Nitrogen Transfer Within and Between Plants Through Common Mycorrhizal Networks (CMNs)

Mycorrhizae play a critical role in nutrient capture from soils. Arbuscular mycorrhizae (AM) and ectomycorrhizae (EM) are the most important mycorrhizae in agricultural and natural ecosystems. AM and EM fungi use inorganic NH₄ ⁺ and NO₃ ^?, and most EM fungi are capable of using organic nitrogen. The heavier stable isotope ¹⁵N is discriminated against during biogeochemical and biochemical processes. Differences in ¹⁵N (atom%) or δ¹⁵N (‰) provide nitrogen movement information in an experimental system. A range of 20 to 50% of one-way N-transfer has been observed from legumes to nonlegumes. Mycorrhizal fungal mycelia can extend from one plant's roots to another plant's roots to form common mycorrhizal networks (CMNs). Individual species, genera, even families of plants can be interconnected by CMNs. They are capable of facilitating nutrient uptake and flux. Nutrients such as carbon, nitrogen and phosphorus and other elements may then move via either AM or EM networks from plant to plant. Both ¹⁵N labeling and ¹⁵N natural abundance techniques have been employed to trace N movement between plants interconnected by AM or EM networks. Fine mesh (25～45 μm) has been used to separate root systems and allow only hyphal penetration and linkages but no root contact between plants. In many studies, nitrogen from N₂-fixing mycorrhizal plants transferred to non-N₂–fixing mycorrhizal plants (one-way N-transfer). In a few studies, N is also transferred from non-N₂–fixing mycorrhizal plants to N₂-fixing mycorrhizal plants (two-way N-transfer). There is controversy about whether N-transfer is direct through CMNs, or indirect through the soil. The lack of convincing data underlines the need for creative, careful experimental manipulations. Nitrogen is crucial to productivity in most terrestrial ecosystems, and there are potential benefits of management in soil-plant systems to enhance N-transfer. Thus, two-way N-transfer warrants further investigation with many species and under field conditions.     

Effects of timing and supply of nitrogen on nitrogen remobilization from vegetative organs and redistribution to developing seeds of sunflower

A glasshouse study was made of the distribution of ¹⁵N among vegetative organs of sunflower and its later remobilization and redistribution to seeds, as influenced by the developmental stage at which ¹⁵N was provided, and by the N status of the plants. Plants of Hysun 30 sunflower were grown in sand culture and provided with K¹⁵NO₃ for a 3-day period at: (a) 3 days before the end of floret initiation; (b) 3 days before anthesis; (c) the start of anthesis; (d) full anthesis; and (e) 8 days after full anthesis. The plants were grown on a range of N supply rates, from severely deficient to more than adequate for maximum growth. Nitrogen-15 was distributed to all parts of the plant at the end of the ¹⁵N uptake periods. With the exception of the most N-stressed plants, subsequent remobilization of ¹⁵N from roots, stems and leaves occurred irrespective of the time the ¹⁵N was taken up. However, the percentage redistribution to seeds of ¹⁵N taken up at the end of floret initiation was less than for ¹⁵N taken up at anthesis. Remobilization of ¹⁵N from leaves and roots was higher (70%) for ¹⁵N taken up during and after anthesis than for ¹⁵N taken up at the end of floret initiation (45%), except for plants grown on the lowest N supply. By contrast, remobilization of ¹⁵N from the stem was lower for ¹⁵N taken up after full anthesis (40%) than before or during anthesis (>70%). The proportion of ¹⁵N remobilized from the top third of the stem was less than that from the bottom third, and decreased with increasing plant N status. Nitrogen-15 taken up over the 3-day supply periods during anthesis contributed from 2 to 11% of the total seed N at maturity; the contribution to seeds was greatest for plants grown on the highest N supply. Nitrogen taken up just before and during anthesis contributed most of the N accumulated in mature seeds of plants grown on an adequate N supply, but N taken up between the end of floret initiation and just before anthesis, or after full anthesis seemed to make an equally important contribution to mature seeds as N taken up during anthesis for plants grown on a very low N supply. It was concluded that the development of florets and seeds of sunflower is supported by N taken up by the plant between the end of floret initiation and anthesis, and by N redistributed from vegetative organs. Unless soil N is so low as to impair early growth, split applications of N fertilizer would be best made just before the end of floret initiation (‘star stage’) and just before anthesis.     

Nitrogen fixation by white clover in pastures grazed by dairy cows: Temporal variation and effects of nitrogen fertilization

Effects of rate of nitrogen (N) fertilizer and stocking rate on production and N₂ fixation by white clover (Trifolium repens L.) grown with perennial ryegrass (Lolium perenne L.) were determined over 5 years in farmlets near Hamilton, New Zealand. Three farmlets carried 3.3 dairy cows ha^–1 and received urea at 0, 200 or 400 kg N ha^–1 yr^–1 in 8–10 split applications. A fourth farmlet received 400 kg N ha^–1 yr^–1 and had 4.4 cows ha^–1.There was large variation in annual clover production and total N₂ fixation, which in the 0 N treatment ranged from 9 to 20% clover content in pasture and from 79 to 212 kg N fixed ha^–1 yr^–1. Despite this variation, total pasture production in the 0 N treatment remained at 75–85% of that in the 400 N treatments in all years, due in part to the moderating effect of carry-over of fixed N between years.Fertilizer N application decreased the average proportion of clover N derived from N₂ fixation (P_N; estimated by ¹⁵N dilution) from 77% in the 0 N treatment to 43–48% in the 400 N treatments. The corresponding average total N₂ fixation decreased from 154 kg N ha^–1 yr^–1 to 39–53 kg N ha^–1 yr^–1. This includes N₂ fixation in clover tissue below grazing height estimated at 70% of N₂ fixation in above grazing height tissue, based on associated measurements, and confirmed by field N balance calculations. Effects of N fertilizer on clover growth and N₂ fixation were greatest in spring and summer. In autumn, the 200 N treatment grew more clover than the 0 N treatment and N₂ fixation was the same. This was attributed to more severe grazing during summer in the 0 N treatment, resulting in higher surface soil temperatures and a deleterious effect on clover stolons.In the 400 N treatments, a 33% increase in cow stocking rate tended to decrease P_N from 48 to 43% due to more N cycling in excreta, but resulted in up to 2-fold more clover dry matter and N₂ fixation because lower pasture mass reduced grass competition, particularly during spring.     

土壤干旱条件下氮素营养对小麦水分状况和光合作用的影响

轻度土壤干旱下,小麦叶片仍能维持较好的水分状况,高氮营养对叶片光合作用有明显的促进作用。中度以上土壤干旱下,叶片水势和相对含水量明显降低,高氮叶片降低的幅度显著大于低氮,同时叶片净光合率(P_n)也趋于降低,高氮叶片降低的幅度较大。高氮叶片的叶肉光合活性明显大于低氮叶片,干旱下P_n降低与其气孔限制作用较大有关。高氮叶片的渗透调节大于低氮叶片,但渗透调节对气孔导度和P_n的维持有限。     

分次追施N肥对苹果砧木—平邑甜茶吸收15N-尿素以及叶片衰老的影响

以盆栽平邑甜茶(Malus hupenhensis)为实验材料,研究等氮(N)量分次追施N肥(一次、二次和三次)对平邑甜茶叶片衰老及15N-尿素吸收、利用的影响.采用15N示踪技术,研究不同施肥处理下植株的生长、酶活性和15N吸收利用等参数.研究结果表明:植株的株高、茎粗、叶面积和叶绿素含量(SPAD)在生长前期均以一次性追肥处理最高,三次追肥处理最低,且与一次追肥处理差异显著;在生长中期均以二次追肥处理最高,一次追肥处理最低;在生长后期均以三次追肥处理最高,一次追肥处理最低,且与三次追肥处理差异显著;叶片的超氧化物歧化酶(SOD)、过氧化物酶(POD)、过氧化氢酶(CAT)活性在生长前期均以一次追肥处理最高,三次追肥处理最低,且与一次追肥处理差异显著;在生长中期均以二次追肥处理最高,一次追肥处理最低;在生长后期均以三次追肥处理最高,一次追肥处理最低,且与三次追肥处理差异显著;生长后期植株各器官从肥料中吸收分配到的15N量对该器官全N量的贡献率差异显著,三次追肥处理显著高于一次和二次追肥处理;生长后期三次追肥处理植株的总N量、吸收的15N量及15N肥料利用率均为最大.三次追肥处理能提高叶片全N量,延缓生长后期叶片衰老,提高N肥利用率.     

Pulmonary NO uptake in interstitial lung disease

Because lung nitric oxide (NO) diffusing capacity (DL) represents alveolar-capillary gas diffusion, we queried as to whether disturbances of pulmonary gas exchange in interstitial lung disease (ILD) are appropriately reflected by using NO. In this pilot study, we applied the (15)N-labeled stable isotope (15)NO (relative abundance 0.37% of total NO) in order to ignore the endogenous NO production. In 10 ILD-outpatients, we measured DL (15)NO by performing the single-breath method. Lung function parameters as well as arterial oxygen partial pressure (PaO(2)) were also tested. Values of DL (15)NO ranged within 50-151 ml (15)NO/(mmHg min). Ratios of DL (15)NO/reference were between 43 and 108% of predicted data as taken from our previous work on healthy volunteers [Eur. J. Physiol. 446 (2003) 256]. We found a significant reduction of DL (15)NO/reference in five patients. Additionally, values of PaO(2) were significantly correlated to ratios of DL (15)NO/reference (adjusted R2 +/-SEE=0.407+/-8.051). In conclusion, (15)NO represents an appropriate indicator gas for reflecting an ILD-induced impairment of alveolar-capillary gas exchange.     

不同氮处理下速生柳对水体氮的吸收、分配及生理响应

采用水培法,研究了旱柳苗在外源添加不同氮水平(贫氮、中氮、富氮、过氮)的铵态氮(NH+4-N)和硝态氮(NO-3-N)的生长、氮吸收、分配和生理响应。结果表明:一定范围氮浓度的增加能够促进旱柳苗的生长,但过量氮会抑制其生长,且NH+4-N的抑制作用大于NO-3-N;两种氮处理下,旱柳表现出对NH+4-N的吸收偏好,在同一氮水平时,旱柳各部位氮原子百分含量Atom%15N(AT%)、15N吸收量和来自氮源的N%(Ndff%)均为NH+4-N处理大于NO-3-N处理,且随着氮浓度的增加,差异增大,且在旱柳各部位的分布为根﹥茎﹥叶;2种氮素过量和不足均会对旱柳根和叶生理指标产生不同的影响,其中在过氮水平时,NH+4-N和NO-3-N处理下根系活力比对照减少了50.61%和增加了19.53%;在过氮水平时,NH+4-N处理柳树苗根总长、根表面积、根平均直径、根体积和侧根数分别对照下降了30.92%、29.48%、19.44%、27.01%和36.41%,NO-3-N处理柳树苗相应的根系形态指标分别对对照下降了1.66%、5.65%、1.49%、5.06%和25.72%。可见,高浓度NH+4-N对旱柳苗的胁迫影响大于NO-3-N,在应用于水体氮污染修复时可通过改变水体无机氮的比例,削弱其对旱柳的影响,从而提高旱柳对水体氮污染的修复效果。     

Fertilizer vs. organic matter contributions to nitrogen leaching in cropping systems of the Pampas: 15N application in field lysimeters

Nitrogen (N) export from soils to streams and groundwater under the intensifying cropping schemes of the Pampas is modest compared to intensively cultivated basins of Europe and North America; however, a slow N enrichment of water resources has been suggested. We (1) analyzed the fate of fertilizer N and (2) evaluated the contribution of fertilizer and soil organic matter (SOM) to N leaching under the typical cropping conditions of the Pampas. Fertilizer N was applied as ¹⁵N-labeled ammonium sulfate to corn (in a corn/soybean rotation) sown under zero tillage in filled-in lysimeters containing two soils of different texture representative of the Pampean region (52 and 78 kg N ha^-1, added to the silt loam and sandy loam soil, respectively). Total fertilizer recovery at corn harvest averaged 84 and 64% for the silt loam and sandy loam lysimeters, respectively. Most fertilizer N was removed with plant biomass (39%) or remained immobilized in the soil (29 and 15%, for the silt loam and sandy loam soil, respectively) whereas its loss through drainage was negligible (<0.01%). We presume that the unaccounted fertilizer N losses were related to volatilization and denitrification. Throughout the corn growing season, subsequent fallow and soybean crop, which took place during an exceptionally dry period, the fertilizer N immobilized in the organic pool remained stable, and N leaching was scarce (7.5 kg N ha^-1), similar at both soils, and had a low contribution of fertilizer N (0–3.5%), implying that >96% of the leached N was derived from SOM mineralization. The inherent high SOM of Pampean soils and the favorable climatic conditions are likely to propitiate year-round production of nitrate, favoring its participation in crop nutrition and leaching. The presence of ¹⁵N in drainage water, however, suggests that fertilizer N leaching could become significant in situations with higher fertilization rates or more rainy seasons.     

Plant Growth Based on Interrelation between Carbon and Nitrogen Translocation from Leaves

In individual leaves, the photon-saturated photosynthetic activity (P _sat, expressed on a dry mass basis) was closely related to the nitrogen content (Nc) as follows: P _sat = Cf Nc + P _sat0, where Cf and P _sat0 are constants. On a whole plant basis, the relative growth rate (RGR) was closely related to Nc in canopy leaf as follows: RGR = DMf Nc + RGR₀, where DMf and RGR₀ are constants. However, the coefficients Cf and DMf were markedly different among plant species. To explain these differences, it is suggested that carbon assimilation (or dry matter production) is controlled by both the Nc in a leaf (or leaves) and by the net N translocation from leaves. This is supported by the finding that P _sat is related to the rate of ³⁵S-methionine translocation from leaves. We propose another estimation method for the net N translocation rate (NFR) from leaves: Nc, after full leafing, is expressed as a function of time: Nc = (Nc₀ – Ncd) exp(–Nft) + Ncd, where Nf is a coefficient, t is the number of days after leaf emergence, Nc₀ is the initial value of Nc, and Ncd is the Nc of the dead leaf. The NFR is then calculated as NFR = Nc/t = –Nf (Nc – Ncd). Thus Nf is the coefficient for the NFR per unit Nc. NFR is a good indicator of net N translocation from leaves because NFR is closely related to the rate of ³⁵S-methionine translocation from leaves. Since P _sat is related to the ¹⁴C-photosynthate translocation rate, Cf (or DMf) corresponds to the coefficient of saccharide translocation rate per unit amount of Nc. Cf (or DMf) is closely related to the Nf of individual leaves (or the Nf of canopy leaf). This indicates that C assimilation and C translocation from leaves are related to Nc and N translocation from leaves (net translocation of N). Cf and Nf are negatively correlated with leaf longevity, which is important because a high or low CO₂ assimilation rate in leaves is accompanied by a correspondingly high or low N translocation in leaf, and the degree of N translocation in leaves decreases or increases leaf longevity. Thus, since a relatively high P _sat (or RGR) is accompanied by a rapid Nc decrease in leaves, it is difficult to maintain a high P _sat (or RGR) for a sustained time period.     

不同林龄杉木氮素的获取策略

为了探讨不同林龄杉木人工林氮素获取策略,选择了江西千烟洲森林生态研究站红壤区的3种林龄杉木人工林(5年生幼龄林、13年生中龄林和30年生成熟林)作为研究对象,利用稳定性同位素~(15)N示踪技术研究了它们的氮素吸收策略。结果表明,杉木对硝态氮的吸收受林龄影响,成熟林的吸收速率最高,为(5.72±0.24)μg N g~(-1)干重h~(-1),而中龄林和幼龄林的吸收速率相当,分别为(1.57±0.13)μg N g~(-1)干重h~(-1)和(2.36±0.22)μg N g~(-1)干重h~(-1)。幼龄林((34.33±1.20)μg N g~(-1)干重h~(-1))和成熟林((34.18±2.32)μg N g~(-1)干重h~(-1))对铵态氮的吸收速率相似,均显著高于中龄林((23.33±1.39)μg N g~(-1)干重h~(-1))。杉木对甘氨酸的吸收不受林龄的影响。3种年龄的杉木均对铵态氮表现出强的获取能力,其中成熟林杉木对硝态氮的获取能力明显弱于对铵态氮的获取,但却强于对甘氨酸的获取。这样的结果反映了林龄能影响杉木人工林对无机氮的吸收,但未影响对有机氮的吸收;杉木偏好吸收铵态氮,对硝态氮和甘氨酸的吸收很少。如果能把氮素形态考虑进对杉木人工林的施肥管理当中,那么可能会极大地改善杉木的生产力。     

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.     

Nitrogen incorporation and remobilization in different shoot components of field-grown winter oilseed rape (Brassica napus L.) as affected by rate of nitrogen application and irrigation

The seasonal course of nitrogen uptake, incorporation and remobilization in different shoot components of winter oilseed rape (Brassica napus L.) was studied under field conditions including three rates of ¹⁵N labelled nitrogen application (0, 100 or 200 kg N ha^-1) and two irrigation treatments (rainfed or watered at a deficit of 20 mm). The total amount of irrigation water applied was 260 mm, split over 13 occasions in a 7-week-period ranging from 1 week before onset of flowering until 4 weeks after flowering.Nitrogen application and irrigation increased plant growth and nitrogen accumulation. Irrespective of N and irrigation treatment more than 50% of total shoot N was present in the stem when flowering started. At the end of flowering, pod walls were the main N store containing about 30–40% of shoot N. The quantities of N remobilized from stems and pod walls amounted in all treatments to about 70% of the N present in these organs at mid-flowering. At harvest, stem and pod walls each contained about 10% of total shoot N, the remaining 80% being incorporated into seeds. The main component contributing to the response of seed N accumulation to nitrogen application and irrigation was pods in axillary racemes. Up to 20 kg N ha^-1, corresponding to about 10% of final shoot N content, was lost from the plants by leaf drop.Irrigation increased the recovery at harvest of applied N from 30% to about 50%, while the level of N application did not affect the N recovery. ¹⁵N labelled (fertilizer derived) nitrogen constituted a greater proportion of the N content in old leaves than in young leaves and increased with age in the former, but not in the latter. Relative to soil N, fertilizer derived N also contributed more to the N content of vegetative than to that of reproductive shoot components. Small net changes in shoot N content after flowering reflected a balance between N import and export, leading to continuous dilution of ¹⁵N labelled N with unlabelled N.     

Nitrogen Transfer Between Plants: A 15N Natural Abundance Study with Crop and Weed Species

An increasing amount of evidence indicates that N can be transferred between plants. Nonetheless, a number of fundamental questions remain. A series of experiments was initiated in the field to examine N transfer between N₂-fixing soybean (Glycine max [L.] Merr.) varieties and a non-nodulating soybean, and between N₂-fixing peanut (Arachis hypogaea L.) or soybean and neighboring weed species. The experiments were conducted in soils with low N fertilities and used differences in N accumulation and/or ¹⁵N natural abundance to estimate N transfer. Mixtures of N₂-fixing and non-nod soybean indicated that substantial inter-plant N transfer occurred. Amounts were variable, ranging from negligible levels to 48% of the N found in the non-nod at maturity. Transfer did not appear to strongly penalize the N₂-fixing donor plants. But, in cases where high amounts of N were transferred, N content of donors was noticeably lowered. Differences were evident in the amount of N transferred from different N₂-fixing donor genotypes. Results of experiments with N₂-fixing crops and the weed species prickly sida (Sida spinosa L.) and sicklepod (Senna obtusifolia [L.] Irwin & Barneby) also indicated substantial N transfer occurred over a 60-day period, with amounts accounting for 30–80% of the N present in the weeds. Transfer of N, however, was generally very low in weed species that are known to be non-hosts for arbuscular mycorrhizae (yellow nutsedge, Cyperus esculentus L. and Palmer amaranth, Amaranthus palmeri [S.] Watson). The results are consistent with the view that N transfer occurs primarily through mycorrhizal hyphal networks, and they reveal that N transfer may be a contributing factor to weed problems in N₂-fixing crops in low N fertility conditions.     

氮素营养水平对冬小麦碳氮运转的影响

在大田试验条件下,研究了不同施氮水平对2种穗型冬小麦品种花后干物质和氮素积累与运转的影响及其与产量和品质的关系,以探讨氮素营养水平对冬小麦碳氮运转的影响.结果显示,适宜的施氮量（180 kg·hm^-2）能够极显著增加2种穗型冬小麦品种叶片、茎鞘等营养器官花前贮藏物质及花前贮藏氮素的再运转量和运转率以及总再运转量和运转率,也能够极显著增加成熟期籽粒氮素含量和花前贮藏氮素总运转量对籽粒氮素含量的贡献率.各施氮处理对2种穗型小麦品种花后氮素积累量对籽粒氮素含量贡献率的影响效应不明显.结果表明,适宜的施氮量有利于小麦籽粒和蛋白质产量的提高.     

Fertilization rates and clay fixed ammonium in two Quebec soils

Clay fixed NH₄ ⁺ can provide a significant sink for fertilizer N, as well as a source of N for plant uptake. Knowledge or soil NH₄ ⁺ fixing capacity and release for crops is necessary to develop long-term fertilizer programs. Field experiments with corn (Zea mays L.) were carried out to investigate soil NH₄ ⁺ fixing capacity and subsequent release as influenced by fertilizer rates using ¹⁵N in a Ste. Rosalie clay (fine, mixed, frigid, Typic Humaquept) and a Chicot sandy clay loam (fine-loamy, mixed, frigid, Typic Hapludalf). With high N rates increased NH₄ ⁺ fixation occurred only in the Ste. Rosalie soil. At the end of the first growing season, fertilizer N recovery as clay fixed NH₄ ⁺ for high and normal rates of fertilizer in the Ste. Rosalie soil was 17.8% and 28.7%, respectively and the recovery for the high and normal rates in the Chicot soil was 4.6 and 10.5%, respectively. Significant amounts of clay fixed NH₄ ⁺-N were released in the soil profile in the second year after ¹⁵N application on the Chicot soil. Recently clay fixed fertilizer NH₄ ⁺N was released more rapidly than that of the native fixed NH₄ ⁺, from the surface layer of the Ste. Rosalie soil. The fertilizer fixed NH₄ ⁺ seems to be in a more labile N pool than the native fixed NH₄ ⁺-N in the Chicot soil.     

Nitrogen uptake and transformation in a midwestern U.S. stream: A stable isotope enrichment study

This study presents a comprehensive analysis ofnitrogen (N) cycling in a second-order forestedstream in southern Michigan that has moderatelyhigh concentrations of ammonium (mean,16 g N/L) and nitrate (17 g N/L). Awhole-stream ¹⁵NH₄ ⁺ addition wasperformed for 6 weeks in June and July, and thetracer ¹⁵N was measured downstream inammonium, nitrate, and detrital and livingbiomass. Ancillary measurements includedbiomass of organic matter, algae, bacteria andfungi, nutrient concentrations, hydrauliccharacteristics, whole-stream metabolism, andnutrient limitation assays. The resultsprovide insights into the heterotrophic natureof woodland streams and reveal the rates atwhich biological processes alter nitrogentransport through stream systems.Ammonium uptake lengths were 766–1349 m anduptake rates were 41–60 g N m^–2min^–1. Nitrate uptake could not bedetected. Nitrification rates were estimatedfrom the downstream increase in¹⁵N-enriched nitrate using a simulationmodel. The ammonium was removed bynitrification (57% of total uptake),heterotrophic bacteria and fungi associatedwith detritus (29%), and epilithic algae(14%). Growth of algae was likely limited bylight rather than nutrients, and dissolvedO₂ revealed that the stream metabolism washeterotrophic overall (P:R = 0.2). Incubationsof detritus in darkened chambers showed thatuptake of ¹⁵N was mostly heterotrophic.Microbial N in detritus and algal N inepilithon appeared to reach isotopic steadystate with the dissolved ammonium, but theisotopic enrichment of the bulk detritus andepilithon did not approach that of ammonium,probably due to a large fraction of organic Nin the bulk samples that was not turning over. The actively cycling fraction of total N inorganic compartments was estimated from theisotopic enrichment, assuming uptake ofammonium but not nitrate, to be 23% forepilithon, 1% for fine benthic organic matter,5% for small woody debris, and 7% for leaves. These percentages agree with independentestimates of epilithic algal biomass, whichwere based on carbon:chlorophyll ratios in bulksamples and in algal fractions separated bydensity-gradient centrifugation in colloidalsilica, and of microbial N in the detritus,which were based on N released by chloroformfumigations.     

15NO2胁迫下三角梅不同器官的氮素吸收分配动态及代谢规律

近年来研究园林植物消减大气污染物的修复技术及其原理,理清氮氧化物污染对植物生理生态的影响机制,对城市生态环境保护和文明建设具有重要意义。以三角梅(Bougainvillea spectabilis Willd)小苗为研究材料,通过人工模拟熏气法,设计短时间高浓度¹⁵NO₂胁迫处理,以CK为对照,比较8.0μL/L ¹⁵NO₂处理和4.0μL/L ¹⁵NO₂处理对三角梅各器官¹⁵N的吸收量和各器官¹⁵N-氨基酸含量的影响,探究¹⁵NO₂胁迫下三角梅各器官内氮素的吸收分配动态及代谢规律研究。结果表明,¹⁵NO₂胁迫后显著提高了三角梅各器官¹⁵N含量,其中叶片是¹⁵N的主要积累器官。8.0μL/L ¹⁵NO₂处理下三角梅各器官¹⁵     

Nitrogen uptake and use of two contrasting maize hybrids differing in leaf senescence

In eastern Canada, the use of fertilizer N has been identified as the most energy-consuming component of maize (Zea mays L.) grain production. As the economic and environmental costs of excessive N fertilization rise, there is an increased emphasis on selection of hybrids with greater N use efficiency (NUE; defined as the ratio of the amount of ¹⁵N recovered in grain or stover dry matter to the amount of fertilizer ¹⁵N applied to the soil in this study). Using an ¹⁵N-labelling approach, a field study was conducted on a tile-drained Brandon loam soil (Typic Endoaquoll) on the Central Experimental Farm at Ottawa, Canada (45°22 N, 75°43 W) in 1993 and 1994. Fertilizer N uptake and partitioning within the plant in relation to dry matter changes were monitored during development of a current stay-green maize hybrid and an older early-senescing hybrid grown with three fertilizer N levels (0, 100, 200 kg N ha^-1). Dry matter, N concentration and¹⁵ N atom% enrichment of plant components were determined at five growth stages. The current stay-green hybrid, Pioneer 3902 had greater NUE than the old early-senescing hybrid, Pride 5, which was associated with 24% more dry matter production and 20% more N uptake during grain fill for Pioneer 3902. There was no indication of greater allocation of N to the grain in Pioneer 3902. Our data suggest that prolonged maintenance of green leaf area for photosynthate production during grain fill and the ability to take up available soil N later in grain filling are characteristics of maize hybrids with greater NUE.     

Nitrogen fixation in breeding lines of Phaseolus vulgaris L.

Nitrogen fixation in nine common bean (Phaseolus vulgaris L.) lines was estimated using the ¹⁵N isotope dilution method at two locations in two seasons. In the first season at one location no N₂ fixation was detected while in the second season up to 51 kg N ha^–1 were estimated. There were significant differences between lines and correlations between trials were significant for the amounts of N₂ fixed, but not for total shoot nitrogen. The plants that fixed the most nitrogen nodulated rapidly after germination. Differences in maximum nodule mass, but not specific nodule activity, were detected also.