燕麦-绿豆间作效应及氮素转移特性

为探究燕麦(Avena sativa)-绿豆(Phaseolus radiatus)间作效应及氮素转移特性, 在不施氮肥的大田试验条件下, 设置3种种植模式(燕麦单作、绿豆单作和燕麦-绿豆间作), 采用传统挖根法和¹⁵N同位素标记法进行研究。结果表明, 间作系统中燕麦侵袭力强于绿豆, 绿豆生长受到抑制。整个生育期, 间作燕麦地上部干物质积累量比单作增加14.9%-33.1%, 2年成熟期间作燕麦的氮素积累量比单作分别提高53.1%和44.8%; 间作减少了开花结荚期绿豆氮素积累量和根瘤重量, 降低了绿豆的固氮效率, 绿豆的固氮效率2年平均降低23.7%, 生物固氮量平均减少11.66%。间作绿豆向燕麦的氮素转移率2年平均值达31.7%, 氮素转移量为212.16 kg∙hm^-2。燕麦-绿豆间作降低了开花结荚期绿豆的根瘤固氮酶活性和固氮效率, 但绿豆体内氮素转移增加了燕麦对氮素的吸收利用, 实现了地上部与地下部生长的相互调节和促进, 优化了农田生态系统的氮素管理。     

水稻-雍菜间作系统中种间关系和水稻的硅、氮营养状况

间作是一种优良的生态农业模式,但以水稻为主的水生作物间作研究很少.本试验以水稻和雍菜为研究对象,开展了连续两年(2014—2015年)四季的大田试验,研究水稻和雍菜间作条件下产量、种间关系以及水稻的硅、氮营养状况.试验共设置5个处理,包括水稻单作、雍菜单作、水稻-雍菜2∶2间作、3∶2间作、4∶2间作.结果表明: 水稻和雍菜间作显著增加水稻的产量,其中2∶2间作、3∶2间作和4∶2间作在单位面积上的增产幅度分别为77.5%～120.6%、64.9%～80.9%、37.7%～56.0%,但间作显著降低了雍菜的产量.从土地当量比(LER)来看,水稻和雍菜间作可增加系统的综合产量,3种间作的LER全部大于1,其中3∶2间作模式最佳.从竞争指数来看,在间作系统中,水稻比雍菜有更强的竞争能力,特别是在早季.与水稻单作相比,水稻-雍菜间作显著增加水稻叶片对硅和氮的吸收量以及成熟期水稻叶片的硅含量,但是并没有增加水稻叶片的氮含量,甚至在成熟期略低于单作;而对土壤有效硅、铵态氮和硝态氮含量没有显著影响.在整个试验期间,与水稻单作和间作相比,雍菜单作始终有最高的土壤有效硅、铵态氮和硝态氮含量.本研究表明,水稻和雍菜间作可以促进水稻对硅和氮的吸收,增加水稻的竞争能力.     

不同间作模式对辣椒养分利用、主要病虫害及产量的影响

在云南省丘北辣椒示范区对辣椒-花生、辣椒-大豆和辣椒-玉米间作模式进行调查研究.结果表明,总体上,间作系统中辣椒叶片N、P和 K含量均显著高于辣椒单作,其中辣椒-玉米(10 ∶2)间作系统中辣椒叶片N、P和K含量分别比单作增加12.93%、 5.17%和22.64%.与辣椒单作相比,辣椒间作显著提高了盛果期辣椒的株高和单株结果数,提高幅度分别为1.57%～20.89%和3.06%～307.52%;有效控制了辣椒病毒病、疫病和烟青虫的发生,控制效果分别达24.01%、6.87%～23.80%和4.31%～36.40%;辣椒间作显著提高了辣椒的生物量和产量,辣椒产量的增幅为9.73%～53.52%,起到了明显的增产、增值效果.初步筛选出的辣椒-花生(15∶5)、辣椒-大豆(8∶2)和辣椒-玉米(10 ∶2)三种辣椒间作模式供进一步生产示范.     

减量施氮对玉米-大豆套作体系中作物产量及养分吸收利用的影响

通过田间试验研究了种植方式(玉米单作、大豆单作、玉米-大豆套作)和施氮水平(0、180、240 N kg·hm-2)对玉米和大豆产量、养分吸收及氮肥利用的影响.结果表明:与单作相比,玉米-大豆套作体系中玉米籽粒产量、地上部植株N、P、K吸收量及收获指数略有降低,而大豆籽粒产量、地上部植株N、P、K吸收量及收获指数显著提高.玉米-大豆套作系统的套作优势随施氮量的增加而降低,与当地农民常规施氮量(240 kg·hm-2)相比,减量施氮(180kg·hm-2)处理下玉米和大豆产量、经济系数,以及N、P、K吸收量和收获指数、氮肥农学利用率、氮肥吸收利用率显著提高,土壤氮贡献率降低;与不施氮相比,减量施氮降低了玉米带土壤的全N、全P含量,提高了大豆带土壤的全N、全P、全K含量和玉米带土壤的全K含量.减量施氮水平下,玉米-大豆套作系统的周年籽粒总产量、地上部植株N、P、K总吸收量均高于玉米和大豆单作,土地当量比(LER)达2.28;玉米-大豆套作系统的氮肥吸收利用率比玉米单作高20.2%,比大豆单作低30.5%,土壤氮贡献率比玉米和大豆单作分别低20.0%和8.8%.玉米-大豆套作减量一体化施肥有利于提高系统周年作物产量和氮肥利用率.     

减量施氮与大豆间作对蔗田氮平衡的影响

通过2010—2013年的大田试验,探讨了2个施氮水平(300和525 kg·hm-2)和3种种植模式(甘蔗、大豆单作及甘蔗-大豆1∶2间作)对蔗田大豆固氮、甘蔗和大豆氮素累积及氨挥发和氮淋溶的影响.结果表明:与大豆单作相比,甘蔗-大豆间作的大豆固氮效率下降,但不同施氮水平间作模式之间无显著差异.不同施氮水平和种植模式对甘蔗、大豆氮素累积无显著影响.减量施氮水平下氨挥发量低于常规施氮处理,不同施氮水平和种植模式对氮淋溶量无显著影响.除2011年甘蔗单作减量施氮水平下出现蔗田氮素亏缺(-66.22 kg·hm-2)外,其余不同年份不同种植模式下氮素都处于盈余状态(73.10~400.03 kg·hm-2),施氮水平显著影响了蔗田的氮素盈亏,且常规施氮水平下氮素盈余量显著高于减量施氮处理,过高的氮素盈余增加了氮素污染农田环境的风险.从培肥地力、降低氮素污染环境的风险和节约生产成本等方面考虑,减量施氮水平下甘蔗-大豆间作模式具有一定的生态合理性.     

紫云英翻压量与不同施氮量对水稻生长和氮素吸收利用的影响

为了筛选出紫云英翻压量和氮肥的最佳配施比例,从而为实际生产提供理论依据,本试验采用裂区设计,以空闲、不施氮为对照处理CK1,以空闲、常规施氮为对照处理CK2,紫云英翻压量设翻压27000、45000 kg·hm-2两个水平,施氮量设不施氮、施氮量60、120和180 kg·hm-2四个水平,研究紫云英翻压量与不同施氮量对水稻产量、干物质积累和氮素吸收利用的影响。结果表明:紫云英27000 kg·hm-2+N≥120 kg·hm-2和紫云英45000 kg·hm-2+N≥60 kg·hm-2即可保证水稻产量和生长,其中处理M1N2的产量最高,较常规施氮处理CK2高出11.56%;成熟期处理M2N1的干物质积累量最大,比CK2高21.41%;处理M2N3的氮素吸收量最大,比CK2高5.32%;而氮肥表观利用率和氮肥真实利用率均随着氮肥施用量的增加而减小;所以紫云英27000 kg·hm-2+N120 kg·hm-2和紫云英45000 kg·hm-2+N 60 kg·hm-2两种施肥方式能够在保证水稻产量的同时,有效提高氮肥利用率,有利于资源的高效利用。     

施氮对间作蚕豆根际微生物区系和枯萎病发生的影响

通过田间小区试验,研究了小麦、蚕豆间作条件下4个施氮水平(0,56.25,112.5kg.hm-2和168.75kg.hm-2)对蚕豆根际微生物区系和蚕豆枯萎病发生的影响。结果表明,单作和间作条件下,施氮显著增加了蚕豆根际的微生物数量,在N2(112.5kg.hm-2)水平下达到最高值;施氮对土壤微生物多样性无显著影响,但减轻了单、间作蚕豆枯萎病的发生,且在N2水平下发病最轻。与单作相比,间作显著增加了蚕豆根际的细菌、真菌、放线菌数量、微生物总数和微生物多样性,尤其在N0、N1(56.25kg.hm-2)和N2(112.5kg.hm-2)水平下间作对蚕豆根际微生物的促进效应明显,且以真菌和放线菌的增幅较大.N0、N1和N2水平下间作显著降低了蚕豆枯萎病的发病率和病情指数。小麦蚕豆间作下适量施氮能有效调节蚕豆根际微生物区系,是抑制蚕豆枯萎病发生的有效措施。     

甘蔗-甜玉米间作对甘蔗产量、品质及经济效益的影响

通过甘蔗田间定位试验研究了种植模式(甘蔗单作、甘蔗-甜玉米间作(1∶1、2∶1)和施氮水平(300、525 kg·hm-2)对甘蔗群体经济效益、甘蔗产量、生物量积累动态变化及品质的影响。结果表明:低氮水平(300 kg·hm-2)下,甘蔗-甜玉米间作(1∶1、2∶1)的经济效益分别高于单作甘蔗52.67%和20.59%,土地当量比(LER)均大于1,且甘蔗-甜玉米1∶1间作模式的LER高于甘蔗-甜玉米2∶1间作31.50%;高氮水平(525 kg·hm-2)下,甘蔗-甜玉米1∶1间作的经济效益和土地利用率分别高于单作26.25%和36.00%,而甘蔗-甜玉米2∶1间作与甘蔗单作相比无间作优势;甘蔗-甜玉米间作中,因间作甘蔗最大生长速率(v m)减小,理论最大值(w m)、最快生长日(t m)等生物量动态累积特征参数的协调性劣于单作甘蔗,使间作甘蔗产量低于单作甘蔗9.72%~33.17%,而间作甜玉米产量比单作甜玉米高14.10%~24.43%;相比甘蔗单作,甘蔗-甜玉米间作对甘蔗品质无显著影响;甘蔗-甜玉米间作是实现甘蔗优质、高效种植的可行途径,其中甘蔗-甜玉米1∶1间作模式更为优化。     

土著从枝菌根真菌(AMF)与不同形态氮对紫色土间作大豆生长及氮利用的影响

在紫色土上,探究接种土著AMF(indigenous arbuscular mycorrhizal fungi)及不同形态氮肥施用对间作大豆Glycine max生长及氮利用的影响,为提高间作大豆对土壤不同形态氮素的吸收与利用,减少土壤无机氮残留提供理论依据。采用盆栽试验,设2种种植方式(大豆单作和玉米/大豆间作),不同丛枝菌根真菌处理[不接种(NM)、接种土著AMF]和3个氮处理[不施氮(N0)、施无机氮(ION120)、施有机氮(ON120)],以期揭示土著AMF和不同形态氮施用对间作大豆生长及氮素吸收利用的影响。结果表明:与N0相比,施ION120和ON120处理显著增加了土壤无机氮的累积量。NM条件下,无论何种施氮处理的间作土壤NH_4~+-N、NO_3~--N含量均低于单作,其中当接种土著AMF时,与单作相比,间作对减少土壤无机氮的积累能力得到进一步加强。无论单作或是间作,相同菌根处理下,ION120和ON120处理的大豆地上部和根系生物量,大豆地上部和根系氮含量及大豆地上部和根系氮吸收量均不同程度地高于N0处理,其中间作-土著AMF条件下,ION120处理的根系生物量、根系氮含量及氮吸收量均显著高于ON120处理。间作-ION120条件下,土著AMF处理的大豆地上部氮含量、吸收量及根系氮含量、氮吸收量较NM处理分别提高了9.8%、69.8%和8.1%、54.8%,四者差异均达到显著水平。除根系氮吸收量外,地上部氮含量、氮吸收量及根系氮含量均在间作-土著AMF-ION120处理下显著提高,间作与土著AMF互作优势明显。间作-土著AMF条件下,ION120和ON120处理的大豆根系氮吸收效率高于N0处理,分别提高了2%和6%。总体来看,土著AMF与ION120氮肥施用对促进间作大豆生长与提高氮素利用率尤为明显,可望减少土壤氮素残留而减轻氮素流失的风险。     

不同氮水平下作物养分吸收与利用对玉米马铃薯间作产量优势的贡

玉米与马铃薯间作是重要的间作种植模式,具有较突出的资源利用和产量优势,但养分吸收和利用对作物产量优势的贡献及这种贡献对施氮量的响应机制尚不清楚.本研究采用玉米单作、马铃薯单作和玉米与马铃薯间作3种种植模式,分别设置N_0(0 kg·hm~(-2))、N_1(125 kg·hm~(-2))、N_2(250 kg·hm~(-2))和N_3(375 kg·hm~(-2))4个氮水平,通过2年田间小区试验,研究不同氮水平下间作产量优势的营养基础.结果表明:随着施氮量的增加,氮、磷、钾的单作加权平均吸收量逐渐增加,间作则先增加后减少.间作在N_1水平时具最高的养分吸收优势,分别较单作加权平均值增加氮吸收14.9%、磷吸收38.6%、钾吸收27.8%;间作在N0和N3时具有更高的养分利用效率,较单作可提高氮利用效率3.5%~14.3%、磷利用效率3.5%~18.5%、钾利用效率10.6%~31.6%.N_0和N_1时玉米与马铃薯间作具有显著产量优势,其营养基础在N0时主要是提高了作物养分利用效率,而N_1时则是促进养分吸收的结果.充分发挥间作促进养分吸收对玉米与马铃薯间作产量优势的贡献,需要合理控制氮肥的投入.     

L value determination under paddy soil condition

Summary The L values of four paddy soils and one United Kingdom soil were determined under water-logged and aerobic conditions over a period of 7 weeks using rice and ryegrass as the respective test crops.Under water-logged conditions, the L values attained a constant level in the course of the growing period, indicating that isotopic equilibrium between the added P³² and the soil was achieved.Under aerobic conditions, the equilibrium L values tended to be lower than those determined under water-logged conditions.This was taken as an indication of an increase of labile soil phosphorus by reduction of ferric iron.     

覆盖旱作水稻群体发育特征分析

通过田间试验,研究了不同覆盖旱作水稻处理与水作处理水稻的群体生育特征。结果表明,旱作水稻营养生长期较水作长,叶片变短、变窄,群体LAI变小,光合生产能力下降,最终粒数变少、粒重变轻,不同旱作处理之间表现为地膜覆盖旱作处理分蘖发生多,成穗率低,穗分化和籽粒形成与灌浆时间缩短,半腐解秸秆覆盖旱作和裸地旱作分蘖发生少,成穗率高,穗分化时间缩短,籽粒形成与灌浆的时间延长,产量表现为水作处理>地膜覆盖旱作>半腐解秸秆覆盖旱作>裸地旱作。     

Host response of rice genotypes to the rice root-knot nematode (Meloidogyne graminicola) under aerobic soil conditions

Aerobic rice is a production system where adapted rice varieties are established via direct seeding in non-puddled, non-flooded, non-saturated fields and grown under conditions similar to upland conditions. On land cultivated continuously with aerobic rice, a yield reduction has been observed. The rice root-knot nematode Meloidogyne graminicola is considered one of the possible causes of these yield reductions. Resistance to and tolerance for M. graminicola are essential traits for aerobic rice cultivars in alleviating this problem. In our study, the host response of nineteen aerobic, seven upland and four lowland rice genotypes which are either being used in the International Rice Research Institute’s aerobic rice breeding programme or already cultivated by farmers in Asia was evaluated under aerobic soil conditions in an outdoor raised-bed experiment. Our study showed a large variation in susceptibility and sensitivity to M. graminicola infection among the rice genotypes examined. Resistance comparable to the resistant reference genotypes included in the experiment (CG14, TOG5674, TOG7235) was not found but in terms of susceptibility, the upland genotype Morobereken may be an interesting less-susceptible genotype. Tolerance was found and in terms of sensitivity, the high yielding aerobic genotype IR78877-208-B-1-2 may be an interesting tolerant genotype. Our study also allowed the identification of rice genotypes that are either highly susceptible or sensitive to M. graminicola infection and of which the cultivation should be discouraged. On average, M. graminicola caused an almost 30% reduction in yield. Excluding the two susceptible and three resistant reference genotypes included in the experiment, most affected was dry-shoot biomass (23.6% reduction) followed by root length, which was more affected than fresh-root weight (19.8 vs. 8%) and grain filling (17.3%), while plant height and the number of spikelets/panicle were less affected (10.2 and 8.1%, respectively). Neither tillering nor the number of panicles/plant were affected.     

Soil Texture and Cultivar Effects on Rice (Oryza sativa,L.) Grain Yield,Yield Components and Water Productivity in Three Water Regimes

The objective of this study was to determine the effects of water regime/soil condition (continuous flooding, saturated, and aerobic), cultivar (‘Cocodrie’ and ‘Rondo’), and soil texture (clay and sandy loam) on rice grain yield, yield components and water productivity using a greenhouse trial. Rice grain yield was significantly affected by soil texture and the interaction between water regime and cultivar. Significantly higher yield was obtained in continuous flooding than in aerobic and saturated soil conditions but the latter treatments were comparable to each other. For Rondo, its grain yield has decreased with soil water regimes in the order of continuous flooding, saturated and aerobic treatments. The rice grain yield in clay soil was 46% higher than in sandy loam soil averaged across cultivar and water regime. Compared to aerobic condition, saturated and continuous flooding treatments had greater panicle numbers. In addition, panicle number in clay soil was 25% higher than in sandy loam soil. The spikelet number of Cocodrie was 29% greater than that of Rondo, indicating that rice cultivar had greater effect on spikelet number than soil type and water management. Water productivity was significantly affected by the interaction of water regime and cultivar. Compared to sandy loam soil, clay soil was 25% higher in water productivity. Our results indicated that cultivar selection and soil texture are important factors in deciding what water management option to practice.     

From Flooded to Aerobic Conditions in Rice Cultivation: Consequences for Zinc Uptake

Scarcity of water causes a shift from flooded to aerobic conditions for rice production in zinc deficient areas in Northern China. This shift alters soil conditions that affect zinc availability to the crop. This paper concerns the effect of aerobic compared to flooded conditions on crop biomass production, grain yield and zinc content. A field experiment was done with six rice genotypes (Oryza sativa L.) grown on a calcareous soil, both with (23 kg Zn ha⁻¹) and without Zn fertilization. Sampling was conducted at tillering and physiological mature stage. Zn concentration in the shoots was significantly lower at both stages in plants grown in the aerobic field. At maturity, Zn uptake, biomass production, grain yield and Zn-harvest index [grain Zn/(shoot + grain Zn)] were lower under aerobic cultivation. Rice genotypes including aerobic rice and lowland rice differ in degree of response to low Zn supply. A twofold difference was found among aerobic genotypes in grain yield and Zn uptake. Also Zn-harvest index varied significantly. Zn application affected neither grain yield nor grain Zn content, although it significantly improved biomass production in both systems in most genotypes. These results demonstrate that introduction of aerobic rice systems on calcareous soils may increase Zn deficiency problems.     

不同水分管理方式下水稻的水分利用效率与产量

采用温室微区试验研究常规水作、裸地旱作、覆膜旱作和覆草旱作等土壤水分管理下水稻生长及其对水分的利用状况。结果表明,几种旱作水稻的需水量为349-473mm,常规水和水稻需水量为762.5mm。旱作水稻的水分籽粒和干物质生产效率为0.899-1.273g·kg^-1和1.655-2.321g·kg^-1之间,而相同条件下常规水作水稻水分的籽粒和干物质生产效率为0.766g·kg^-1和1.459g·kg^-1左右。覆草旱作水稻可以获得相当于常规水作水稻90％的经济产量。     

直播旱作水稻的吸氮特征与土壤氮素表观盈亏

水稻旱作是水稻节水栽培中最有效的方式。通过田间试验研究旱作直播条件下水稻对氮素的吸收利用特征以及土壤矿质氮的动态变化 ,并对土壤氮素的表观盈亏量进行了估算。结果表明 ,直播旱作水稻较水作水稻更注重中后期对氮素养分的吸收 ,尤其是对土壤氮素的吸收 ;幼穗分化后水稻的土壤吸氮量占阶段吸氮总量的 6 9.5 % ,比水作水稻多 17.8%。对 0～ 4 0 cm土层土壤矿质氮含量时空变化的研究表明 ,直播旱作水稻生育前期土壤表层矿质态氮大量累积 ,在灌水和降雨的影响下 ,向下层的迁移增加 ,基肥施用后裸地处理 2 0～ 4 0 cm土层的矿质氮高达 10 4 kg N/hm2 。对水稻各生育期土壤氮素盈亏的计算结果表明 ,自分蘖盛期后旱作各处理都表现出土壤氮素不同程度上的表观亏缺 ,然而就全生育期土壤氮素盈余量而言 ,旱作处理平均高达 12 7kg N/hm2 ,生育前期氮肥的大量投入是氮素盈余的主要原因。本试验结果表明 ,直播旱作水稻生育前期对施用的肥料氮吸收很少 ,提高直播旱作水稻氮肥利用效率的关键在于减少生育前期肥料氮的投入     

Alleviating soil sickness caused by aerobic monocropping: responses of aerobic rice to soil oven-heating

“Aerobic rice” system is the cultivation of nutrient-responsive cultivars in nonflooded and nonsaturated soil under supplemental irrigation. It is intended for lowland areas with water shortage and for favorable upland areas with access to supplementary irrigation. Yield decline caused by soil sickness has been reported with continuous monocropping of aerobic rice grown under nonflooded conditions. The objective of this study was to determine the growth response of rice plant to oven heating of soil with a monocropping history of aerobic rice. A series of pot experiments was conducted with soils from fields where rice has been grown continuously under aerobic or anaerobic (flooded) conditions. Soil was oven heated at different temperatures and for various durations. Plants of Apo, an upland variety that does relatively well under the aerobic conditions of lowland, were grown aerobically without fertilizer inputs in all six experiments. Plants were sampled during vegetative stage to determine stem number, plant height, leaf area, and total biomass. Heating of soil increased plant growth greatly in soils with an aerobic history but a relatively small increase was observed in soils with a flooded history as these plants nearly reached optimum growth. A growth increase with continuous aerobic soil was already observed with heating at 90°C for 12 h and at 120°C for as short as 3 h. Maximum plant growth response was observed with heating at 120°C for 12 h. Leaf area was most sensitive to soil heating, followed by total biomass and stem number. We conclude that soil heating provides a simple and quick test to determine whether a soil has any sign of sickness that is caused by continuous cropping of aerobic rice.     

The effect of deep placement and surface application of nitrogen fertilizers at different light intensities on growth and yield of wetland rice

Summary Lowland rice (RD 3) was cultivated in containers of clay soil submerged with 5 cm water under controlled conditions in the phytotron. Deep placement of urea supergranules 5 cm in the soil significantly enhanced both plant growth and fertilizer efficiency when the plants were cultivated under high light intensity (70 Wm^–2). At the highest urea level grain yield increased 119% above the control level, while growth and fertilizer efficiency was not as high when deep placement of calcium nitrate was used.The application of urea prills and calcium nitrate (18.4g Nm^–2) in two split doses on the soil surface increased grain yield as much as 91% above the control level. At the lower nitrogen concentration (9.2 g N m^–2), the urea prills were more efficient than calcium nitrate as indicated by the grain yield. The height of those plants fertilized by surface application was affected by the concentration and not the type of fertilizer. The number of tillers, however, was significantly higher on urea fertilized plants.When the rice plants were cultivated under low light intensity 930 Wm^–2), neither the nitrogen fertilizers nor the method of application had a significant effect on growth and yield.     

Effects of Amendments and Water Conditions on the Chemical Speciation of Cd and Pb in Contaminated Paddy Soil in a Mining Area

Lime, sepiolite and peat were used as amendments to study their effects on the chemical speciation of Cd and Pb in a polluted paddy soil under moist and water-logged conditions. The results showed that application of amendments reduced acid-extractable Cd (up to 12.56% and 5.07%) and Pb (up to 6.69% and 2.68%) in moist and water-logged soils, respectively. The reducible Cd and residual Cd was increased while the oxidizable Cd was decreased after adding amendments. However, the oxidizable Pb was increased while the residual Pb was decreased in amended soil, and the reducible Pb presented a different changing trend under moist and water-logged conditions. The soil pH was significantly correlated with different fractions of Cd and Pb in soil, which indicated a distinct influence of soil pH on the redistribution process of Cd and Pb fractions in amended soil.