花后干旱或渍水下氮素供应对小麦光合和籽粒淀粉积累的影响

防雨池栽条件下,设置渍水、干旱和对照3个土壤水分处理,每水分处理下再设置两个施氮水平,研究了花后渍水和干旱逆境下氮素水平对两个蛋白质含量不同的小麦品种光合特性和籽粒淀粉积累的影响.结果表明,与对照相比,花后渍水和干旱处理显著降低小麦旗叶净光合速率和SPAD值,干物质积累量下降.干旱处理下,增施氮肥提高旗叶光合速率和SPAD值,渍水处理下则相反.水分逆境明显降低籽粒可溶性总糖含量,且渍水处理下增施氮肥降低小麦叶片和籽粒可溶性总糖含量,干旱状态下规律相反.渍水处理下增施氮肥降低淀粉积累速率.水分逆境明显降低小麦粒重、产量和淀粉产量,且干旱处理下增施氮肥有利于籽粒重、产量和淀粉产量的提高,而渍水下增施氮肥使粒重和产量进一步降低.试验结果表明,花后渍水和干旱逆境下施用氮肥对小麦旗叶光合速率和籽粒淀粉积累有明显的调节效应.     

花后干旱或渍水逆境下氮素对小麦籽粒产量和品质的影响

 池栽试验条件下,设置渍水、干旱和对照3个水分处理,每个水分处理下设置两个施氮水平 ,研究了花后渍水或干旱逆境下氮素营养对两个不同类型小麦（Triticum aestivum） 品种籽粒产量和品质性状的影响。结果表明,与对照相比,花后渍水或干旱处理显著降低了小麦的千粒重、穗粒数和籽粒产量。在适宜水分和干旱条件下,增施氮肥增加了小麦籽粒产量,而在渍水条件下,增施氮肥降低了产量。干旱处理提高了蛋白质含量,干、湿面 筋含量,沉降值和降落值;而渍水处理则降低了小麦籽粒蛋白质含量和干、湿面筋含量。同 一水分处理下,增施氮肥提高了蛋白质含量,谷蛋白/醇溶蛋白比,支链淀粉含量和支/直链淀粉比。在小麦籽粒主要品质性状上存在显著的水氮互作效应,且水分、氮肥及水氮互作效 应对小麦籽粒产量和品质的影响因品种的不同而异。     

花期渍水逆境下氮素对油菜产量及氮肥利用效率的影响

温室盆栽试验条件下,设置渍水和对照2个水分处理,每个水分处理下设置3个施氮水平(0.05、0.2、0.3 g N·kg^-1土),研究了花后渍水逆境下氮素营养对两个氮高效基因型‘Monty’、‘湘油15’和两个氮低效基因型‘R210’、‘Bin270’油菜产量、产量性能及氮肥利用效率的影响.结果表明:与对照相比,花后渍水处理显著降低了油菜的单株角果数、千粒重、每角粒数和籽粒产量.在适宜水分条件下,增施氮肥显著增加了油菜籽粒产量,而在渍水逆境处理下,增施氮肥对油菜籽粒产量的形成贡献不大.氮高效基因型较氮低效基因型对花后渍水逆境下的籽粒灌浆充实具有一定的促进作用.在同一水分处理下,花后渍水明显降低了油菜氮肥利用率、氮肥偏生产力、氮肥农学利用率、氮素吸收效率和氮收获指数,渍水显著影响了不同基因型油菜的氮素吸收利用能力,而氮高效基因型在渍水逆境下较氮低效基因型更有利于将氮素转运、再分配到角果中,提高籽粒生产效率.油菜产量性能参数存在显著的水氮互作效应,水分、氮肥及水氮互作对油菜籽粒产量和产量性能参数的影响因基因型的不同而异.     

花后干旱和渍水对不同品质类型小麦籽粒品质形成的影响

 防雨池栽条件下研究了花后干旱和渍水胁迫对两个不同品质类型小麦（Triticum aestivum）品种籽粒产量和品质形成的影响。结果表明,花后渍水和干旱处理明显降低了小麦籽粒产量和蛋白质产量。在整个灌浆期内干旱处理明显提高了籽粒蛋白质和醇溶蛋白含量,而渍水处理降低了籽粒蛋白质及其组分的积累量。籽粒总淀粉和直链淀粉含量以渍水处理最高,而支链淀粉以对照最高。干旱处理提高了籽粒干、湿面筋含量、沉降值和降落值,而渍水处理降低了上述品质指标。试验表明干旱和渍水胁迫对小麦籽粒蛋白质与淀粉的含量和组分及面粉品质等均有不同程度的影响,从而改变了不同品质类型小麦的籽粒品质。     

灌浆期高温和水分逆境对冬小麦籽粒蛋白质和淀粉含量的影响

灌浆期高温和水分逆境是影响小麦籽粒产量和品质的关键气候因子。以扬麦9号、徐州26和豫麦34三个小麦品种为材料,利用人工气候室模拟灌浆期高温和水分胁迫环境,研究了花后高温及温度和水分互作对小麦籽粒蛋白质和淀粉形成的影响。结果表明,高温显著提高了小麦籽粒蛋白质含量及清蛋白、球蛋白和醇溶蛋白含量,但降低了谷蛋白含量,导致麦谷蛋白／醇溶蛋白比值降低。高温显著降低了籽粒总淀粉和支链淀粉含量及支／直比。籽粒蛋白质和淀粉及其组分形成所需的适宜昼夜温差随小麦品质类型而异,但温度水平对籽粒蛋白质和淀粉的影响较温差大。在高温和水分逆境下,温度对籽粒蛋白质和淀粉含量的影响较水分逆境大,且存在显著的互作效应。小麦籽粒蛋白质含量均表现为干旱〉对照〉渍水,以高温干旱最高,适温渍水最低;淀粉含量为对照〉干旱〉渍水,以适温对照最高,而高温渍水最低。高温和水分逆境显著提高了籽粒醇溶蛋白含量而降低了谷蛋白含量及支链淀粉含量,使蛋白质谷／醇比和淀粉支／直比降低,以高温渍水对籽粒蛋白质和淀粉组分的影响最为显著。不同品种之间,高蛋白小麦籽粒蛋白质和组分的形成受高温和水分逆境的影响更大,而低蛋白品种籽粒淀粉形成显著受温度和水分逆境的调节。分析表明,在高温和水分逆境下籽粒蛋白质含量与清蛋白和醇溶蛋白显著正相关,籽粒淀粉含量与谷蛋白、支链淀粉含量及支／直比显著正相关。     

高温下干旱和渍水对冬小麦花后旗叶光合特性和物质转运的影响

以蛋白质含量不同的两个冬小麦品种扬麦9号和豫麦34为材料,研究了不同温度和水分条件下小麦花后旗叶光合特性的变化、营养器官花前贮藏干物质和氮素转运特征及其与籽粒产量和品质形成的关系.结果表明,高温及干旱和渍水均明显降低了旗叶光合速率和叶绿素含量（SPAD值）,但高温下干旱和渍水对光合作用的影响加重.小麦营养器官花前贮藏干物质、氮素转运量和转运率在适温下表现为干旱>对照>渍水,高温下则表现为对照>干旱>渍水.适温下花后同化物积累量表现为对照>渍水>干旱,高温下则表现为对照>干旱>渍水.花后氮素积累量在适温和高温下均表现为对照>渍水>干旱.籽粒淀粉含量以适温适宜水分处理最高,高温渍水下最低;蛋白质含量以高温干旱下最高,适温渍水下最低.温度和水分逆境下小麦粒质量和淀粉含量的降低与花后较低的光合能力及干物质积累有关,而蛋白质含量则与花前贮藏氮素的转运量和转运率有关.     

施氮量和花后土壤含水量对小麦旗叶衰老及粒重的影响

在防雨池栽培条件下,研究了施氮量和花后土壤含水量对小麦旗叶衰老和粒重的影响.结果表明：各氮肥处理下,小麦旗叶SPAD值、可溶性蛋白质含量、超氧化物歧化酶（SOD）活性、过氧化氢酶（CAT）活性和光合速率（P_n）均表现为：花后土壤含水量60%～70%处理>80%～90%处理>40%～50%处理,小麦旗叶丙二醛（MDA）含量表现为：花后土壤含水量40%～50%处理>80%～90%处理>60%～70%处理,表明花后土壤含水量过高或过低均可导致小麦旗叶早衰,影响籽粒灌浆,降低粒重.在花后相同土壤含水量条件下,旗叶SPAD值、可溶性蛋白质含量、SOD活性、CAT活性和P_n均随施氮量的增加而升高,MDA含量随施氮量的增加而降低,表明增施氮肥可以延缓小麦旗叶衰老,但过量施用氮肥则不利于小麦粒重的提高,尤其是在花后土壤缺水的情况下,施用过多氮肥可导致小麦粒重下降.在小麦生产中可以将施用氮肥和控制花后土壤水分含量相结合,延缓小麦植株衰老,提高粒重.     

灌浆前期高温和干旱胁迫对小麦籽粒蛋白质含量和氮代谢关键酶活性的影响

为探讨花后逆境胁迫影响小麦籽粒氮代谢及蛋白质合成的生理机制,采用盆栽和人工气候室模拟花后高温的方式,研究了灌浆前期短暂高温和干旱胁迫对两个不同品质类型小麦品种籽粒蛋白质含量、组分及谷氨酰胺合成酶(GS)、谷丙转氨酶(GPT)活性的影响。结果表明,灌浆前期高温、干旱及其复合胁迫均显著提高两品种籽粒蛋白质及组分含量,但降低谷/醇比。逆境胁迫使蛋白质积累量和粒重显著下降,其中高温处理使两品种蛋白质产量分别下降20.7%和12.4%,粒重下降23.2%和24.0%;干旱胁迫使两品种蛋白质产量分别下降16.2%和11.9%,粒重下降18.0%和16.0%;复合胁迫使两品种蛋白质产量分别下降26.1%和15.8%,粒重下降29.9%和28.9%。高温、干旱及其复合胁迫下两品种籽粒氮代谢关键酶活性升高。花后8,17,23,29 d的GS活性和花后11,17 d的GPT活性与蛋白质含量呈显著或极显著正相关,花后23,35 d的GS和花后8,17,23 d的GPT活性与蛋白质产量呈显著或极显著负相关,花后8,17,23,29,35 d的GS和花后8,11,17,23 d的GPT活性与籽粒产量呈显著或极显著负相关。试验条件下,高温处理对籽粒蛋白质合成的影响大于干旱胁迫,二者具有叠加效应,强筋小麦品种郑麦366受逆境胁迫的影响较大。     

旱地小麦休闲期覆盖增磷对籽粒蛋白质积累的影响

为探索旱地小麦休闲期覆盖保水配施磷肥高产、优质的技术途径,在山西农业大学闻喜试验基地采用大田试验研究了休闲期覆盖或不覆盖条件下低(75 kg/hm2)、中(112.5 kg/hm2)、高(150 kg/hm2)施磷水平对土壤水分、籽粒蛋白质形成的影响及其生理机制。结果表明:休闲期覆盖后,播种期0-100 cm土壤蓄水量显著提高,达39-42 mm,而开花期60-100 cm土层降低。覆盖后,花后旗叶和籽粒GS和GOGAT活性提高,籽粒游离氨基酸和灌浆后期GMP含量提高,籽粒蛋白质及其组分含量、谷/醇均提高。增加施磷量,开花期20-60 cm、80-100 cm土层蓄水量降低,而花后旗叶和籽粒GS活性提高,且覆盖条件下花后0-15 d、20 d旗叶GOGAT活性,花后5 d、15 d、25-30 d籽粒GOGAT活性,籽粒游离氨基酸含量、籽粒GMP含量提高,籽粒蛋白质及其组分含量、谷/醇、蛋白质产量显著提高,产量提高940-1452 kg/hm2。此外,休闲期覆盖配施磷肥条件下,开花期深层土壤水分与旗叶GS和GOGAT活性密切相关,旗叶和籽粒GS和GOGAT活性均与游离氨基酸含量、谷/醇、蛋白质产量关系密切。总之,旱地小麦休闲期覆盖有利于提高底墒,且配合施磷量150 kg/hm2可促进根系吸收深层土壤水分,提高产量的同时也提高了籽粒蛋白质含量、GMP含量和谷/醇。     

土壤水分对强筋小麦‘豫麦34’氮素同化酶活性和籽粒品质的影响

 以强筋型小麦(Triticum aestivum)品种‘豫麦34号’为材料,采用盆栽方法研究了土壤水分对氮素同化酶活性及籽粒品质的影响。结果表明：旗叶硝酸还原酶（NR）活性于花后呈下降趋势,且土壤含水量为田间持水量（FC）60%的处理活性最强,其次为40%FC,活性最低的是80%FC。旗叶和籽粒中谷氨酰胺合成酶（GS）活性于开花15 d前均呈下降趋势,15 d后均为上升趋势,各水分处理间酶活性大小关系是：80%FC＞60%FC＞40%FC。各水分处理间旗叶和籽粒谷氨酸合成酶（GOGAT）活性的大小关系同GS。60%FC籽粒产量及品质最优,80%FC产量次之,40%FC产量最低;40%FC品质次之,80%FC品质最低。不同水分处理下籽粒蛋白质含量与叶片NR、GS 和籽粒GOGAT活性均呈正相关,与旗叶GOGAT活性呈负相关。且40%FC和80%FC下籽粒蛋白质含量只与旗叶GS活性相关性达显著水平, 60%FC下蛋白质含量则与旗叶NR和籽粒GS活性均达显著相关,与旗叶GS活性达极显著相关。     

香蕉苗期氮素亏缺与补偿对植株生长和根系形态的影响

为探究氮素亏缺及亏缺后补偿供氮对蕉苗生长及其根系形态特征的影响,该研究以主要栽培品种基因组类型(AAA型和ABB型)的香蕉品种为材料,通过石英砂基质培养结合氮素亏缺与补偿处理,分析其株高、叶长、叶宽、新增绿叶数、地上部和根系的鲜重和干物质质量、根长和根表面积及根体积等指标的变化。结果表明:(1)亏缺30 d,香蕉苗呈现明显的缺氮表型症状,株高、叶长、叶宽及新增绿叶数均显著降低,根系干物质积累增加,品种Ⅰ、Ⅱ根系干物质分别提高64.71%、87.50%,根冠比增加,总根表面积分别增加4.38%、11.85%,体积分别增加71.78%、66.55%。(2)亏缺68 d,干物质积累受到明显抑制,品种Ⅰ、Ⅱ全株干物质质量降低33.74%、42.04%,根系干物质质量与常规处理无显著差异,根系形态参数变化趋势与轻度亏缺一致。(3)亏缺后补偿供氮,缺氮症状消失,植株生长指标恢复正常水平; 品种Ⅰ、Ⅱ根系干物质质量显著增加51.22%、52.38%,根冠比显著高于常规处理,根系趋向正常形态生长,并且总根体积分别增加61.80%、45.92%; 轻度氮素亏缺后适时补偿供氮,缺氮蕉苗可恢复正常生长,根系干物质质量及体积显著高于常规处理且幼苗的长势更好。综上认为,生产中可以综合利用亏缺胁迫后补偿供氮的方式来培育香蕉苗,以利于其在田间栽培的生长。     

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.     

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。