Nitrogen metabolism of young barley plants as affected by NaCl-salinity and potassium

Summary In a solution culture experiment with 31 days old barley plants (var. Miura) the influence of NaCl-salinization (80 mM) and KCl addition (5 and 10 mM) on the uptake and turnover of labelled nitrogen (¹⁵NH₄ ¹⁵NO₃) was studied. Labelled N was applied for 24 h at the end of a 20 days' salinization period. Salinization impaired growth and incorporation of labelled N into the protein fraction paralleled by accumulation of labelle dinorganic N. All salt effects were much more pronounced in the shoots than in the roots.Potassium addition enhanced N uptake (total¹⁵N-content) and incorporation into protien, reduced the accumulation of inorganic N and improved the growth of salinized plants.The presented data support the point of view that impairment of protein (enzyme) metabolism is an important aspect of salt stress which is probably induced by the disturbance of the K/Na balance of the tissues under saline conditions.This work was supported by a grant from the Alexander von Humboldt foundation.     

Nitrogen and phosphorus cycling in relation to stand age of Eucalyptus regnans F. Muell

Lupins, canola, ryegrass and wheat fertilized with Na₂ ³⁵SO₄ and either ¹⁵NH₄Cl or K¹⁵NO₃(N:S=10:1), were grown in the field in unconfined microplots, and the sources of N and S (fertilizer, soil, atmosphere, seed) in plant tops during crop development were estimated. Modelled estimates of the proportion of lupin N derived from the atmosphere, which were obtained independently of reference plants, were used to calculate the proportion of lupin N derived from the soil. Total uptake of N and S and uptake of labelled N and S increased during crop development. Total uptake of S by canola was higher than lupins, but labelled S uptake by lupins exceeded uptake by canola. The form of N applied had no effect on uptake of labelled and unlabelled forms of N or S. Ratios of labelled to unlabelled S and ratios of labelled to unlabelled N derived from soil sources decreased during growth, and were less for S than for N for each crop at each sampling time. Although ratios of labelled to unlabelled soil-derived N were similar between crops at 155, 176 and 190 days after sowing, ratios of labelled to unlabelled S for lupins were higher than for the reference crops and declined during this period. The ratios of labelled to unlabelled S in lupins and the reference plants therefore bore no relationship either to ratios of labelled to unlabelled soil-derived N in the plants, or to total S uptake by the plants. Therefore the hypothesis that equal ratios of labelled N to unlabelled soil-derived N in legumes (Rleg) and reference plants (Rref) would be indicated by equal ratios of labelled to unlabelled S was not supported by the data. The results therefore show that the accuracy of reference plant-derived values of Rleg cannot be evaluated by labelling with ³⁵S.     

Mineralization of organically bound nitrogen in soil as influenced by plant growth and fertilization

Summary A loam soil containing an organic fraction labelled with¹⁵N was used for pot experiments with spring barley, rye-grass and clover. The organically bound labelled N was mineralized at a rate corresponding to a half-life of about 9 years. Fertilization with 106 and 424 kgN/ha of unlabelled N in the form of KNO₃ significantly increased uptake of labelled N from the soil in barley and the first harvest of rye-grass crops. The fertilized plants removed all the labelled NH₄ and NO₃ present in the soil, whereas the unfertilized plants removed only about 80%. The second, third and fourth harvests of the unfertilized rye-grass took up more labelled N than the fertilized rye-grass. The total uptake in the four harvests was similar whether the plants were fertilized or not. Application of KCl to barley plants in amounts equivalent to that of KNO₃ resulted in a small but insignificant increase in uptake of labelled N. The uptake of labelled N in the first harvest of clover which was not fertilized but inoculated with Rhizobium was similar to that of the fully fertilized rye-grass indicating that the biological fixation of N had the same effect as addition of N-fertilizer. N uptake in the following harvests was lower and the total uptake by four harvests of clover was similar to that of rye-grass. There was no indication that fertilization with KNO₃ accelerated the mineralization of the organically bound labelled N. The observed apparent ‘priming effect’ of the fertilizer on the uptake of labelled N was compensated by subsequent crops and harvests, and it seems to arise from a more thorough search of the soil volume by a better developed root system of the fertilized plants.     

Comparative Toxicities of Salts on Microbial Processes in Soil

Soil salinization is a growing threat to global agriculture and carbon sequestration, but to date it remains unclear how microbial processes will respond. We studied the acute response to salt exposure of a range of anabolic and catabolic microbial processes, including bacterial (leucine incorporation) and fungal (acetate incorporation into ergosterol) growth rates, respiration, and gross N mineralization and nitrification rates. To distinguish effects of specific ions from those of overall ionic strength, we compared the addition of four salts frequently associated with soil salinization (NaCl, KCl, Na₂SO₄, and K₂SO₄) to a nonsaline soil. To compare the tolerance of different microbial processes to salt and to interrelate the toxicity of different salts, concentration-response relationships were established. Growth-based measurements revealed that fungi were more resistant to salt exposure than bacteria. Effects by salt on C and N mineralization were indistinguishable, and in contrast to previous studies, nitrification was not found to be more sensitive to salt exposure than other microbial processes. The ion-specific toxicity of certain salts could be observed only for respiration, which was less inhibited by salts containing SO₄²⁻ than Cl⁻ salts, in contrast to the microbial growth assessments. This suggested that the inhibition of microbial growth was explained solely by total ionic strength, while ion-specific toxicity also should be considered for effects on microbial decomposition. This difference resulted in an apparent reduction of microbial growth efficiency in response to exposure to SO₄²⁻ salts but not to Cl⁻ salts; no evidence was found to distinguish K⁺ and Na⁺ salts.     

KINETICS OF NITROGEN-15 LABELLED AMMONIUM UPTAKE BY CAULERPA CUPRESSOIDES (CHLOROPHYTA)1,2,3

The incorporation of ¹⁵NH₄⁺ as a function of time and concentration was used to estimate ammonium uptake by Caulerpa cupressoides (West) C. Agardh, taken from its habitat on the sediments of Tague Bay lagoon, St. Croix, U.S. Virgin Islands. ¹⁵N-based uptake rates followed Michaelis-Menten type saturation kinetics; the maximum uptake rate was 8.7 ± 3.0 μmol N/g dry wt·h at 26° C and the half-saturation constant was 48 ± 10 μM (X?± SE). The high half-saturatiaon constant reflects the dependence of Caulerpa on sediment pore waters as a nitrogen source. Calculations of uptake from isotope time course data were compared to estimates made from ammonium depletion. More ammonium disappeared than could be accounted for by the incorporation of ¹⁵N in Caulerpa, and isotope dilution of the ammonium pool is shown not to be responsible for underestimates of uptake, primarily because large ¹⁵N additions (40–300 μM) were used. It is suggested that either (1) a secondary ammonium sink such as wall sorption or bacterial uptake significantly influenced ammonium concentrations, or (2) ¹⁵N was lost as labelled dissolved organic nitrogen or volatilized during ¹⁵N sample preparation.     

Characterizing nitrogen dynamics, retention and transport in a tropical rainforest stream using an in situ15N addition

1. This study was part of the Lotic Intersite Nitrogen eXperiment (LINX); a series of identical ¹⁵NH₄ tracer additions to streams throughout North America. ¹⁵NH₄Cl was added at tracer levels to a Puerto Rican stream for 42 days. Throughout the addition, and for several weeks afterwards, samples were collected to determine the uptake, retention and transformation pathways of nitrogen in the stream. 2. Ammonium uptake was very rapid. Nitrification was immediate, and was a very significant transformation pathway, accounting for over 50% of total NH₄ uptake. The large fraction of NH₄ uptake accounted for by nitrification (a process that provides energy to the microbes involved) suggests that energy limitation of net primary production, rather than N limitation, drives N dynamics in this stream. 3. There was a slightly increased ¹⁵N label in dissolved organic nitrogen (DON) the day after the ¹⁵NH₄ addition was stopped. This DO¹⁵N was < 0.02% of DON concentration in the stream water at the time, suggesting that nearly all of the DON found in‐stream is allochthonous, or that in‐stream DON production is very slow. 4. Leptophlebiidae and Atya appear to be selectively feeding or selectively assimilating a very highly labelled fraction of the epilithon, as the label found in the consumers became much higher than the label found in the food source. 5. A large spate (>20‐fold increase in discharge) surprisingly removed only 37% of in‐stream fine benthic organic matter (FBOM), leaves and epilithon. The fraction that was washed out travelled downstream a long distance (>220 m) or was washed onto the stream banks. 6. While uptake of ¹⁵NH₄ was very rapid, retention was low. Quebrada Bisley retained only 17.9% of the added ¹⁵N after 42 days of ¹⁵N addition. Most of this was in FBOM and epilithon. Turnover rates for these pools were about 3 weeks. The short turnover times of the primary retention pools suggest that long‐term retention (>1 month) is minimal, and is probably the result of N incorporation into shrimp biomass, which accounted for < 1% of the added ¹⁵N.     

Interactive Effects of Nitrogen and Phosphorus on Soil Microbial Communities in a Tropical Forest

Elevated nitrogen (N) deposition in humid tropical regions may exacerbate phosphorus (P) deficiency in forests on highly weathered soils. However, it is not clear how P availability affects soil microbes and soil carbon (C), or how P processes interact with N deposition in tropical forests. We examined the effects of N and P additions on soil microbes and soil C pools in a N-saturated old-growth tropical forest in southern China to test the hypotheses that (1) N and P addition will have opposing effects on soil microbial biomass and activity, (2) N and P addition will alter the composition of the microbial community, (3) the addition of N and P will have interactive effects on soil microbes and (4) addition-mediated changes in microbial communities would feed back on soil C pools. Phospholipid fatty acid (PLFA) analysis was used to quantify the soil microbial community following four treatments: Control, N addition (15 g N m⁻² yr⁻¹), P addition (15 g P m⁻² yr⁻¹), and N&P addition (15 g N m⁻² yr⁻¹ plus 15 g P m⁻² yr⁻¹). These were applied from 2007 to 2011. Whereas additions of P increased soil microbial biomass, additions of N reduced soil microbial biomass. These effects, however, were transient, disappearing over longer periods. Moreover, N additions significantly increased relative abundance of fungal PLFAs and P additions significantly increased relative abundance of arbuscular mycorrhizal (AM) fungi PLFAs. Nitrogen addition had a negative effect on light fraction C, but no effect on heavy fraction C and total soil C. In contrast, P addition significantly decreased both light fraction C and total soil C. However, there were no interactions between N addition and P addition on soil microbes. Our results suggest that these nutrients are not co-limiting, and that P rather than N is limiting in this tropical forest.     

Effects of atrazine on the assimilation of inorganic nitrogen in cereals

The inclusion of sub-lethal amounts ofthe herbicide atrazine [2-chloro-4-(ethylamino)-6-(isopropylamino)-s-triazine] in the nutrient solution supplied to maize and barley increased the growth of the root and shoot and the uptake of nitrate. The activities of nitrate and nitrite reductases, glutamine synthetase and glutamate synthase were enhanced and the amino acid and nitrate contents of the xylem sap increased. All these effects of atrazine were found only in plants grown with nitrate as the nitrogen source. The uptake of ¹⁵NO₃^? and its incorporation into protein in the root and shoot of maize and barley seedlings was significantly greater in the atrazine treated plants. However, a stimulation in the incorporation of leucine-[¹⁴C] into TCA-precipitable protein of detached leaves from 7-day-old barley seedlings was obtained only in the absence of a supply of combined nitrogen either in the culture medium or in the in vitro incubation mixture containing the labelled amino acid.     

Nitrogen transformation in soil during humification of straw labelled with15N

Summary The decomposition and humification of oat straw labelled with¹⁵N were followed in the soil during 80 days. The influence of NaNO₃ and (NH₄)₂ SO₄ on these processes were also investigated. It was ascertained that addition of NH₄–N acted more efficiently than NO₃–N on both the decomposition of straw and the mineralization of the organic nitrogen compounds of the soil. In the presence of NH₄–N, straw¹⁵N predominated in humic acids, while in the presence of NO₃–N it predominated in fulvic acids.The incorporation of straw¹⁵N into the humic compounds occurred in proportion to the progressing decomposition of straw. The greatest similarity in the proportions of soil-N and straw-¹⁵N in isolated fractions was ascertained after 80 days of incubation in the presence of NH₄–N.     

Plant Effects on Spatial and Temporal Patterns of Nitrogen Cycling in Shortgrass Steppe

Because of the water-limited nature and discontinuous plant cover of shortgrass steppe, spatial patterns in ecosystem properties are influenced more by the presence or absence of plants than by plant type. However, plant type may influence temporal patterns of nutrient cycling between plant and soil. Plants having the carbon-3 (C₃) or carbon-4 (C₄) photosynthetic pathway differ in phenology as well as other attributes that affect nitrogen (N) cycling. We estimated net N mineralization rates and traced nitrogen-15 (¹⁵N) additions among plant and soil components during May, July, and September of 1995 in native plots of C₃ plants, C₄ plants, or mixtures of C₃ and C₄. Net N mineralization was significantly greater in C₃ plots than in C₄ plots during both July and September. C₃ plots retained significantly more ¹⁵N in May than did mixed and C₄ plots; these differences in ¹⁵N retention were due to greater ¹⁵N uptake by C₃ plants than by C₄ plants during May. There were no significant differences in total ¹⁵N retention among plant communities for July and September. Soil ¹⁵N was influenced more by presence or absence of plants than by type of plant; greater quantities of ¹⁵N remained in soil interspaces between plants than in soil directly under plants for July and September. Our results indicate that plant functional type (C₃ versus C₄) can affect both the spatial and the temporal patterns of N cycling in shortgrass steppe. Further research is necessary to determine how these intraseasonal differences translate to longer-term and coarser-scale effects of plants on N cycling, retention, and storage. Received 8 December 1997; accepted 6 May 1998.     

Nitrogen uptake in needles of Scots pine (Pinus sylvestris L.) when exposed to gaseous ammonia and ammonium fertilizer in the soil

Young saplings of Pinus sylvestris L. were exposed to gaseous NH₃ at 53 or 105 g m^–3 for one year in open-top chambers. Saplings received ¹⁵N-labelled (NH₄)₂SO₄ via the soil. To examine the importance of foliar N uptake, changes in the concentration of total and labelled N in the needles were followed. Increase in needle biomass and N concentration were found in trees exposed to NH₃, confirming that atmospheric NH₃ acted as a N fertilizer. NH₃ had a greater and quicker effect than (NH₄)₂SO₄: compared with the growth in ambient air, the N concentration in the needles exposed to NH₃ had increased by 49% in four months, while the increase after highest N-fertilization (200 kg N ha^–1 y^–1) was only 8%. The small contribution of NH₄ ⁺ fertilization to the total N concentration was not due to a deficient N uptake: the ¹⁵N concentration in the needles increased significantly with time. On the other hand, NH₃ uptake in shoots may have a negative effect on the NH₄ ⁺ root uptake. The relation between plant N and atmospheric NH₃ concentration was non-linear and possible reasons for this observation are discussed. Fumigation with NH₃ significantly decreased the ratios of K/N and P/N, showing that fumigation disrupted the nutrient balance.     

Decomposition nitrogen is better retained than simulated deposition from mineral amendments in a temperate forest

Nitrogen (N) deposition (N_DEP) drives forest carbon (C) sequestration but the size of this effect is still uncertain. In the field, an estimate of these effects can be obtained by applying mineral N fertilizers over the soil or forest canopy. A ¹⁵N label in the fertilizer can be then used to trace the movement of the added N into ecosystem pools and deduce a C effect. However, N recycling via litter decomposition provides most of the nutrition for trees, even under heavy N_DEP inputs. If this recycled litter nitrogen is retained in ecosystem pools differently to added mineral N, then estimates of the effects of N_DEP on the relative change in C (?C/?N) based on short‐term isotope‐labelled mineral fertilizer additions should be questioned. We used ¹⁵N labelled litter to track decomposed N in the soil system (litter, soils, microbes, and roots) over 18 months in a Sitka spruce plantation and directly compared the fate of this ¹⁵N to an equivalent amount in simulated N_DEP treatments. By the end of the experiment, three times as much ¹⁵N was retained in the O and A soil layers when N was derived from litter decomposition than from mineral N additions (60% and 20%, respectively), primarily because of increased recovery in the O layer. Roots expressed slightly more ¹⁵N tracer from litter decomposition than from simulated mineral N_DEP (7.5% and 4.5%) and compared to soil recovery, expressed proportionally more ¹⁵N in the A layer than the O layer, potentially indicating uptake of organic N from decomposition. These results suggest effects of N_DEP on forest ?C/?N may not be apparent from mineral ¹⁵N tracer experiments alone. Given the importance of N recycling, an important but underestimated effect of N_DEP is its influence on the rate of N release from litter.     

Interaction between Light Intensity and NaCl Salinity and Their Effects on Growth, CO(2) Assimilation, and Photosynthate Conversion in Young Broad Beans

Seedings of Vicia faba were grown for four weeks at two different light intensities (55 and 105 watts per square meter) in a saline (50 millimolar NaCl) and nonsaline nutrient solution. NaCl salinity depressed growth and restricted protein formation, CO₂ assimilation, and especially the incorporation of photosynthates into the lipid fraction. Conversion of photosynthates in leaves was much more affected by salinity than was photosynthate turnover in roots. The detrimental effect of NaCl salinity on growth, protein formation, and CO₂ assimilation was greater under low than under high light conditions. Plants of the high light intensity treatment were more capable of excluding Na⁺ and Cl⁻ and accumulating nutrient cation species (Ca²⁺, K⁺, Mg²⁺) than plants grown under low light intensity. It is suggested that the improved ionic status provided better conditions for protein synthesis, CO₂ assimilation, and especially for the conversion of photosynthates into lipids.     

Effects of aluminium on nitrate uptake and assimilation

A study was conducted to examine the hypothesis that the effects of external Al on NO₃^? uptake and assimilation depend upon the concentration of Al present. Young soybean seedlings [Glycine max (L.) Merrill, cv. Essex], growing under moderate acidity stress at pH 4-2, were exposed to a range of {A1³⁺} in solution for 3d, and to labelled 99 atom %¹⁵NO₃^? during the final hour of Al exposure. Uptake of ¹⁵NO₃^?g^?1 root dry weight was increased by about 28% in the presence of Al at {A1³⁺} below 10 mmolm^?3, and NO₃^? uptake was decreased by about 12% when the {A1³⁺} increased to 44mmoln^?3. The stimulation phase closely paralleled stimulation of root elongation. At higher {A1³⁺}, the inhibition of root elongation was much more severe than that of NO₃^? uptake. There was no indication of a separate effect of Al on root ¹⁵NO₃^? reduction in situ, as the accumulation of reduced ¹⁵N in the root remained a similar percentage of ¹⁵NO₃^? uptake at all {A1³⁺}. At higher {A1³⁺}, the atom %¹⁵N enrichment of the insoluble reduced-N (protein) fraction of root tips increased. This suggests that the Al inhibition of root elongation did not result from disruption of the N supply to the root apex.     

Nitrogen dynamics during O3-induced accelerated senescence in hybrid poplar

Experiments were conducted to determine the fate of nitrogen (N) remobilized as a result of ozone (O₃)‐induced accelerated senescence in hybrid poplar subjected to declining N availability concurrent with O₃ stress. Cuttings were grown in sand culture where the supply of N to the plant could be controlled on a daily basis and reduced in half of the plants when desired. Plants all initially received 3·57 mm N daily until approximately the 20 leaf stage after which daily supply of N was reduced to 0·71 mm . Plants were grown in open‐top chambers in the field (Rock Springs, PA, USA) and received charcoal‐filtered air, half also received supplemental O₃ to a level of 0·08 µL L^?1. Allocation of newly acquired N was determined with ¹⁵N. The specific allocation (mg labelled N mg^?1 total N) of labelled N to upper, expanding leaf N was not affected by O₃, but was strongly affected by N treatment. However, O₃ increased the relative partitioning of labelled N to the expanding leaves and the roots. The balance between partitioning of newly acquired N to the upper leaves and roots was not affected by O₃, but was reduced by N withdrawal. Calculated net N flux was strongly negative in the lower leaves of O₃‐exposed, N withdrawal plants. Nitrogen uptake was not reduced by O₃. The allometric relationships between the roots and shoots were not affected by O₃ or N availability. The relative contribution of newly acquired versus remobilized N to new growth appears to be determined by N supply. Ozone exposure alters the allocation of newly acquired N via alterations in plant size, whereas N availability exerts a strong effect upon both plant size and N allocation.     

Influence of light intensity on the distribution of carbon and consequent effects on mineralization of soil nitrogen in a barley (Hordeum vulgare L.)-soil system

A pot experiment was conducted in a ¹⁴C-labelled atmosphere to study the influence of living plants on organic-N mineralization. The soil organic matter had been labelled, by means of a 200-days incubation, with ¹⁵N. The influence of the carbon input from the roots on the formation of microbial biomass was evaluated by using two different light intensities (I). Mineralization of ¹⁵N-labelled soil N was examined by following its fate in both the soil biomass and the plants. Less dry matter accumulated in shoots and roots at the lower light intensity. Furthermore, in all the plant-soil compartments examined, with the exception of rhizosphere respiration, the proportion of net assimilated ¹⁴C was lower in the low-I treatment than in the high-I treatment. The lower rates of ¹⁴C and ¹⁵N incorporation into the soil biomass were associated with less root-derived ¹⁴C. During the chamber period (¹⁴CO₂-atmosphere), mineralized amounts of ¹⁵N (measured as plant uptake of ¹⁵N) were small and represented about 6.8 to 7.8% of the initial amount of organic ¹⁵N in the soil. Amounts of unlabelled N found in the plants, as a percentage of total soil N, were 2.5 to 3.3%. The low availability of labelled N to microorganisms was the result of its stabilization during the 210 days of soil incubation. Differences in carbon supply resulted in different rates of N mineralization which is consistent with the hypothesis that roots induce N mineralization. N mineralization was higher in the high-I treatment. On the other hand, the rate of mineralization of unlabelled stable soil N was lower than labelled soil ¹⁵N which was stabilized. The amounts of ¹⁵N mineralized in planted soil during the chamber period (43 days) which were comparable with those mineralized in unplanted soil incubated for 210 days, also suggested that living plants increased the turnover rate of soil organic matter.     

Effect of elevated potassium on phospholipid and inositol metabolism of isolated nerve endings

Synaptosomes were isolated from rat cerebra, and incubated in the presence of labelled phosphate and inositol. When the potassium concentration of the medium was increased by replacing NaCl with KCl, there was a marked increase in phosphate labeling of phosphatidic acid (PA) and phosphatidylinositol (PI). This was evident with [K⁺] above 12 mM and peaked at about 40 mM KCl. In normal calcium buffers, phosphate labeling of PI but not PA declined sharply with [KCl] above 40 mM. In low calcium buffers, the phosphate labeling response was greatly attenuated for both lipids, but PI labeling did not decline at higher [K⁺].The phosphate labeling response was confined to PA and PI, and was specific for the increase in [K⁺]₀. The same response was seen in constant (105 mM) sodium buffers, and atropine had no effect. The specific radioactivity of ATP was increased by elevated potassium, but not enough to account for the increased labeling of PA. Further, this appeared to be a result of the loss of stored ATP rather than an increase in turnover.Increasing [K⁺]₀ produced a decline in [³H]inositol incorporation into PI in parallel with the increase in its labeling by ³³PO₄. This was the same in constant sodium and in low calcium buffers. It could be attributed to an inhibition of synaptosomal uptake of labelled inositol from the medium. Synaptosomal inositol content was unaffected.Elevated potassium had a greater effect on PA labeling than on PI, and it was more effective in increasing phosphate labeling of PA than was acetylcholine (ACh). When ACh and elevated potassium were combined at their maximally effective concentration, they acted synergistically to stimulate phosphate incorporation into PA but elevated potassium blocked the increase in [³H]inositol incorporation into PI normally produced by ACh. These results indicate that elevated potassium and ACh act upon the same population of synaptosomes, but affect different biochemical steps. Elevated potassium probably effects phospholipid labeling by a calcium dependent increase in diglyceride production from lipids other than PA or PI.     

Habitat-Specific Nitrogen Dynamics in New Zealand Streams Containing Native or Invasive Fish

Streams are important sites of nutrient transport and transformation in the landscape but little is known about the way in which individual taxa or individual habitats (riffles and pools) influence nutrient dynamics within stream reaches. We used 5-week additions of a stable isotope (¹⁵NH₄Cl) tracer to investigate nitrogen dynamics in pools and riffles of two New Zealand streams, one with native fish (Galaxias depressiceps) and the other with invasive brown trout (Salmo trutta). In New Zealand, brown trout initiate a trophic cascade leading to increased algal biomass that we predicted would lead to higher N uptake and retention. Uptake of NO₃, but not ammonium, was greater in the trout stream. Rather than causing a large increase in N demand, trout may induce a reallocation of N uptake and retention among food web compartments in different habitats. The largest differences between streams were apparent in riffles, where most uptake and retention of N occurred. In the trout stream, uptake rate by epilithon in riffles was more than six times greater than uptake rates of any other compartment. In the Galaxias stream, several compartments in both habitats had similar uptake rates. Epilithon also accounted for a larger percentage of the ¹⁵N retained in the study reach in the trout stream (51%) than the Galaxias stream (34%). Our results show that an individual predatory taxon (in our case an invader) can influence N dynamics in streams but that the magnitude and location of the impact depend on a range of abiotic and biotic factors involved in N dynamics in streams.     

Role of Cation and Anion Uptake in Salt-stimulated Elongation of Lettuce Hypocotyl Sections

The role of cation and anion uptake in salt-stimulated growth of light-grown, GA₃-treated lettuce (Lactuca sativa L.) hypocotyl sections was investigated. Potassium chloride (10 mm) causes a 2-fold increase in the growth rate of GA₃-treated hypocotyl sections without affecting the growth rate of sections incubated in the absence of GA₃. Salt uptake is the same in both treatments, and furthermore the uptake of cation and anion is stoichiometric during the first 24 hours under all incubation conditions. The importance of the anion for cation uptake is demonstrated in experiments with benzenesulfonate⁻ and iminodiacetate²⁻. When K⁺ and Na⁺ are supplied only as the benzenesulfonate and iminodiacetate salts, growth and cation uptake are markedly reduced compared to KCl and NaCl. Calculation of the osmotic potential of salt-treated sections based on measurement of K⁺ and Cl⁻ uptake suggests that the observed increase in tissue osmolality is a result of salt uptake. Similarly, uptake of ions can account for the shift in water potential when sections are incubated in 10 mm KCl. We conclude that the change in growth rate of light-grown, GA₃-treated sections caused by the addition of KCl or NaCl to the incubation medium results solely from decreased water potential of the tissue due to ion uptake.     

Immobilisation, remineralisation and residual effects in subsequent crops of dairy cattle slurry nitrogen compared to mineral fertiliser nitrogen

About 50–60% of dairy cattle slurry nitrogen is ammonium N. Part of the ammonium N in cattle slurry is immobilised due to microbial decomposition of organic matter in the slurry after application to soil. The immobilisation and the remineralisation influence the fertiliser value of slurry N and the amount of organic N that is retained in soil. The immobilisation and the remineralisation of 15 N-labelled dairy cattle slurry NH₄-N were studied through three growing seasons after spring application under temperate conditions. Effects of slurry distribution (mixing, layer incorporation, injection, surface-banding) and extra litter straw in the slurry on the plant utilisation of labelled NH₄-N from slurry were studied and compared to the utilisation of ¹⁵N-labelled mineral fertiliser. The initial immobilisation of slurry N was influenced by the slurry distribution in soil. More N was immobilised when the slurry was mixed with soil. Surface-banding of slurry resulted in significant volatilisation losses and less residual ¹⁵N in soil. Much more N was immobilised after slurry incorporation than after mineral fertiliser application. After 2.5 years the recovery of labelled N in soil (0–25 cm) was 46% for slurry mixed with soil, 42% for injected slurry, 22% for surface-banded slurry and 24% for mineral fertiliser N. The total N uptake in a ryegrass cover crop was 5–10 kg N/ha higher in the autumn after spring-application of cattle slurry (100–120 kg NH₄-N/ha) compared to the mineral fertiliser N reference, but the immobilised slurry N (labelled N) only contributed little to the extra N uptake in the autumn. Even in the second autumn after slurry application there was an extra N uptake in the cover crop (0–10 kg N/ha). The residual effect of the cattle slurry on spring barley N uptake was insignificant in the year after slurry application (equivalent to 3% of total slurry N). Eighteen months after application, 13% of the residual ¹⁵N in soil was found in microbial biomass whether it derived from slurry or mineral fertiliser, but the remineralisation rate (% crop removal of residual ¹⁵N) was higher for fertiliser- than for slurry-derived N, except after surface-banding. Extra litter straw in the slurry had a negligible influence on the residual N effects in the year after application. It is concluded that a significant part of the organic N retained in soil after cattle slurry application is derived from immobilised ammonium N, but already a few months after application immobilised N is stabilised and only slowly released. The immobilised N has negligible influence on the residual N effect of cattle slurry in the first years after slurry application, and mainly contributes to the long-term accumulation of organic N in soil together with part of the organic slurry N. Under humid temperate conditions the residual N effects of the manure can only be optimally utilised when soil is also covered by plants in the autumn, because a significant part of the residual N is released in the autumn, and there is a higher risk of N leaching losses on soils that receive cattle slurry regularly compared to soils receiving only mineral N fertilisers.