Nitrogen as a limiting factor in the development of beech forests in the Sierra de la Demanda (Spain)

The leaf nitrogen contents of beech growing in the Sierra de la Demanda are studied, relating the contents with other structural population characteristics. For this, different experiments were conducted: (a) To analyze of nitrogen levels in shed leaves, in leaf biomass and in leaves decomposing on a test plot in the Tres Aguas beech forest. (b) To study leaf nitrogen contents over a vegetative cycle in the above beech forest. (c) To study the leaf nitrogen contents of thirty beech stands in the Sierra de la Demanda located at different altitudes and corresponding to three beech budding isophenes. Annual nitrogen accumulation in leaf biomass was 79.4 kg ha^-1yr^-1, of which 22.9 kg ha^-1yr^-1 return to the soil substrate through shedding and 2.1 kg ha^-1yr^-1 are actually incorporated into the soil. Nitrogen cannot be a limiting factor for the development of the beech stands studied because all of them surpassed the leaf deficiency threshold. Only other factors such as those of the soil or silvicultural treatment have a decisive effect on the production of the stands studied. Study of the correlations for leaf nitrogen contents and the structural population characteristics explored reveals that leaf nitrogen was only slightly correlated with the mean height of the trees at the plot.     

Changes in diversity and storage function of ectomycorrhiza and soil organoprofile dynamics after introduction of beech into Scots pine forests

Diversity and storage function of mycorrhiza as well as soil organoprofile formation were investigated in a chronosequence of a pure Scots pine (Pinus sylvestris L.) stand, of Scots pine stands that were underplanted with beech (Fagus sylvatica L.) and in three pure beech stands of different age. Mycorrhiza diversity was higher in the pure beech stands compared to the pure pine stand. Beech and pine trees in the mixed stands had similar dominant mycorrhiza morphotypes. However, trees in two of the three pure beech stands were mycorrhized with other types. Mycorrhizal abundance and nutrient amounts of mycorrhizae associated with beech trees were higher in the mixed and in the pure beech stands compared to pine mycorrhizae indicating that nutrient uptake was higher in older beech than in older pine trees. Humus quality varied from pine to beech stands. Plant litter storage in the humus layer was highest in the youngest mixed stand and lowest in the oldest beech stand. Humus forms changed from moder grass-type in the pure Scots pine stand to mor-like moder and moder rich in fine humus with increasing age of beeches in the mixed stands. The older beech stands were characterised by oligomull and mull-like moder as the dominating humus forms. The ecologically favourable humus forms, i.e., nutrient rich humus forms in the older beech stands correlate well with the higher mycorrhizal diversity and abundance as well as the higher nutrient storage of their mycorrhizae in these stands. The results are also discussed with regard to the 'base-pump effect' of beech trees.     

Foliar free polyamine and inorganic ion content in relation to soil and soil solution chemistry in two fertilized forest stands at the Harvard Forest,Massachusetts

Polyamines (putrescine, spermidine, and spermine) are low molecular weight, open-chained, organic polycations which are found in all organisms and have been linked with stress responses in plants. The objectives of our study were to investigate the effects of chronic N additions to pine and hardwood stands at Harvard Forest, Petersham, MA on foliar polyamine and inorganic ion contents as well as soil and soil solution chemistry. Four treatment plots were established within each stand in 1988: control, low N (50 kg N ha^-1 yr^-1 as NH₄NO₃), low N + sulfur (74 kg S ha^-1 yr^-1 as Na₂SO₄), and high N (150 kg N ha^-1 yr^-1 as NH₄NO₃). All samples were analyzed for inorganic elements; foliage samples were also analyzed for polyamines and total N. In the pine stand putrescine and total N levels in the foliage were significantly higher for all N treatments as compared to the control plot. Total N content was positively correlated with polyamines in the needles (P 0.05). Both putrescine and N contents were also negatively correlated with most exchangeable cations and total elements in organic soil horizons and positively correlated with Ca and Mg in the soil solution (P 0.05). In the hardwood stand, putrescine and total N levels in the foliage were significantly higher for the high N treatment only as compared to the control plot. Here also, total foliar N content was positively correlated with polyamines (P 0.05). Unlike the case with the pine stand, in the hardwood stand foliar polyamines and N were significantly and negatively correlated with foliar total Ca, Mg, and Mn (P 0.05). Additional significant (P 0.05) relationships in hardwoods included: negative correlations between foliar polyamines and N content to exchangeable K and P and total P in the organic soil horizon; and positive correlations between foliar polyamines and N content to Mg in soil solution. With few exceptions, low N + S treatment had effects similar to the ones observed with low N alone for both stands. The changes observed in the pine stand for polyamine metabolism, N uptake, and element leaching from the soil into the soil solution in all treatment plots provide additional evidence that the pine stand is more nitrogen saturated than the hardwood stand. These results also indicate that the long-term addition of N to these stands has species specific and/or site specific effects that may in part be explained by the different land use histories of the two stands.     

Spatial variability of NO and NO2 flux rates from soil of spruce and beech forest ecosystems

In order to evaluate differences in the magnitude of NO and NO₂ flux rates between soil areas in direct vicinity to tree stems and areas of increasing distance to tree stems, we followed in 1997 at the Höglwald Forest site with a fully automated measuring system a complete annual cycle of NO and NO₂ fluxes from soils of an untreated spruce stand, a limed spruce strand, and a beech stand using at each stand measuring chambers which were installed onto the soils in such a way that they formed a stem to stem gradient. Flux data obtained since the end of 1993 from measuring chambers placed at the interstem areas of the stands, which had been used for the calculation of the long year annual mean of NO and NO₂ flux rates from soils of the stands, are compared to both (a) those obtained from the interstem chambers in 1997 and (b) those from the stem to stem gradient chambers. Daily mean NO fluxes obtained in 1997 were in a range of 0.3 – 280.1 g NO-N m^–2 h^–1 at the untreated spruce stand, 0.5 – 273.2 g NO-N m^–2 h^–1 at the limed spruce stand and 0.5 - 368.8 g NO-N m^–2 h^–1 at the beech stand, respectively. Highest NO emission rates were observed during summer, lowest during winter. Daily mean NO₂ fluxes were in a range of –83.1 – 7.6 g NO₂-N m^–2 h^–1 at the untreated spruce stand, -85.1 – 2.1 g NO₂-N m^–2 h^–1 at the limed spruce stand and –77.9 to –2.0 g NO₂-N m^–2 h^–1 at the beech site, respectively. As had been observed for the years 1994–1996, also in 1997 NO emission rates were highest at the untreated spruce stand and lowest at the beech stand and liming of a spruce stand resulted in a significant decrease in NO emission rates. For NO₂ no marked differences in the magnitude of flux rates were found between the three different stands. Results obtained from the stem to stem gradient experiments revealed that at all stands studied NO emission rates were significantly higher (between 1.6- and 2.6-fold) from soil areas close to the tree stems and decreased – except at the beech stand - with increasing distance from the stems, while for NO₂ deposition no marked differences were found. Including the contribution of soil areas in direct vicinity to the beech stems in the estimation of the annual mean NO source strength revealed that the source strength has been underestimated by 40% in the past.     

Influence of anions on the potassium status and productivity of kiwifruit (Actinidia deliciosa) vines

The effects of K fertiliser (160 kg ha^-1) applied with Cl^- or SO₄ ^2- as the accompanying anion on the K nutrition of kiwifruit (Actinidia deliciosa var. deliciosa) were assessed in a field experiment, using vines with varying degrees of K deficiency. Leaf K concentrations in spring were significantly higher for vines receiving KCl, compared to those receiving K₂SO₄. This effect did not interact significantly with the degree of K deficiency, and persisted for about 6 weeks. Subsequently there was no significant difference between the leaf K concentrations for the vines receiving KCl or K₂SO₄. Applying K as KCl increased the leaf Cl concentration, especially in spring, while applying K as K₂SO₄ had no significant effect on the leaf S concentration at that time. These results implied a greater requirement for organic acid anions for K⁺ uptake from K₂SO₄ than from KCl, and the importance of organic acid anions for K⁺ uptake from different sources of K fertiliser is discussed. This transient effect of the accompanying anion on leaf K status was associated with large effects on flowering, and fruit yields were about 28% higher for plants receiving KCl rather than K₂SO₄.The effects on growth and tissue nutrient composition of varying the concentrations of Cl^-, NO₃ ^-, SO₄ ^2- and H₂PO₄ ^- around the roots of kiwifruit vines were examined in a solution culture experiment. For H₂PO₄ ^-, plant growth was very similar over a wide range of rates of addition. For the other anions, the range between deficiency and toxicity was clearly delineated. For Cl^- and NO₃ ^-, toxicity was associated with high tissue concentrations of Cl and N, respectively, and was consistent with competition for uptake between Cl^- and NO₃ ^-. However, for SO₄ ^2-, toxicity was associated with only a small increase in the tissue S concentration relative to that associated with maximum growth, and appeared to result more from effects on uptake of other anions and cations rather than from direct effects of high tissue S concentrations.It is concluded that the sensitivity of kiwifruit to the anion accompanying K⁺ in fertiliser may be related to the unusually high requirement for Cl previously reported for this species.     

Relationship of Cell Sap pH to Organic Acid Change During Ion Uptake

Excised roots of barley (Hordeum vulgare, var. Campana) were incubated in KCl, K₂SO₄, CaCl₂, and NaCl solutions at concentrations of 10⁻⁵ to 10⁻² n. Changes in substrate solution pH, cell sap pH, and organic acid content of the roots were related to differences in cation and anion absorption. The pH of expressed sap of roots increased when cations were absorbed in excess of anions and decreased when anions were absorbed in excess of cations. The pH of the cell sap shifted in response to imbalances in cation and anion uptake in salt solutions as dilute as 10⁻⁵ n. Changes in cell sap pH were detectable within 15 minutes after the roots were placed in 10⁻³ n K₂SO₄. Organic acid changes in the roots were proportional to expressed sap pH changes induced by unbalanced ion uptake. Changes in organic acid content in response to differential cation and anion uptake appear to be associated with the low-salt component of ion uptake.     

Distribution of greenhouse gases, nitrite, and δ13C of dissolved inorganic carbon in Lake Biwa: Implications for hypolimnetic metabolism

The vertical distribution of dissolved greenhouse gases (CH₄,CO₂ and N₂O), NO ,and ¹³C of CO₂ in Lake Biwa during a stagnantperiod was precisely determined. CO₂ as well as NO was accumulated in the hypolimnion, whereas NO and CH₄concen\-trations were generally higher in theepilimnion than in the hypolimnion. In August, NO andCH₄ were ephemerally accumulated at the thermocline. Theconcentration of CH₄ always exceeded equilibrium with respectto air/water exchange. N₂O was rather uniformly distributed inboth time and space, and remained near equilibrium with respect toair/water exchange. All of these observations are similar to otherstratified, oligotrophic lakes, in which the hypolimnia were welloxygenated. The ¹³C of CO₂ became morenegative with increasing depth, and showed a strong negativecorrelation with apparent oxygen utilization. From the data, the ¹³Cvalue of organic matter decomposed into CO₂ inthe hypolimnion was calculated by isotope mass-balance, and found tobe in a similar range to ¹³C of phytoplankton and benthic algaeand distinctively higher than ¹³C of both terrestrial andsedimentary organic matters. This suggests that autochthonous organicmatter was the major source of CO₂.     

Water-soluble organic matter in forest soils

By applying a modified gel permeation technique, the molecular-size distribution (MSD) and complexing properties of water-soluble organic matter (WSOM), isolated from the A_h horizon under stands with either Douglas-fir, European beech or Scots pine were established. Both with respect to MSD and complexing properties, the dissolved organic matter was highly similar. WSOM was comprised of compounds apparently high in molecular weight (>1 kDa) and with a complexing capacity of 1.0±0.1 mol mg^–1 carbon as determined for Cu(II) at pH 5.5 and 0.01 M ionic strength. The effect of WSOM on the partitioning of cations between soil solid phase and soil solution was evaluated in several soil batch experiments using loamy sand or sandy soil material. Although a large part of WSOM was sorbed to the soil matrix, Al, Cu, Fe and Pb were solubilized in considerable amounts by complexation. The Mn concentration in the soil solution was also significantly increased but this probably resulted from a redox reaction, with certain constituents of WSOM serving as electron donor. With a decrease in soil pH, cation mobilization by WSOM was significantly lower as a result of increased sorption and a decrease in complexing capacity of the soluble organics. Application of several low MW aliphatic and phenolic acids gave results similar to the results obtained with WSOM.     

Effect of some nitrogenous salts on nitrogen transfer and protease activity in germinatingZea mays L. seeds

Maize seeds were allowed to germinate in the presence of different nitrogenous salts for 72 h. Changes in the ethanol soluble and insoluble nitrogen were studied in the embryo and in the endosperm. Supply of Ca(NC₃)₂ enhanced germination and protease activity in the endosperm resulting in greater solubilisation of protein to soluble nitrogen in the seeds. NH₄NO₃ and (NH₄)₂SO₄ were less effective as compared to Ca(NO₃)₂. Cycloheximide inhibited germination and protease activity. Pretreatment also resulted in increase in growth, soluble and insoluble nitrogen, and nitrate reductase activity in the primary leaves. Ca(NO₃)₂ was more effective than NH₄NO₃ and (NH₄)₂SO₄.     

Geochemical controls for Al, Fe, Mn, Cd, Cu, Pb, and Zn during experimental acidification and recovery of Little Rock Lake, WI, USA

Concentrations of Al, Fe, Mn, Cd, Cu, Pb, and Zn were measured in thereference and treatment basins of Little Rock Lake (Vilas County, Wisconsin), alow-alkalinity, seepage system (pH 6.1, alkalinity25eq/L) during six years of a whole-basinacidificationand the first four years of the lake's recovery. The treatment basin wasacidified with H₂SO₄ in three two-year steps to pH5.6, 5.1, and 4.7. By the end of year 4 of recovery, treatmentbasin pH increased to 5.3 as a result of internal alkalinity generation.During acidification, dissolved Mn and Fe (0.4mpore-size filters) increased at pH 5.6; dissolved Al, Cd, and Zn becameelevated at pH 5.1; and dissolved Pb at pH 4.7. Dissolved Cu remainedsimilar in both basins to pH 4.7. Al, Fe and Mn levels declinedsignificantly during the recovery period, approaching values at pH 5.3intermediate between the concentrations at pH 5.6 and 5.1 during acidification.Dissolved Al and Fe in the reference basin were near the equilibrium levels forsolubility of gibbsite (Al(OH)₃) and amorphousFe(OH)₃(s).The acidified basin was undersaturated relative to gibbsite, and dissolved Alwas limited by pH disequilibrium between the water column and sediments andpossibly by Al-DOC precipitation. Dissolved Fe apparently was controlled bysolubility of amorphous Fe(OH)₃(s) and Fe-DOC precipitation.Dissolved Mn levels in both basins were consistent with manganite[-MnOOH(s)] solubility. Elevated levels of Cd, Pb, and Zn in thetreatment basin during acidification probably resulted from less efficientscavenging of atmospherically-deposited Cd, Pb, and Zn by settling particles.     

Postsynaptic currents in phasic and tonic muscle fibers of the rat extraocular muscle

Focal extracellular recordings were made of postjunctional currents produced at synapses of the inferior rectus eye muscle fibers by the spontaneous release of quanta of transmitter. These consisted of miniature endplate currents, or MEPC, in phasic fibers and miniature postjunctional currents, or MPJC, in tonic fibers. Open time of ionic channels (_chan) was also registered. In tonic fibers, MPJC lasted considerably longer than MEPC did in phasic fibers: rising time, decay time, and _chan in the former measured respectively 2.5, 4–5, and 2.2 times higher than in the latter. Acetylcholinesterace (AChE) inhibition produced a much greater (4.4-fold extension of current decay in phasic than in tonic fibers, where a 1.8-fold increase was seen, thereby reducing the gap between the decay time of currents in these fibers to a difference of 1.6 times. The more protracted decay of MPJC in tonic fibers compared with MEPC in phasic fibers is determined by the lower functional activity of AChE as well as the higher value of _chan. Duration of MEPC and magnitude of _chan in the "slow" phasic fibers of rat skeletal muscles fell well below the same parameters measured in the tonic fibers of the ocular muscle.I. M. Sechenov Institute of Evolutionary Physiology and Biochemistry, Academy of Sciences of the USSR, Leningrad. Translated from Neirofiziologiya, Vol. 19, No. 1, pp. 120–129, January–February, 1987.     

Greater accumulation of litter in spruce (Picea abies) compared to beech (Fagus sylvatica) stands is not a consequence of the inherent recalcitrance of needles

Background and aims

Replacement of beech by spruce is associated with changes in soil acidity, soil structure and humus form, which are commonly ascribed to the recalcitrance of spruce needles. It is of practical relevance to know how much beech must be admixed to pure spruce stands in order to increase litter decomposition and associated nutrient cycling. We addressed the impact of tree species mixture within forest stands and within litter on mass loss and nutritional release from litter.

Methods

Litter decomposition was measured in three adjacent stands of pure spruce (Picea abies), mixed beech-spruce and pure beech (Fagus sylvatica) on three nutrient-rich sites and three nutrient-poor sites over a three-year period using the litterbag method (single species and mixed species bags).

Results

Mass loss of beech litter was not higher than mass loss of spruce litter. Mass loss and nutrient release were not affected by litter mixing. Litter decay indicated non-additive patterns, since similar remaining masses under pure beech (47%) and mixed beech-spruce (48%) were significantly lower than under pure spruce stands (67%). Release of the main components of the organic substance (C_org, N_tot, P, S, lignin) and associated K were related to mass loss, while release of other nutrients was not related to mass loss.

Conclusions

In contradiction to the widely held assumption of slow decomposition of spruce needles, we conclude that accumulation of litter in spruce stands is not caused by recalcitrance of spruce needles to decay; rather adverse environmental conditions in spruce stands retard decomposition. Mixed beech-spruce stands appear to be as effective as pure beech stands in counteracting these adverse conditions.     

Effects of multiple stresses on radish growth and resource allocation

Summary Acclimation of wild radish plants to a simultaneous combination of SO₂ fumigation and decreasing nitrate availability was investigated. Plants were grown for 24 d under continuous daytime (10h) exposure to 0 or 0.4 ppm SO₂ and were grown in a nutrient solution with stable nitrate concentrations of 100 M for the first 15 d, 50 M from day 15 to day 19, and 25 M from day 19 to day 24. Analysis of relative growth rates (RGR) showed that radish plants responded rapidly to changes in nitrate availability and that SO₂ treatment affected those responses. Shoot RGR of plants from both treatments and root RGR of control plants showed rapid declines and subsequent recoveries in response to decreasing nitrate availability. Root RGR of SO₂-treated plants declined rapidly in response to decreased nitrate availability, but did not recover as quickly or completely as root RGR of control plants. Analysis of specific leaf weights and tissue nitrogen concentrations showed that control plants had significantly higher amounts of nitrogen in tissues after nitrate availability was lowered, and had higher rates of nitrate uptake in comparison to SO₂-treated plants; especially when nitrate availability was highest. Furthermore, control plants had temporarily higher rates of root respiration in comparison to SO₂-treated plants, suggesting that control plants temporarily allocated more resources to physiological processes occurring in roots, such as nutrient uptake. Although SO₂-induced changes in growth and resource allocation of plants were relatively small, it was probable that SO₂ treatment of radish plants affected plant nitrogen balance, and subsequently affected the ability of plants to respond to decreased nitrate availibility, by affecting resource partitioning to nitrate uptake and root growth.     

Stable sulfur isotope analysis of SO2 pollution impact on vegetation

Summary The ³⁴S value of SO₂ emitted by natural gas refineries is about +25, which is higher than that for non-industrial sulfur sources in our study areas. Terrestrial mosses absorb SO₂ from the atmosphere and have a ³⁴S value which is directly related to the degree of SO₂ stress to which they are subjected. The ³⁴S values for conifer needles are lower than for mosses at the same collection site, which indicates that trees obtain sulfur from both atmospheric and soil sources.Potted conifers were transferred to sites differing in their degree of SO₂ stress. This difference is reflected by the change of ³⁴S values of their needles. SO₂ absorbant pot covers, such as charcoal and moss, reduce the amount of airborne sulfur which is available to tress. Moss also may reduce SO₂ absorbed by soils in forest stands. We have used analysis of ³⁴S values to (1) help define SO₂ dispersion patterns; (2) reveal the rates at which plants accumulate this pollutant; and (3) associate suspected SO₂ injury more closely to an emission source.     

Soluble minerals in chemical evolution

The adsorption of 5-AMP and 5-CMP was studied in saturated solutions of several soluble mineral salts (NaCl, Na₂SO₄, MgCl₂·6H₂O, MgSO₄·7H₂O, CaCl₂·2H₂O, CaSO₄·2H₂O, SrCl₂·6H₂O, SrSO₄, and ZnSO₄·7H₂O) as a function of pH, ionic strength, and surface area of the solid salt. The adsorption shows a pH dependence; this can be correlated with the charge on the nucleotide molecule which is determined by the state of protonation of the N-1 nitrogen of 5-AMP or N-3 nitrogen of 5-CMP and the phosphate oxygens. The adsorption which results from the binding between the nucleotide molecule and the salt surface is proposed as being due to electrostatic forces. It was concluded that the adsorption was reversible in nature. The adsorption shows a strong dependence upon ionic strength and decreases with increasing ionic strength. Surface area is shown to be an important factor in evaluating and comparing the magnitude of adsorption of nucleotides onto various mineral salts. The implications of the results of the study are discussed in terms of the importance of soluble mineral salts as adsorption sites in the characterization of the adsorption reactions of an adsorbed template in biogeochemical cycles.     

Canopy throughfall of Picea abies (L.) Karst. as depending on trace gas concentrations

At six sites in central Germany consequences of SO₂, NO_X and O₃ deposition and of acid precipitation on canopy throughfall of sulphate, nitrate, ammonium, organic acids and of metal cations from Norway spruce crowns were investigated in the field. Measured canopy throughfall rates (mmol ion kg^-1 needle dw a^-1 are separated in (i) background ion throughfall rates in clean air and (ii) trace gas-(or acid interception)-dependent throughfall rates at ambient trace gas concentrations. Based on synchronously measured pollution, precipitation and canopy throughfall data, statistical response functions are given, which allow the separate estimation of annual rates of sulphur and nitrogen deposition into spruce canopies if only annual means of SO₂ or NO₂ concentrations in air are known. The specific SO₂ deposition rate of (0.841±0.214) mmol S kg^-1 needle dw a^-1 (nPa SO₂ Pa^-1)^-1 is 2.3 times higher than the specific stomatal SO₂ uptake. The NO₂-dependent nitrogen deposition of (2.464±0.707) mmol N kg^-1 needle dw a^-1 (nPa NO₂ Pa^-1)^-1 is 2.2 times higher than the specific stomatal NO_X (NO₂+NO) uptake. These ratios (2.32.2) are explained by the percentage of annual hours with open needle stomata. The shape of observed epicuticular SO₂ and NO_X deposition curves and of stomatal SO₂ and NO_X uptake curves are congruent. As for stomatal NO_X uptake, there is an apparent compensation point at (5 to 8) nPa NO₂ Pa^-1. There is significant SO₂-dependent canopy throughfall of Ca>K>Al>Mg>Fe in this order of relative importance. NO_X deposition in spruce canopies reduces K⁺ throughfall and it weakly promotes throughfall of Mn²⁺ and Zn²⁺. There was no significant codeposition of sulphate and ammonium and no ion exchange of intercepted H₃O⁺ with nutrient cations at the measured ambient pH values of the precipitation water. In the presence of O₃, throughfall of Mn²⁺ is reduced and throughfall of K⁺, Ca²⁺ and Al³⁺ is enhanced. In the cooperative presence of SO₂, NO₂ and O₃ pollution in the field there is a 1.3-fold increase of the annual K⁺ demand and a 1.5-fold Mg²⁺ demand of spruce canopies relative to the situation in clean air. This trace gas-dependent additional cation demand of spruce canopies corresponds to a needle loss percentage of (23 to 33)% if the additional K⁺ and Mg²⁺ throughfall could not be recycled in spruce ecosystems. Observed canopy thinning ranges from (13 to 26)% at the investigated six spruce stands.Abbreviations A_spec Specific needle surface area per kg needle dry matter (m²kg^-1 needle dw) - A_tot Total needle surface of spruce stands (ha ha^-1) - [gas]_a Ambient trace gas concentration (gas=SO₂; NO₂ or O₃) in air (nPa Pa^-1=ppb) - GP Number of days per annual growth period d a^-1) - IC_H30 ⁺ Acid interception rate (Eq H₃O⁺ kg^-1 needle dw a^-1) - k_o Trace gas-independent ion throughfall rate constant (mmol kg^-1 needle dw a^-1) - k_gas SO₂-,NO₂-or O₃-dependent ion throughfall rate per unit of trace gas pollution (mmol kg^-1 needle dw a^-1 (nPa Pa^-1)^-1) - k_H30 Specific H₃O⁺/Me⁺ exchange ratio (mol mol^-1) - L_o Background throughfall rate at [gas]_a=0 (mmol kg^-1 needle dw a^-1) - L_ion Canopy throughfall rate of ions (mmol kg^-1 needle dw a^-1) - L'_ion Trace gas dependent ion throughfall (mEq kg^-1 needle dw a^-1 (nPa Pa^-1)^-1) - LAI Leaf area index of the canopy (m² projected needle surface m^-2 ground) - Me⁺ Equivalents of metal cations (Eq) - N Stock of needles of spuce stands in the field (kg needle dw ha^-1) - P_% Percentage of needle loss relative to a healthy reference (%) - r Pearson correlation coefficient (no dimension) - R COO^--Sum of all organic anion equivalents Cat⁺ - An^- (Eq kg^-1 needle dw a^-1) - An^- Sum of all measured inorganic anion equivalents (Eq kg^-1 needle dw a^-1) - Cat⁺ Sum of all measured inorganic cation equivalents (Eq kg^-1 needle dw a^-1)     

Two steady states in membrane potential deflection in relation to chemoreception and chemotaxis byPhysarum polycephalum

Summary In the plasmodium ofPhysarum polycephalum application of various monovalent cation salts elicited either a depolarization or a hyperpolarization of the membrane potential. The hyperpolarization was restricted to phosphates and bicarbonates of large cations (Na⁺, Li⁺, NMe₄ ⁺, NEt₄ ⁺). More than 50 other combinations of cations (K⁺, Rb⁺, Cs⁺, NH₄ ⁺) and anions (Cl^–, NO₃ ^–, SO₄ ^2–, acetate, lactate, citrate, etc.) induced the depolarization. In both cases the magnitude of the deflection in membrane potential () varied linearly with logarithm of concentration above the threshold C_th (10^–4 M for all monovalent cation salts examined) according to the following equation: =± R log (C/C_th).The value of R was 10–15 mV, and plus and minus signs correspond to depolarization and hyperpolarization, respectively. Depolarizing and hyperpolarizing agents competed with each other and exhibited a sharp transition between the two states of the membrane which were characterized by — R and R in the above equation or displayed a strong hysteresis, depending on which agents had first been applied to the plasmodial membrane. This transition in the membrane potential corresponded to the transition between positive and negative taxis at the behavioral level.     

2D and 3D sulfate-water supramolecular networks templated via triazole-nickel(II) complexes

Tuning the substituents of triazoles, we obtained di- and tri-nuclearic triazole-nickel complexes [Ni₂(deatrz)₄(H₂O)₅](SO₄)₂ · 7H₂O (1) and [Ni₃(dmtrz)₆(H₂O)₆](SO₄)₃ · 21H₂O (2) (deatrz = 3,5-diethanyl-4-amino-1,2,4-triazole; dmtrz = 3,5-dimethanyl-1,2,4-triazole). The X-ray single-crystal diffraction results reveal that sulfate anions and water clusters form supramolecular networks in both complexes. In 1, a supramolecular two-dimensional structure was fabricated by nano-sized grid with novel tetramer water rings templated via binuclear-nickel(II) cations, while in 2, water molecules and sulfate anions construct the first sulfate-water three-dimensional supramolecular network as host to encapsulate trinuclear-nickel guests.     

Influence of SO2 and NO2 Exposure on Glutathione, Superoxide Dismutase and Glutathione Reductase Activities in Scots Pine Needles

A 50-year-old Pinus sylvestris L. stand was exposed for 2 yearsto low concentrations of SO₂ and NO₂ in an open-air exposureexperiment in northern Sweden. The mean SO₂ concentrations inthe centre of the exposed plot during the 1988 exposure from14 June to 25 September, and during the 1989 exposure from 6June to 30 September were 15 nl 1^–1 and 12 nl 1^–1,respectively. The corresponding values for NO₂ were 15 nl 1^–1and 10 nl 1^–1, respectively. The concentration in thecontrol plot was never higher than a few ppb, and mostly below1 nl 1^–1. Needles sampled from the SO₂ and NO₂-exposed area showed reducedactivities of glutathione reductase (GR; EC 1.6.4.2 [EC] ) and superoxidedismutase (SOD; EC 1.15.1.1 [EC] ) compared with controls. The GRactivity showed decreased levels in autumn and winter, whilethe exposure had ceased, and SOD showed decreased activity duringthe second summer of exposure. Neither membrane-bound nor water-solubleanti-oxidants such as -tocopherol, carotenoids or glutathionechanged due to the exposure. The sulphur/nitrogen ratio wasincreased in needles that were exposed to SO₂ and NO₂ implyinga changed nutrition balance. The results suggest that the capacityof SOD and GR in the ascorbate-glutathione pathway was reduceddue to the exposure to air pollutants. Key words: Anti-oxidants, -tocopherol, glutathione, pigments, Pinus sylvestris L