Enhancement of callose production by a combination of aluminum and iron in suspension-cultured tobacco (Nicotiana tabacum) cells

In nutrient medium, aluminum (A1) enhances ferrous ion [Fe(II)] -mediated per oxidation of lipids, which results in the loss of the plasma membrane integrity and the accumulation of A1 in tobacco cells. Under these conditions, the mechanism of callose production and possible involvement of callose in the accumulation of Al were investigated. Callose production was enhanced by both Al and Fe(II), but not by A1 or Fe(II) alone, and the enhancement was inhibited by a lipophilic antioxidant, suggesting that the enhancement of callose production is caused by the A1-enhanced, Fe(II)-mediated peroxidation of lipids. The enhancement of callose production depended on the presence of external Ca²⁺ in the treatment medium. The activity of β-l,3-glucan synthase in the microsomes was increased several times by the addition of Ca²⁺ in the assay medium, although the activity in the microsomes was reduced by the treatment of cells with Al and Fe(II) together. Therefore, it is likely that callose production is enhanced by exogenous Ca²⁺ via the AI-enhanced, Fe(II)-mediated peroxidation of lipids. During the exposure of the cells to Al and Fe(II), callose production started and increased simultaneously with Al accumulation. However, the digestion of callose in the cell wall materials prepared from the A1-treated cells by laminarinase did not release A1, suggesting that callose is not involved in the binding or trapping of A1.     

Responses to aluminium of suspension-cultured tobacco cells in a simple calcium solution

In a simple solution containing 3 mM CaCl₂ and 3% sucrose (pH 4.5), tobacco cells (Nicotiana tabacum L.) at the logarithmic phase of growth remained viable at least for 24 h. In this medium, the toxic effect of aluminium (Al) on the plasma membrane was investigated for up to 24 h. After the addition of Al to the cell suspension, Al started to accumulate immediately in the cells, and a maximum value was observed at 9 h. Al induced callose deposition, but did not enhance significantly the uptake of Evans blue (a nonpermeating dye), the per oxidation of lipids and the leakage of potassium (K) ions. Furthermore, the AI-treated cells were stained with fluorescein diacetate (FDA) as much as untreated control cells. These results suggest that the accumulation of Al does not damage the membrane. The addition of Fe(II) to the cells which had been exposed to Al for 12 h resulted in immediate lipid peroxidation and Evans blue uptake several hours later. A combination of Al and Fe(II) caused the K leakage, and enhanced the deposition of callose more than Al alone. These results suggest that the accumulation of Al sensitizes the membrane to the Fe(II)-mediated peroxidation of lipids, and that the Al-enhanced per oxidation of lipids is a direct cause of the loss of integrity of the plasma membrane (or cell death) in the Ca medium.     

Research on the Threshold of Aluminum Toxicity and the Alleviation Effects of Exogenous Calcium,Phosphorus, and Nitrogen on the Growth of Chinese Fir Seedlings under Aluminum Stress

Chinese fir (Cunninghamia Lanceolata Lamb, Hook) is generally considered a superior timber in southern China and other areas in the world. In the past few decades, aluminum (Al) toxicity has become one of biggest stress factors in the production and growth of Chinese fir, although this species prefers an acidic environment. To date, the selection of indicator species for Al toxicity remains critical in the field, and Al toxicity has not been successfully treated by artificially controlling Chinese fir plantations. To assess the Al toxicity risk, the height of the dominant tree, the concentration of calcium (Ca²⁺)/Al³⁺ in soil solution, and the concentration of Ca²⁺?/?[Ca²⁺ + iron (Fe³⁺) + Al³⁺] in litter leached organic acids were introduced. The results indicated that eight plots had suffered Al toxicity. The threshold of Al toxicity was 37.53 mg kg^?1 in soil or 1.39 mmol L^?1 in soil solution, a pH of 4.15, a Ca²⁺?/?(Ca²⁺ + Fe³⁺ + Al³⁺) molar ratio of 0.487, and a Ca²⁺/Al³⁺ molar ratio of 1.599. The positive effects of exogenous nutrition (Ca, phosphorus [P], and nitrogen [N]) on the growth of Cunninghamia lanceolata seedlings was also studied in pot experiments based on results in the field. The cation nutrition can lead to detoxification, and the exogenous nutrition thresholds were Ca²⁺/?Al³⁺ ≥ 2.8, phosphorus (P)/?Al³⁺ ≥ 4.4, ammonium (NH₄ ^?)–nitrogen (N)?/?Al³⁺ ≥ 4.5. The data presented in this study are very helpful for the understanding of the degree of Al toxicity and have notable significance for the management of Chinese fir plantations.     

The role of the apoplast in aluminium toxicity and resistance of higher plants: A review

In acid mineral soils excess of aluminium ions (AI) is one of the most important factors determining plant species and ecotype distribution, and limiting growth and yield of crops. Aluminium preferentially accumulates in the root tips as sites of cell division and cell elongation. Whether inhibition of cell-division rate is due to direct interaction of Al with the chromatin in the nuclei is rather questionable because of the low radial mobility of Al in the root and the rapidity of cessation of root elongation after Al addition to the growth medium. Externally applied Al instantaneously binds to binding sites in the apoplast. Cross binding of pectates by Al may affect extensibility and water permeability of the cell wall. Interaction of Al with other cell-wall constituents is most likely but needs clarification. Aluminium also affects plasma-membrane characteristics. Ca²⁺ influx and K⁺ efflux are inhibited, and synthesis of callose is induced. Induction of callose suggests an increase rather than a decrease in cytosolic Ca²⁺ as initial response to Al. There is little evidence suggesting major disruption of plasma membrane and cytoplasmic functions by AI. K⁺ uptake, H⁺ extrusion, Fe(III) reducing capacity and lipid peroxidation are hardly affected even in roots severely inhibited in elongation by Al. Al uptake and physiological/biochemical effects of Al on intact plant roots can be mimicked even more sensitively using cell suspension cultures which, therefore, represent a powerful tool for the study of Al toxicity. Large differences in Al resistance exist between plant species and cultivars of a species. Root elongation-rate and callose formation can be used as indicators for Al injury. Since short term Al injury is mainly expressed in the apoplast. Al resistance requires exclusion of Al from or/and inactivation of Al in the apoplast. Generally, Al-resistant genotypes are characterized by lower Al accumulation of the root apical meristems. This is achieved by a lower cation-exchange capacity/surface negativity or complexation of Al through root exudates (mucilage, organic acids). Long term exposure of plants to Al also inhibits shoot growth via induction of nutrient (Mg, Ca, P) deficiencies, drought stress and phytohormone imbalances. Such longer term effects have to be taken into consideration when selecting genotypes for high yielding capacity on acid soils high in available Al.     

Determination of Fe2+ in Rice Leaves (Oryza sativa L.) by Using the Chelator BPDS Alone or Combined with the Chelator EDTA

Abstract

Iron toxicity is a problem in many areas of wetland rice. Since Fe²⁺ is considered to be the toxic form of iron, the objective of this research was to determine the Fe²⁺ concentration in rice leaves using the chelator bathophenanthroline disulfonate (BPDS), disodium salt alone or combined with the chelator ethylenediaminetetraacetate (EDTA), disodium salt, where BPDS should solely chelate the Fe²⁺ and EDTA chelate only Fe³⁺. Thus, the combination of these chelators should stabilize the Fe oxidation states. It was also tested whether the chelators BPDS and EDTA could stabilize the oxidation states of Fe during the extraction of rice leaves. Extractions of rice leaves were carried out using an 1 mM BPDS or BPDS‐EDTA extractant solution. To test the stabilization of the Fe oxidation states by the combination of BPDS with EDTA, the extraction solution for one part of the samples contained 0.07 mM Fe³⁺. An extraction without plant material as control was also taken into consideration. The results indicated that the chelators were able to stabilize the oxidation states of Fe in the control (extraction without plant material). However, in the presence of plant material, Fe³⁺ was partly reduced to Fe²⁺, i.e., the chelators could not stabilize the oxidation states of Fe. Accordingly, we concluded that the BPDS‐EDTA method may function for the Fe²⁺ determination in water and soil, but it is apparently not suited for rice leaves.     

Relationship between Callus Growth and Mineral Nutrients Uptake in Salt-Stressed Indica Rice Callus

ABSTRACT

One month old rice calli were exposed to 0, 50, and 100 mol m^?3 sodium chloride (NaCl) in the liquid LS basal medium supplemented with 2.5 mg L^?1 2,4-dichlorophenoxy acetic acid (2,4-D) and 0.5 mg L^?1 kinetin. Callus relative growth rate (RGR; fresh) of both cultivars indicated a progressive decrease; however, callus dry weight increased as the NaCl level increased in the culture medium. Salinity stress increased the callus sodium (Na⁺), manganese (Mn²⁺), and magnesium (Mg²⁺) contents while potassium (K⁺), calcium (Ca²⁺), and iron (Fe²⁺) contents decreased. ‘Basmati-385’ showed less reduction in callus RGR, K⁺, and Ca²⁺ contents and a larger increase in callus dry weight, Na⁺, Mn²⁺, and Mg²⁺ contents as compared to ‘Basmati-Karnal’. However, the reverse was true for Fe²⁺ contents. K⁺/Na⁺ and Ca²⁺/Na⁺ ratios generally decreased under salt stress. Overall, reduction in callus relative growth rate was found to be inversely correlated with decrease in K⁺, Ca²⁺, and Fe²⁺ uptake and directly correlated with increased Na⁺ and Mg²⁺ concentration in callus tissue.     

古土壤地球化学的某些问题——黄土风化过程中元素的变化

对黄土中埋藏古土壤的研究有过许多报道^[2,5,8].但对黄土风化过程中元素的变化讨论则不多.笔者是在近年来对陕西洛川黄土剖面工作的基础上,讨论了不同类型古土壤中元素的含量与分布,古土壤剖面中元素的变化.并将古土壤的化学组成与黄土母质进行比较,进而论述了在古气候变迁的影响下,黄土剖面中元素迁移、积聚的地球化学特征.这对探讨黄土的堆积环境和生物气候条件的演变,以及地层划分等均有十分重要意义.     

Uptake of cations by annual ryegrass as related to cations adsorbed onto root exchange sites

Abstract

Previously published results on exchange capacities for Ca²⁺, Mg²⁺, Mn²⁺, and K⁺ in the Donnan free space of roots of two ryegrass cultivars (Lolium multiflorum Lam. cv. Marshall and Wilo) grown at two Al levels in the nutrient solution (0 and 74 μM) were correlated with the average net uptakes of the same cations. For Al‐treated plants regressed separately, significant correlations r=0.906 and r=0.963 were found for Mn²⁺ and Ca²⁺/Mg²⁺, respectively. No significant correlations were observed for these cations in control plants. In contrast, when data of control and Al‐treated plants were combined, significant linear correlations r=0.805, r=0.924, and r=0.968 were found for Ca²⁺, K⁺, and K⁺/(Ca²⁺+Mg²⁺)^1/2, respectively. The influence of cations adsorbed onto the root exchange sites and the effect of Al on the cation uptake processes were discussed.     

土壤有机矿质复合体研究──X.有机矿质复合体转化的初步研究

本文研究铁键、铝键、钙键复合体与溶液中Ｃａ＾２＋、Ｆｅ＾３＋、Ａｌ＾３＋金属离子的相互作用,结果显示,复合体上键合的Ｆｅ＾３＋,不能被溶液中的Ｃａ＾２＋、Ａｌ＾３＋置换,复合体上键合的Ａｌ＾３＋仅少量被Ｆｅ＾３＋、Ｃａ＾２＋置换进入溶液,复合体上键合的Ｃａ＾２＋则可较多地被Ａｌ＾３＋、Ｆｅ＾３＋置换进入溶液,置换的量与ＰＨ及粘土矿物类型有一定关系,尽管复合体上键合的Ｆｅ＾３＋、Ａｌ＾３＋、Ｃａ＾３     

Abstracts of Nippon Dojo-Hiryogaku Zasshi (Japanese Journal of Soil Science and Plant Nutrition)

The electrokinetic behavior of colloidal particles in three waterlogged soils at 38°C was investigated with reference to the stability changes of soil colloidal suspensions under reductive conditions. The dispersed clay particles of the three soils exhibited a negative zeta (ζ) potential. The absolute value of the ζ-potential, |-ζ|, of these soils in the earlier period of waterlogging decreased, which caused the flocculation of clay particles. The concentrations of divalent cations, i.e., Fe²⁺ and Ca²⁺ in the soil solutions were estimated to be higher than their critical flocculation concentrations (CFCs) on the basis of the observed CFCs of Fe²⁺ and Ca²⁺ for the clay suspension of halloysite as a reference. With the progression of the reduction process, clay particles of one soil still exhibited a low |- ζ| and flocculated. The concentrations of Fe²⁺ and Ca²⁺ in the soil solutions were estimated to be higher than their CFCs, respectively. The clay particles of two sandy soils, however, showed an increase in |- ζ| due to the increase in pH and dispersed. The concentrations of Fe²⁺ and Ca²⁺ in the soil solutions were estimated to be lower than their CFCs, respectively. The stability changes of the soil colloidal suspensions by these divalent cations under sequential soil-reduction can be explained by the alteration of the Stern potential (- ψ _s ), which determines the repulsion energy related to the potential energy of interaction between two particles. The apparent decrease in the Ca²⁺ concentration of the soil solutions in the later period of waterlogging was explained largely by the re-adsorption of water-soluble Ca²⁺ on the exchange sites of soil clays with the decrease in the Fe²⁺ concentration in the soil solution.     

Suppression of Methane Production via the Promotion of Fe2+ Oxidation in Paddy Fields

ABSTRACT

Methane is a greenhouse gas, mainly generated from paddy fields and lakes by methanogens using hydrogen and acetic acid as substrates. In anaerobic environments with adequate Fe³⁺, iron-reducing microorganisms utilize these substrates, thus suppressing methane generation. We promoted Fe²⁺ oxidation to Fe³⁺ by physically stirring paddy soil and using a chelating agent (nitrilotriacetic acid; NTA) to evaluate the feasibility of the suppression of methane generation using Fe³⁺-reducing bacteria. Under anaerobic conditions, Fe³⁺ reduction to Fe²⁺ began immediately in the slurry made by adding water into air-dried paddy soil. Methane generation began on the 6th day when most Fe³⁺ was reduced. Under anaerobic conditions for 10 days followed by aerobic conditions, Fe²⁺ oxidation hardly progressed under static conditions. On stirring the slurry, Fe²⁺ oxidation progressed over 12 h (67% Fe²⁺ oxidized to Fe³⁺). When NTA was added under anaerobic conditions followed by stirring under aerobic conditions, Fe²⁺ oxidation was promoted further. The idea of physical stirring of paddy soil in the actual environment was derived from the effects of paddy soil stirring by ducks in interrelated rice–duck farming. In such farming, paddy soil contains more Fe³⁺ in its surface water compared with normal farming, resulting in suppressed methane generation.     

Coupled diffusion and oxidation of ferrous iron in soils: III. Further development of the model and experimental testing

Equations are developed to predict the distribution of Fe²⁺ between solid and solution phases in a reduced soil undergoing oxidation at different pHs, based on cation-exchange equilibria and electrical neutrality in the solid and solution. The equations satisfactorily explained experimental results. They are incorporated in the model of Fe²⁺ diffusion and oxidation developed in Part II, and the model is also extended to allow for O₂ consumption in processes other than Fe²⁺ oxidation. The resultant predictions are tested against measured profiles of Fe(II), Fe(III) and pH in cylinders of reduced soil exposed to O₂ at one end. When oxidation rate constants measured in stirred soil suspensions were used to run the model, the predicted rates of O₂ consumption were too great and the spread of the oxidation front too small. Satisfactory agreement was achieved for oxidation rate constant values about one-eighth of those measured in the stirred suspensions. The findings are consistent with the rate of Fe²⁺ oxidation in soil being controlled by access of O₂ to Fe²⁺ sorption sites, as suggested in Part I. The revised model allows a study of the effects of Fe²⁺ oxidation on the mobility of other cations in reduced soils, e.g. nutrient cations in the rice rhizosphere. Fez+ oxidation and the accompanying acidification may greatly impede cation mobility in reduced soils.     

Aluminium and uptake of base cations by tree roots: A critique of the model proposed by Sverdrup et al.

Sverdrupet al. (1992) proposed a model intended to evaluate effects of soil solution (Ca²⁺+Mg²⁺/Al³⁺ ratios on the uptake of Ca²⁺ and Mg²⁺ (here called base cations=BC) by tree roots. They considered the adsorption of BC on exchange sites on root surfaces to be a major step, and the competition between Al³⁺ and BC for exchange sites on roots to be crucial. Although this may certainly affect the rates of uptake, it will not exclude base cations from entering the root cells through ion channels or by carriers. Above all, the model overlooks important gradients in the rhizosphere, e.g. pH-gradients and root exudates, which have profound influences on the speciation of Al. One should instead consider modifying existing models accounting for processes in a buffered soil medium and handling gradients in the rhizosphere (e.g. Nye and Tinker, 1977). This would also require considerations on mycorrhizas and possible changes in the capacity for uptake of certain ions, which could be induced by deficiencies.     

Factors related to iron uptake by dicotyledonous and monocotyledonous plants. II. The reduction of Fe3+ as influenced by roots and inhibitors

In a companion paper (10), varieties of four plant species [two monocotyledons (oats and corn) and two dicotyledons (soybeans and tomato)] were shown to differ widely in their ability to respond to Fe‐stress. The ability of the more Fe‐efficient varieties was manifested by a lowering of the pH of the ambient medium of the root and/or by loss of reductants from the root. Both effects can enhance uptake of Fe by the roots, since Fe is taken up primarily, if not entirely, as Fe²⁺ ions. Thus, a given stressed plant has a means, under some degree of metabolic control, for modifying the root environment and, thereby, alleviating its chlorotic condition.

The present investigation deals with environmental factors, particularly chemical inhibitors, modifying the effectiveness of the stress response. Without inhibitors, excised root samples of the four species exhibited a wide range of abilities to reduce Fe³⁺ to Fe²⁺. Roots of the dicotyledonous species reduced about twice as much Fe³⁺ as did equal weights of the monocotyledonous species. Iron‐efficient tomato, soybean, and oat roots reduced more Fe³⁺ than did roots of the Fe‐inefficient varieties. The two corn varieties were about equal in their effectiveness.

Comparable samples of roots were also exposed to chemicals that induce or aggravate Fe chlorosis. Those found to be very effective inhibitors of Fe³⁺ reduction by the roots included: hydroxide, orthophosphate, pyrophosphate, Cu²⁺ and Ni²⁺. Other ions (includ ing Mn²⁺, Zn²⁺ and molybdate) and ethyl ammonium phosphate also inhibited Fe³⁺ reduction but to a lesser degree. Citrate, however, enhanced Fe³⁺ reduction. The degree of inhibition or enhancement differed for each of the varieties. In general, the Fe‐efficient plants were best able to reduce Fe³⁺ in spite of the inhibitory influence of the imposed treatments. Thus, our findings indicated that inhibition of the Fe³⁺ ‐reduction process at, or near, the periphery of the root is an apparent cause of Fe chlorosis.     

Fe,Al, Mn,and S chemistry of Sphagnum peat in four peatlands with different metal and sulfur input

Comparisons among 4 peatland sites representing a gradient of increasing Fe, Al, Mn, and S loading revealed significant accumulation of total Fe, Al, and S, but not Mn, in surface (0 to 20 cm deep) peat along the gradient. Iron and Al accumulation were contributed mainly by organically bound fractions, with oxides contributing to a lesser extent. Although SO₄ ^2? and Fe sulfides showed significant increases in concentration along the gradient, most of the accumulation of total S was contributed by organic, rather than inorganic S. Laboratory studies of Fe²⁺ adsorption by peat indicated that increasing the pH of added Fe²⁺ solutions (pH values of 3, 4, 5, and 6) did not significantly affect Langmuir equation estimates of either maximum Fe²⁺ adsorption capacity or the affinity of peat for Fe²⁺. Regardless of the pH of the added Fe²⁺ solutions, final solution pH values were relatively uniform, averaging about 3.4, reflecting a considerable bufferring capacity of Sphagnum peat. Factors affecting the accumulation of metals and S in peat remain topics for further investigation.     

Use of organic phosphorus byRhizobium leguminosarum biovarviceae phosphatases

Rhizobium leguminosarum biovarviceae strain TAL 1236 growing on different organic P compounds as sources of phosphate exhibited phosphatase activities. The strain was able to produce both acid and alkaline phosphatase. However, its ability to produce alkaline phosphatase was much higher. When cellular phosphate fell to 0.115% of cell protein, cellular and extracellular phosphatase activities were enhanced. Mg²⁺, Co²⁺, and Ca²⁺ stimulated the activity of alkaline phosphatase more than acid phosphatase. However, Mn²⁺ and Fe²⁺ activated acid phosphatase rather than alkaline phosphatase. It may be concluded thatR. leguminosarum contributes significantly to the release of P from organic compounds through the action of phosphatase which can be activated by a range of cations.     

Sites and processes of nutrient accumulation in the subsoil through water percolation from the plow layer in a submerged paddy soil microcosm

The leaching of nutrients from the plow layer by water percolation and their accumulation in the subsoil observed in a Japanese paddy field (Katoh et al. 2004: Soil Sci. Plant Nutr., 50, 721-729) were determined semi-quantitatively in a soil column experiment. Ca²⁺, Mg²⁺, K⁺, Mn²⁺, Fe²⁺, and phosphate in percolating water from the plow layer soil column were retained in the subsoil columns that were connected to the plow layer soil column. Fe²⁺, K⁺, and phosphate accumulated in the uppermost part of the subsoil. Accumulation of Fe²⁺ in the uppermost part of the subsoil was presmnably due to the cation exchange process with concomitant desorption of Ca²⁺. In contrast, Ca²⁺ and Mg²⁺ in percolating water from the plow layer soil colmnn accumulated once in the subsoil, and translocated downwards slowly with successive water percolation. Considerable amounts of inorganic carbon (IC) and dissolved organic carbon (DOC) in percolating water from the plow layer soil column were also retained in the subsoil columns. IC did not accumulate a gaseous form.     

Effects of iron toxicity on the morphological and biological characteristics of rice root border cells

Toxicity of Fe²⁺ is one of the major constraints for lowland rice production in tropical and subtropical areas. The root tip is a primary site of iron (Fe²⁺) toxicity in rice. To explore the effects of iron toxicity on the morphological and biological characteristics on the border cells in rice (Oryza sativa L.), experiments were carried out using the border cells in two cultivars. The experimental results revealed the following properties of border cells shared by both rice cultivars: the first border cells appeared almost synchronously with the emergence of the primary root tip; the number of border cells reached maximum when the root was 25 mm long; the border cells were most viable when the root length was 20 mm; and the relative activity of pectin methylesterase (PME) was the highest when the root length was 2 mm. The two rice cultivars exhibited different trends in their response to Fe²⁺ toxicity: the number of root border cells in Fe²⁺-resistant Zhongyou 9288 increased when experiencing low levels of Fe²⁺ treatment, but then declined at higher Fe²⁺ levels. The number of root border cells in Fe²⁺-sensitive Shanyou No. 10, however, declined rapidly when the concentration of Fe²⁺ increased. The results also showed that Fe²⁺ toxicity hindered the development of root border cells of both rice cultivars, but the Fe²⁺ sensitive variety experienced thickened the root cap cell walls that led to programmed cell death.     

Growth and ion uptake of four Brassica species as affected by Na/Ca ratio in saline sand culture

The influence of supplemental Ca² in saline nutrient solutions on germination, growth, and ion uptake of four Brassica species, B. campestris L., B. carinata, A.Br., B. juncea (L.) Czern. and Coss., and B. napus L. was studied in sand culture. The addition of 11.25 mM CaC1² to nutrient solution containing 225 mM NaC1 improved percentage of germination of B. napus and B. juncea, but had no significant effect on the germination speed of the four species. There was no significant effect of additional amount of Ca² in the saline medium (150 mM NaC1) on the shoot biomass and seed yield of B. carinata and B. campestris. By contrast, shoot dry matter of B. napus and B. juncea increased significantly with the increased in Ca² concentration of the growth medium, but their seed yield remained unaffected. Decreased Ca² concentrations of the saline growth medium reduced percent oil content in B. carinata, B. juncea, and B. campestris. Increasing Na/Ca ratio of the external medium affected ion uptake differently in different species. In B. carinata, a relatively salt-tolerant species, the concentrations of Na⁺ and K⁺ in the shoots remained unaffected, but the C1 concentration was reduced linearly with the increase in external Na/Ca ratios. Root K⁺ and Ca²⁺ of the species decreased with the decrease in Ca²⁺ supply. In B. campestris increasing Na/Ca ratios of the saline medium had no effect on the concentrations of Na⁺, C1, and Ca²⁺ in the shoots and Na⁺, C1, and K⁺ in the roots. Only shoot K⁺ and root Ca²⁺ decreased consistently. In the highly salt-sensitive species, B. napus, the shoot Na⁺ was reduced by the addition of Ca²⁺ in the salt treatment, whereas the C1 and Ca²⁺ uptake was promoted by supplemental Ca²⁺. The root K⁺ concentrations decreased with the increase in Na/Ca. In B. juncea, which was similar to B. napus in biomass production, high Ca²⁺ concentration in the salt treatment reduced the shoot Na⁺ and root C1 concentrations and promoted the K⁺ uptake. Shoot Na/Ca and Na/K ratios were increased in B. napus and B. juncea at the highest Na/Ca ratio of the growth medium. Shoot K⁺ selectivity, S^K,Na (determined as molar ratio of K: Na in tissue to molar ratio of K:Na in external medium) of all species remained unaffected except for B. juncea in which it decreased significantly at the highest Na/Ca ratio. The root K⁺ selectivity increased in B. carinata.     

Nitrite stability influenced by iron compounds

The decomposition of nitrite was studied in the presence of (1) different amounts of ferrous iron and (2) an amorphous and a crystalline (haematite) iron product at different pH and Eh conditions. It was found that ferrous iron positively influenced the nitrite decomposition. Even at pH 6, where self-decomposition is excluded, some nitrite was decomposed. It was shown that at all studied pH values the second order decomposition rate increased as the amount of ferrous iron increased. From the calculation of the activation energy it was found that the dependence of the rate constant on temperature increased when the medium was more acid, or when the amount of Fe²⁺ increased at the same pH. The nitrite half-life was longest at pH 6, 25°C and 200 mg Fe²⁺ l^?1; it was shortest at pH 4, 30°C and 800 mg Fe²⁺ l^?1. The experiments with Fe²⁺ derived from solid iron compounds showed that all conditions favouring a high amount of ferrous iron in solution, such as low redox potential, low pH, amorphous or less crystalline material, enhanced nitrite decomposition.