光照强度和氮水平对白三叶幼苗生长与光合生理特性的影响

采用植物生长箱溶液培养方式,对白三叶幼苗进行了不同光强(2个水平)和氮浓度(5个水平)处理,探讨其生长、生物量和光合生理特征对生境变化的响应.结果表明:两种光强下白三叶幼苗茎和叶生物量随氮素浓度呈先升高后降低,而根系生物量和根冠比则随氮素浓度增高而降低.光照强度降低使白三叶幼苗根、茎、叶和整株生物量分别降低67.8%、29.9%、42.5%和45.2%;低光处理使幼苗的根冠比显著下降,而比叶面积(SLA)明显提高.幼苗根系体积随氮素浓度增高而降低,高生长光强根系体积显著高于低生长光强下的白三叶.幼苗根系表面积、根系长度和根系直径随氮素浓度增加呈先增加后降低趋势,两种不同生长光强下幼苗根系长度和根系直径差异显著,而根系表面积差异不明显.白三叶叶片光合速率(Pn)随氮素浓度增加呈先增加后降低趋势,高生长光强白三叶Pn显著高于低生长光强下的白三叶.两种生长光强间叶片气孔导度(Gs),胞间CO2浓度(Ci)和蒸腾速率(Tr)无显著差异,但氮素浓度对叶片Gs、Ci和Tr均有显著影响.光、氮及其交互作用对白三叶幼苗生长发育产生了显著影响,光照不足和氮缺乏都将导致白三叶幼苗生长减弱,但幼苗对这些不利环境具有较强的调节和适应能力.     

棉花花铃期短期干旱下氮素对干物质及氮素累积分配的影响

通过盆栽试验进行水分(正常灌水和干旱后复水)和施氮处理(0、240、480kgN·hm-2),研究花铃期短期干旱再复水后氮素对棉花各器官干物质重、氮素累积与分配及产量与品质的影响.结果表明:花铃期土壤干旱显著降低了棉株各器官的干物质重与氮素累积量,而增大了棉株各器官的氮素含量,同时亦降低了棉株干物质与氮素在叶片中的分配指数,但提高了在根系的分配指数,从而增大了根冠比;增施氮肥可以提高干旱条件下棉株的干物质重与氮素累积量,但亦增大水分胁迫指数.复水对干旱处理棉株生长具有明显的补偿效应,尤其是根系的干物质重与氮素累积量显著高于相应正常灌水处理,且增施氮肥可以提高棉株的补偿效应.花铃期干旱结束时与复水后第10天,干旱处理棉株均以240kgN·hm-2水平下的生殖器官干物质重与分配指数最高,而根冠比最小,地上部与地下部生长最为协调,最终籽棉产量最高、纤维品质最优;而施氮不足(0kgN·hm-2)或过量(480kgN·hm-2)均不利于棉花产量的提高与纤维品质的改善.     

不同育苗方式对移栽后侧柏和白榆幼苗根系生长的影响

不同类型苗木,具有不同的根系结构特征,其根系结构也将影响林木的生长和恢复生态系统的稳定性。以侧柏和白榆为研究对象,对移栽18个月后的种基盘苗与营养钵苗根系的生长进行了调查。结果表明:侧柏种基盘苗的总根长和平均直径比营养钵苗分别增加了316.20 cm和0.05mm,白榆苗则分别增加了651.54 cm和0.88mm。侧柏和白榆种基盘苗的根系表面积比营养钵苗分别增加了40.05%和73.04%。侧柏种基盘苗的根系总体积与营养钵苗的差异不显著,而白榆种基盘苗的根系总体积则比营养钵苗增加了54.70%。侧柏和白榆营养钵苗的一级侧根数量大于种基盘苗,增幅分别为42.31%和30.65%。对于侧柏来说,营养钵苗的根尖总数比种基盘苗的增加324个,但白榆苗差异不显著。各种处理的幼苗总根长与根系表面积都有显著相关性,但与根体积不具有显著相关性。营养钵苗的根系平均直径和根尖数量具有相对独立性,而种基盘的根系平均直径与总根长以及根体积均表现为显著相关。种基盘苗能提高侧柏、白榆幼苗的根冠比,促进幼苗株高、地径和主根的生长。采用种基盘苗进行植被恢复,由于其具有较大的根表面积和根长度,林木便具有了较大的吸收水分和营养的能力,以及较高的固结表层土壤能力。     

氯盐胁迫下氮素对西瓜根系生长的调控作用

为揭示氯盐胁迫下氮素对西瓜根系的调节机制和提供西瓜氯毒害调控理论依据,以西瓜为供试作物,采用土培试验,研究不同施氮量(0,0.1,0.15,0.2,0.25 g/kg)对氯盐胁迫下西瓜根系的影响,并应用主成分分析法对各施氮量下根系生长情况进行综合评价。结果表明,(1)与不施氮相比,施氮0.15 g/kg处理可使西瓜根系生物量、干物质累积量、脯氨酸含量、可溶性糖含量、根系活力分别显著提高58.83%、20.83%、98.33%、70.37%和29.44%,丙二醛含量显著降低40.30%,同时使总根长、总根表面积、根尖数、分枝数分别显著增加103.42%、46.41%、64.44%、87.80%,总根体积和总根系直径分别减少23.05%和40.15%。(2)在本试验氯盐胁迫条件下,施氮0.14~0.17 g/kg时西瓜具有较理想的根系构型和较高的根系活力。(3)根系分枝数、根系活力、总根体积、根尖数可作为氯盐胁迫下氮素对西瓜根系生长影响的综合评价指标,各施氮水平对氯盐胁迫的缓解效果表现为0.15 g/kg>0.20 g/kg>0.10 g/kg>0.25 g/kg。可见,在氯盐胁迫下,适量施氮有助于西瓜建立良好的根系构型,提高根系渗透物质含量,降低细胞渗透势,减少根系丙二醛含量,维持较强的根系活力,增加根系生物量和干物质,缓解高浓度氯盐对西瓜生长的抑制作用。     

根域限制下水氮供应对膜下滴灌棉花根系及叶片衰老特性的影响

在新疆的气候生态条件下, 选用北疆2个棉花(Gossypium hirsutum)主栽品种‘新陆早13号’和‘新陆早33号’为供试材料, 设置限根(RR)与对照(CK)处理, 每个处理设置4个水氮水平: 水氮亏缺(W₀N₀)、水分亏缺(W₀N₁)、氮素亏缺(W₁N₀)与水氮适量(W₁N₁), 组成再裂区试验方案。采用管栽方法, 通过人工改变根系垂直生长深度和水氮供应, 在棉花产量形成期测定根系及叶片抗氧化保护酶系活性、生物量累积及分配等, 探讨根域限制及水氮供应对棉花根系生长及叶片衰老的影响机理。结果表明: 根域限制条件下, 棉花根系生物量、根系与叶片超氧化物歧化酶(SOD)、过氧化物酶(POD)与过氧化氢酶(CAT)活性、棉株总生物量、根冠比均低于对照, 而地上部生物量与籽棉产量显著高于对照。水氮供应能有效地调节根系及叶片的生长, 不同水氮处理间棉花根系与叶片抗氧化保护酶系活性、叶绿素含量、地上部生物量及籽棉产量均表现为W₁N₁ > W₀N₁ > W₁N₀ > W₀N₀, 根冠比与根系生物量的表现与之相反。根域限制与水氮供应表现出互作优势, 根域限制下适量水氮供应处理的地上部生物量与籽棉产量均明显高于其他处理, 根冠比较低。因此, 在棉花根系生长受限的条件下, 优化生育期间水氮供应, 可以增强根系及叶片的抗氧化保护酶系活性、增加光合产物向地上部的分配比例、增加产量, 是进一步挖掘膜下滴灌棉花增产潜力的有效途径。     

大气CO_2浓度和供氮水平对油菜前期生长及氮素吸收利用的影响

采用砂培试验,在2种CO2浓度(自然CO2浓度400μmol·mol-1和高CO2浓度700μmol·mol-1)和2种供氮水平(常氮15 mmol N·L-1和氮胁迫5 mmol N·L-1)下,研究了油菜营养生长阶段的干物质累积和氮素吸收利用的变化。结果表明:高CO2浓度条件下,油菜株高、根茎粗和干物质累积量增加,其中,常氮条件下,根茎粗和地上部干重的增加幅度大于氮胁迫条件,株高和根系干重增加幅度则常氮条件小于氮胁迫条件;高CO2浓度下,根体积、根系活跃吸收面积和总吸收面积在2个供氮水平下均增加,而一级侧根数只在常氮条件下增加,根长只在氮胁迫条件下增加;高CO2浓度条件下,油菜各器官含氮量下降,其中,叶片和根系的含氮素量下降幅度明显大于茎;高CO2浓度条件下,正常供氮时根、茎、叶氮素累积量均增加,氮胁迫时茎氮素累积量增加,而根和叶的氮素累积量减少;高CO2浓度条件下,氮素吸收效率、氮素利用效率和氮效率均增加,常氮条件下增加幅度大于低氮条件,其中,氮素利用效率对氮水平的响应更加明显。     

根域限制和氮素水平对连翘幼苗生长的影响

在植物生长箱通过溶液培养试验,从叶片光合气体交换参数、叶绿素含量及其荧光参数等方面来探讨不同氮素浓度条件下根域体积对连翘幼苗光合生理特性及生长的影响,并采用^15N示踪技术对不同氮素浓度条件下根域体积对连翘幼苗体内氮素转运进行了研究。结果表明：低氮（LN）处理幼苗的地上部和根系干物质重较高氮（HN）处理的高,根域限制对地上部和根系干物质重的影响不同,LN处理幼苗地上部和根系干物质重在低根域体积（10cm×10cm×15cm,LR）处理均较高根域体积（20cm×10cm×15cm,HR）处理的低,HN处理的幼苗响应情况有所不同。LN处理幼苗的叶片净光合速率（Pn）和叶绿素含量较HN处理的高;LN处理幼苗Pn和气孔导度（Gs）在LR处理较HR处理的高,而HN处理幼苗的Pn和Gs随根域体积变化规律与LN处理相反,LN和HN处理叶绿素含量随根域体积变化规律与Pn相反。LN处理幼苗的PSⅡ最大光化学量子效率（Fv／Fm）和PSⅡ电子传递量子效率（ФPSⅡ）均较HN处理的高,不同供氮处理下LR处理幼苗的Fv／Fm均较HR处理的高;而ФPSⅡ的变化规律相反。不同供氮处理时,LR处理幼苗的光化学猝灭系数（qP）均较HR处理的低,而非光化学猝灭系数（qNP）的变化规律相反,LN处理幼苗的qNP较HN处理的高（P〈0．05）。不同供氮处理时,LR处理幼苗根系和地上部氮含量均较HR处理的低,LN处理幼苗根系和地上部氮含量较HN处理的低,幼苗根系和地上部氮含量随氮素浓度变化差异显著（P〈0．05）。LN处理幼苗根系吸收^15N在根系和叶片的分配率均较HN处理的低,而根系吸收^15N在枝和茎的分配率呈相反变化规律。根系吸收氮在叶片和枝的分配率分别为7％～10％和7％～12％,叶片和枝生长需要的氮素主要由其内源N库提供。     

1973-2009年中国玉米品种演替过程中根系性状及其对氮的响应的变化

根系在氮素高效吸收过程中起重要作用,但人们对玉米育种过程中不同年代杂交种的根系生长特性及其对氮素供应的响应了解较少．选用中国1973．2009年育成的11个代表性玉米品种,在水培体系下研究了正常供氮（4retool／L）和低氮（0．04mmol／L）下根系与地上部生长差异．结果表明,与低氮处理相比,正常供氮降低根干重、根冠比和根系相对生长速率,但增加总根长和侧根长．对于20世纪90年代之前育成品种,供氮还降低总轴根长．氮处理不影响种子根数．随育种年代演进,地上部相对生长速率表现明显增加,不同氮水平下表现一致．但是,根系相对生长速率仅在正常供氮条件下表现出与育成年代线性相关．相应地,只在正常供氮条件下玉米总根长、侧根长、轴根长表现为随育成年代增加而明显增加．因此,在过去36年的玉米育种进程中,玉米地上部生长势在不同氮供应水平下均得到提高,而根系生长则只在正常供氮条件下得到提高．进一步改良根系在低氮环境下的生长能力可能提高现代玉米品种的氨吸收效率．     

施氮对干旱胁迫下毛竹幼苗生物量和根系形态的影响

为探讨氮素添加对水分胁迫下毛竹幼苗地上生物量及地下根系形态的调控作用,选取1年生毛竹实生苗为材料,采用水分和施氮双因素完全随机区组设计,以田间持水量的80%～85%作为水分对照(CK)、50%～55%为中度干旱(MD)、30%～35%为重度干旱(HD)设置3个水分水平,氮处理分未施氮(N0,0 mg N·kg^-1)和施氮(N1,100 mg N·kg^-1)2个水平,通过盆栽试验,测定毛竹实生苗根系形态特征及各器官生物量。结果显示：施氮显著增加了同一水分下毛竹幼苗叶、根及整株生物量,其中,N1MD和N1HD分别较N0MD和N0HD地上生物量增加15.6%、11.9%,总生物量分别增加36.7%、25.0%(P<0.05);施氮降低了相同水分处理下毛竹的比根长、茎叶比,显著促进了中度和重度干旱下根冠比的增加(P<0.05);水分胁迫下,除根生物量比显著增加外,茎、叶生物量比均随氮素添加呈减小的趋势;施氮对毛竹幼苗根系形态特征(根长、根表面积、根体积)具有不同程度的促进作用;施氮对中度干旱下毛竹幼苗干物质积累的缓解作用比重度干旱大,但在...     

根际通气状况对盐胁迫下棉花幼苗生长的影响

以溶液培养的棉花(Gossypium hirsutum)幼苗为材料,测定了不同盐胁迫程度和不同通气状况下棉花幼苗株高、根系体积、根系和茎叶生物量以及灰分含量的变化,以探索根际通气状况对盐胁迫下棉花生长的影响。结果表明,盐胁迫抑制棉花植株生长,表现为植株变矮、叶面积减小和干物质积累下降;根际环境通气不良也会导致棉花幼苗生长受抑制、干物质积累下降和矿质元素吸收减少等。进一步比较盐胁迫和根际通气状况及两者组合作用对棉苗生长的影响,发现盐胁迫对株高和总生物量的影响较大,而根际通气状况对根系体积、根系生物量、根冠比和矿质元素吸收的影响较大。总体表现为:盐胁迫对茎叶生长的不利影响较大,而根际通气状况对根系生长的不利影响较大。同时,在根际环境通气良好的条件下,不同程度盐胁迫导致的棉花幼苗株高、根系体积、叶面积、根系生物量和总生物量的变化程度远小于根际环境通气不良条件下的变化程度。实验结果表明,根际环境通气良好可以减弱盐胁迫对棉花生长发育的抑制作用,而根际环境通气不良则会加重盐胁迫的不利影响。     

Total soil nitrogen and nitrogen mineralization

Summary The mineralization capacity of 24 different soils was determined from incubation experiments. Relatively rapid mineralization and nitrification was found with soils from cultivated land, and pastures, but soils under natural vegetative covers of conifers and hardwoods were mostly ammonifying. A close relationship could be established between the total nitrogen content of the soil and the amount of mineral nitrogen formed during incubation. Important connections could also be shown between the available nitrogen contents at different times during the incubation period; these suggest that the incubation period can be considerably shortened.     

Uptake of fertilizer nitrogen and soil nitrogen by rice using15N-labelled nitrogen fertilizer

Data from five field experiments using labelled nitrogen fertilizer were used to determine the relative effects of soil nitrogen and fertilizer nitrogen on rice yield. Yield of grain was closely correlated with total aboveground nitrogen uptake (soil+fertilizer), less closely correlated with soil nitrogen uptake and not significantly correlated with fertilizer nitrogen uptake. When yield increase rather than yield was correlated with fertilizer nitrogen uptake, the correlation coefficient was statistically significant.Contribution from the Laboratory for Flooded Soils and Sediments, Agronomy Dept., Louisiana Agri. Exper. Sta., Louisiana State Univ., Baton Rouge, LA 70803, and Univ. of Florida, Agricultural Research and Education Center, Sanford, FL 32771.     

Root-induced nitrogen mineralisation: A nitrogen balance model

The possibility is examined that carbon (C) released into the soil from a root could enhance the availability of nitrogen (N) to plants by stimulating microbial activity. Two models are described, both of which assume that C released from roots is used by bacteria to mineralise and immobilise soil organic N and that immobilised N released when bacteria are grazed by bacterial-feeding nematodes or protozoa is taken up by the plant. The first model simulates the individual transformations of C and N and indicates that root-induced N mineralisation could supply only up to 10% of the plant's requirement, even if unrealistically ideal conditions are assumed. The other model is based on evidence that about 40% of immobilised N is subsequently taken up by the plant. A small net gain of N by the plant is shown (i.e. the plant takes up more N than it loses through exudation), although with exudate of up to C:N 33:1 less than 6% of the plant's requirement is supplied by root-induced N mineralisation. It is argued, however, that rhizosphere bacteria do not use plant-derived C to mineralise soil organic N to any great extent and that in reality root-induced N mineralisation is even less important than these models indicate.     

The effect of nitrogen fertilization on the release of soil nitrogen

Summary The effect of fertilizer nitrogen on the available amount of soil nitrogen was investigated in a greenhouse experiment. To 9 different soils, 0, 50, 100 and 200 kg N/ha were applied, resp., as (N¹⁵H₄)₂SO₄ with an atom excess N-15 of 1%.No priming effect could be found for any of the treatments. The available amount of soil N, expressed as A_N value, was not affected by rate of N-fertilizer application.     

On the importance of quantifying bioavailable nitrogen instead of total nitrogen

Monitored and modeled data provided the basis for the establishment of two nitrogen (N) budgets covering the Kattegat-Belt Sea area in the period 2000–2009: one for total nitrogen (TN) and one for bioavailable nitrogen (N_bio). Our results show a significant difference between the two budgets, and we argue that N_bio is more important than TN for our understanding of the sources causing marine eutrophication. Consequently, an optimal strategy for abatement of eutrophication aims at minimizing N_bio rather than TN. The TN budget shows that advection from the adjacent seas is the dominant source of N to the Kattegat-Belt Sea area. The loadings from land and atmosphere only account for 14 and 9 % of the TN loadings, respectively. However, when the bioavailability of the different N sources is taken into account, the supply from land and atmosphere becomes relatively more important, now accounting for 21 and 16 %, respectively (37 % in total). The ecological relevance of land and atmosphere loadings is most likely even larger since a fraction of the input from the Skagerrak is exported again before it can support primary production. Water action plans have reduced the direct loadings of TN from land and atmosphere by about 35 % since the 1980s. The contributions from land and atmosphere accounted for 47 % of the N_bio loadings in the 1980s. Hence, loadings from land and atmosphere have only decreased by 10 % points since the 1980s: from 47 to 37 %. The largest sink of TN in the study areas is advection to the adjacent seas (71 %) whereas denitrification and burial only accounts for 17 and 11 %, respectively.     

Prediction of nitrogen responses of corn by soil nitrogen mineralization indicators

Soil nitrogen mineralization potential (N min) has to be spatially quantified to enable farmers to vary N fertilizer rates, optimize crop yields, and minimize N transfer from soils to the environment. The study objectives were to assess the spatial variability in soil N min potential based on clay and organic matter (OM) contents and the impact of grouping soils using these criteria on corn grain (Zea mays L.) yield, N uptake response curves to N fertilizer, and soil residual N. Four indicators were used: OM content and three equations involving OM and clay content. The study was conducted on a 15-ha field near Montreal, Quebec, Canada. In the spring 2000, soil samples (n = 150) were collected on a 30- x 30-m grid and six rates of N fertilizer (0 to 250 kg N ha(-1)) were applied. Kriged maps of particle size showed areas of clay, clay loam, and fine sandy loam soils. The N min indicators were spatially structured but soil nitrate (NO3-) was not. The N fertilizer rate to reach maximum grain yield (N max), as estimated by a quadratic model, varied among textural classes and Nmin indicators, and ranged from 159 to 250 kg N ha(-1). The proportion of variability (R2) and the standard error of the estimate (SE) varied among textural groups and N min indicators. The R2 ranged from 0.53 to 0.91 and the SE from 0.13 to 1.62. Corn grain N uptake was significantly affected by N fertilizer and the pattern of response differed with soil texture. For the 50 kg N ha(-1) rate, the apparent N min potential (ANM) was significantly larger in the clay loam (122 kg ha(-1)) than in the fine sandy loam (80 kg ha(-1)) or clay (64 kg ha(-1)) soils. The fall soil residual N was not affected by N fertlizer inputs. Textural classes can be used to predict N max. The N min indicators may also assist the variable rate N fertilizer inputs for corn production.     

红松混交林凋落物氮储量及分解释放对土壤氮的影响

2012年5—10月,采用直接收获法,研究了小兴安岭地区云冷杉红松混交林和枫桦红松混交林两种林型凋落物的未分解层(L层)、半分解层(F层)和腐殖质层(H层)以及土壤表层(S层)氮储量及凋落物分解释放对土壤氮影响。结果表明:研究期间两种林型凋落物现存量变化范围分别为19.43~27.25和21.25~24.28 t·hm-2,氮储量变化范围分别为287.21~418.22和274.81~351.21 kg·hm-2,各层氮含量大小次序均为LFHS;云冷杉红松混交林各层凋落物现存量及其氮储存量5月和9月达到峰值,每月氮储量从L~H层均增加,凋落物分解释放氮在F和H层易富集,输入到土壤中较少;枫桦红松混交林各层凋落物现存量及其氮储量5月和10月达到峰值,每月氮储量从L~H层均减少,氮在凋落物各层中均易迁移,输入到土壤中的氮比云冷杉红松混交林多;两种林型L、F、H层凋落物现存量以及H层氮含量与S层氮含量之间,L和F层凋落物现存量与H层氮含量之间均呈显著正相关。     

模拟氮沉降对杂草生长和氮吸收的影响

以杂草早熟禾、黑麦草、野燕麦、天蓝苜蓿、白车轴草、北美车前、婆婆纳、无芒稗、牛筋草和刺苋为试验材料,以4.0g·m^-2·yr^-1的N输入为模拟氮沉降浓度,研究了不同杂草功能类群对模拟氮沉降的响应.结果表明,模拟氮沉降处理下,杂草的生物量(总生物量、地上部分生物量、根生物量)呈增加趋势,但不同功能类群对氮增加的响应明显不同,C₄禾本科、C₃豆科及C₃禾本科植物的生物量受到氮沉降的显著促进,但C₃非禾本科和C₄非禾本科植物的生物量则受氮沉降的影响不显著;不同功能类群的根冠比、植株含氮及植株吸收氮的总量对模拟氮沉降的响应无明显规律,但物种间差异显著.氮沉降提高野燕麦和北美车前的生物量的根冠比,但对其他生物种类没有显著影响.没有发现氮沉降对植物体内的含氮量有显著的影响,但氮沉降却显著地提高了除刺苋、早熟禾及婆婆纳之外的所有杂草物种对N的摄收.由于物种对氮沉降的响应不同,未来氮沉降的增加将加速杂草群落组成的变化.     

添加氮素对沙质草地土壤氮素有效性的影响

通过氮素添加(20g.m-2.a-1)试验,研究了科尔沁沙地东南部沙质草地生态系统土壤氮矿化及有效氮的季节变化。对2006年生长季的观测发现,添加氮素显著提高了沙质草地生长季土壤铵态氮、硝态氮、矿质氮的含量以及9月1日至10月15日的净氮矿化速率与硝化速率;添加氮素导致土壤有效氮的季节变异增大,净氮矿化(1.29～11.60mg.kg-1.30d-1)与硝化(-4.15～11.20mg.kg-1.30d-1)速率随时间呈上升趋势,铵态氮含量逐渐降低,硝态氮与矿质氮(6.49～20.66mg.kg-1)含量的变化呈"V"型,最小值出现在生物量生长高峰期的7月中旬。该沙质草地土壤氮的有效性较低,施氮肥可明显提高土壤供氮能力。     

氮肥运筹对稻茬冬小麦土壤无机氮时空分布及氮肥利用的影响

以宁麦9号和豫麦34号为材料,研究了氮肥基追比对土壤无机氮时空变化、氮素表观盈亏和氮肥利用率的影响。结果表明,施用基肥提高了越冬期0-60 cm土层NO3--N和NH4+-N含量,拔节期追肥对孕穗期各土层无机氮含量无显著影响,追施孕穗肥显著提高了开花期0-60 cm土层硝态氮含量和0-20 cm土层铵态氮含量。不施氮处理各生育阶段均表现为氮素亏缺,施氮处理氮素盈亏呈明显的阶段性,播种至孕穗阶段出现氮素盈余,孕穗至成熟阶段出现氮素亏缺;全生育期氮素表观盈余量两品种平均以5∶5处理最低,7∶3处理最高。两品种氮肥农学效率、氮肥表观回收率和产量均随基肥比例的增加呈先增后降的趋势,均以5∶5处理最高。因此,在小麦生产中应适当减少基施氮肥用量,在小麦拔节孕穗期适当增加追肥比例有利于提高产量和氮肥利用效率,并降低土壤氮素损失。