接种丛枝菌根真菌对小麦根内氮转运蛋白基因表达的影响

通过盆栽试验,研究了在低氮(不施氮)和高氮(施氮0.2 g·kg~(-1))水平下接种不同种类丛枝菌根(AM)真菌[Funneliformis mosseae(BGC-NM03D)、Claroideoglomus etunicatum(BGC-NM01B)和Rhizophagus intraradices(BJ09)]对小麦生长、氮吸收及根内4个硝态氮转运蛋白(NRT)基因、1个辅助蛋白(NAR)基因和2个铵态氮转运蛋白(AMT)基因表达的影响。结果表明,3种AM真菌均能够侵染小麦根系,以R.intraradices菌根的侵染率最高;接种R.intraradices或C.etunicatum能够显著提高小麦的生物量或地上部氮吸收量;无论是高氮还是低氮处理,接种AM真菌后均显著下调了小麦根内NRT、NAR和AMT基因的表达水平,且不同AM真菌调控小麦根内氮转运蛋白基因表达的能力具有明显差异。     

不同生态型拟南芥耐铵毒害差异的生理机制

【目的】 利用拟南芥生态型群体研究拟南芥耐铵毒害的生理机制,为挖掘耐铵基因提供生理基础及理论指导。 【方法】 共收集了95份生态型拟南芥材料,采用水培实验方法,将拟南芥幼苗移栽后在正常培养液(2 mmol/L NO₃–-N处理)中培养8天,然后转移至含有1 mmol/L (NH₄)₂SO₄的营养液(2 mmol/L NH₄+-N处理)中培养8天,收获后,测定植株全氮量、地上部游离铵含量,以及谷氨酰胺合成酶 (GS) 活性;培养3天后取样,采用RT-PCR技术分析根部主要的铵态氮转运蛋白基因AMT1;1和AMT1;2的表达水平;拟南芥幼苗移栽后在正常培养液中培养8天,转移至丰度为5%的1 mmol/L (15NH₄)₂SO₄中培养,分别处理3 h、6 h和24 h取样,用于同位素分析。 【结果】 2 mmol/L铵态氮处理下拟南芥群体地上部的生长被显著抑制,并且大量游离铵离子累积于地上部,铵态氮下拟南芥群体体内铵含量是对照硝态氮下的1.5倍以上,其中Si-0生态型在铵态氮下铵含量为19.17 μmol/g, FW,是对照的20倍。在硝态氮培养条件下,内源铵的含量与拟南芥地上部生长呈显著负相关,铵态氮培养条件下,地上部生长与铵含量同样呈较高的负相关性,因此内源铵含量少的生态型拟南芥在铵态氮下亦耐铵,所以本研究以拟南芥群体组织内铵含量为主因子,筛选出耐铵拟南芥生态型Or-1、Ta-0,HSM和铵敏感拟南芥生态型Rak-2、Lpv-18、Hi-0,结果表明铵敏感生态型在硝态氮下铵含量是耐铵生态型的1.7倍至10倍。耐铵拟南芥生态型铵转运蛋白基因AMT1;1和AMT1;2的表达水平较铵敏感拟南芥高,植株全氮和地上部15N标记试验结果表明,耐铵拟南芥铵态氮吸收速率高于敏感型。并且耐铵拟南芥生态型在两种氮形态下其谷氨酰胺合成酶 (GS) 活性均显著高于铵敏感生态型,在硝态氮培养条件下GS活性是铵敏感生态型的1.1～1.8倍,在铵态氮培养条件下是1.2～1.6倍,说明耐铵拟南芥生态型的铵同化能力强于敏感型。 【结论】 耐铵生态型拟南芥是通过更高的谷氨酰胺合成酶 (GS) 活性将大量的游离铵同化以减少植株体内游离铵含量,从而减轻植株铵毒害;而不是通过减少铵态氮的吸收。      

Interaction of Different Wheat Genotypes and Nitrification Inhibitor 3,4-Dimethylpyrazole Phosphate Using 15N Isotope Tracing Techniques

To investigate the effect of applying ¹⁵N-labeled ammonium sulfate with or without a nitrification inhibitor 3,4-dimethylpyrazole phosphate (DMPP) on fertilizer use efficiency and crop productivity of different wheat genotypes, a field trial was conducted at the Nuclear Agricultural Department’s farm of Iran in 2013–2014. The treatments included five wheat genotypes with different 13 C isotope discrimination and three fertilizer treatments, an unfertilized control, ¹⁵N-labeled ammonium sulfate, and ¹⁵N-labeled ammonium sulfate with DMPP in three replications. Soil samples were taken after 2, 4, and 6 weeks after sowing and also at harvest time. Results from ¹⁵N experiment showed that DMPP delayed nitrification of ammonium for 42 days. Genotypes with lower discrimination index had greater uptake of ammonium ions which led to increase crop yield and nitrogen fertilizer use efficiency. The results also suggested that the use of DMPP may not be beneficial in some fast growing wheat genotypes.     

根系高效铵吸收系统是玉米获取氮素的重要补充机制

【目的】本研究旨在通过对植株根系铵吸收特征研究,揭示旱地玉米的氮素营养特征,研究结果为玉米补充氮素营养提供了一定的理论依据。 【方法】以玉米高产品种“郑单 958”为供试材料,采用水培试验模拟了玉米植株生长中的氮素营养环境,研究了玉米幼苗生长对不同氮素形态的反应;采用非损伤微测技术 (NMT),重点研究了不同供氮状况下玉米根系对 NH₄+ 的吸收特征,并与其吸收硝态氮的规律进行了比较;利用实时定量 PCR 技术,初步揭示了玉米根系中的铵吸收蛋白 (AMT) 基因对铵的响应特征。 【结果】单一供应铵态氮条件下,玉米地上部鲜重、全株干重及根系含氮量与纯硝态氮条件下相近,表明铵态氮也可作为玉米的有效氮源。非损伤微测研究结果表明,玉米幼苗根系铵吸收过程呈典型的高亲和吸收特征 (表观 Km 值约为 60 μmol/L),推测这一过程是由高亲和的转运体蛋白介导。氮饥饿预处理使根系的铵吸收速率 Vmax 和 Km 值分别降低了约 3 倍和 1 倍。这一现象与水稻等作物不同,暗示玉米的铵吸收过程可能不存在反馈抑制现象。另外,介质中硝态氮的存在对根系的铵吸收具有显著抑制作用 (抑制效果 > 20%);在供试微摩尔浓度范围内,根系对 NO₃– (100 μmol/L) 的吸收速率显著低于对相同浓度 NH₄+ 的吸收。进一步对主要在玉米根系中表达的铵吸收蛋白基因 ZmAMT1;1a 和 ZmAMT1;3 的定量 PCR 分析表明,上述基因在维持供铵状态下的表达量较缺氮处理均有显著提高,与铵吸收测定结果相符。 【结论】玉米根系中保留着高效铵吸收系统,在低硝态氮浓度下,该系统对铵态氮的高效吸收可作为其获取足够氮源的一个重要的机制。高硝态氮则抑制玉米根系对铵态氮的吸收,以避免氮素吸收利用系统在功能上的冗余。     

Interaction of 15N-labelled ammonium nitrate,urea and ammonium sulphate with soil N during growth of wheat (Triticum aestivum L.) under field conditions

The effects of ¹⁵N-labelled ammonium nitrate, urea and ammonium sulphate on yield and uptake of labelled and unlabelled N by wheat (Triticum aestivum L. cv. Mexi-Pak-65) were studied in a field experiment. The dry matter and N yields were significantly increased with fertilizer N application compared to those from unfertilized soil. The wheat crop used 64.0–74.8%, 61.5–64.7% and 61.7–63.4% of the N from ammonium nitrate, urea and ammonium sulphate, respectively. The fertilizer N uptake showed that ammonium nitrate was a more available source of N for wheat than urea and ammonium sulphate. The effective use of fertilizer N (ratio of fertilizer N in grain to fertilizer N in whole plant) was statistically similar for the three N fertilizers. The application of fertilizer N increased the uptake of unlabelled soil N by wheat, a result attributed to a positive added N interaction, which varied with the method of application of fertilizer N. Ammonium nitrate, urea and ammonium sulphate gave 59.3%, 42.8% and 26.3% more added N interaction, respectively, when applied by the broadcast/worked-in method than with band placement. A highly significant correlation between soil N and grain yield, dry matter and added N interaction showed that soil N was more important than fertilizer N in wheat production. A values were not significantly correlated with added N interaction (r=0.719). The observed added N interaction may have been the result of pool substitution, whereby added labelled fertilizer N stood proxy for unlabelled soil N.     

土壤微生物量氮对小麦各生育期氮素形态的调控

[目的]土壤中氮素的有效性很大程度上影响着作物对氮的吸收.明确各形态氮素对作物吸氮量的贡献,研究调控土壤氮素形态的因素,为培育氮素高效和作物高产的土壤提供理论依据.[方法]试验基于河南新乡的"国家潮土土壤肥力与肥料效益监测基地"长期定位试验,以不施肥 (CK)、施NPK化肥 (NPK) 和1.5倍NPK化肥并配施有机肥...     

Effects of 15N-labelled ammonium nitrate and urea on soil nitrogen during growth of wheat (Triticum aestivum L.) under field conditions

We studied the effects of ¹⁵N-labelled ammonium nitrate and urea on the yield and uptake of labelled and unlabelled N by wheat (Triticum aestivum L., cv. Mexi-Pak-65) in a field experiment. The dry matter and N yields were significantly increased with fertilizer N application compared to those from unfertilized soil. The wheat crop used 33.6–51.5 and 30.5–40.9% of the N from ammonium nitrate and urea, respectively. Splitting the fertilizer N application had a significant effect on the uptake of fertilizer N by the wheat. The fertilizer N uptake showed that ammonium nitrate was a more available source of N for wheat than urea. The effective use of fertilizer N (ratio of fertilizer N in grain to fertilizer N in whole plant) was statistically similar for the two N fertilizers. The application of fertilizer N increased the uptake of unlabelled soil N by wheat, a result attributed to a positive added N interaction, which varied according to the fertilizer N split; six split applications gave the highest added N interaction compared to a single application or two split applications for both fertilizers. Ammonium nitrate gave 90.5, 33.5, and 48.5% more added N interaction than urea with one, two, and six split N applications. A values were not significantly correlated with the added N interaction (r=0.557). The observed added N interaction may have been the result of pool substitution, whereby added labelled fertilizer N replaced unlabelled soil N.     

Glycine,nitrate, and ammonium uptake by classic and modern wheat varieties in a short-term microcosm study

Plants take up nitrogen principally in the form of nitrate and ammonium; however, evidence is growing that they can also use organic N in the form of amino acids. Selecting varieties that better use organic N could be important in maximizing productivity in organic and low-input systems because these varieties may access a wider pool of available nutrients. We tested amino acid-N uptake by wheat (Triticum aestivum L.) seedlings over 24 h over a range of soil glycine concentrations. Wheat was grown in 5 ml pipette tips for 10 days prior to labeling with ¹⁴C-labeled glycine. In a second experiment, uptake of amino acid-N relative to nitrate and ammonium was tested in three pre-1940 wheat varieties (Arco, Idaed, and Red Fife), three modern varieties (Alpowa, Madsen, and Zak), and one perennial wheat variety (unreleased). Glycine-N was detected in all shoots (with the exception of the lowest soil concentration) and increased with increasing soil concentration. There were few differences in uptake between individual varieties tested but seedlings of modern varieties were more efficient at capturing organic N than classic varieties. Glycine-N constituted between 3.9% and 8.1% of total N uptake over 24 h and constituted a significantly greater proportion of total N in perennial wheat than annual wheat varieties. These results show that there may be sufficient varietal differences in organic N uptake in wheat to warrant selection for this trait in breeding programs targeted to improving N use efficiency.     

Effects of a nitrification inhibitor on efficiency of nitrogen utilization by wheat and millet

Abstract

Preliminary soil incubation studies established that the nitrification inhibitor, Dicyandiamide (DCD), could maintain the ratio of NH.‐N to NO₃‐N at predetermined levels. When one part DCD was mixed with 10 parts of the ammonium fertilizer prior to incorporation with the soil, nitrification was inhibited for at least six weeks. In a greenhouse experiment, wheat was grown to maturity and millet to the flowering stage in pots containing nitrate and ammonium fertilizers treated with DCD. Soil analyses during the plant growth period indicated that ammonium oxidation in soil was effectively inhibited. Plants of both species exposed to ammonium only with DCD produced lower yields than those exposed to a mixture of nitrate and ammonium nitrogen with DCD. Plants supplied with nitrate‐only gave somewhat lower yields than the mixtures. The nitrate‐only treatments resulted in the lowest accumulation of reduced nitrogen compounds in shoots of both species. Magnesium uptake by millet and calcium and magnesium uptake by wheat were reduced as the proportion of ammonium in soil was increased.     

Utilization of Existing Technology to Evaluate Spring Wheat Growth and Nitrogen Nutrition in South Dakota

Abstract

Sensor‐based technologies for in‐season application of nitrogen (N) to winter wheat (Triticum aestivum L.) have been developed and are in use in the southern Great Plains. Questions arise about the suitability of this technology for spring wheat production in the northern Great Plains. A field experiment was established in Brookings, SD, to evaluate the GreenSeeker Hand Held optical sensor (NTech Industries, Ukiah, CA) for predicting in‐season N status on three spring wheat cultivars (Ingot, Oxen, and Walworth) across five N treatments. Nitrogen rates were 0, 34, 68, 102, and 136 kg N ha^?1 applied preplant as ammonium nitrate. Sensor readings and plant biomass samples were collected at Feekes 6 and Feekes 10 growth stages. The sensor measures reflectance in the red and near infrared (NIR) regions of the electromagnetic spectrum. A normalized difference vegetation index (NDVI) was calculated. The ability of the sensor readings to predict biomass, plant N concentration, and plant N uptake for each sampling date was determined. In general, biomass, plant N concentration, and N uptake increased with increasing N rate for both sampling dates. Readings collected at Feekes 6 and Feekes 10 showed a significant relationship with plant biomass, N concentration, and N uptake for all varieties. Plant N uptake and NDVI resulted in a higher regression coefficients compared to biomass and plant N concentration for all varieties. Results suggest that existing sensor‐based variable nitrogen technology developed for winter wheat could be utilized in the northern Great Plains for estimating in‐season N need for spring wheat.     

Wheat Grain Nitrogen Uptake,as Affected by Soil Total and Mineral Nitrogen,for the Determination of Optimum Nitrogen Fertilizer Rates for Wheat Production

Determination of appropriate nitrogen (N) fertilization for wheat (Triticum aestivum L.) production with respect to the available resources can result in the enhanced efficiency of agricultural systems and ecosystem health. Hence, a 3-year field experiment was conducted to determine (1) the effects of soil total N and soil mineral N (including nitrate, NO₃-N, and ammonium, NH₄-N) measured at seeding and postseeding for wet and dry soil samples at 0- to-30 cm and 0- to 60-cm depths on wheat grain N uptake and (2) the regression equations that can best explain the variation in wheat grain N uptake by N fertilizer and soil total and mineral N. Determination of wheat grain N uptake as affected by soil NO₃-N in areas with reasonable amounts of organic matter can also be used as a very useful tool for determination of appropriate N fertilization, which is of great agricultural and environmental implications.     

Induction of high affinity nitrate and ammonium uptake systems in wheat

Abstract

The ability of 7 day old wheat seedlings to take up nitrate or ammonium from hydroponic solution was measured. Seedlings were grown under fully aerated hydroponic conditions. The growth solution consisted of either 0.5 mM CaSO₄ alone or in combination with high nitrate (5 mM NO₃ ^‐ ), high ammonium (2 mM NH₄ ⁺) or modified 1/10 Hoaglands solution with nitrate N only (14 mM) or ammonium N only (2 mM). After washing the roots for one hour in CaSO₄, nitrate or ammonium uptake was measured with an ion selective electrode. Plants grown in high nitrate were unable to take up nitrate from a 0.1 mM external solution. Those grown in CaSO₄ were able to take up nitrate at the same external concentration (flux = 10.2 +/‐ 3.0 μmol nitrate/g dry wtlbh). The same result was seen for plants grown in high ammonium vs those grown in CaSO₄ (flux = 21.0 +/‐ 10.0 μmol/g dry wtlbh). Similar results were obtained when modified Hoagland's solution was substituted for the high N solutions. These data indicate that wheat roots possess both high and low affinity nitrate and ammonium uptake systems. The data further indicate that, for a given ion, the high and low affinity systems do not operate simultaneously under high N conditions. The high affinity system is switched off in the range of 1 mM for both ionic forms of N. Developmental studies show that the expression of the high affinity trait is reversible and may be induced (repressed) by conditioning for 24 h in low (high) N media. Plants grown in high N solutions showed efflux of the ion under assay conditions. Neither ion interfered with the induction/repression of the high affinity trait for the other under the conditions used in this study.     

Effect of sewage sludge and ammonium nitrate on wheat yield and soil profile inorganic nitrogen accumulation 1

The beneficial effect of sewage sludge in crop production has been demonstrated, but there is concern regarding its contribution to nitrate (NO₃) leaching. The objectives of this study were to compare nitrogen (N) rates of sewage sludge and ammonium nitrate (NH₄NO₃) on soil profile (0–180 cm), inorganic N [ammonium nitrate (NH₄‐N) and nitrate nitrogen (NO₃‐N)] accumulation, yield, and N uptake in winter wheat (Triticum aestivum L.). One field experiment was established in 1993 that evaluated six N rates (0 to 540 kg·ha^‐1·yr^‐1) as dry anaerobically digested sewage sludge and ammonium nitrate. Lime application in 1993 (4.48 Mg ha^‐1) with 540 kg N ha^‐1·yr^‐1 was also evaluated. A laboratory incubation study was included to simulate N mineralization from sewage sludge applied at rates of 45, 180, and 540 kg N ha^‐1·yr^‐1. Treatments did not affect surface soil (0–30 cm) pH, organic carbon (C), and total N following the first (1994) and second (1995) harvest. Soil profile inorganic N accumulation increased when ≥270 kg N ha^‐1 was applied as ammonium nitrate. Less soil profile inorganic N accumulation was detected when lime was applied. In general, wheat yields and N uptake increased linearly with applied N as sewage sludge, while wheat yields and N uptake peaked at 270 kg N ha^‐1 when N was applied as ammonium nitrate. Lime did not affect yields or N uptake. Fertilizer N immobilization was expected to be high at this site where wheat was produced for the first time in over 10 years (previously in native bermudagrass). Estimated N use efficiency using sewage sludge in grain production was 20% (average of two harvests) compared to ammonium nitrate. Estimated plant N recovery was 17% for sewage sludge and 27% for ammonium nitrate.     

植物吸收铵态氮的分子生物学基础

植物对铵离子的吸收和铵离子在细胞间的转运是铵转运蛋白介导的需能主动运输过程。植物铵转运蛋白位于细胞膜上,含有101～1个跨膜域,分子量约为48.kD。研究表明,植物体内的铵转运蛋白由小基因家族成员编码,在表达特性上不同成员具有时空特异性。植物体内铵转运蛋白在功能、生化特性和转录调节水平上存在差异。在不同氮素水平下,铵转运蛋白基因通过转录和翻译调控,对于保持植株的适宜氮素供应以及氮胁迫条件下维持植物细胞中氮素的内稳态具有重要作用。     

Organic and Inorganic Amendments Affect Soil Concentration and Accumulation of Cadmium and Lead in Wheat in Calcareous Alkaline Soils

Irrigation with untreated effluent in periurban agriculture could result in accumulation and bioconcentrations of cadmium (Cd) and lead (Pb). Different amendments were used to investigate their effect on availability, concentration, and uptake of metals by wheat in texturally different soils. Crop was irrigated with water containing Cd and Pb at 20 mg L^?1, thereby adding 260 mg pot^?1 of each metal. Amendments included calcium carbonate at 6 or 12%, gypsum at 50 or 100% of the soil gypsum requirement, farm manure at 7.50 or 15.00 g kg^?1 soil, and a control. Amendments decreased ammonium bicarbonate diethylenetriaminepentaacetic acid (AB-DTPA)–extractable Cd and Pb concentrations and uptake by wheat. Dry matter, concentration, uptake, and extractability of Cd and Pb were greater in sandy loam soil compared with those in sandy clay loam soil irrespective of amendments. Sequential extraction showed that more metals were extracted from the control in all fractions and that predominantly metals were found in the carbonate fraction.     

低pH影响大豆和菜豆对氮素形态的响应

通过室内水培试验，模拟了植株生长的缺氮、纯铵、纯硝3个不同氮素营养环境，研究了两种豆科作物（大豆和菜豆）幼苗生长对氮素及氮素形态的响应，同时对溶液pH进行了实时监测；在单一供铵的基础上，研究了在不同pH（pH 4.5，pH 6.5）下两种豆科作物对铵态氮的响应特征，并利用实时定量PCR技术，探究了植株体内的铵转运蛋白（AMT）基因对pH的响应规律；通过构建系统进化树、关键位点序列比对，对不同物种的AMT蛋白进行了生物信息学分析。研究结果表明：与缺氮处理相比，纯硝处理显著增加了大豆和菜豆的生物量，尤其是根系生物量，而纯铵处理下无显著变化；但是纯铵与纯硝处理下植株体内的氮积累量基本相同，且发现纯铵处理下溶液pH显著下降。通过控制纯铵处理的溶液pH，我们发现相比于pH 6.5，pH 4.5显著降低了两种豆科作物的生物量。进一步研究了大豆体内的主要铵转运蛋白基因的表达情况，结果显示相比于pH 6.5，pH 4.5显著降低了大多数铵转运蛋白基因的表达量；生物信息学分析表明，大豆和菜豆的AMT在亲缘关系上高度相近，而与喜铵作物水稻的亲缘关系较远。本研究表明大豆和菜豆对铵态氮的吸收会导致根际环境酸化，从而限制植株生长，这为田间提高豆科作物的氮素营养提供了一个视角。     

Nmin−Gehalt im Boden,mineralische N-Düngung und N-Entzug von Winterweizen im Internationalen Organischen Stickstoffdauerdüngungsversuch (IOSDV) Berlin-Dahlem

N_mim content in the soil, N-fertilization and N uptake of winter wheat in the international organic nitrogen long-term fertilization experiment (IOSDV) Berlin-Dahlem During the 9th and 10th year of the long-term IOSDV field experiment micro plots were put in three treatments. Labelled¹⁵ N (160 resp. 110 kg/ha N as ammonium sulfate) was fertilized to winter wheat subdivided into three portions. N_min in soil was determined five times during the season, plant biomass was harvested at different growth stages and N uptake was calculated. Using the¹⁵ N-technique permitted a discrimination between fertilizer-N and soil-N. Preferential uptake of fertilizer-N by the wheat crop but also immobilisation in soil were observed until June. Subsequently the immobilized N was remineralized and assimilated by wheat. But the native N_min of soil was minimaly utilized during the initial growth of wheat. Therefore the absolute amount of soluble N temporarily increased caused by a mineralisation of the organic matter.     

Localized application of sewage sludge improved plant nitrogen and phosphorus uptake by rhizobox‐grown spring wheat

Sewage sludge (SS) can be used as an alternative fertilizer in agriculture. It is normally broadcasted and plowed into soil, but it is not clear if it has a potential as a placement fertilizer. A rhizobox experiment was conducted to investigate the placement effect of SS and mineral nitrogen (N) fertilizer on shoot and root growth as well as nutrient uptake of spring wheat (Triticum aestivum L.). The treatments included localized SS, mixed SS, localized SS and ammonium, localized ammonium, and a control without addition of SS and ammonium to examine the effect of SS placement and, further, if ammonium co‐localization would enhance the placement effect. The results show that SS fertilization improved soil N and P availability, which significantly increased plant N and P uptake and enhanced shoot growth, while root length was significantly reduced compared to the control. Localized SS increased root proliferation in the placement region, resulting in enhanced uptake of P from the SS patch compared to homogenous application. However, co‐localized application of ammonium with SS significantly depressed plant shoot and root growth. Localized ammonium markedly restricted root proliferation in the placement region and reduced soil pH in both bulk soil and placement region, contributing to decreased nutrient uptake and plant growth.     

施氮量对土壤无机氮分布和微生物量氮含量及小麦产量的影响

在高肥力土壤条件下,研究了施氮量对土壤无机氮分布和微生物量氮含量及小麦产量的影响。结果表明,小麦生长期间,施氮处理0100.cm土层硝态氮积累量显著大于不施氮处理;当施氮量大于150.kg/hm2时,随施氮量增加,0100.cm土层硝态氮积累量显著增加;随小麦生育进程推进,施氮处理上层土壤硝态氮下移趋势明显,至小麦成熟时,施氮1952～85.kg/hm2处理60100.cm土层硝态氮含量显著大于其它处理。小麦生长期间,0100.cm土层铵态氮积累量较为稳定,施氮处理间亦无显著差异。与不施氮肥相比,施氮提高小麦生长期间040.cm土层土壤微生物量氮含量;当施氮量小于240.kg/hm2时,随施氮量增加,土壤微生物量氮含量增加。小麦的氮肥利用率随施氮量增加而降低;施氮1051～95.kg/hm2,收获时小麦植株吸氮量、生物产量、子粒产量和子粒蛋白质含量提高;而施氮量大于240.kg/hm2时,小麦生育后期的氮素积累量降低,收获时植株吸氮量、生物产量和子粒蛋白质含量降低。说明本试验条件下,施氮1051～50.kg/hm2可满足当季小麦氮素吸收利用,获得较高的子粒产量和蛋白质含量。继续增加施氮量,土壤微生物量氮含量增加,但土壤中残留大量硝态氮,易淋溶损失。