Chemical composition of soil solutions extracted from New Zealand beech forests and West German beech and spruce forests

Concentrations of ions were measured in soil solutions from beech (Nothofagus) forests in remote areas of New Zealand and in solutions from beech (Fagus sylvatica) and Norway spruce (Picea abies) forests in North-East Bavaria, West Germany, to compare the chemistry of soil solutions which are unaffected by acid deposition (New Zealand) with those that are affected (West Germany). In New Zealand, soil solution SO₄ ^2– concentrations ranged between <2 and 58 mol L^–1, and NO₃ ^– concentrations ranged between <1 and 3 mol L^–1. In West Germany, SO₄ ^2– concentrations ranged between 80 and 700 mol L^–1, and NO₃ ^– concentrations at three of six sites ranged between 39 and 3750 mol L^–1, but was not detected at the remaining three sites. At all sites in New Zealand, and at sites where the soil base status was moderately high in West Germany, pH levels increased, and total Al (Al_t) and inorganic monomeric Al (Al_i) levels decreased rapidly with increasing soil depth. In contrast, at sites on soils of low base status in West Germany, pH levels increased only slightly, and Al levels did not decline with increasing soil depth.Under a high-elevation Norway spruce stand showing severe Mg deficiency and dieback symptoms in West Germany, soil solution Mg²⁺ levels ranged between 20 and 60 mol L^–, and were only half those under a healthy stand. Al_t and Al_i levels were substantially higher the healthy stand than under the unhealthy stand, indicating that Al toxicity was not the main cause of spruce decline.     

Influence of acid rain and liming on fluxes of NO and NO2 from forest soil

Flux measurements of nitric oxide (NO) and nitrogen dioxide (NO₂) were performed in a coniferous forest (Höglwald) in southern Germany using a fully automated measuring system based on the dynamic chamber method. The forest soil was predominately a source of NO, but mean flux rates of NO ranged from –26.3 (deposition) to 55 g N m^-2 h_-1 (emission). NO₂ was deposited on the forest soil with mean flux rates ranging from –4 to –72 g N m^-2 h_-1 . Removal of forest floor vegetation did not influence NO or NO₂ fluxes. Apparently, forest floor vegetation was neither a source of NO nor a significant sink of NO₂. When the organic layer of the forest soil was removed, net NO flux changed from emission to deposition. Thus NO emitted to the atmosphere was produced almost exclusively in the organic layer of the forest soil. Liming caused a significant decrease in the rate of NO emission by 43 to 100%, whereas irrigation with simulated acid rain increased the emission of NO by a factor of 3.1. Irrigation with simulated normal rain decreased the emission of NO by 35 to 100%. No such effects could be detected for the deposition of NO₂.     

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.     

Reversibility of damages to forest floor plants by episodes of elevated hydrogen- and aluminium-ion concentrations in the soil solution

Herbs and grasses may episodically be exposed to elevated concentrations of potentially toxic elements as H⁺ and Al³⁺ due to considerable temporal variability in the chemical composition of soil solutions in the uppermost layer of the soil profile. Greenhouse experiments were performed to test the effect of episodes of different length (1 and 2 weeks) and concentrations of H⁺ and Al³⁺ (pH 3.8, 4.0, 4.2 and 4.5; 0, 20 and 70 M Al) on root and shoot growth, designed to elucidiate the reversibility of growth inhibition. Three forest floor species were studied-Galium odoratum and Lamium galeobdolon, having similar pH distribution ranges in the field and Poa nemoralis which also occurs at slightly lower pH. The plants were grown for 5 weeks (episode and recovering time) in a synthetic soil solution in a flowing solution system without recirculation. The species reacted in three different ways. Galium odoratum was the most sensitive species and seemed to be irreversibly damaged (ceased growth) by 2 week episodes of pH4.0 and Al20 M at pH4.2. Lamium galeobdolon was about equally sensitive during the episodes but it had a much greater ability to recover. Poa nemoralis was rather insensitive to the episode treatments tested. It is concluded that episodes of elevated H⁺ and Al³⁺ concentrations may be decisive for plant performance. It is therefore important to consider the extreme environmental conditions which plants may be exposed to in the field, in addition to long-term averages of e.g. soil solution concentration of potentially toxic elements, when studying species distribution and performance in relation to soil chemical properties.     

Water relations and growth of shrubs before and after fire in a semi-arid woodland

Summary Plant water relations and shoot growth rate of shrubs resprouting after fire or unburnt were measured in a semi-arid poplar box (Eucalyptus populnea) shrub woodland of eastern Australia. In vegetation unburnt for about 60 years, the dawn xylem water potential (_x) of the dominant shrub species was about-1.0 MPa when the soil was wet and-8.0 MPa when the soil was very dry. At any one time, the dominant shrub species,Eremophila mitchellii, E. sturtii, Geijera parviflora andCassia nemophila, were similar in _x butAcacia aneura andDodonaea viscosa were consistently higher in _x than this group when the soil was moist and lower when the soil was dry. The dominant tree species,Eucalyptus populnea andE. intertexta, appeared to have access to additional water beneath the hardpan which is located 60–80 cm below the surface. When shrubs were under extreme water stress (_x of-8 MPa), the trees had a _x of-3 to-3.6 MPa. Following a fire, both _x and leaf stomatal conductance (g _s) of resprouting shrubs were higher for about 5 years than comparable-aged unburnt vegetation, with relative differences in _x increasing with drought stress. Elongation rate of resprouts was positively linked to prefire shrub height in 3 of 4 species. However, shrubs resprouting after high intensity fires had substantially higher rates of shoot elongation than after low intensity fires which were in turn higher than for foliar expansion of unburnt shrubs. It is concluded that the growth rate of resprouting shrubs is primarily determined by physiological/ morphological factors associated with plant size but is also assisted by greater availability of water and possibly nutrients for a period after fire.     

Effect of substrate concentration,inorganic nitrogen,O2 concentration,temperature and pH on dehydrogenase activity in soil

Summary Dehydrogenase activity was measured in a sandy loam soil under a variety of incubation conditions using the reduction of 2-(p-iodophenyl-3-(p-nitrophenyl)-5-phenyl tetrazolium chloride (INT) to iodonitrotetrazolium formazan (INT-formazan). There was a high positive correlation between dehydrogenase activity and substrate concentration, incubation temperature, and soil pH. Dehydrogenase activity also displayed a high negative correlation with O₂ concentrations. Ammonium sulfate at concentrations from 40 to 120 g/g soil had no significant effect on dehydrogenase activity. However, at concentrations of 160 and 200 g/g, dehydrogenase activity was significantly reduced. Potassium nitrate at concentrations ranging from 40 to 200 g/g had no significant effect on soil dehydrogenase activity, whereas sodium nitrite significantly inhibited activity at concentrations of 120 and 160 g/g soil.     

Cotton root and shoot response to localized supply of nitrate,phosphate and potassium: Split-pot studies with nutrient solution and vermiculitic soil

Vertical stratification of plant-available K in vermiculitic soil profiles contributes to a late-season K deficiency that limits cotton (Gossypium hirsutum L.) yields on affected soils. Split-root solution culture and split-pot soil experiments were conducted to determine whether root distribution and cultivar differences in root extension in these stratified profiles result from a compensatory response to localized enrichment with NO₃-N, PO₄-P, and/or K in the root zone. Compensatory root growth was greatest in response to localized NO₃-N enrichment. For two cultivars examined in solution culture, 74% of new root development occurred in the half-pot providing 90% of the total NO₃-N supply. Only 60% of cultivar root development occurred in the half-pot providing 90% of the PO₄-P. No compensatory root growth was observed in response to localized K enrichment. In the split-pot system, the proportion of total root surface area developing in a half-pot was highly correlated with localized soil NO₃-N levels (r²=0.81), while increased K availability in one half of the root zone did not affect root distribution. Mean soil NO₃-N supply to the whole root system determined shoot N accumulation (r²=0.97). Shoot K accumulation was not related to soil K availability but was strongly correlated with mean root surface area density (r²=0.86). Cultivar Acala GC510, known to be less sensitive to K deficiency than Acala SJ-2, had significantly larger root diameter in all nutrient-supply environments. Under conditions of K stress, Acala GC510 had increased root branching and allocated greater dry matter to roots relative to shoots than Acala SJ-2. The results demonstrate that K acquisition by cotton is strongly influenced by the quantity and distribution of NO₃-N in the root zone through its effects on root proliferation, and that distinct cultivar differences associated with crop performance on low K soils can be detected in short-term, solution culture growth systems.     

Physiological effects of a long term exposure to low concentrations of NH3, NO2 and SO2 on Douglas fir (Pseudotsuga menziesii)

The above-ground parts of two years old seedlings of Douglas fir (Pseudotsuga menziesii) were exposed to filtered air, NH₃, NO₂₊, SO₂ (66, 96 and 95 μg m^?3, respectively), to a mixture of NO₂+NH₃ (55 + 82 μg m^?3) or SO₂+NO₂ (128 + 129 μg m^?3), for 8 months in fumigation chambers. Both chlorophyll fluorescence and gas exchange measurements were carried out on shoots which had sprouted at the beginning of the exposure period. The chlorophyll fluorescence measurements were performed after 3 and 5 months of exposure (average shoot age 70 and 140 days, respectively). Light response curves of electron transport rate (J) were determined, in which J was deduced from chlorophyll fluorescence. In addition, light response curves of net CO₂ assimilation were determined after 5 months of exposure. After 3 months of exposure (average shoot age 70 days) all exposure treatments showed a lower maximum electron transport rate (J_max) as compared to the control shoots (filtered air). A large reduction (45%) was observed for shoots exposed to SO₂+NO₂. During the exposure period between 3 and 5 months (average shoot age 70 and 140 days, respectively) a decrease of J_max was observed for all treatments. J_max had further declined some time after termination of the exposure, when average shoot age was 310 days. Shoots exposed to SO₂ and SO₂+NO₂ also showed a reduction in maximum net CO₂ assimilation (P_max) as compared to the control shoots. However, shoots exposed to NO₂ showed no reduction and even a higher P_max was observed for shoots exposed to NH₃ or NO₂+NH₃. Needles of these treatments also showed a higher chlorophyll content which might explain the contradictory results obtained for these treatments: the increased amount of photosynthetic units counteracts the reduction in J_max and consequently no reduction in P_max is measured. Shoots exposed to SO₂ and SO₂+NO₂ also showed a reduction in maximum stomatal conductance (g_s). However, the stomatal opening was larger than could be expected on basis of their (maximum) CO₂ assimilation rate. Consequently, water use efficiency of these shoots was lower than that of the control shoots. Also shoots exposed to NO₂ had a lower water use efficiency due to a significantly higher maximum g_s. Shoots exposed to NH₃ showed a high transpiration rate in the dark, indicating imperfect stomatal closure.     

Sulfur accumulation in western wheatgrass exposed to three controlled SO2 concentrations

Summary Sulfur concentrations of western wheatgrass tillers and individual leaves were measured from plants exposed to four SO₂ concentrations (9, 52, 105 and 183 g·m^–3). Sulfur concentration of plants was a linear function of either time of exposure or concentration.Young leaves and the youngest portion of leaves contained less sulfur than their older counterparts irregardless of whether they had or had not been exposed to SO₂.Current hypotheses which relate plant sensitivity to amount of sulfur taken up do not apply for western wheatgrass.     

A method for collecting soil percolate and soil solution in the field

Summary A soil-water extractor is described which uses an absorbent sponge material for sampling soil percolate and solution. Good agreement existed between soil extracts (1:5 soil:water) and extracts obtained from the extractor sponge after equilibration at low water tensions (pF 0–2.5) in the range, 0–100 g/g soil (0–1400 g/ml solution) for solute anions (Cl^-, NO₂ ^- and NO₃ ^–, R² > 0.98), and for ammonium ions (NH₄ ⁺, R²=0.93).Percolate was recovered in a field soil in volumes sufficient to permit analysis of constituents. Concentrations of solute Cl^- ions in these percolates were similar to those in the added water and in percolate from a zero-tension lysimeter. Poor relationships were obtained in the field between soil solution extracts from the sponge and 1:10 soil water extracts. For the present, the soil extractor may be used for sampling and monitoring movement of percolate and solute fronts, in the wetter range of soil water content.     

Nitrification in soils of secondary vegetational successions from Eucalyptus forest and grassland to cool temperate rainforest in Tasmania

Rates of nitrification in well drained granitic soils from forest stands and grassland of differing successional status and from beneath isolated individuals of several tree species were compared in a series of laboratory experiments. Fresh samples were perfused with distilled water or nutrient solution for 10 to 14 weeks at 20°C. The following treatments were applied to the soils singly and in combination: 200 and 400 g N g^–1 as (NH₄)₂SO₄; 100 g P g^–1 as KH₂PO₄; 4000 g CaCO₃ g^–1; inoculation of non-nitrifying soil with nitrifying soil; perfusion of nitrifying soil with leachate from non-nitrifying soil.Nitrification was absent or occurred at only a low rate in many soils; it generally increased as succession proceeded from nature grassland or eucalypt forest towards climax temperate rainforest, but decreased in mature climax forests. However, the influence of individual tree species was often paramount. Nitrification was stimulated by disturbance of a stand by disease. A possible inhibitor of nitrification in a rainforest soil could not be removed by leaching with water, nor transferred via the leachate to a nitrifying soil. Addition of P was without effect on either total amount of nitrate produced or on net mineralisation of soil N, but sometimes increased the rate of nitrification of added ammonium. Non-nitrifying rainforest soil of pH 4.3 was induced to nitrify only after addition of (NH₄)₂SO₄, inoculation with a nitrifying soil, and addition of CaCO₃ to raise pH by 3 units. However, once nitrification had commenced it could continue with little change in rate while pH decreased to a value of 3.4.It was concluded that rate of nitrification is dependent upon the presence of particular tree species in a stand, upon its history of disturbance, and hence in part upon the stand's successional status. It is not limited by pHper se within the range found in these soils, although an increase in pH may be necessary to initiate nitrification. In some soils the rate of nitrification may be limited by the level of ammonium substrate, and nitrifiers are virtually absent from others. Overall microbial activity is limited by lack of utilisable carbon substrate.     

Sulfur dynamics in mineral horizons of two northern hardwood soils. A column study with 35S

Sulfur dynamics of two Spodosols were ascertained using soil columns constructed from homogenized mineral soil from nothern hardwood ecosystems at the Huntington Forest (HF) in the Adirondack Mountains of New York and Bear Brook Watershed in Maine (BBWM). Columns were leached for 20 weeks with a simulated throughfall solution with³⁵SO₄ ^2-. Sulfur constituents were similar to those of other Spodosols, with the organic S fractions (C-bonded S and ester sulfate) constituting over 90% of total S. HF soil columns had higher total S (14.9 mol S g^-1) than that for the BBWM soil columns (7.4 mol g^-1) primarily due to higher C-bonded S in the former.Initially, adsorbed SO₄ ^- accounted for 5 and 4% of total S for the BBWM and HF soil columns, respectively. After 20 weeks, adsorbed SO₄ ^2- decreased (81%) in BBWM and increased (33%) in HF soil columns. For both HF and BBWM soil columns, C-bonded S increased and ester sulfate decreased, but only for HF columns was there a net mineralization of organic S (5.6% of total S). The greatest decrease in ester sulfate occurred at the top of the columns.Leaching of³⁵S was less than 0.5% of the³⁵S added due to its retention in various S constituents. There was an exponential decrease in³⁵S with column depth and most of the radioisotope was found in C-bonded S (70–88 and 70–91% for BBWM and HF, respectively). The rapid turnover of adsorbed SO^2- ₄ was reflected in its high specific activity (834 and 26 kBq mol^-1 S for BBWM and HF, respectively). The lower specific activity of adsorbed SO₄ ^2- in HF was attributable to greater isotopic dilution by non-radioactive SO^2- ₄ derived from greater organic S mineralization in the HF versus the BBWM columns.Both soil columns initially had high levels of NO^- ₃ which resulted in the generation of H⁺ and net retention of SO₄ ^2- in the early phase of the experiment due to pH dependent sulfate adsorption; later NO₃ ^- decreased and SO₄ ^2- was desorbed. Leaching of NIO₃ ^- and SO₄ ^2- was correlated with losses of Mg²⁺ and Ca²⁺ of which the latter was the dominant cation.Analyses using both S mass balances and radioisotopes corroborate that for BBWM soil columns, SO^2- ₄ adsorption-desorption dominated the S biogeochemistry while in HF soil columns, organic S mineralization-immobilization processes were more important. It is suggested that similar techniques can be applied to soils in the field to ascertain the relative importances of SO₄ ^2- adsorption processes and organic S dynamics.     

Replacement of nutrient losses caused by acidification of a beech forest soil and its effects on transplanted field-layer species

Acidification of south Swedish forest soils has caused considerable decreases in pH and exchangeable cations during recent decades. The lowered abundance of several field-layer species is probably related to the altered soil chemistry. The present study focuses on the importance for the vegetation of reduced amounts of Ca, Mg and K. These elements were applied separately or mixed as C1+SO₄, six times the current exchangeable amount of the topsoil of an acid beech forest soil (pH H₂O 4.1). Soil pH was raised to 7 by Na₂CO₃ application and Na was also given as C1+SO₄. Survival and growth of the seven transplanted species were measured during three years (Dentaria bulbifera, Gagea spathacea, Galium odoratum, Lamium galeobdolon, Melica uniflora, Mercurialis perennis and Viola reichenbachiana.Half a year after the treatment the exchangeable amounts of K, Ca and Mg had increased by ca. 2.5 times when applied separately. Howerver, the retention of Mg was strongly disfavoured by the application of all other elements. Exchangeable K and Na thereafter decreased while the effects on Ca and Mg were persistent during the study. D. bulbifera, G. odoratum and M. perennis hardly survived any treatment, possibly due to the low soil pH, while 40–70% of the other species survived. Growth to normal size was only attained by G. spathacea, M. uniflora and V. reichenbachiana. The application of Ca+Mg+K was positive for G. spathacea, L. galeobdolon and M. perennis and Na (as C1+SO₄) for D. bulbifera, L. galeobdolon, M. uniflora and M. perennis. The effects of the Na treatment may partly be caused by the increased pH (5.3). Application of Mg favoured M. uniflora and Na₂CO₃ V. reichenbachiana. Addition of K gave no positive effects.It can be concluded that addition of Ca, Mg and K without raising pH was insufficient for a normal growth for all studied species but M. uniflora and V. reichenbachiana. These two species also had a relatively high survival in the control plots but performance was enhanced by Mg or Na₂CO₃ application.     

The role of stomata in sensitivity of Betula papyrifera seedlings to SO2 at different humidities

Summary Stomata of paper birch (Betula papyrifera Marsh.) seedlings were more open at high humidity than at low humidity and responded rapidly to changes in vapor pressure deficit. SO₂ at 0.2 or 0.8 l l^-1 caused partial stomatal closure. Seedlings fumigated with SO₂ at 0.2 or 0.5 l l^-1 for 30 h or 0.2 l l^-1 for 75 h took up more SO₂ at high than at low humidity. Differences in pollutant uptake could be explained by stomatal conductance with no need to invoke changes in mesophyll conductance. Betula seedlings were more sensitive to SO₂ when fumigated at high humidity, as manifested in more leaf necrosis, increased leaf abscission, and greater growth inhibition compared to seedlings fumigated at low humidity. Amount of injury to leaves increased with rate of SO₂ uptake, and inhibition of root growth increased with total SO₂ uptake.Abbreviations RH relative humidity - VPD vapor pressure deficit - RGR mean relative growth rate - PPFD photosynthetic photon flux density (400–700 nm) - LDC leaf diffusive conductance - water potential Research supported by the College of Agricultural and Life Sciences, University of Wisconsin-Madison     

Response of liquid flow resistance to soil drying in seedlings of four deciduous angiosperms

Summary Soil-leaf resistance to liquid water flow (R) in moist and drying soil was compared in three-month-old seedlings of two drought tolerant (white [Quercus alba L.], post oak [Q. stellata Wangenh.]) and two drought sensitive forest species (sugar maple [Acer saccharum Marsh.], black walnut [Juglans nigra L.]). At high soil moisture (_s–0.3 MPa), R was higher in J. nigra than in the other species, and as soil water was depleted R increased most in this species. In contrast, the lowest resistance at all levels of soil moisture was observed in Q. stellata. At _s of –1.5 MPa, R of drought-sensitive J. nigra and A. saccharum was about twice as high as that of the two drought-tolerant Quercus species. The difference in R between the two Quercus species was much smaller than that between this pair and the other two species. These differences among species in flow resistance may be attributable to: 1) variation in the balance between root surface area and leaf area, 2) variation in the inherent absorption capacity of the root systems and in xylem water conducting systems or 3) differences in root permeability, shrinkage and mortality in severely stressed seedlings. As the soil dried, seedlings of all species exhibited pronounced reductions in transpiration rate, which prevented development of large water potential gradients between leaves and the soil. Reduction in transpiration in J. nigra was especially pronounced, resulting in a decrease in the soil-to-leaf water potential gradient in dry soil despite high flow resistance. The observed differences among species in flow resistance are correlated with natural distribution patterns.     

Transport properties of charged membranes undergoing conformational transitions

Summary The permeability and reflection behavior of cross-linked collagen films in dilute salt solutions have been investigated by measurements of net volume flow, isotopic exchange of THO and of Ca⁴⁵, and osmotic pressure. Complementary measurements of swelling, membrane resistance, membrane potential, and streaming potential are presented. Measurements were performed in the pH range of 5 to 1.5, at temperatures between 25 and 52 °C, and in the presence of KCl, 10^–2 m or CaCl₂, 10^–3 m. Under the conditions adopted, the membrane carries a net positive charge and undergoes large changes in degree of swelling (Donnan effect) and structure (crystal amorphous transition). The results indicate that when pH is lowered the filtration coefficientL _p decreases in the crystalline state (pH 5 to 3), increases during the conformational transition (pH 3 to 2), and decreases in the amorphous state (pH<2). It appears thatL _p is affected more by such properties as structure and porosity (i.e., mechanical resistance to flow) than properties related to the charged character of the membrane. The reflection coefficient increases when pH is lowered until pH 3, and decreases upon further lowering of pH. Such behavior is described in terms of the competition between swelling (due to both the Donnan effect and the melting transition) and fixed-charge density. Values of fixed-charge density derived on the basis of a theoretical expression for were found to be in good agreement with independent titration data.     

Early diagnosis of SO2-stress by volatile emissions in some crop plants

Summary Fumigation experiments with SO₂ performed on the seedlings of three plant species viz, tomato (Lycopersicon esculentum), mung bean (Vigna radiata) and maize (Zea mays) resulted in the emission of volatiles. Acetaldehyde and ethanol were produced in the fumigated plants. In addition, there was also an increased production of ethylene and ethane. The production of these volatiles was positively correlated to the SO₂ concentrations of 4.2 and 8.3 mol m^–3 (0.1 and 0.2 ppm). Ethylene was emitted primarily from SO₂-stressed yet healthy leaves, whereas high ethane levels were detected in leaves with visible injury symptoms. However, with the appearance of visible injury symptoms, there was a decline in ethylene, acetaldehyde and ethanol emissions. Synthesis of ethylene and ethane seems to be a result of different metabolic pathways. Ethane evolution and its inhibition by antioxidants indicate SO₂-mediated lipid peroxidation by free radical species formed during sulphite oxidation. Perturbation in the cellular respiratory machinery results in the formation of acetaldehyde and ethanol. Since the rates of emissions of ethane, acetaldehyde and ethanol fromplant species were positively correlated to their relative resistance to SO₂, the production of these gases could be used as a reliable diagnostic tool for biomonitoring air pollution (SO₂) stress.Abbreviations ADH alcohol dehydrogenase - NaHSO₃ sodium metabisulphite - O ₂ ^– superoxide radical - OH hydroxyl radical - pO₂ oxygen partial pressure - SO₂ sulphur dioxide - SO ₃ ^– sulphite radical - SOD superoxide dismutase     

Gas exchange and SO2 fumigation studies with irrigated and unirrigated field grown Diplacus aurantiacus and Heteromeles arbutifolia

Summary Experiments were performed on an evergreen (Heteromeles arbutifolia) and a drought deciduous shrub (Diplacus aurantiacus) to determine, 1) whether approaches for evaluating SO₂ absorption by leaves in laboratory studies could be extended to field studies, 2) the effects of irrigation on metabolism and SO₂ responses of the study species during a season when water was limiting, 3) to interpret SO₂ responses on the basis of SO₂ flux rates. Laboratory-developed approaches for evaluating SO₂ absorption by leaves were found to be suitable for use with field plants, despite field plants having lower gas exchange rates. Supplementing water during times of deficit did not override all the biological and environmental factors that limited photosynthesis (A). Irrigation increased leaf longevity of D. aurantiacus, and stomatal conductance to water vapour (g); g was also shown to increase with H. arbutifolia on irrigation. Irrigation profoundly influenced plant response to SO₂. Unwatered D. aurantiacus had only a small g and therefore a reduced capacity to absorb SO₂ and respond to SO₂; which resulted in apparent SO₂ avoidance. Water availability and SO₂ both affect g and therefore, SO₂ flux rates into the mesophyll. Different ambient SO₂ concentrations of 8.3 and 26.2 mol m^-3 (0.2 and 0.6 ppm) were both found to result in similar SO₂ flux rates into the leaf, due to variations in g in response to water availability. Changes in g did not always result in changes in A, implying that carbon fixation may be little affected by some SO₂ exposures, although still potentially affecting such processes as maintenance of leaf water potential, transpirational cooling and nutrient uptake.Abbreviations SO₂ sulphur dioxide - A net photosynthesis - E transpiration - g stomatal conductance to water vapour - W Water vapour mole fraction difference between the leaf and air - WUE water use efficiency (mol CO₂ uptake per mol H₂O transpired)     

Responses of nitrogen-fixing and nitrate-supplied alfalfa (Medicago sativa L.) to iron chelates in an alkaline hydroponic medium

Ferric ethylenediamine di-(o-hydroxyphenylacetate) (FeEDDHA) and ferric hydroxyethylethylenediaminetriacetic acid (FeHEDTA) were evaluated as Fe sources for hydroponic growth of alfalfa (Medicago sativa L., cv. Mesilla), either dependent on N₂ fixation or supplied with NO₃. The hydroponic medium was maintained at pH 7.5 by addition of CaCO₃. Nitrogen-fixing cultures were inoculated with Rhizobium meliloti 102 F51 and grown in medium without added nitrogen. After five to seven weeks of growth under greenhouse conditions, plants were harvested. Nitrogen fixation was measured by the acetylene reduction method.When FeEDDHA was supplied, growth of alfalfa, whether dependent on N₂ fixation or supplied with NO₃, was severely limited at concentrations typically used in hydroponic medium (10 or 20 M). Maximum yield of NO₃-supplied alfalfa was obtained at 100 M while maximum yield of N₂-fixing alfalfa was obtained in the range of 33 to 200 M FeEDDHA. Nodule fresh weights and N₂ fixation rates increased with FeEDDHA concentration up to 33 M and remained essentially constant up to 200 M. With FeHEDTA, maximum yields of both NO₃-grown and N₂-fixing alfalfa were obtained at 10 M. Growth of NO₃-supplied plants was inhibited at 200 M FeHEDTA while growth of N₂-fixing plants was inhibited at 100 M FeHEDTA. The numbers of nodules per plant increased between 3.3 and 10 M FeHEDTA; however, inhibition of nodule formation occurred at a concentration of 33 M or higher. Nodule weights per plant and N₂ fixation rates were depressed at 3.3 M as well as at 100 M FeHEDTA. The results suggest that alfalfa dependent on N₂ fixation is more sensitive to limited Fe availability than alfalfa supplied with NO₃.     

Measurement of internal pH in the coccolithophoreEmiliania huxleyi using 2′,7′-bis-(2-carboxyethyl)-5(and-6)carboxyfluorescein acetoxymethylester and digital imaging microscopy

Internal pH (pH_i) was determined inEmiliania huxleyi (Lohmann) using the probe 2,7-bis-(2-carboxyethyl)-5(and-6)carboxyfluoresceinacetoxymethylester (BCEF-AM) and digital imaging microscopy. The probe BCECF-AM was taken up and hydrolysed to the free acid by the cells. A linear relationship was established between pH_i and the 490/450 fluorescence ratio of BCECF-AM over the pH range 6.0 to 8.0 using the ionophore nigericin. Two distinct pH domains were identified within the cell, the cytoplasmic domain (approx. pH 7.0) and the chloroplast domain (approx. pH 8.0). The average pH_i was 7.29 (±0.11) for cells in the presence of 2 mM HCO ₃ ^– . In the absence of HCO ₃ ^– the pH_i was decreased by 0.8 pH unit. The importance of these changes in pH_i is considered in relation to inorganic-carbon uptake.Abbreviations AM acetoxymethylester - BCECF 2,7-bis-(2-carboxyethyl)-5(and-6)carboxyfluorescein - Hepes 4-(2-hydroxyethyl)-1-piperazine ethanesulfonic acid - pH_i intracellular pH