usually updated from structural templates constructed from many holoprotein structures. Such templates usually do not include structural water, the important contributor to the ion binding energy. Structural templates are also inconvenient for taking into account structural modifications around the binding site at apo-/holo- transitions. An approach based upon statistical potentials readily takes into account structural modifications associated with binding as well as contribution of structural water molecules. Here, we construct a set of statistical potentials for Mg²⁺, Ca²⁺, and Zn²⁺ contacting with protein atoms of a different type or structural water oxygens. Each type of the cations tends to form tight contacts with protein atoms of specific types. Structural water contributes relatively more into the binding pseudo-energy of Mg²⁺ and Ca²⁺ than of Zn²⁺. We have developed PIONCA (Protein-Ion Calculator), a fast CUDA GPGPU-based algorithm that predicts ion-binding sites in apoproteins. Comparative tests demonstrate that PIONCA outperforms most of the tools based on structural templates or docking. Our software can be also used for locating bound cations in holoprotein structures with missing cation heteroatoms. PIONCA is equipped with an interactive web interface based upon JSmol.     

Effects of limestone and gypsum application to a Malaysian ultisol on soil solution composition and yields of maize and groundnut

A field experiment was conducted on an Ultisol in Malaysia to assess changes in soil solution composition and their effects on maize and groundnut yields, resulting from limestone and gypsum application. The results showed that soil solution Ca in the lime treatment remained mainly in the zone of incorporation, but in the gypsum treatment some Ca moved into 15–30 cm zone. Al³⁺ and AlSO₄ ⁺ were dominant Al species in the soil solution of nil treatment. Liming decreased Al³⁺ and AlSO₄ ⁺, but increased hydroxy-Al monomer activities. However, gypsum application resulted in an increase of AlSO₄ ⁺ activity and in a decrease of Al³⁺ activity. Relative maize and groundnut yields were negatively correlated with Al³⁺, Al(OH)²⁺ and Al_sum activities. Likewise, relative yields were negatively correlated with Al concentration and the Al concentration ratio and positively correlated with soil solution Mg concentration and Ca/Al ratio.     

Extracellular Ca2+ controls outward rectification by apical cation channels in toad urinary bladder: Patch-clamp and whole-bladder studies

Summary Outward rectifying. cation channels were observed in the epithelial cells of the urinary bladder of the toad.Bufo marinus. As studied in isolated cells using the patch-clamp technique, the channel has an average conductance of 24 and 157 pS for pipette potentials between 0 and +60 mV and –60 to –100 mV, respectively, when the major cation in both bath and pipette solutions is K⁺. The conductance of the cannel decreasen with increasing dehydration energy of the permeant monovalent cation in the oder Rb⁺=K⁺>Na⁺>Li⁺. Reversal potentials near zero under biionic conditions imply that the permeabilities for all four of these cations are smiliar. The channel is sensitive to quinidine sulfate but not to amiloride. It shares several pharmacological and biophysical properties with an outwardly-rectifying, vasopressin-sensitive pical K⁺ conductive pathway described previously for the toad urinary bladder. We demonstrate, in both single-channel and whole-bladder studies, that the outward rectification is a consequence of interaction of the chanel with extracellular divalent cations, particularly Ca²⁺, which blocks inward but not outward current. Various divalent cations impart different degrees of outward rectification to the conductive pathway. Concentrations of Mg²⁺ and Ca²⁺ required for halfmaximal effect are 3×10^–4 and 10^–4 m, resopectively. For Co²⁺ the values are 10^–6 m at +50 mV and a 10^–4 m at +200 mV. The mechanism of blockade by divalent cations is not established, but does not seem to involve a voltage-dependent interaction in which the blocker penetrates the transmembrane electric field. In the absence of divalent cations in the mucosal solution, the magnitudes of inward current carried by Rb⁺, K⁺, Na⁺ and Li⁺ through the apical K⁺ pathway at any transepithelial voltage, are in the same order as in the single-channel studies. We propose that the cation channel observed by us in isolated epithelial cells is the single-channel correlate of the vasopressin-sensitive apical K⁺ conductive pathway in the toad urinary bladder and is also related to the oxytocin- and divalent cation-sensitive apical condictivity observed in frog skin and urinary bladder.     

Mineral nutrient economy in competing species of Sphagnum mosses

Bog vegetation, which is dominated by Sphagnum mosses, depends exclusively on aerial deposition of mineral nutrients. We studied how the main mineral nutrients are distributed between intracellular and extracellular exchangeable fractions and along the vertical physiological gradient of shoot age in seven Sphagnum species occupying contrasting bog microhabitats. While the Sphagnum exchangeable cation content decreased generally in the order Ca²⁺ ≥ K⁺, Na⁺, Mg²⁺ > Al³⁺ > NH₄ ⁺, intracellular element content decreased in the order N > K > Na, Mg, P, Ca, Al. Calcium occurred mainly in the exchangeable form while Mg, Na and particularly K, Al and N occurred inside cells. Hummock species with a higher cation exchange capacity (CEC) accumulated more exchangeable Ca²⁺, while the hollow species with a lower CEC accumulated more exchangeable Na⁺, particularly in dead shoot segments. Intracellular N and P, but not metallic elements, were consistently lower in dead shoot segments, indicating the possibility of N and P reutilization from senescing segments. The greatest variation in tissue nutrient content and distribution was between species from contrasting microhabitats. The greatest variation within microhabitats was between the dissimilar species S. angustifolium and S. magellanicum. The latter species had the intracellular N content about 40% lower than other species, including even this species when grown alone. This indicates unequal competition for N, which can lead to outcompeting of S. magellanicum from mixed patches. We assume that efficient cation exchange enables Sphagnum vegetation to retain immediately the cationic nutrients from rainwater. This may represent an important mechanism of temporal extension of mineral nutrient availability to subsequent slow intracellular nutrient uptake.     

Calcium-dependent K current in plasma membranes of dermal cells of developing bean cotyledons

In developing seeds of bean (Phaseolus vulgaris L.), phloem‐imported assimilates (largely sucrose and potassium) are released from coats to seed apoplasm and subsequently retrieved by the dermal cell complexes of cotyledons. To investigate the mechanisms of K⁺ uptake by the cotyledons, protoplasts of dermal cell complexes were isolated and whole‐cell currents across their plasma membranes were measured with the patch‐clamp technique. A weakly rectified cation current displaying a voltage‐dependent blockade by external Ca²⁺ and acidic pH, dominated the conductance of the protoplasts. The P haseolus v ulgaris Cotyledon Dermal‐cell pH and Calcium‐dependent Cation Conductance (Pv‐CD‐pHCaCC) was highly selective for K⁺ over Ca²⁺ and Cl^–. For K⁺ current through Pv‐CD‐pHCaCC a sigmoid shaped current–voltage (I–V) curve was observed with negative conductance at voltages between ?200 and ?140 mV. This negative K⁺ conductance was Ca²⁺ dependent. With other univalent cations (Na⁺, Rb⁺, NH₄⁺) the currents were smaller and were not Ca²⁺ dependent. Reversal potentials remained constant when external K⁺ was substituted with these cations, suggesting that Pv‐CD‐pHCaCC channels were non‐selective. The Pv‐CD‐pHCaCC would provide a pathway for K⁺ and other univalent cation influx into developing cotyledons. These cation influxes could be co‐ordinated with sucrose influx via pH and Ca²⁺dependence.     

Plant induced alteration in the rhizosphere and the utilisation of soil heterogeneity

Plant-soil interactions result in a special rhizosphere soil chemistry, differing from that of the bulk soil found only a few mm from the root. The aim of this study was to investigate adaptation mechanisms of herbs growing in acid soils through studying their rhizosphere chemistry in a greenhouse experiment and in a field study. Ten herbs were grown in acid soil (pH 4.2 in the soil solution) in the greenhouse. The concentrations of NO₃ ^-, SO₄ ^2-, phosphates, Ca²⁺, Mg²⁺, Mn²⁺, K⁺, Na⁺, NH₄ ⁺ and pH were analysed in soil solutions obtained by centrifugation. The general pattern found was a depletion of nutrients in the rhizosphere compared with their concentrations in the bulk soil. The pH increase (up to 0.7 units) in the rhizosphere soil appeared to be caused by plant uptake of NO₃ ^- (r²=0.88). The ion concentrations in the soil solution of the rhizosphere were dependent on plant species and biomass increase. Although species with a larger biomass and higher growth rates showed a higher degree of ion depletion (except for Na⁺, SO₄ ^2-) in the rhizosphere, there were also species specific responses. A field study of five herbs at five oak forest sites in Southern Sweden (Scania) was also carried out. In addition to the soil solution concentrations, the loss on ignition (LOI) and the concentrations of 0.1 M BaCl₂ extractable K⁺, Mg²⁺, Mn²⁺, Ca²⁺, and Al ions were measured. The amount of soil solution Al was determined as free ionic (quickly reacting) Al. For all species and sites, the LOI and the concentrations of exchangeable cations were higher in the rhizosphere than in the bulk soil, apparently due to the roots preferably growing at organic-rich microsites. The concentrations of the ions as measured in the centrifuged soil solution, were either higher in the rhizosphere than in the bulk soil or were the same in both, except for NO₃ ^- and quickly reacting Al. The lower concentrations of quickly reacting Al in the rhizosphere, compared with the bulk soil could indicate the uptake of Al by the plant or the exudation of complexing substances. The pH differences were only small and mostly non-significant. Plant-soil interactions and the ability of plants to utilise heterogeneity of the soil appear to be more important for plant growth in acid soils than recognised heretofore. Rhizosphere studies provide an important means of understanding plant strategies in acid soils. This revised version was published online in June 2006 with corrections to the Cover Date.