Nitrogen fixation by nodulated soybean under tropical field conditions estimated by the 15N isotope dilution technique

The contribution of biological N₂ fixation to the N nutrition of nodulated soybean was estimated using the ¹⁵N isotope dilution technique and a non-nodulating soybean isoline as a non-fixing control plant. The plants were grown in the field in concrete cylinders (60 cm dia) and harvested at seven stages of plant growth. Labelled N was added to the soil either as labelled organic matter before planting or in seven small additions (2kg N ha^?1) of (NH₄)₂SO₄ during the growing period.There was good agreement between isotope dilution estimates of nitrogen fixation for the two labelling methods. Acetylene reduction assays on intact root systems greatly underestimated N₂ fixing activity. The difference in total N between nodulated and non-nodulated plants generally gave higher estimates compared with the isotope technique. The data indicate that this was because nodulated plants recovered more N from the soil than the non-nodulated plants. After 92 days of growth, the soybean derived approximately 250kg N ha^?1 from biological N₂ fixation.     

Estimating N2-fixation in the field using 15N-labelled fertilizer: Some problems and solutions

The ¹⁵N-labelled fertilizer dilution technique provides a method of obtaining estimates of biological N₂-fixation in the field over the growing season. Field estimates of fixation obtained using peas, french beans, field beans and clover depended on the non-fixing control used. Differences in the N uptake patterns of the legume and control combinations, together with a decrease in the enrichment of plant available soil N with time, were major factors causing this dependency. A simple model of plant N accumulation at decreasing soil enrichment is presented, which explains these errors and allows a more rational choice of non-fixing control. The use of gypsum pelleted ¹⁵N fertilizer, or any other treatment which leads to a more stable soil enrichment, reduces errors caused by mismatched N uptake patterns in the two crops.     

Nitrous oxide and methane emissions from a surface drip‐irrigated system combined with fertilizer management

Drip‐fertigated systems have variable distributions of water and nutrients in the soil, which influence soil microbial activity. Because there is a lack of data on greenhouse gas (GHG) fluxes for these systems, a field experiment comparing drip irrigation systems (fertigated and non‐fertigated) was carried out in a melon crop. For the fertigated treatment, nitrogen (N) as NH₄NO₃ was dissolved in irrigation water and split into six applications (Fertigation treatment). In the non‐fertigated soil (ANS treatment), granular NH₄NO₃ was incorporated homogeneously into the upper part of soil surface at planting. A control treatment without N fertilizer was also included. In order to evaluate the pattern of nitrous oxide (N₂O) and methane (CH₄), measurements were made at six different distances from the irrigation distributor point (dripper). An additional field experiment with ¹⁵N‐labelled N fertilizer was carried out in parallel, with the aim of evaluating the contribution of nitrification and denitrification to the total N₂O flux. Two different sources of ¹⁵N were applied: ¹⁵NH₄NO₃ (20 at% excess ¹⁵N) (¹⁵NH₄⁺ treatment, TR1) and NH₄¹⁵NO₃ (20 at% excess¹⁵N) (¹⁵NO₃^? treatment, TR2). Results indicated that both treatments (ANS and Fertigation) had small emission fluxes of N₂O (< 0.1% of N applied). However, Fertigation produced larger emissions (175.3 g N₂O‐N ha^?1) than ANS (90.1 g N₂O N ha^?1), with the pattern of N₂O emission being strongly influenced by nitrification in both systems. Denitrification also contributed to emissions of ¹⁵N₂O but mainly on the day after fertilizer application in the Fertigation treatment. Methane fluxes were also affected by N fertilizer, with a decrease in the sink effect for CH₄ when NH₄⁺ was present in the soil.     

Influence of different agricultural practices (type of crop, form of N-fertilizer) on soil nitrous oxide emissions

 N₂O emissions were periodically measured using the static chamber method over a 1-year period in a cultivated field subjected to different agricultural practices including the type of N fertilizer (NH₄NO₃, (NH₄)₂SO₄, CO(NH₂)₂ or KNO₃ and the type of crop (rapeseed and winter wheat). N₂O emissions exhibited the same seasonal pattern whatever the treatment, with emissions between 1.5 and 15 g N ha^–1 day^–1 during the autumn, 16–56 g N ha^–1 day^–1 in winter after a lengthy period of freezing, 0.5–70 g N ha^–1 day^–1 during the spring and lower emissions during the summer. The type of crop had little impact on the level of N₂O emission. These emissions were a little higher under wheat during the autumn in relation to an higher soil NO₃ ^– content, but the level of emissions was similar over a 7-month period (2163 and 2093 g N ha^–1 for rape and wheat, respectively). The form of N fertilizer affected N₂O emissions during the month following fertilizer application, with higher emissions in the case of NH₄NO₃ and (NH₄)₂SO₄, and a different temporal pattern of emissions after CO(NH₂)₂ application. The proportion of applied N lost as N₂O varied from 0.42% to 0.55% with the form of N applied, suggesting that controlling this agricultural factor would not be an efficient way of limiting N₂O emissions under certain climatic and pedological situations. Received: 1 December 1997     

Acetylene and N-serve effects upon N2O emissions from NH4+ and NO3− treated soils under aerobic and anaerobic conditions

N₂O emissions from soils treated with NH₄⁺-N under aerobic conditions in the laboratory were 3- to 4-fold higher than those from controls (no extra N added) or when NO₃^?-N was added. Although the emission of N₂O-N in these field and laboratory experiments represented only 0.1–0.8% of the applied fertilizer NH₄⁺-N and are therefore not significant from an agronomic standpoint, these studies have conclusively demonstrated that the oxidation of applied ammoniacal fertilizers (nitrification) could contribute significantly to the stratospheric N₂O pool.Like N-serve, acetylene was shown to be a potent inhibitor of nitrification as it stopped the oxidation of NH₄⁺-N to (NO₃⁺-N + NO₂^?)-N and hence reduced the evolution of N₂O from nitrification within 60 min after its addition.Although high amounts of NO₃^?-N were present, the rate of denitrification was very low from soils with moisture up to 60% saturation. The further increase in the degree of saturation resulted in several-fold increase of denitrification which eventually became the predominant mechanism of gaseous N losses under anaerobic conditions.     

Evidence that fungi can oxidize NH4+ to NO3− in a grassland soil

The contribution of bacteria and fungi to NH₄⁺ and organic N (N_org) oxidation was determined in a grassland soil (pH 6.3) by using the general bacterial inhibitor streptomycin or the fungal inhibitor cycloheximide in a laboratory incubation study at 20°C. Each inhibitor was applied at a rate of 3 mg g^?1 oven‐dry soil. The size and enrichment of the mineral N pools from differentially (NH₄¹⁵NO₃ and ¹⁵NH₄NO₃) and doubly labelled (¹⁵NH₄¹⁵NO₃) NH₄NO₃ were measured at 3, 6, 12, 24, 48, 72, 96 and 120 hours after N addition. Labelled N was applied to each treatment, to supply NH₄⁺‐N and NO₃^?‐N at 3.15 μmol N g^?1 oven‐dry soil. The N treatments were enriched to 60 atom % excess in ¹⁵N and acetate was added at 100 μmol C g^?1 oven‐dry soil, to provide a readily available carbon source. The oxidation rates of NH₄⁺ and N_org were analysed separately for each inhibitor treatment with a ¹⁵N tracing model. In the absence of inhibitors, the rates of NH₄⁺ oxidation and organic N oxidation were 0.0045 μmol N g^?1 hour^?1 and 0.0023 μmol N g^?1 hour^?1, respectively. Streptomycin had no effect on nitrification but cycloheximide inhibited the oxidation of NH₄⁺ by 89% and the oxidation of organic N by more than 30%. The current study provides evidence to suggest that nitrification in grassland soil is carried out by fungi and that they can simultaneously oxidize NH₄⁺ and organic N.     

Effect of phosphorus fertilizer application on the performance of maize/soybean intercrop in the southern Guinea savanna of Nigeria

Field experiments were conducted at the Teaching and Research Farm, Ladoke Akintola University of Technology, Ogbomoso, Nigeria in 2007 and 2008 to determine the effects of phosphorus fertilizer application on performance of intercropped maize and soybean. The experiments, arranged as a split plot in a randomized complete block design, replicated four times. A cropping system with sole maize, sole soybean and maize/soybean intercrop formed the main plot treatments while P rates with 0, 15 and 30 kg P₂O₅ ha^?1 were the subplot treatments. For both years, neither P fertilizer application nor cropping systems had a significant effect on maize grain yield. However, soybean grain yield was significantly higher (92.3% in 2007 and 44.5% in 2008) under sole cropping than under maize/soybean intercropping. On average, N fixed by soybean increased with the increase in P rate (from 51.8% without P to 60.5% with 30 P), but there was no significant difference in N fixed by sole soybean and soybean/maize intercrop. However, the interaction effect on N fixed between cropping systems and P rates was significant (P ≤ 0.05). N, P and K contents in maize grain were significantly higher (>100%) in intercropped maize than in sole maize. The cropping systems had no significant effect on post-harvest soil chemical characteristics. The land equivalent ratio was 1.52 in 2007 and 1.78 in 2008. The result shows that in utilizing legumes for N enrichment, the alleviation of P deficiency can enhance N₂-fixation by legumes. Furthermore, P replenishment in a maize/soybean intercrop may improve maize grain quality even though yield is not increased.     

Nitrogen fertilizers promote denitrification

A laboratory study was conducted to compare the effects of different N fertilizers on emission of N₂ and N₂O during denitrification of NO₃ ^– in waterlogged soil. Field-moist samples of Drummer silty clay loam soil (fine-silty, mixed, mesic Typic Haplaquoll) were incubated under aerobic conditions for 0, 2, 4, 7, 14, 21, or 42 days with or without addition of unlabelled (NH₄)₂SO₄, urea, NH₄H₂PO₄, (NH₄)₂HPO₄, NH₄NO₃ (200 or 1000 mg N kg^–1 soil), or liquid anhydrous NH₃ (1000 mg N kg^–1 soil). The incubated soil samples were then treated with ¹⁵N-labelled KNO₃ (250 mg N kg^–1 soil, 73.7 atom% ¹⁵N), and incubation was carried out under waterlogged conditions for 5 days, followed by collection of atmospheric samples for ¹⁵N analyses to determine labelled N₂ and N₂O. Compared to samples incubated without addition of unlabelled N, all of the fertilizers promoted denitrification of ¹⁵NO₃ ^–. Emission of labelled N₂ and N₂O decreased in the order: Anhydrous NH₃>urea<$>\gg<$> (NH₄)₂HPO₄>(NH₄)₂SO₄≃NH₄NO₃≃NH₄H₂PO₄. The highest emissions observed with anhydrous NH₃ or urea coincided with the presence of NO₂ ^–, and ¹⁵N analyses indicated that these emissions originated from NO₂ ^– rather than NO₃ ^–. Emissions of labelled N₂ and N₂O were significantly correlated with fertilizer effects on soil pH and water-soluble organic C. Received: 17 January 1996     

Immobilization of 15N in forest litter studied by 15N CPMAS NMR spectroscopy

Solutions labelled with ¹⁵N were applied as (¹⁵NH₄)₂SO₄ or K¹⁵NO₃ to isolated microplots in the floor of mountain beech forest (Nothofagus solandri var. cliffortioides) and incubated for 135 days under field conditions of moisture and temperature. Solid state ¹⁵N CPMAS NMR spectra of the forest litter layer showed that more than 80% of the total signal intensity was attributable to the secondary amide-peptide peak. The degree of ¹⁵N enrichment or form of N did not alter the relative intensity of signals attributable to ¹⁵N in peptides, nucleic acids and aliphatic amine groups (amino sugars and free NH₂ on amino acids). Combinations of ¹³C and ¹⁵N-NMR spectra, edited by a process that exploited differences in proton spin properties between distinct categories of organic matter, indicated incorporation of ¹⁵N in humified organic matter rather than partly degraded plant material. This application demonstrated that solid state ¹⁵N CPMAS NMR has potential for use in studies of N immobilization under field conditions and with materials containing little N and small ¹⁵N enrichment.     

Free-living nitrogen-fixing bacteria in temperate cropping systems: Influence of nitrogen source

Sustainable cropping systems rely on a minimum of external inputs. In these systems N is largely acquired in animal manures and leguminous green manures. Little is known of how these organic forms of N fertilizer influence the presence and activity of free-living N₂-fixing bacteria. High concentrations of inorganic N in soil inhibit N₂-fixation in cyanobacteria and Azotobacter spp. It is likely that manure and fertilizer applications would result in concentrations of inorganic N capable of inhibiting N₂ fixation and, ultimately, the presence of these organisms. We investigated the effect of synthetic and organic N fertilizer sources on the populations and N₂-fixation potential of free-living N₂-fixing bacteria in the Farming Systems Trial at the Rodale Research Institute. Field plots received the following N treatments prior to corn (Zea mays L.) production: (1) Legume rotations and green manures supplying about 165 kg N ha^-1; (2) beef cattle manure applied at a rate of 220 kg N ha^-1 (plus 60 kg N ha^-1 from 1994 hay plow-down); or (3) fertilizer N (urea and NH₄NO₃) applied at a rate of 145 kg N ha^-1. Soil samples were collected at two depths from corn plots four times during the growing season, and analyzed for soil moisture, soil pH, numbers of N₂-fixing cyanobacteria and Azotobacter spp., extractable NH _inf4 ^sup+ and NO _inf3 ^sup- , and potentially mineralizable N. Soil samples collected in mid-July were analyzed for nitrogenase activity (by C₂H₂ reduction) and total C and N. Populations of Azotobacter spp. and cyanobacteria were influenced only slightly by treatment; however, cyanobacteria species composition was notably influenced by treatment. Nitrogenase activity in surface soils was greatest in legume-N plots and in subsurface plots levels were greatest in fertilizer-N plots. Populations and activity of free-living N-fixing bacteria appeared to be somewhat reduced in all plots as a result of low soil pH levels and high concentrations of inorganic N across all treatments. Annual applications of N to all plots resulted in high levels of potentially mineralizable N that in turn may have reduced non-symbiotic N₂-fixation in all plots.     

Denitrification in grass swards is increased under elevated atmospheric CO2

Emissions of N₂O and N₂ were measured from Lolium perenne L. swards under ambient (36 Pa) and elevated (60 Pa) atmospheric CO₂ at the Swiss free air carbon dioxide enrichment experiment following application of 11.2 g N m⁻² as ¹⁵NH₄¹⁵NO₃ or ¹⁴NH₄¹⁵NO₃ (1 at.% excess ¹⁵N). Total denitrification (N₂O+N₂) was increased under elevated pCO₂ with emissions of 6.2 and 19.5 mg ¹⁵N m⁻² measured over 22 d from ambient and elevated pCO₂ swards, respectively, supporting the hypothesis that increased belowground C allocation under elevated pCO₂ provides the energy for denitrification. Nitrification was the predominant N₂O producing process under ambient pCO₂ whereas denitrification was predominant under elevated pCO₂. The N₂-to-N₂O ratio was often higher under elevated pCO₂ suggesting that previous estimates of gaseous N losses based only on N₂O emissions have greatly underestimated the loss of N by denitrification.     

Physiological aspects of N2-fixation by a Spirillum from Digitaria roots

Studies of the physiology of the Spirillum lipoferum recognized as the major organism responsible for N₂-fixation in the roots of Digitaria decumbens cv transvala were performed in order to improve the methods of culture and help to explain the physiology of this N₂-fixing grass bacterial association.Methods for isolation, purification and N₂-fixation assays are described. Acetylene concentrations used for N₂-ase activity measurements should be at least 12%. the Vmax of cultures in the log phase being at a pC₂H₂ of 0.12 atm and the apparent K_m 0.022 atm. Optimal temperatures for N₂-dependent growth are between 32 and 40°C. and little N₂-fixation is observed below 24°C. At 42°C the N₂-ase is inactivated. When cultures grown at 28 or 36°C are transferred to lower temperatures nitrogenase activity declines rapidly. One hour after transfer to 17°C activity is about half that before transfer and is maintained at this level for at least 8 h. After transfer to 10°C activity ceases after 1 h. Growth is very pH dependent, optimal growth on N₂ occurring only between pH 6.8 and 7.8. Nitrogen fixation below pH 5.5 and above 8.0 is less than one-quarter of the optimal. No N₂-fixation occurs in the absence of O₂ and maximal N₂-dependent growth is reached at 1.5% O₂ in the gas mixture bubbled through liquid cultures.In contrast to previous reports, several sugars including glucose can be used by the Spirillum for N₂-fixation, but only when small amounts of starter nitrogen or organic acids are added to the medium. Efficiencies of N₂-fixation on malate and glucose are similar and about 60% of that of cells incorporating NH⁺₄-N. Efficiency of NO^-₃ incorporation is 74% of that of NH⁺₄-N grown cultures. High observed efficiencies (52 mg N₂ fixed g^?1 malate or glucose) are attributed to carbon limited growth at optimum or O₂ limited conditions, both facilitated by slow diffusion rates through the semi-solid agar medium used.     

Heterotrophic N2-fixation in arid soil crusts

The cryptogamic soil crusts of the Great Basin Artemisia, Ceratoides, and Atriplex plant communities contain a significant heterotrophic N₂-fixing microbial population in addition to the predominating filamentous cyanobacteria. The bacterial association with the cyanobacteria exhibits a phycosphere-like effect. Heterotrophically fixed N gains reached 17.5 μg N· g^?1 of soil (23.1% increase above the initial soil N content) and 45.9 μg N·g^?1 of soil (57.4% increase) after 3 and 5 weeks, respectively. (NH₄)₂SO₄ and native plant material amendments to soil resulted in a 41–100% reduction in N₂-fixation. The potential input of N to soil crusts may be reduced in the presence of shrub-produced allelochemic agents and by concurrent denitrification.     

脲酶抑制剂/硝化抑制剂对土壤中尿素氮转化及形态分布的影响

运用^15N尿素示踪技术,以壤质草甸棕壤和春小分别作供试土壤和作物进行盆栽试验,结果表明,与单^15N尿素或^15N尿素＋氢素＋氢醌（HQ）相比,配施双氰胺（DCD）尤其与HQ组合可使土壤保持较高的^15N回收率,其中有^15N占相当大的比例,在小麦孕穗期前,上述两处理可有效地保持尿素解后土壤中NH^ 4 -^15N含量,并显著降低（NO^ 3 NO^-2)-^15N的富集;促进肥料^15N固持－矿化的周转,HQ与DCD配合施用对尿素施用后土壤中残留^15N量及有机^15N的再矿化和NH^ 4-^15N含量具有一定的协同作用。     

Effect of Nitrogen Fertilizer Forms on Growth,Photosynthesis, and Yield of Rice Under Cadmium Stress

ABSTRACT

A pot experiment was conducted to study the influence of four nitrogen (N) fertilizer forms [Urea; calcium nitrate, Ca(NO₃)₂; ammonium sulfate, (NH₄)₂SO₄; and organic N] on growth, photosynthesis, and yield of rice under two cadmium (Cd) levels (0 and 100 mg Cd kg^?1 soil). Cadmium addition significantly reduced photosynthetic rate, and the reduction varied with N fertilizer form, with ammonium (NH₄ ⁺)-N and urea treated plants having more reduction. Nitrogen form had a distinct effect on SPAD value, and the effect was also dependent on Cd level and growth stage. Cadmium-stress significantly reduced flag leaf area, but for the second leaf, only the plants supplied with organic N showed the reduction. There was a significant difference in plant height among four N forms, with NH₄ ⁺- and nitrate (NO₃ ^?)-treated plants having the highest and lowest height, respectively. Cadmium stress caused significant reduction in grains per panicle and total plant weight, and the reduction varied with N form, with organic N treatment showing more reduction. There were significant differences among N forms in N and Cd concentrations of the plants subjected to Cd stress, with NH₄ ⁺-N treated plants having highest N and lowest Cd concentrations and NO₃ ^?-treated plants having lowest N and highest Cd uptake. The results showed that the inhibition of Cd stress on growth and yield formation of rice is closely related to N fertilizer form.     

Matrix Based Fertilizers Reduce Nitrogen and Phosphorus Leaching in Greenhouse Column Studies

We tested the efficacy of matrix based fertilizer formulations (MBF) that reduce NH₄, total phosphorus (TP), total reactive phosphorus (TRP) and dissolved reactive phosphorus (DRP) in leachate. The MBF formulations cover a range of inorganic N and P in compounds that are relatively loosely bound (MBF1) to more moderately bound (MBF2) and more tightly bound compounds (MBF3) mixed with Al(SO₄)₃ H₂O and/or Fe₂(SO₄)₃ and with the high ionic exchange compounds starch, chitosan and lignin. Glomus interadicies, a species of arbuscular mycorrhizal fungal spores that will form mycorrhizae in high nutrient environments, was added to the MBF formulations to increase plant nutrient uptake. When N and P are released from the inorganic chemicals containing N and P the matrix based fertilizers likely bind these nutrients to the Al(SO₄)₃ H₂O and/or Fe₂(SO₄)₃ starch–chitosan–lignin matrix. We tested the efficacy of the MBFs to reduce N and P leaching compared to Osmocote^® 14-14-14, a slow release fertilizer (SRF) in sand filled columns in a greenhouse study. SRF with and without Al and Fe leached 78–84% more NH₄, 58–78% more TP, 20–30% more TRP and 61–77% more than MBF formulations 1, 2, and 3 in a total of 2.0 liters of leachate after 71 days. The concentration and amount of NO₃ leached among SRF and MBF formulations 1 and 2 did not differ. The SRF treatment leached 34% less NO₃, than MBF3. Total plant weight did not differ among fertilizer treatments. Arbuscular mycorrhizal infection did not differ among plants receiving SRF and MBF formulations 1, 2 and 3. Although further greenhouse and field testing are called for, results of this initial investigation warrant further investigation of MBFs.     

Nitrification and Denitrification Estimates in a Louisiana Swamp Forest Soil as Assessed by 15N Isotope Dilution and Direct Gaseous Measurements

The transformations of applied (100 kg N ha^-1)¹⁵ N labelled NO₃ and NH₄ in Mississippi River deltaic plain swamp forest soil which receives agriculture run-off from adjacent sugarcane fields were determined. Using an isotopic dilution technique, the rates of NO³ production (nitrification) and reduction in the ¹⁵NO₃ treated soil-water-columns were approximately 240 and 2,320 g N ha^-1 d^-1, whereas NH₄ production (mineralization) and removal rates in the ¹⁵NH₄ treated soil-water-columns were 270 and 2160 g N ha^-1 d^-1, respectively. It was shown that if nitrification and NH₄ assimilation were the primary processes responsible for NH₄ removal, average NH₄ assimilation would be 145 g N ha-1 d^-1. Based on labelled N₂-emission, denitrification was 3 fold greater in the NO₃ treatment compared to the NH₄ treated soil water-columns with rates of 818 and 266 g N ha^-1 d^-1 respectively. Even though the rate was lower in the NH₄ treatment, results show that nitrification-denitrification of NH₄ is a significant process. Nitrogen losses determined by¹⁵ N₂ emissions were 20.4 and 6.4% and N₂O emissions were 0.10 and 0.03% of the applied NO₃-N and NH₄-N, respectively, over 32 days of incubation. Fertilizer loss through N₂O emission was only of minor significance compared to the fertilizer loss through N₂ evolution. Nitrous oxide fluxes from the control soil-water-columns averaged 9.4 g N ha^-1 d^-1. Addition of NO₃-N to the columns increased N₂O production 56% as compared to a 15% increase from the NH₄-N addition. Results show that this wetland soil has a large capacity to process inorganic nitrogen entering the system as a result of agriculture run-off.     

Evaluation of methods for nitrogen‐15 analysis of inorganic nitrogen in soil extracts: I. Steam‐distillation methods

Abstract

A study was conducted to evaluate conventional steam‐distillation techniques for N‐isotope analysis of inorganic forms of N in soil extracts. Extracts obtained with 2 M KCl from 10 diverse soils were treated with: (i) (¹⁵NH₄)₂SO₄ and KNO₃, (ii) (NH₄)₂SO₄ and K¹⁵NO₃, or (iii) KNO₃and Na¹⁵NO₂. Steam distillations were performed sequentially to determine NH₄ ⁺‐N and NO₃ ^‐‐N, and were also carried out to determine (NO₃ ^‐ + NO₂ ^‐)‐N or (NH₄ ⁺ + NO₃ ^‐ + NO₂ ^‐)‐N; a pretreatment with sulfamic acid was used to determine NO₃ ^‐‐N in the presence of NO₂ ^‐‐N. Recovery of added N ranged from 95 to 102%. Significant isotopic contamination was observed in sequential distillation of unlabeled NO₃ ^‐‐N following labeled NH₄ ⁺‐N; otherwise, analyses for ¹⁵N were usually within 1% of the values calculated by isotope‐dilution equations.     

Drought and nitrogen source effects on nitrogen nutrition,seed growth,and yield in soybean

Drought in soybean [Glycine max (L.) Merr.] decreases yield‐related processes and N₂ fixation is more sensitive to drought than are many other of these processes. Therefore, application of nitrogen (N) fertilizer may increase drought tolerance over those plants primarily dependent on N₂ fixation. In a field experiment, NH₄NO₃ applications (+N) to drought‐stressed soybean resulted in biomass and N accumulation rates similar to those rates for an irrigated treatment without N fertilizer (‐N). In contrast, biomass and N accumulation rates were decreased for the ‐N treatment. N fertilization increased seed growth rate and decreased seed fill duration for irrigated and drought treatments. In the drought treatment, N application increased seed number per unit area, which resulted in higher yields. In a greenhouse experiment, fertilization with either KN0₃ or NH₄C1 increased biomass and N accumulation rates during drought over those of plants dependent solely on N₂ fixation. It was concluded that application of N fertilizer to soybean increases drought tolerance because of the extreme sensitivity of N₂ fixation to drought.     

土壤水湿状况和肥料碳氮比对稻田肥料氮素转化的影响

本文应用¹⁵N示踪法,测定并探讨了土壤中三种水分状况及四种不同C/N值肥料对肥料氮素转化的影响,试验结果表明:土壤水分和肥料C/N值均对水稻产量有较大的影响,相比之下,土壤水分的影响似更大.水稻对肥料氮的吸收利用率,淹水栽植高于旱植,氮素固定在旱地条件下作用加强,淹水并有一定渗漏的土壤上肥料氮的损失最大,示踪结果说明从土壤渗漏液中淋失的氮素80%以上为土壤固有氮素,相对而言肥料氮的损失较低.试验还表明肥料中碳氮值与肥料氮的吸收利用率之间呈负相关,与肥料残留率呈正相关.此外,本试验还测定了土壤水湿状况和肥料碳氮值在土壤氮素转化中的作用,讨论了当土壤氮素矿化和固定作用相等时,有机肥的碳氮临界值及其实用意义.