水氮互作下直播稻群体质量与氮素利用特征的关系

探讨水氮耦合下直播稻群体质量和氮素利用特征可为直播水稻丰产高效生产提供理论基础和实践依据。以杂交稻‘F优498’为试验材料,设置淹水灌溉(W₁)、干湿交替灌溉(W₂)、旱种(W₃)3种灌水方式和基肥∶蘖肥∶穗肥分别为5∶3∶2(N₁)、3∶3∶4(N₂)、3∶1∶6(N₃)3种氮肥运筹模式,以不施氮处理(N₀)为对照,研究水氮互作对直播稻群体质量和氮素利用特征的影响,并探讨水氮互作下直播稻群体质量构建与氮素利用特征和产量的关系。结果表明:灌溉方式和氮肥运筹对直播稻各生育时期干物质积累、稻谷收获指数、抽穗及抽穗20 d高效叶(上3叶)干重、结实期群体透光率、氮素积累总量、氮肥表观利用率、氮肥偏生产力、氮肥生理利用率和产量均存在显著的互作效应。综合直播稻群体质量、产量和氮肥利用特征,各灌溉方式下,氮肥后移比例均以占总量的20%～40%(N₁～N₂)为宜,氮肥后移比例达到总量的60%(N₃)和W₃处理均会显著降低直播稻群体质量、产量、氮肥农学利用率和氮肥偏生产力。相关分析表明,水氮互作下直播稻产量和氮素利用特征与最终有效分蘖数、结实期干物质积累、其余叶(除上三叶以外叶片)干重减少量、总叶片干重减少量,以及群体中部和基部受光率均呈显著或极显著正相关。干湿交替灌溉(W₂)可以提高直播稻茎蘖成穗率、各时期干物质积累、稻谷收获指数、氮肥吸收总量、氮肥农学利用率和最终产量,配合N₂的氮肥运筹模式可优化调控直播稻群体质量,实现高产与氮肥高效利用的协调统一,为本试验最优组合。     

水分管理调控水稻氮素利用研究进展

水、氮是调控水稻生长发育的两个重要环境因子。通过"以水调氧"增加根际溶氧量(如干湿交替、好氧栽培等)能够提升土壤硝化势和氧化还原电位,刺激土壤氮的矿化作用,使水稻处于NH+4与NO-3混合营养中,并能通过诱导水稻的生理特性及改善根系的吸收功能增强其抗旱性能,提高水稻产量及氮素利用率。光合作用是形成干物质的主要途径,土壤氮水平、氮形态与水稻光合速率紧密相关,提高叶片光合速率将有助于提高水稻的氮素利用率和产量。从稻田水分管理对土壤氮素形态特征、水稻氮吸收利用、光合速率及氮环境效应的影响等方面综述了国内外相关研究进展,并指出进一步的研究方向。     

不同灌水模式对冬小麦籽粒产量和水、氮利用效率的影响

在田间试验条件下,以冬小麦品种泰农18为材料,设置灌底墒水(CK)、底墒水+拔节水(W1)、底墒水+拔节水+越冬水与灌浆水交替灌溉(越冬/灌浆水交替灌溉模式,W2)、底墒水+拔节水+开花水(优化传统灌溉模式,W3)、底墒水+越冬水+拔节水+灌浆水(传统灌溉模式,W4)5种灌溉模式,每处理每次灌水量均为600 m3·hm-2,研究了山东泰安偏旱年份(2009-2010年)不同灌溉模式对小麦籽粒产量、水分利用效率和氮素利用效率的影响.结果表明:在小麦全生育期119.7 mm降水量条件下,越冬/灌浆水交替灌溉模式(W2)与传统灌溉模式(W4)籽粒产量差异不显著,但水分利用效率显著高于传统灌溉模式,与灌水量相同的优化传统灌溉模式(W3)相比,其小麦籽粒产量明显提高,水分利用效率无显著差异;越冬/灌浆水交替灌溉模式和传统灌溉模式的氮肥偏生产力最高,且籽粒收获后越冬/灌浆水交替灌溉模式在0 ～100 cm土层的硝态氮积累量显著高于传统灌溉模式和优化传统灌溉模式,降低了硝态氮的淋溶损失.在本试验条件下,越冬/灌浆水交替灌溉模式(W2)是可以兼顾小麦籽粒产量、水分利用效率和氮素利用效率的最佳灌溉模式.     

不同水分和氮素处理对寒地水稻生育及产量的影响

为了探讨不同水分和氮素处理对寒地水稻生长发育及产量的影响,以水稻品种空育131、龙粳21为试验材料,于2010—2011年度在黑龙江建三江进行水分、氮素处理大田试验,水分为雨养、间歇灌溉、水层灌溉3个水平,氮素为不施氮、常规施氮(112—135 kg/hm2)、高氮(142—173 kg/hm2)3个水平。结果表明:与水层灌溉相比,雨养水稻生育期缩短1—5 d,生长指标明显降低,产量显著降低,间歇灌溉水稻生育期、生长指标与其相似,产量差异不显著。与常规施氮相比,不施氮生育期缩短2—5 d,高氮条件下延长2—4 d;施氮量增加,生长指标增大,产量显著增加;低氮条件下,水分不足的限制作用明显,高氮能一定程度弥补水分的限制,促进水稻生长。增加施氮量及灌溉水平可以显著地提高有效穗数、每穗粒数。在试验条件下,水氮互作效应不显著。间歇灌溉及高氮管理具有较好的增产效应及资源利用率,研究可为寒地水稻生产进行水氮科学管理、实现高产高效提供理论依据。     

不同水分管理模式下免耕抛秧水稻立苗期根系生长特性

在免耕条件下,对3种水分管理模式(水层淹灌、干湿交替灌溉和湿润灌溉)的立苗期根系特性进行了研究。结果表明,除抛栽后第2天,无论晚季或早季,整个立苗期干湿交替灌溉处理的根冠比、单株根生物量、总根数、白根数、一次分枝数量、根系活力、发根力均显著或极显著高于水层淹灌和湿润灌溉处理。水层淹灌处理利于二次分枝根的发生与根系的伸长。湿润灌溉处理更能促进早季稻根毛区生长。     

不同测墒补灌水平对小麦水氮利用及土壤硝态氮淋溶的影响

于2012—2014年两个小麦生长季,以全生育期不灌水(W_0)为对照,设置3个测墒补灌处理,即拔节和开花期使0~140 cm土层土壤平均相对含水量分别为65%(W_1)、70%(W_2)和75%(W_3),研究其对土壤水利用、小麦氮素积累转运和土壤硝态氮分布及籽粒产量的影响.结果表明:W_2处理土壤贮水消耗量及占总耗水量的比例和灌溉水占总耗水量的比例较高,且吸收利用100~140 cm土层土壤贮水量较高.开花期营养器官氮素积累量及开花后氮素积累量均为W_2、W_3W_1W_0,成熟期营养器官氮素积累量为W_3W_2W_1W_0,营养器官氮素向籽粒中的转移量和成熟期籽粒氮素积累量均为W2W3W1W0.成熟期0~60cm土层硝态氮含量表现为W_0W_1W_2W_3,80~140 cm土层为W3显著高于其他处理,140~200 cm土层各处理间无显著差异.W_2处理的籽粒产量、水分利用效率、氮素吸收效率及氮肥偏生产力均最高.在本试验条件下,综合考虑籽粒产量、水分利用效率、氮素吸收效率及土壤硝态氮的淋溶,W_2处理是高产节水生态安全的最佳灌溉处理.     

不同水分管理下优质稻花后植株碳氮流转与籽粒生长及品质的相关性

以桂华占、八桂香为材料,在干湿交替灌溉、亏缺灌溉、淹水灌溉3种水分条件下,研究优质稻花后植株碳氮流转与籽粒生长及品质的相关性。结果表明:不同水分管理下,桂华占和八桂香花后碳氮流转与籽粒的生长间存在密切相关。主要表现在:(1)茎鞘和叶片干物质转运对籽粒干物质积累的贡献率为16.86%～25.68%,花后茎叶干物质运转速度和运转率与籽粒起始灌浆势呈显著甚至极显著正相关;籽粒最大灌浆速率、活跃灌浆期、持续灌浆时间与叶片干物质运转速度和运转率呈极显著正相关,与茎鞘干物质运转速度和运转率呈极显著负相关;(2)茎鞘碳同化物转运对籽粒的产量和淀粉产量的贡献率则为干湿交替灌溉>亏缺灌溉>淹水灌溉;但叶片碳同化物转运对籽粒的产量和淀粉产量的贡献率则为淹水灌溉>亏缺灌溉>干湿交替灌溉;茎叶可溶性糖积累量的减少和籽粒直链淀粉含量和积累量增加是同步的,且茎叶可溶性糖积累量快速递减期(花后3～12d)与直链淀粉含量和积累量快速递增期(花后6～12d)同步;(3)茎鞘和叶片氮素转运对籽粒氮素积累的贡献率为44.05%～117.66%,叶片总氮转运对籽粒氮素积累的贡献率大于茎鞘,茎鞘和叶片氮同化物对籽粒氮素的贡献率以淹水灌溉处理的最大,亏缺灌溉处理的次之,干湿交替灌溉处理的最小。     

莱州海涂海水灌溉下菊芋生理生态特性研究

 在山东莱州对菊芋(Helianthus tuberosus)进行了海水灌溉浓度及其灌溉次数的田间试验,结果表明：1） 灌溉1次的处理中,全淡水同海淡水比例为1∶9、1∶4、1∶3的3种处理的菊芋块茎产量（鲜重）没有显著差异;菊芋生长中灌溉2次,以海淡水比例为1∶3处理的菊芋块茎产量最高,但各处理间菊芋块茎产量差异没有达到显著水平;无论何种比例海淡水灌溉,在莱州湾,灌溉两次菊芋块茎产量显著高于灌溉1次;2） 灌溉处理后连续5天内,菊芋光合速率与土壤表层盐分动态变化趋势一致：第一、二天,1∶9比例海淡水灌溉菊芋光合速率显著高于其它处理,而1∶4、1∶3比例海淡水处理在前二、三天光合速率同全淡水灌溉处理基本没有差异,第五天时,海淡水比例为1∶3的处理,菊芋光合速率显著低于其它处理;在灌溉后盐分变化达到平稳的较长时间内,土壤水分含量成为影响菊芋光合速率的主导因子,1∶3处理因土壤表层土壤水吸力较低而菊芋光合速率显著高于其它处理;3） 第一次灌溉60 d后,以全淡水灌溉处理菊芋的叶面积指数显著高于其它处理,1∶3处理显著低于其它处理,1∶9、1∶4两处理间没有差异。     

氮素水平对不同品种茶树光合及叶绿素荧光特性的影响

为探明氮素水平对不同品种茶树的光合系统的影响机制,以‘福鼎大白茶’、‘保靖黄金茶1号’、‘白毫早’两年生茶苗为材料,设置不施氮N_0(0g)、低氮N_1(11g)、中氮N_2(22g)和高氮N_3(33g)4个氮素[(NH_4)_2SO_4]水平的盆栽实验,研究了铵态氮对3个品种茶树的生长势、叶片叶绿素含量、光合参数与叶绿素荧光参数的影响。结果表明:(1)施氮处理能够显著促进茶树的生长,提高茶树叶片叶绿素含量、净光合速率(Pn)、气孔导度(Gs)、蒸腾速率(Tr),降低胞间CO_2浓度(Ci),并以N_2处理最好,但水分利用率(WUE)在3个品种茶树间表现不同。(2)在N_2处理下,3个茶树品种的叶片光系统Ⅱ(PSⅡ)暗适应下的最大光化学效率(F_v/F_m)、光化学猝灭系数(qP)、PSⅡ的相对电子传递速率(rETR)亦增加最大,非光化学淬灭系数(NPQ)降低。(3)茶树叶片叶绿素含量与光合参数间存在着一定的联系,并且具有品种特异性。研究发现,适量施氮能够显著增加茶树叶绿素含量、气孔导度、光合活性,从而使得各品种茶树净光合速率增加;氮素水平对各茶树品种的光合及荧光特性影响存在差异,水分利用率亦具有品种特异性;生产中应综合叶绿素含量、光合作用参数、叶绿素荧光参数,可快速、直观地评价不同品种茶树对氮素营养的内在需求,为茶园施肥管理提供指导。     

不同土壤水分处理对水稻光合特性及产量的影响

为探明土壤水分对水稻生长发育的影响机理,以武香粳14和两优培九为试验材料,分析了不同土壤水分处理下(W1、W2、W3和CK分别表示土壤体积含水量为20%、30%、40%和5cm水层灌溉)的水稻光合特性、产量及水分生产率等。结果表明,轻度水分胁迫(W3)具有处理间最大的叶片气孔导度、蒸腾速率和净光合速率,其他处理规律不显著。灌浆初期各水分处理下叶位间光合指标均表现为:剑叶＞顶2叶＞顶3叶>顶4叶,其他生育期规律不显著。与对照处理(CK)相比,武香粳14的W1、W2和W3处理的产量分别减少61.14%和29.13%、增加0.96%,水分生产率分别减少10.69%、增加1.53%和20.61%;两优培九的产量分别减少64.11%和28.76%,增加2.08%,水分生产率分别减少16.39%,增加2.46%和22.13%。研究结果为水稻精确灌溉和节水生产提供了技术支撑。     

Electron transport-linked nitrous oxide synthesis and reduction by Paracoccusdenitrificans monitored with an electrode

The nitrous oxide reductase activity of $\text{Paracoccus}\text{denitrificans}$ can be conveniently measured using an electrochemical method for determining N₂O. Introduction of this procedure has shown that (i) N₂O reductase activity is reversibly inhibited by oxygen; (ii) antimycin strongly inhibits electron flow to N₂O and that the inhibition is bypassed by tetramethyl-p-phenylenediamine; (iii) ascorbate plus tetramethyl-p-phenylenediamine, presumably by donating electrons to cytochrome c, is an effective reductant for nitrous oxide reductase; (iv) in the presence of the nitrous oxide reductase inhibitor, acetylene, N₂O is promptly produced from nitrite, consistent with the product of nitrite reductase being N₂O.     

冬玉米对氮肥的吸收利用和需求

在不同施氮量下 ,研究了冬玉米对氮肥的吸收利用 ,结果表明 :(1 )冬玉米地上各部分中氮的累积随着用氮量的增加而增加 ,花丝期前的吸收量均多于后期 ,但高氮区的前期吸氮比大于低氮区 ;(2 )营养体氮的转移率随施氮量的增加而降低 ,但绝对量依然是高氮处理大于低氮处理 ,其中雄穗的转移率最高 ,叶的转移量最大 ;(3 )氮肥利用率随施氮量的增加而提高 ,但氮的生产力下降。根据试验结果 ,在肥力好的土地上种植冬玉米以 1 80～ 2 70 kg N/hm2比较适宜     

EUF-N fractions in different soils during a vegetation period in pot and field experiments

Summary Mobilization of soil-borne N, N fertilization and N removal by crops influence EUF-NO₃-N contents as well as EUF-N_org contents in the course of a vegetation period. N mobilization alone (no N fertilization) increases the EUF-N_org contents only temporarily (mainly in May and July), while in December they are almost the same as in March (Table 1). The EUF-NO₃ contents, on the contrary, increase during the vegetation period, so that an increment in NO₃ is registered in unplanted pots in December. This increment is larger the higher the EUF-N_org contents are in March (Table 2).N fertilization increases the contents of both EUF-N_org and EUF-NO₃, so that there is an increment in EUF-N_org as well as EUF-NO₃ in December (Table 2). This finding also applies to field experiments under fallow (Figs. 4 and 5). However, in contrast to the pot experiment, the EUF-N contents in the field experiment were only temporarily increased by N mobilization alone. This means that N immobilization had taken place which had not been observed in the pot experiment under stable moisture conditions (Fig. 4 and Table 1).A close correlation between hot-water-soluble N contents and EUF-N_org is found only under uniform management conditions (uniform N-fertilizer rates). Depending on the time of sampling different regression equations are, however, obtained because of changes in EUF-N_org due to N mobilization, whereas the hot-water-soluble N contents hardly show any variations during the vegetation period (Fig. 6 and Table 3).     

Distribution and remobilization of symbiotically fixed nitrogen in soybean (Glycine max)

Partitioning of nitrogen by soybeans ( Glycine max L. Merr. cv. Hodgson) grown in natural conditions was studied by successive exposures of root systems to ¹⁵N₂ and periodical measurements of ¹⁵N distribution. Nitrogen derived from the atmosphere was mainly found in the aerial parts of the plants, and the stage of development exerted a strong influence on the initial ¹⁵N distribution (measured one week after incorporation). Until day 69 after sowing, leaf blades contained 47 to 57% of the fixed N. After that, reproductive structures attracted increasing proportions, 10 to 60% between days 69 and 92. Around day 82, stems and petioles stored up to 30% of the newly fixed N. During pod development and pod filling and until maturity, fixed N was remobilized from vegetative tissues and pod walls to seeds. These transfers first concerned the newly incorporated N, but at maturity 80 to 90% of the total was recovered in the seeds. The high mobility of N originating from the atmosphere as compared to that coming from the soil (vegetative tissues exported only 50% of their total N) seems to indicate that fixed N was at least partially integrated in a special pool. This was certainly the case at the later stage of N₂ fixation, when a large portion of fixed N accumulated in the stems and petioles, probably in the form of storage compounds such as ureides for later transfer to the developing seeds. Further research is needed in order to investigate the nature and role of this pool in the nitrogen nutrition of soybeans.     

Prediction of long-term fertilizer nitrogen requirements of maize in the tropics using a nitrogen balance model

A simple N balance model was used to calculate fertilizer requirement for a target N uptake by maize. Nitrogen uptake from soil sources and target uptake of N with fertilizer N additions were obtained from fertilizer trials in Africa and Latin America. Most experiments had data for only one cropping period, although some from Latin America had data for four to six crops. The transfer coefficient of fertilizer N to the crop was adjusted to realize maximum recovery of fertilizer N under best methods of fertilizer application. The time constants of transfer of soil N to the crop were allowed to vary and were affected mainly by soil texture. Where 4 to 6 cropping periods were available good agreement between actual and predicted fertilizer N requirements was obtained. With this approach long-term fertilizer N requirements for 14 sites were predicted using first cropping period N uptake. This study showed that pools of organic N in more coarse-textured soils were usually smaller and declined more rapidly than in fine-textured soils. Labile organic N pools declined with time under all simulations, but approached equilibrium within 10 croppings seasons. Equilibrium N uptake from the soil organic N pool was predicted to be 31 kg ha^–1 for the more coarse-textured soils and 36 kg ha^–1 for the fine-textured soils. Long-term projections of fertilizer requirements using input data of the field experiments were reasonable, and effects of legume green manures and other amendments could be clearly evaluated.     

P effects on N uptake and remobilization during regrowth of Italian ryegrass (Lolium multiflorum)

The influence of P deficiency on the utilization of two sources of N, mineral N (exogenous N) and reserved N (endogenous N), for regrowth of Italian ryegrass (Lolium multiflorum) was studied. P-sufficient (+P) or P-free (−P) nutrition solution was applied from 7 days before defoliation to 24 days of regrowth and the N flows derived from two different N sources within the plant were quantified by ¹⁵N pulse-chase labeling. Shoot regrowth significantly reduced by 12 days of regrowth, while root growth was more in −P plants. Inorganic P (P_i) concentration was highly reduced by P deprivation more in the stubble and regrowing shoots and less in the roots. At defoliation, P deprivation had induced a higher accumulation for all N compounds in the stubble and for amino acids in the roots. The previously incorporated ¹⁵N in stubble and roots as nitrate and amino acids was much decreased in −P plants especially for the first 6 days of regrowth. Total N content in the regrowing leaves was not significantly different between +P and −P plants, but percentage contribution of remobilized N for total leaf N formation was significantly higher in −P plants (78%) than in +P plants (69%) at 6 days of regrowth. From day 12, the utilization of both endogenous and exogenous N was apparently inhibited in −P plants.     

Simulation of nitrogen assimilation by heterotrophic soil microbial biomass

Assimilation of N by heterotrophic soil microbial biomass is associated with decomposition of organic matter in the soil. The form of N assimilated can be either low molecular weight organic N released from the breakdown of organic matter (direct assimilation), or NH⁺₄ and NO⁻₃ from the soil inorganic N pool, into which mineralized organic N is released (mineralization immobilization turnover). The kinetics of C and N turnover in soil is quantifiable by means of computer simulation models. NCSOIL was constructed to represent the two assimilation schemes. The rate of N assimilation depends on the rate of C assimilation and microbial C/N ratio, thereby rendering it independent of the assimilation scheme. However, if any of the N forms is labeled, a different amount of labeled N assimilation will be simulated by the different schemes. Experimental data on inorganic N and ¹⁵N and on organic ¹⁵N dynamics in soils incubated with ¹⁵N added as NH⁺₄ or organic N were compared with data simulated by different model schemes. Direct assimilation could not account for the amount of ¹⁵N assimilated in any of the experimental treatments. The best fit of the model to experimental data was obtained for the mineralization immobilization turnover scheme when both NH⁺₄ and NO⁻₃ were assimilated, in proportion to their concentration in the soil.     

Localization of Cu and heme a on cytochrome c oxidase polypeptides.

After mild dissociation of cytochrome $\text{c}$ oxidase protomers, and polyacrylamide gel electrophoresis, copper was found predominantly in polypeptides of Bands V (m.w. 12,100) and VII (m.w. 3,400), and heme a predominantly in polypeptides of Bands I (m.w. 35,300) and II (m.w. 21,000). Some copper was found in Band II – III, and heme a in Band V.