Nitrogen Fixation in the Canopy of Temperate Forest Trees: A Re-examination

¹⁵N₂ studies and acetylene reduction assays of leaves and shootsof Douglas fir and other forest trees do not confirm previousreports that extensive nitrogen fixation occurs on leaf surfacesand it is concluded that the importance of nitrogen fixationin the canopy of forest trees has been exaggerated. The presenceof nitrogen-fixing bacteria on the leaves of trees is confirmed,however, and they have been identified as Enterobacter agglomerans,Clostridium butyricum and Bacillus sp. Their distribution onleaves is fortuitous since dead oak leaves and artificial leavesbecome colonized to the same extent as living oak leaves. nitrogen fixation, acetylene reduction, Enterobacter agglomerans, Clostridium butyricum, Bacillus sp, Douglas fir, Pseudotsuga menziensii, larch, Larix x oak, Quercus petraea.     

Nitrogen Fixation in the Phyllosphere of the Douglas Fir, Pseudotsuga douglasii

Nitrogen-fixing bacteria have been isolated from the leaf surfacesof the Douglas Fir. ¹⁵N tracer studies have shown that thesebacteria fix nitrogen in culture and in the field on the trees.A considerable proportion of the annual requirement for nitrogenby Douglas Fir may be provided by nitrogen-fixing bacteria onthe leaves and in the soil.     

Economy of Symbiotically Fixed Nitrogen in Red Clover (Trifolium pratenseL.)

The seasonal dynamics of symbiotic fixation, distribution andfate of nitrogen (N) were studied on two successive crops ofred clover (Trifolium pratenseL.) grown outdoors in soil containersunder the Mediterranean climate of southern France. Nitrogenaseactivity was followed throughout the growing season using acetylene(C₂H₂) reduction assays. The distribution and transfer of symbioticallyfixed N were followed by periodic measurements of¹⁵N distributionin plants after exposure of the root systems to labelled dinitrogen(¹⁵N₂). In both years there were two peaks of nitrogenase activity,one in spring and one in late summer, separated by a sharp decreaseduring the flowering period. Over the entire growth cycle, symbioticallyfixed N accounted for 61 to 96% of the total plant N. Once weekafter incorporation, 60 to 90% of N derived from the atmospherewas recovered in the aerial parts of the plants. More than 50%of this was in the leaves, but there were differences in distributionaccording to the stage of development. The maximum percentage(20–28%) recovered from nodulated roots occurred in May–June,during maximum growth of the vegetative organs, and in September.Above-ground symbiotically fixed N was highly mobile with time,moving from the rosette leaves to the leaves attached to theelongated stems and then to the seeds, where 25 to 50% of Nfixed in May and June was recovered in September. Because of:(1) the high turnover rate of leaves; and (2) the relativelyhigh N content of dead leaves, as much as 50% of the symbioticallyfixed N in a year was potentially available to the soil micro-organismsas litter. The maximum transfer was in spring and winter. Ofthe remainder, 20 to 35% was recovered in living plant partsduring regrowth in March of the second year. Transfers to andfrom the root system were less pronounced, but significant decreasesin N content of the roots occurred early in the second yearjust after foliage regrowth was initiated. It is concluded that,because of its high foliage productivity and turnover rate,and high yield of symbiotically fixed N, red clover is a goodcandidate to provide substantial amounts of N to the soil throughoutthe year and therefore restore N fertility. Red clover; Trifolium pratenseL.; forage legumes; labelled dinitrogen (¹⁵N₂) reduction; acetylene reduction; nitrogen fixation; nitrogen distribution; nitrogen transfer     

Assimilation and transport of nitrogen in rice I. 15N-labelled ammonium nitrogen

The assimilation and transport of ¹⁵N-labelled ammonium nitrogenin rice plants (Oryza sativa L.) was studied. Plants assimilatedlarge amounts of nitrogen from labelled ammonium into theiramides and amino acids, particularly in the roots and stem,at the end of a 4-day ¹⁵N feeding and 10 days later in the upperleaves, especially in the blades. Although the incorporationof ¹⁵N into all the nitrogen fractions of the newly emergedpanicle was evident, it was particularly pronounced in the amidesand amino acids of the soluble fractions. The upper leaves hada greater ¹⁵N incorporation in their organic N-fractions thandid the lower ones. Amides and amino acids are considered tobe the main forms of nitrogen transported to the shoot fromthe ammonium assimilated in the roots. The transport of theorganic forms of nitrogen was possibly greater to the upperleaves than to the lower ones. The nitrite fraction had more ¹⁵N than did the nitrate fractionin all parts of the plant, particularly in the upper leaf blades.It appeared that some of the ammonia might have been oxidizedto nitrite, then to nitrate in some parts of the plant; probablyin the upper leaves. The synthesis of protein and nucleic acid occurred rapidly inthe upper leaves, especially in the blades, also in the rootsas evidenced by the considerable incorporation of ¹⁵N in theinsoluble fractions of these parts. The variation in ¹⁵N-distribution,during the 10 days, in the different plant parts suggests thatthe nitrogen incorporated during protein synthesis in the rootsand tillers was remobilized and transported to the upper partsof the shoot. A concept for the transport of organic nitrogenouscompounds from the roots to shoot through the phloem and xylemof the rice plant stem is discussed. (Received May 11, 1974; )     

Direct measurement of nitrogen fixation by Trifolium repens L. and Alnus glutinosa L. using 15N2

A closed-system flow-through enclosure apparatus was used tomeasure symbiotic nitrogen fixation directly. A legume-basedsystem comprising 6-week-old Trifolium repens L. (white clovercv. Blanca) growing with Lolium perenne L. (perennial ryegrasscv. Trani) in an agricultural soil was incubated for 19 d ina ¹⁵N-enriched atmosphere (mean value 3.663 atom%). An actinorhizal-basedsystem comprising 1 -year-old Alnus glutinosa L. (alder) saplingsgrowing with Festuca rubra L. (red fescue) in open-cast coalspoil was incubated for 21 d in a ¹⁵N-enriched atmosphere (meanvalue 3.265 atom%). Indirect estimates of N2 fixation were carriedout concurrently using N difference and ¹⁵N isotope dilutiontechniques. The theory underlying the three techniques and modificationswhich were adopted for comparative purposes are discussed. Thedirect measurements of N2 fixation were then compared with theindirect estimates using P_inc, the proportion of the N incrementduring the measurement period that was derived from fixation.The simple N difference method gave similar values for Pinc(0.94 and 0.97) as those derived from more complicated isotopemethodologies, both indirect (0.91) and direct (0.90). Valuesfor alder were far more variable, ranging from 0.16 to 0.92;this was due largely to variability within the trees and a verysmall N increment during the measurement period. Key words: N₂ fixation, ¹⁵N₂, white clover, alder, enclosure apparatus     

Contribution from Stolons and Roots to Estimates of the Total Amount of N2Fixed by White Clover (Trifolium repensL.)

Growth and N-accumulation rates in leaves, stolons and rootsof individual white clover plants were studied in three experimentsusing two methods. In a growth chamber experiment, the relativedifferences between tissues were found to be almost constantfor a wide range of clover plant sizes. The stolon dry matter(DM) production was 56% and the root DM production 40% of theDM production in leaves. The N yield of stolons was 30% whileN yield in roots was 34% of N yield in leaves. The effect ofN application on these relations was investigated in a glasshouseexperiment. Application of N reduced the root:shoot N ratiofrom 0.50 to 0.28, whereas the stolon+root:leaf N ratio (i.e.for abovevs.below cutting-height tissues) was only reduced from0.97 to 0.80. In a field trial with two contrasting N regimes,growth and N accumulation were measured on individual cloverplants. Dinitrogen fixation was estimated by¹⁵N isotope dilutionbased on analysis of leaves-only or by including stolons. Usingleaves-only did not affect the calculation of percentage ofclover N derived from N₂fixation (% Ndfa) since the¹⁵N enrichmentwas found to be uniform in all parts of the clover. A correctionfactor of 1.7 to account for N in below cutting-height tissueis suggested when N₂fixation in white clover is estimated byharvesting the leaves only.Copyright 1997 Annals of Botany Company Leaves; N accumulation; N₂fixation; ¹⁵N isotope dilution; pastures; roots; root/shoot ratio; stolons; Trifolium repensL.; white clover     

Nitrogen fixation,transfer and turnover in upland and lowland grass-clover swards,using15N isotope dilution

The stable isotope¹⁵N is particularly valuable in the field for measuring N fixation by isotope dilution. At the same time other soil-plant processes can be studied, including¹⁵N recovery, and nitrogen transfer between clover and grass. Three contrasting sites and soils were used in the present work: a lowland soil, an upland soil, and an upland peat. Nitrogen fixation varied from 12 gm^–2 on lowland soil to 2.7 gm^–2 on upland peat. Most N transfer occurred on upland soil (4.2 gm^–2) which, added to nitrogen fixed, made a total of 8.7 gm² input during summer 1985.¹⁵N recovery for the whole experiment was small, around 25%.Measurement of dead and dying leaves, stubble and roots, suggests that plant organ death is the first stage in N transfer from white clover to ryegrass, through the decomposer cycle. Decomposition was fastest on lowland soils, slowest on peat. On lowland soil this decomposer nitrogen is apparently subverted before transfer, probably by soil microbes.Variations in natural abundance of¹⁵N in plants were found in the two species on the different soils. These might be used to measure nitrogen fixation without adding isotope, but the need for many replicates and repeat samples would limit throughput.     

Assimilation of Nitrogen in Mutants Lacking Enzymes of the Glutamate Synthase Cycle

¹⁵N labelling was used to investigate the pathway of nitrogenassimilation in photorespiratory mutants of barley (Hordeumvulgare cv. Maris Mink), in which the leaves have low levelsof glutamine synthetase (GS) or glutamate synthase, key enzymesof ammonia assimilation. These plants grew normally when maintainedin high CO₂, but the deletions were lethal when photorespirationwas initiated by transfer to air. Enzyme levels in roots weremuch less affected, compared to leaves, and assimilation oflabelled nitrate into amino acids of the root showed very littledifference between wild type and mutants. Organic nitrogen wasexported from roots in the xylem sap mainly as glutamine, levelsof which were somewhat reduced in the GS-deficient mutant andenhanced in the glutamate synthase deficient mutant. In theleaf, the major effect was seen in the glutamatesynthase mutant,which had an extremely limited capacity to utilize the importedglutamine and amino acid synthesis was greatlyrestricted. Thiswas confirmed by the supply of [¹⁵N]-glutamine directly to leaves.Leaves of the GS-deficient mutant assimilatedammonia at about75% the rate found for the wild type, and this was almost completelyeliminated by addition of the inhibitormethionine sulphoximine.Root enzymes, together with residual levels of the deleted enzymesin the leaves, have sufficient capacityfor ammonia assimilation,through the glutamate synthase cycle, to provide adequate inputof nitrogen for normal growth of themutants, if photorespiratoryammonia production is suppressed. Key words: Hordeum vulgare, ¹⁵N, glutamine synthetase, glutamate synthase, ammonia assimilation     

The Effect of Lenient Defoliation on the Nitrogen Economy of White Clover: The Contribution of Mineral Nitrogen to Plant Nitrogen Accumulation During Regrowth

Single plants of white clover (Trifolium repens L.) were grownfrom stolon cuttings rooted in sand. All plants were inoculatedwith Rhizobium trifolii, and for 14 weeks received nutrientsolution containing 0.5 mg N each week, as either ammonium ornitrate. Plants were then leniently defoliated or were leftintact and a ¹⁵N-labelled N source was applied at intervalsof 4 d to replace the unlabelled N. Lement defoliation removedfully expanded leaves only; the remaining immature leaves accountedfor 39–44% of the total. At harvests over the following21 d, leaf numbers were counted and dry matter (DM), N contentsand ¹⁵N enrichments of individual plant organs were determined. Rates of leaf emergence and expansion were accelerated in defoliatedplants; numbers of young leaves were similar in defoliated andintact plants. Total DM and N content were less in defoliatedthan intact plants and were not affected by form of N supplied.DM of young leaves, growing points and stolons and N contentof young leaves were, however, greater when ammonium ratherthan nitrate N was supplied. Rates of increase in the contentof plant total N were 8.2 ± 1.36 mg N d^-1 and 10.2±1.82 mg N d^-1 in defoliated and intact plants respectively.The increases were predominantly due to N₂ fixation, since recoveryof ¹⁵N showed that less than 1% of the increment in plant totalN was assimilated mineral N. Nevertheless, the contributionof mineral N to plant total N was 50% more in defoliated thanin intact plants; higher amounts of mineral N were found particularlyin young leaves and growing points. Partitioning of mineralN to nodulated roots increased over time and was greater whenammonium rather than nitrate N was present. White clover, Trifolium repens L. cv. S184, lenient defoliation, N accumulation, N₂ fixation     

Symbiotic N2 fixation of Alnus incana ssp. rugosa in shrub wetlands of the Adirondack Mountains, New York, USA

Surface waters in forested watersheds in the Adirondack Mountains and northern New York State are susceptible to nitrogen (N) saturation. Atmospheric deposition of N to watersheds in this region has been measured but the extent of internal N inputs from symbiotic N₂ fixation in alder-dominated wetlands is not known. We estimated N₂ fixation by speckled alder in these wetlands by the ¹⁵N natural abundance method and by acetylene reduction using a flow-through system. Foliar N derived from fixation (%N_dfa) was estimated for five wetlands. The '¹⁵N of speckled alder foliage from four of the five sites did not differ significantly (PА.05) from that of nodulated speckled alders grown in N-free water culture (-1.2ǂ.1‰). Estimates from the ¹⁵N natural abundance method indicated that alders at these sites derive 85-100% of their foliar N from N₂ fixation. At one of the sites, we also measured biomass and N content and estimated that the alder foliage contained 43 kg N ha^-1 of fixed N in 1997. This estimate was based on a foliar N content of 55.4lj kg N ha^-1 (mean-SE), 86dž%N_dfa, and an assumption that 10% of foliar N was derived from reserves in woody tissues. At this site, we further estimated via acetylene reduction that 37ᆞ kg N ha^-1 was fixed by speckled alders in 1998. This estimate used the theoretical 4:1 C₂H₂ reduction to N₂ fixation ratio and assumed no night-time fixation late in the season. Nitrogen inputs in wet and dry deposition at this site are approximately 8 kg N ha^-1 year^-1. We conclude that speckled alder in wetlands of northern New York State relies heavily on N₂ fixation to meet N demands, and symbiotic N₂ fixation in speckled alders adds substantial amounts of N to alder-dominated wetlands in the Adirondack Mountains. These additions may be important for watershed N budgets, where alder-dominated wetlands occupy a large proportion of watershed area.     

Inhibition of Nitrogen Fixation in Non-Legume Root Nodules by Hydrogen and Carbon Monoxide

The effect of the presence of hydrogen and of carbon monoxideon the fixation of nitrogen in detached root nodules of non-legumeshas been studied, fixation being measured by the use of ¹⁵N.Parallel tests on legumes (pea and soya bean) have been included.Fixation in the nodules of Casuarina, Alnus, and Myrica is inhibitedin the presence of substantial proportions of hydrogen, to adegree resembling that shown in legumes. Fixation in Alnus andMyrica is arrested in the presence of small proportions of carbonmonoxide, and here again the sensitiveness is of the same orderas in legumes.     

The uptake and distribution of 15N2 into the various organs of Typha latifolia L.

Direct evidence of heterotrophic dinitrogen fixation associated with the emergent aquatic angiosperm, Typha latifolia L., was obtained through the exposure of actively growing plants to ¹⁵N₂ gas for 7 days in a gas-tight exposure vessel. Highest enrichments of ¹⁵N were found in roots/rhizomes and leaf bases. Slight enrichments were also found in the leaves due to translocation from the roots, rhizomes and leaf bases. Total fixed ¹⁵N values were 71.8 μg for the plant and 49.1 μg for the soil.Plants growing in silica sand, which received a nutrient solution containing combined nitrogen, exhibited higher enrichments and fixed 86% more ¹⁵N after exposure to ¹⁵N₂ gas than plants which received a nutrient solution lacking combined nitrogen. It is hypothesized that the concentration of combined nitrogen added was insufficient to repress nitrogen fixation and resulted in an increase in nitrogen fixation by associated microorganisms.Propane was used to trace the loss and movement of gases from the ¹⁵N₂ vessel and between the upper leaf chamber and the lower root chamber. Gas was rapidly exchanged between the upper and lower chambers through the leaves and roots of T. latifolia. Further investigations showed that propane moved at a rate of 1223 μmol day⁻¹ from the leaves to the roots and 2652 μmol day⁻¹ from the roots to the leaves. These data demonstrated that gases diffuse rapidly through the plant body of T. latifolia.     

Evaluation of the 15N Natural Abundance Method and Xylem Sap Analysis for Assessing N2 Fixation of Understorey Legumes in Jarrah (Eucalyptus marginata Donn ex Sm.) Forest in S.W. Australia

Hansen, A. P. and Pate, J. S. 1987. Evaluation of the ¹⁵N naturalabundance method and xylem sap analysis for assessing N₂ fixationof understorey legumes in jarrah (Eucalyptus marginata Donnex Sm.) forest in S.W. Australia.—J. exp. Bot 38: 1446–1458. Nodulated seedlings of Acacia pulchella, A. alata and A. extensawere grown in glasshouse sand culture under a range of levels(0–16 mol m³) of nitrate, supplied as ¹⁵NO₃, or as unenrichedlaboratory grade nitrate (¹⁵N value 5·5%_o). Nitrate at8·0 mol m ³ or above was highly inhibitory to growthof all species. Using ¹⁵N dilution analysis of the ¹⁵N enrichedcultures to measure symbiotic dependency, it was shown that¹⁵N values of the parallel unenriched cultures increased innear linear fashion from close to zero in fully symbiotic plantsto values close to that of the supplied NO₃ in plants experiencingnitrate levels (4·0 mol m³ or above) inhibiting N₂ fixationby over 90%. Xylem sap analyses (0·4 mol m³ NO₃ treatments)showed asparagine as the major nitrogenous solute, relativelylittle spill-over of free nitrate, and no evidence of majorshifts in balance of amino compounds with increasing dependenceon nitrate. This essentially invalidated use of the techniqueas a field assay for N₂ fixation by the species. ¹⁵N values for total N of soil sampled at 64 widely distributedsites in jarrah forest ranged from – 2·15 to +5·4(mean +2·1). Comparable values for soil mineral N (NH⁺₄and NO₃) were +0·3 to + 14·2 (mean +5·1).¹⁵N values of the total plant N of the legumes and of non-N₂-fixingreference species were also highly variable between sites, withlittle evidence of reference plant N accurately reflecting the¹⁵N abundance of soil nitrogen, or of visibly well nodulatedlegume components showing consistently lower ¹⁵N values thantheir companion reference plants. At one site it was possibleto compare ¹⁵N values of first season seedling legumes withpreviously published estimates of their progressive N₂ fixationusing C₂H₂ reduction assays. It was concluded that heterogeneity in ¹⁵N discrimination ofsoil within the ecosystem precluded effective use of the ¹⁵Nnatural abundance technique for assessing legume N₂ fixation. Key words: Acacia spp., ¹⁵N natural abundance,, xylem sap analysis,, nitrogen fixation.     

The Significance of Transpirationally Derived Nitrogen in Protein Synthesis in Fruiting Plants of Pea (Pisum sativum L.)

Feeding of ¹⁵N-nitrate, ¹⁵N(amide)-L-glutamine, or ¹⁵N-L-glutamicacid to detached shoots of pea through the transpiration streamresults in the soluble and insoluble nitrogen of stem, leaves,and fruits becoming extensively enriched with isotopic nitrogen.The time course of labelling suggests that non-reproductiveparts are the principal centres of uptake and assimilation andthat from them translocation takes place to the developing seeds. Distribution patterns for ¹⁵N in free and protein-bound aminoacids of leaf and seed indicate that each labelled source donatesnitrogen to a wide range of amino compounds, with no evidenceof consistent differences in the manner in which each is assimilated.Alanine, glutamic acid, homoserine, and -aminobutyric acid,are the main recipients of ¹⁵N in the soluble fraction of theleaves, whilst in the insoluble fraction nitrogen of the aminoacids serine, glycine, alanine, threonine, glutamic acid + glutamine,and aspartic acid + asparagine achieves high specific labelling.Amino acids of the seeds are labelled more uniformly with ¹⁵N. A complementary ¹⁴C-labelling experiment on the translocationof photosynthetically fixed carbon from leaf to seed is describedand the labelling patterns obtained for amino acids in leaf,seed, and phloem exudate are discussed in relation to thosefor ¹⁵N.     

Assimilation and transport of nitrogen in rice II. 15N-labelled nitrate nitrogen

An investigation was made to study the assimilation and transportof ¹⁵N-labelled nitrate nitrogen in rice plant (Oryza sativaL.). Nitrogen from labelled nitrate at the end of plant feedingwas found mainly in nitrate form, and was more prevalent inroots, stem and leaf sheaths. The nitrite fraction had the nextlargest ¹⁵N enrichment. The ¹⁵NO₃ assimilation in the newlyemerged panicle was mainly in amide and amino acid. The ¹⁵N-incorporation at day 0 was greatest in amino acid andnitrate of roots and decreased towards the stem and leaves.Incorporation in these fractions considerably decreased fromday 0 to day 10. Probably most of the nitrogen from the nitratesource was transported from the roots to the shoot in nitrateand amino acid forms. A decrease of ¹⁵N-incorporation in the soluble N fraction andincrease in the insoluble N fraction from day 0 to day 10 inplant parts, particularly the blades, suggested that proteinsynthesis occurred mostly in young parts of the shoot duringthis period. The marked variation in ¹⁵N distribution in differentparts of the plant during the 10 days indicated that the nitrogenin roots and tillers was probably remobilized and transportedto other parts, particularly the upper leaf blades. Ammonium and nitrate nitrogen transport in rice plant are compared. (Received May 11, 1974; )     

Planktonic nitrogen transformations during a declining cyanobacteria bloom in the Baltic Sea

The uptake of ¹⁵N-labelled nitrogen nutrients (ammonium, urea,nitrate) was studied during the decline of a bloom of nitrogen-fixingcyanobacteria in the Baltic Sea. This was done by sampling anorth-south transect of stations, representing different stagesof the bloom. Comparison with nitrogen fixation data showedthat this process was of minor importance, and that the nitrogenuptake was dominated by regenerated nitrogen, mainly ammonium.From time series incubations for studying nutrient uptake, itappears that the regeneration of ammonium was substantial, butthat the production of urea or nitrate was slow. The integrateddaily uptake was calculated for the 0–15 m interval atfour stations and values ranged between 6 and 21 mmol N m^–2day^–1, of which the regenerated nutrients, ammonium andurea, constituted 71–93%. Nitrate was of minor importanceand the highest nitrate uptake rates were found close to thethermocline (at 15 m) and in the southern part of the Baltic.Comparison with carbon fixation data reported from simultaneousmeasurements at two stations gave C/N uptake ratios of 4.9 and2.1 for integrated daily uptake. Contrary to earlier findings,the concentration of DON increased with increasing salinity(from 15 to 17 µmol l^–1). This was correlated withthe declination of the bloom and is suggested to be a resultof a gradual release of less easily utilized DON from the degradationof cyanobacteria. The C/N ratio of DOM was high, 21–23.     

The Uptake of Gaseous Ammonia by the Leaves of Italian Ryegrass

Lockyer, D. R. and Whitehead, D. C. 1986. The uptake of gaseousammonia by the leaves of Italian ryegrass.—J. exp. Bot.37: 919–927. Plants of Italian ryegrass (Lolium multiflorum Lam.) grown insoil with two rates of added ¹⁵N-labelled nitrate were exposed,in chambers, for 40 d to NH₃ in the air at concentrations of16, 118 and 520 µg m^–3. At the highest concentrationof NH₃, this source provided 47?3% of the total nitrogen inplants grown with the lower rate of nitrate addition (100mgN kg^–1 dry soil) and 35?2% with the higher rate (200mgN kg^–1 dry soil) At the intermediate concentration ofNH₃, the contributions to total plant N were 19?6% and 10?8%,respectively, at low and high nitrate while, at the lowest concentrationof NH₃, they were 5?1% and 32%. Most of the N derived from theNH₃ remained in the leaves, but some was transported to theroots. The amount of N derived from the NH³ that was presentin the leaves was not reduced by washing the leaves in waterat pH 5?0 before harvesting, indicating that the N was assimilatedby the plant and not adsorbed superficially. Rates of uptakeof NH₃ per unit leaf area ranged from 1?7 µg dm^–2h^–1 at a concentration of 16 µg m^–3 to 29?0µg dm^–2 h^–1 at a concentration of 520 µgm^–3 and with the lower rate of nitrate addition. Increasingthe supply of nitrate to the roots slightly reduced the rateof uptake of NH₃ per unit leaf area. Uptake of N from the higherrate of nitrate was reduced at the highest concentration ofNH₃ in the air. Key words: Ammonia, nitrogen, leaf sorption, Lolium multiflorum     

Nitrogen Turnover in Marine and Brackish Habitats II. Use of 15N in Measuring Nitrogen Fixation in the Field

A technique for measuring nitrogen fixation in situ by naturalpopulations of blue-green algae is described. It involves exposingtest samples of known area to a gas mixture containing molecularnitrogen enriched with ¹⁵N and measuring the rate of incorporationof the isotope over a standard 24-h exposure period. The accuracyof the method is not seriously affected by changes in pH, pCO²and humidity which may occur during the exposure period, orby the degassing procedure used to remove air from the exposureflask prior to introduction of the isotope. Temperature andpN² values inside the exposure flask are different from thoseto which natural populations are exposed outside, and correctionsfor these have to be made in calculating the final results.The minimum pN² which allows optimum fixation by Calothrix scopulorumin the presence of 0.2 atm. oxygen is 0.4 atm. In an area ofthe supra-littoral fringe of a rocky shore and in an area ofsand dune-slack over a 12-month period nitrogen fixation ishigh in spring and autumn and negligible in winter. On the rockyshore fixation is low in summer; in the dune-slack summer nitrogenfixation is erratic. Nitrogen-fixing efficiency in terms ofnitrogen fixed per unit weight of test material is high whenalgal recolonization is occurring. The mean fixation rate perannum corresponds to approximately 2.5 g/m2/annum for the rockyshore. The nitrogen fixed per annum represents approximately41 per cent and 21 per cent of the mean total nitrogen presentper annum on the rocky shore and in open areas of the sand dune-slackrespectively.     

Partitioning of Nitrogen Derived from N2 Fixation and Reserves in Nodulated Medicago sativa L. During Regrowth

Nodul{macron}ted alfalfa plants were grown hydroponically. Inorder to quantify N₂ fixation and remobilization of N reservesduring regrowth the plants were pulse-chase-labelled with ¹⁵N.Starch and ethanol-soluble sugar contents were analysed to examinechanges associated with those of N compounds. Shoot removalcaused a severe decline in N₂ fixation and starch reserves within6 d after cutting. The tap root was the major storage site formetabolizable carbohydrate compounds used for regrowth; initiallyits starch content decreased and after 14 d started to recoverreaching 50% of the initial value on day 24. Recovery of N₂fixation followed the same pattern as shoot regrowth. Afteran initial decline during the first 10 d following shoot removal,the N₂ fixation, leaf area and shoot dry weight increased sorapidly that their levels on day 24 exceeded initial values.Distribution of ¹⁵N within the plant clearly showed that a significantamount of endogenous nitrogen in the roots was used by regrowingshoots. The greatest use of N reserves (about 80% of N incrementin the regrowing shoot) occurred during the first 10 d and thencompensated for the low N₂ fixation. The distribution of N derivedeither from fixation or from reserves of source organs (taproots and lateral roots) clearly showed that shoots are thestronger sink for nitrogen during regrowth. In non-defoliatedplants, the tap roots and stems were weak sinks for N from reserves.By contrast, relative distribution within the plant of N assimilatedin nodules was unaffected by defoliation treatment. Key words: Medicago sativa L., N₂ fixation, N remobilization, N₂ partitioning, regrowth     

中国森林生态系统N平衡现状

由于N饱和生态系统的出现,森林生态系统作为环境污染储蓄库的认识受到挑战。收集了近十余年来全国各地森林N素循环的研究资料,通过对目前大气N沉降、森林生物固N、森林生态系统N的流失、淋失、挥发等各项收支参数的分析,借助农田养分收支平衡的估算思路和方法对全国森林生态系统N平衡进行了估算。结果表明,我国森林生态系统N的输入大于输出,全国森林生态系统年容纳大气N约为736万t,其中约176万t来自于大气N沉降,约599万t来自于生物固N。而进入到森林生态系统中的N约16万t固定在木材中用以维持森林蓄积的增加,其余绝大部分则保存于森林土壤,使得森林土壤全N含量大约以每年0.002%的速率增长。但不断增加的N素输入并未导致森林生态系统N饱和,全国的森林蓄积仍保持增长的趋势,森林生态系统在N的生物地球化学循环过程中起着重要的调节作用,仍是环境N的储蓄库,对于调节气候,防治污染具有重大作用。