限水灌溉下施氮量对冬小麦产量、氮素利用及氮平衡的影响

2008~2009年通过大田试验,研究了限水灌溉条件下,不同施氮量对冬小麦产量、氮素利用、土壤硝态氮动态变化及氮素平衡的影响。结果表明,施用氮肥显著增加小麦穗数和穗粒数,对千粒重无显著影响。作物产量、吸氮量与施氮量均呈抛物线关系,施氮量超过N240 kg/hm2,产量和吸氮量随施氮量增加略有降低。小麦起身期后,0—100 cm土层都有硝态氮分布,且随土层深度增加而减少;相同土层则随施氮量的增加而增加。土壤硝态氮积累量随生育期推进而降低,N0和N120处理分别在拔节期和开花期后表现出氮素亏缺;成熟期,土壤表观盈余以残留为主,表观损失量占小部分。氮肥表观利用率、农学利用率随施氮量增加呈降低趋势,而氮素残留率随施氮量增加呈增加趋势。在本试验条件下,施氮量在N 180~220 kg/hm2水平可以达到产量、氮素表观利用率、氮素残留率的较好结合,是限水灌溉下兼顾经济效益与环境效益的适宜施氮量。     

Increased Dryland Winter Wheat Yields by Nitrogen Fertilizer Topdressing and its Relationship to Soil Moisture,Available N,P and K in Northwestern China

Winter wheat (Triticum aestivum L.) production in northwestern China as a monoculture is hampered by unfertile soil and drought. With the fast-developing Chinese chemical fertilizer industry, many farmers now use more nitrogen (N) fertilizer as topdressing for winter wheat in early spring, in addition to a basal dose of N fertilizer applied in the previous autumn at seeding time. The objective of this study was to evaluate the increase in grain yield of dryland winter wheat by early spring N fertilizer topdressing, and its relationship to soil moisture, available N, phosphorus (P) and potassium (K). Field experiments with no N fertilizer topdressing (F_b) and N fertilizer topdressing (F_b+t) treatments were carried out over two growing seasons at 54 site-years to assess the relationship between increase in winter wheat grain yield by early spring N fertilizer topdressing and soil moisture, available N, P and K in Changwu county, Shaanxi province, China. Compared to F_b treatment, the F_b+t treatment produced grain yields lower at 10 site-years, and increased by <10% at 21 site-years and by >10% at 23 site-years. The results indicated that topdressing N fertilizer could increase wheat grain yield when soil nitrate-N accumulation in the 0–20, 20–40 and 40–60 cm depths was less than 121.7, 36.4 and 24.1 kg N ha^?1, and soil moisture content in the 40–60, 60–80 and 80–100 cm depths was more than 15.7%, 16.7% and 16.9%, respectively. The findings also suggested that it is not necessary to analyze soil for ammonium-N, available P and K before topdressing N fertilizer. It is necessary to analyze 0–60 cm soil profile for nitrate-N and 40–100 cm depth for soil moisture before topdressing N fertilizer for winter wheat in dryland areas of northwestern China.     

过量施氮对旱地土壤碳、氮及供氮能力的影响

【目的】过量施氮会影响土壤有机碳、氮的组成与数量,进而改变土壤供氮能力,但关于西北旱地长期过量施用氮肥后土壤有机碳、氮及土壤供氮能力变化的研究尚缺乏。本文在长期定位试验的基础上,通过分析不同氮肥水平特别是过量施氮条件下土壤硝态氮,有机碳、氮和微生物量碳、氮的变化,探讨长期过量施氮对土壤有机碳、氮及供氮能力的影响。【方法】长期定位试验位于陕西杨凌西北农林科技大学农作一站。在施磷(P2O5)100kg/hm2的基础上,设5个氮水平,施氮量分别为N 0、80、160、240、320 kg/hm2。重复4次,小区面积40 m2,完全随机区组排列。种植冬小麦品种为小堰22。本文选取其中3处理,以不施氮为对照(N0)、施氮量N 160 kg/hm2为正常施氮(N160),施氮量N 320 kg/hm2为过量施氮(N320),分别于2012年6月小麦收获后和10月下季小麦播前采集土壤样品,进行测定分析。【结果】过量施氮导致下季小麦播前0—300 cm各土层硝态氮含量显著增加,平均由对照的2.8 mg/kg增加到15.5 mg/kg;同时,0—60 cm和0—300 cm土层的硝态氮累积量分别由对照的47.2和108.9 kg/hm2增加到76.5和727.7 kg/hm2。过量施氮也增加了夏闲期间0—300 cm土层土壤有机氮矿化量,由对照的72.4 kg/hm2增加到130.7 kg/hm2。但过量施氮未显著增加土壤的有机碳含量,却显著增加了土壤有机氮含量,过量施氮0—20、20—40 cm土层土壤有机碳分别为9.24和5.39 g/kg,有机氮分别为1.05和0.71 g/kg,较对照增加52.2%和54.3%。同样,过量施氮未显著影响0—20、20—40 cm土层土壤微生物量碳含量,其平均含量分别为253和205 mg/kg,却显著提高了0—20、20—40 cm土层土壤微生物量氮含量,由对照的24.1和7.5 mg/kg提高到43.6和16.1 mg/kg。【结论】过量施氮可以显著增加旱地土壤剖面中的硝态氮累积量、夏闲期氮素矿化量、小麦播前土壤氮素供应量和土壤微生物量氮含量,但对土壤有机碳和微生物量碳没有显著性影响,同时过量施氮增加了土壤硝态氮淋溶风险,故在有机质含量低的黄土高原南部旱地冬小麦种植中不宜施用高量氮肥,以减少土壤氮素残留和农业投入,达到保护环境和培肥土壤的目的。     

Influence of Cocoa Pod Husk-Based Compost on Nutrient Uptake of Okra (Abelmoschus esculentus (L.) MOENCH) and soil properties on an Alfisol

This experiment evaluated the potentials of cocoa pod husk (CPH)-based compost on okra and soil chemical properties. Three CPH-based compost: CPH+ Neem leaf (CPH+ NL), CPH+ Poultry manure (CPH+ PM) and CPH+ PM+ NL were prepared. The treatments; 25, 50, 75, 100 kg N/ha of each compost and NPK mineral fertilizer at 40, 50, 60 kg N/ha and control, were applied to 5 kg soil each and arranged in a completely randomized design in three replicates. Two varieties of okra (NH47-4 and LD88) were grown for six weeks and residual effect evaluated. The Nitrogen, Phosphorus, and Potassium uptake of okra were determined. Pre- and post-cropping soil analyses were done. Data were analyzed using ANOVA and means separated by Duncan Multiple Range Test at α_0.05. The results showed that the nutrient uptake of okra consistently increased with CPH-based compost compared to control in both main and residual cropping. Nitrogen uptake ranged from 53.6 (60 kg N/ha NPK) to 106.7 (50 kg N/ha CPH+ PM) and 16.10 (50 kg N/ha NPK) to 55.06 (25 kg N/ha CPH+ PM+ NL); Phosphorus uptake ranged from 6.9 (25 kg N/ha CPH+ NL) to 24.1 (60 kg N/ha NPK) and 3.70 (25 kg N/ha CPH+ NL) to 9.98 (50 kg N/ha CPH+ PM+ NL), while potassium uptake ranged from 166.4 (25 kg N/ha CPH+ NL) to 244.48 (25 kg N/ha CPH+ PM+ NL) and 64.06 (40 kg N/ha NPK) to 122.29 (75 kg N/ha CPH+ NL) mg/plant in main and residual cropping, respectively. Organic carbon, pH, nitrogen (N), phosphorus (P), potassium (K), magnesium (Mg) and sodium (Na) were also significantly increased by the CPH-based compost. It could, therefore, be concluded that CPH-based compost could be a good fertilizer for okra production.     

Rabbiteye blueberry plant response to nitrogen and phosphorus

Acid, sandy soils selected for blueberry production are usually deficient in plant available phosphorus. Fertilizer addition at planting has not been a recommended practice. This research was designed to evaluate potted blueberry (Vaccinium ashei Reade) plant growth response to P applied at establishment and interacted with N applied during the growing season. Four liter containerized ‘Tifblue’ rabbiteye blueberry plants were transplanted into 4.4 kg of 1:1 v/v loamy sand:peat mixture in an 8‐liter container. Preplant P was incorporated into the mixture at 0, 20, 40, 60, and 80 kg/ha rates. Nitrogen was split‐applied post‐plant four times at 60‐day intervals beginning 30 days after blueberry bushes were transplanted. Total N rates were equivalent to 0, 112, 224, or 336 kg/ha. Plants were harvested 270 days after transplanting. Phosphorus at the 60 and 80 kg/ha rates increased plant growth 40 and 31%, respectively. Plant growth responded linearly to increasing N rate. Leaf and stem weight increases contributed to this linear response while root weight was not affected by fertilizer N. Total plant dry weight was increased by N rates at the 60 and 80 kg/ha P levels. Phosphorus applications increased leaf P levels, but did not increase soil test P. Leaf redness, caused by cool temperatures, was reduced by high N rates. The optimum P rate for fertilization of the soilrpeat mixture in the planting hole under conditions of this experiment was the equivalent of 60 kg/ha.     

Nitrogen application method for improving yield and protein content of “Kitanokaori”, a new variety of winter wheat for bread use in Hokkaido

(Jpn. J. Soil Sci.Plant Nutr., 77, 273–281, 2006)

“Kitanokaori” is a new variety of winter wheat (Triticum aestivum L.) for bread use bred at the National Agricultural Research Center for Hokkaido Region. The grain protein content of wheat for bread use should be higher than 120 g kg?1. Much nitrogen application is necessary to obtain high grain protein content. Therefore, it is necessary to determine the optimum amount of nitrogen to obtain the required protein content and to prevent nitrogen from remaining in the soil. Field experiments were conducted for four years from sowing in 2000 to study the effect of the amount of nitrogen and the time of top-dressing. In the experiment in which sowing was carried out in 2003, nitrogen treatments were 40, 40–60, 40–60–0–60, 40–60–0–60–30, 40–60–0–60–60, 40–60–60–60, 40–60–60–60–30, 40–60–60–60–60, 40–60–30–30, 40–60–30–30–30 and 40–60–30–30–60 (each value showing the amount of applied nitrogen at sowing · re-growing stage · panicle formation stage · flag leaf stage · full heading stage, kg ha?1). The experiments were conducted in Andosol, which has moderate nitrogen fertility, and in Histosol, which is fertile soil.

Kitanokaori did not lodge with high-applied nitrogen, and both yield and protein content increased with an increase in applied nitrogen. In a moderate climate, Kitanokaori reached a protein content of 120 g kg?1 when the amount of absorbed nitrogen was about 190 kg ha?1, and the yield was about 7·8 Mg ha?1 at that time.

The top-dressing at the panicle formation stage was effective to raise the yield and the top-dressing at the full heading stage was effective to raise the grain protein content. It is recommended that the amount of applied nitrogen should be 160 kg ha?1 until the flag leaf stage, and additional nitrogen should be applied at the full heading stage to obtain a grain protein content of more than 120 g kg?1. Nutritional diagnosis at the full heading stage will be necessary to determine whether more nitrogen is needed to achieve the required protein content.

When the amount of total applied nitrogen did not exceed 220 kg ha?1, the amount of absorbed nitrogen was over 90% of applied nitrogen, and there was little inorganic nitrogen in the soil after harvest. Therefore, it was considered that the residue of nitrogen in the soil was small within 220 kg ha?1 of nitrogen application, while favorable growth and high yield were obtained.     

Contribution of chickpea nitrogen fixation to increased wheat production and soil organic fertility in rain-fed cropping

Nitrogen balances, i.e. the difference between N ₂ fixation inputs and N in harvested products (outputs), and rotational benefits of chickpea ( Cicer arietinum) on soil organic fertility and wheat ( Triticum aestivum) yields were quantified for rain-fed systems in the northern Punjab, Pakistan. The experiments were conducted during 1995–2000 at three sites. The four treatments were continuous wheat (0 N), continuous wheat (+N), chickpea-wheat (0 N) and chickpea-wheat (+N). The +N fertiliser rate was 100 kg N ha ^-1 applied to the wheat. Grain yields of the wheat with 0 N varied in the range 1.0–3.0 t ha ^-1, compared with 2.0–3.2 t ha ^-1 for the N-fertilised wheat. Chickpea grain yields were in the range 0.6–2.0 t ha ^-1. Chickpea N ₂ fixation was assessed using the natural ¹⁵N abundance method. Percentage of chickpea N derived from N ₂ fixation (%Ndfa) estimates were 58% (Mandra), 65% (Taxila) and 86% (Islamabad). The overall mean %Ndfa was 78%. Crop N fixed by the chickpea varied between sites (87–186 kg N ha ^-1) and essentially reflected crop biomass. The overall mean N balance for chickpea (crop N fixed minus N removed in grain and above-ground residues) was +28 kg N ha ^-1. Wheat grain yields responded to chickpea (19–73% increase for the three sites), to fertiliser N (99–136% increase) and to the combination of chickpea and fertiliser N (106–145% increase). Chickpea in the rotation increased soil organic C by 30% and soil N by 38%, relative to the continuous wheat with 0 N. These experiments indicated that chickpea could have a positive N balance, even when shoot residues were removed, and confirmed the rotational benefits of chickpea for improving soil organic fertility and yield of a following wheat crop.     

氮、硫配施对冬小麦氮素利用效率及产量的影响

【目的】氮(N)、硫(S)是生物所必需的营养物质,对小麦籽粒产量和品质起着重要作用。硫素供应不足,特别是在当前大量氮素供应情况下引起的作物生理性缺硫将导致作物产量和含硫氨基酸蛋白质含量下降。本文旨在探索氮、硫配施对冬小麦氮素利用效率和籽粒产量的促进效果并提出合理的区域氮、硫施肥技术。【方法】20122013年,在河南温县以国审冬小麦品种豫麦49-198为供试材料,进行大田试验。设置不同施氮量0、120、180、240和360 kg/hm2(分别以N0、N120、N180、N240和N360表示)和施硫0和60 kg/hm2(S0和S60)试验,调查氮、硫对冬小麦干物质积累、氮素积累分配、籽粒产量和氮素利用效率的影响。【结果】对冬小麦生育后期干物质积累分析表明,干物质积累随施氮量增多而提高,相同施氮量条件下施硫较不施硫小麦干物质积累量显著提高,其中成熟期干物质积累量N180S60、N240S60和N360S60分别较N180S0、N240S0和N360S0提高2225、3607和3120 kg/hm2,而且氮素低的处理添加硫后干物质积累量高于氮素高不加硫处理,如N180S60N240S0、N240S60N360S0,处理间差异均达显著水平。随施氮量增多,冬小麦植株氮素积累总量增加,在N 240和360 kg/hm2水平,硫素供应显著增加小麦植株氮素积累。不同施氮量条件下施硫较不施硫均显著提高了小麦籽粒产量,分别提高了10.5%、18.3%、5.2%、5.6%和4.9%。随施氮量增多,氮肥偏生产力下降,氮回收效率、生理效率和农学效率则均以N 180达最高值。不同施氮水平下,施硫均显著提高了冬小麦氮素回收效率,但对氮生理效率影响不显著,其中在施N量为120、180和240kg/hm2时,施硫较不施硫氮肥偏生产力和农学效率均显著提高。【结论】在当前小麦生产中,采用控氮或减氮增硫技术措施,可实现小麦氮利用效率和籽粒产量的同步提高。在本试验地区小麦生产中,达到冬小麦稳产高效或增产高效的适宜施氮量为180 240 kg/hm2配合60 kg/hm2硫肥施用。     

长期不同氮、 磷用量对冬小麦籽粒锌含量的影响

【目的】小麦是我国西北地区主要的粮食作物,主要种植在低锌的石灰性土壤上,其籽粒锌含量普遍较低,难以满足人们的锌营养需求,因此提高冬小麦籽粒中的锌含量对保证人体健康具有非常重要的意义。氮素、 磷素供应不足或过量会影响冬小麦对锌的吸收与利用,本文基于黄土高原南部9年的长期定位试验,研究了长期不同氮、 磷肥用量对旱地冬小麦籽粒锌含量的影响及籽粒锌含量与氮、 磷吸收与分配的关系,以期为有效调控冬小麦籽粒锌营养品质和优化旱地冬小麦氮、 磷肥管理提供理论依据和切实可行的措施。【方法】田间定位试验开始于2004年10月,位于陕西杨凌西北农林科技大学农作一站。采用单因素完全随机区组设计,重复4次。供试小麦品种为小偃22,整个生育期不灌水。试验一为小麦施氮量试验,在施磷量为P2O5100 kg/hm2的基础上,设置0、 80、 160、 240、 320 kg/hm2 5个氮肥(N)水平;试验二为小麦施磷量试验,在施氮量为N 160 kg/hm2的基础上,设置P2O5 0、 50、 100、 150、 200 kg/hm2 5个磷肥水平。分别于2011～2013年连续两年进行田间取样,测定小麦籽粒产量及其构成因素,籽粒、 茎叶和颖壳中的氮、 磷、 锌含量,计算小麦地上部的氮、 磷、 锌吸收量。【结果】小麦施氮量试验表明,氮肥用量不超过N 320 kg/hm2时,小麦籽粒锌含量和地上部锌吸收量与施氮量呈极显著的正相关关系,施氮量每增加N 100 kg/hm2,籽粒锌含量平均提高4.0 mg/kg,地上部锌吸收量平均提高36.4 g/hm2;籽粒中的锌含量与氮含量之间、 地上部的锌吸收量与氮吸收量之间也均呈极显著的正相关关系,籽粒氮含量每增加1 g/kg,籽粒锌含量平均提高2.0 mg/kg,地上部氮吸收量每增加100 kg/hm2,其锌吸收量平均提高142.9 g/hm2。小麦施磷量的试验结果表明,施磷量不超过200 kg/hm2时,籽粒锌含量与施磷量呈极显著的负相关关系,施磷量每增加P2O5 100 kg/hm2,籽粒锌含量平均下降9.2 mg/kg;籽粒锌含量与磷含量也呈极显著的负相关关系,籽粒磷含量每增加1 g/kg,籽粒锌含量平均降低24.0 mg/kg;地上部锌吸收量与施磷量、 地上部磷吸收量之间均没有显著相关关系。【结论】综合考虑冬小麦籽粒产量和籽粒锌含量,建议这一地区冬小麦的施氮量和施磷量分别控制在N 160～240 kg/hm2和P2O5 50～100 kg/hm2。     

华北平原冬小麦/夏玉米轮作体系对氮素环境承受力分析

通过田间试验研究了华北地区冬小麦/夏玉米轮作体系对氮素的环境承受力。结果表明,冬小麦和夏玉米达到最高产量时的施氮量分别是112和180.kg/hm2。氮肥利用率和农学利用率随施氮量的增加而降低,生理利用率表现出抛物线的趋势。在农户习惯施氮条件下,冬小麦和夏玉米的氮肥利用率分别是10%和6%,每千克氮肥分别增产2和3千克。灌水和集中降雨是引起土壤硝态氮明显下移的主要因素。氮素平衡计算的结果表明,低施氮量时,氮素盈余以残留Nmin为主,高量施氮则以表观损失为主。将收获后090.cm土壤中的硝态氮的量控制到150kg/hm2,可以在兼顾环境的前提下获得较高的产量;此时冬小麦季的施氮量是122.kg/hm2,产量(干物重)达到最高产量4331.kg/hm2;夏玉米季的施氮量是145.kg/hm2,产量(干物重)是7965.kg/hm2,达到最高产量的97%。     

Response of mustard to seed treatment with pyridioxine and basal and foliar application of nitrogen and phosphorus

In a simple randomised field trial conducted during 1985–86/ 1986–87, the effect of basal nitrogen (45 and 60 kg N/ha) and basal phosphorus (15 and 20 kg P/ha) applications together with the soaking of seeds in 0.025% aqueous pyridoxine hydrochloride solution for 4h and foliar applications of 15 kg N/ha and 5 kg P/ha in two installments at 70 and 90 days after sowing (DAS) was studied on the performance of mustard (Brassica juncea L.). Recommended basal applications of 90 kg N/ha and 30 kg P/ha (BN₉₀P₃₀) was used as the control. The parameters studied included leaf area index (LAI) at 60, 80, and 100 DAS, net assimilation rate at 60–80 and 80–100 day intervals, and pods/plant, seeds/pod, seed yield, oil content, and oil yield at harvest. In general, the pyridoxine treatment proved superior over water soaking. The higher basal fertilizer dose was effective and foliar application of N and P gave higher values as compared to the water foliar application alone. The combination of pyridoxine + BN₆₀P₂₀+ FN₁₅FP₅ significantly enhanced the performance of the crop and enhanced seed yield and oil yield by 15.8 and 13.5%, respectively, over the check BN₉₀P₃₀ treatment.     

Optimum N concentration in winter wheat grown in the coastal plain region of Virginia

Abstract

Limited information is available on optimum N levels in winter wheat (Triticum aestivum L.), particularly at higher yield levels. Three experiments were conducted in the Coastal Plain region of Virginia where N was applied at rates of 0, 67, 90 and 112 kg/ha to Wheeler, Mc Nair 1003 and Coker 747 soft red winter wheat varieties. Yields ranged from 2.33 to 5.83 Mg/ha in the study. Nitrogen fertilization increased yield up to the 67 kg/ha rate and increased N concentration in the plant tissue up to 67 or 112 kg of N/ha, depending on variety. Optimum N concentration, i.e., N concentration at maximum (100%) yield for Wheeler, Mc Nair 1003 and Coker 747, over the three experiments, was 4.54%, 4.52% and 4.81%, respectively, for entire above‐ground plant samples collected at Feekes growth stage 4 and 4.72%, 4.73% and 4.44% for flag leaf samples collected at Feekes growth stage 10. A N sufficiency range of 4.00–5.00% is suggested for use for the plant parts sampled for both growth stages.     

Effect of Clinoptilolite Addition to Soil on Wheat Yield and Nitrogen Uptake

Abstract

During the past years, appreciable amounts of zeolite‐rich tuff that contains more than 70% clinoptilolite (Cp) have been discovered in Greece. The present study evaluates the ability of natural Greek Cp to increase the efficiency of nitrogen (N) fertilizer uptake in wheat. A pot experiment with winter wheat was conducted in a Typic Xerorthent that was fertilized with ammonium sulfate and amended with 0 to 60 ton/ha of Cp. Clinoptilolite application resulted in an increase of the cation exchange capacity of the soil from 9.5 to 13.6 meq/100 g (i.e., 43%). Soil ammoniacal N was greater in the samples amended with Cp at the boot stage, as was NO₃‐N. Clinoptilolite addition increased total wheat yield (dry matter of hay plus seed) 52% (from 21.1 g/pot in the control to 32.0 g/pot) in the treatment with 60 ton/ha of Cp. The influence was greater for seed yield than hay yield. Clinoptiloite addition resulted in high increase in total N uptake, about 141% (from 156 mg/pot in the control to 376 mg/pot) in the treatment with the highest Cp rate. For hay, the increase was 133% (from 125 mg/pot to 291 mg/pot), whereas for seed it was 126% (from 31 mg/pot to 70 mg/pot) from control to the treatment with the highest Cp rate, resulting in a more efficient N fertilizer use. The optimum Cp addition rate was estimated as large as 15 ton/ha.     

潮土小麦–玉米轮作体系氮肥用量阈值及土壤硝态氮年际变化

  【目的】  合理施氮是粮食高产、稳产的重要保证。研究不同施氮水平下作物产量的可持续指数以及土壤硝态氮年际迁移特征,对指导黄淮海地区冬小麦–玉米轮作体系下农田氮肥的合理施用具有重要意义。  【方法】  长期定位试验始建于2006年,设置10个施氮水平:0、60、120、180、240、300、360、420、500和600 kg/hm2。测定冬小麦和夏玉米产量及土壤剖面 (0—200 cm) 硝态氮含量的年际变化特征。  【结果】  施氮水平显著影响冬小麦–夏玉米轮作体系下作物产量,施肥年限以及施肥年限与施肥量间的交互作用对小麦、玉米产量也存在极显著影响。施N 0～240 kg/hm2的处理,小麦、玉米产量随施氮量的增加逐渐增加;施N 300～600 kg/hm2的处理作物产量基本稳定,处理间差异不显著 (P > 0.05)。施氮能显著提高冬小麦产量的可持续性指数 (P < 0.05),但对夏玉米产量的可持续指数影响较小。随着施氮量增加,土壤硝态氮含量呈现逐渐增加的趋势,且施N量低于300 kg/hm2时,0—200 cm土层硝态氮含量均处于较低水平,施氮量超过300 kg/hm2后,土壤硝态氮含量显著增加。另外,随着试验年限的延长,土壤硝态氮累积峰逐渐下移,2008、2011和2017年土壤硝态氮含量峰值分别在40—60 cm、80—120 cm和80—160 cm。  【结论】  黄淮海盐化潮土区,冬小麦–夏玉米轮作制度下氮合理用量在冬小麦上的阈值为240 kg/hm2、在夏玉米上的阈值为180 kg/hm2,在此氮肥用量下,长期施肥既可保证作物 (小麦、玉米) 稳产,又不会显著增加土壤硝态氮残留及向下迁移。     

秸秆还田下氮肥运筹对白土田水稻产量和氮吸收利用的影响

【目的】研究小麦秸秆直接还田条件下不同氮肥基追比例运筹方式对白土稻田水稻产量和氮素吸收利用的影响, 为华中低产白土稻田水稻合理施肥提供科学依据。【方法】设置2种小麦秸秆还田量(0和3000 kg/hm2)及3种氮肥基肥-分蘖肥-穗肥施用比例(80-0-20、 60-20-20 和40-30-30)和不施氮的对照, 共7个处理, 分别为N80-0-20、 N60-20-20、 N40-30-30、 N80-0-20+S、 N60-20-20+S、 N40-30-30+S和CK。水稻收获期采集代表性样品考察水稻产量结构性状, 同时测定水稻籽粒和秸秆产量, 分析籽粒和秸秆氮素含量, 计算水稻氮素吸收量和氮肥利用效率。【结果】基肥-分蘖肥-穗肥施用比例60-20-20的处理水稻籽粒产量最高, 两年试验较不施分蘖肥的对照分别增产9.4%~12.9%和7.4%~8.9%。实施小麦秸秆直接还田后, 水稻籽粒产量较不施秸秆的对照分别提高10.2%~23.4%和0.8%~5.5%。不施秸秆条件下, 基-蘖-穗肥施用比例60-20-20的处理水稻籽粒含氮量最高, 较不施氮的对照提高11.3%, 而秸秆含N量随中后期追肥比例的加大而提高。秸秆还田条件下, 氮肥后移能明显提高水稻籽粒和秸秆含氮量。水稻籽粒氮素吸收量, 基-蘖-穗肥比例60-20-20处理最多, 2011年较对照N80-0-20分别增加13.7%和24.8%, 2012年提高14.5%和9.2%; 秸秆氮素积累量则随中后期追肥用量的增加而增多, 基-蘖-穗肥比例40-30-30处理最多。不施秸秆条件下, 基-蘖-穗肥比例60-20-20的处理氮素干物质生产效率、 氮素稻谷生产效率、 氮收获指数均最高, 百公斤籽粒吸氮量最低。秸秆还田条件下, 氮素干物质生产效率和氮素稻谷生产效率均随中后期追肥量的增加而下降, 而百公斤籽粒吸氮量则最高。氮素农学效率、 氮肥回收利用率和偏生产力也是60-20-20比例的处理最高, 较对照N80-0-20农学效率分别提高4.90和2.44 kg籽粒/kg N, 氮肥利用率提高7.82和21.29个百分点, 偏生产力提高4.90和2.44个百分点。【结论】综合水稻产量、 氮素吸收量以及氮肥利用效率, 安徽省江淮丘陵低产白土地区, 小麦秸秆直接还田条件下, 单季中稻氮肥的基肥-分蘖肥-穗肥施用比例, 以60-20-20运筹方式较为适宜。     

施肥对黄土高原旱地冬小麦根系生长的影响

田间试验表明,旱地冬小麦根系集中分布在0～20cm土层中,约占0～60cm土层总根重的60.7%;根系生育规律以根重变化表示在0～20cm土层中,呈逆变态,表现为快、较慢、慢的生长过程,20～40cm土层呈突变态、较慢、快、慢的生长过程,40～60cm土层呈稳定状态,表现为慢、快、慢的生长过程。不同肥料处理对冬小麦根系的影响是:氮肥有增加表层根系的作用,平均日增加4.05g/cm²,影响深度达40cm;磷肥利于根系下扎,可达80cm土层以下;氮磷有机肥并施显着增加根重和生长量,有利于吸收深层水分和养分;旱地冬小麦根系下扎深度为220～240cm,吸收利用土壤水分能力范围在180～210cm。     

施氮水平对黄土旱塬区小麦产量和土壤有机碳、氮的影响

施用氮肥是雨养农业区提高作物产量和土壤有机碳（SOC）、氮[TSN（Total soil N）]含量的重要养分管理措施。利用长期田间试验（1984～2007）,定量评价了常规耕作条件下5个施氮水平N 0（N0）、45（N45）、90（N90）、135（N135）和180（N180）kg/hm2处理下,小麦子粒产量、SOC、TSN和氮肥利用效率的变化。研究了施氮水平对黄土旱塬区旱地小麦产量、SOC和TSN积累的影响。结果表明,1984～2007年期间,N0、N45、N90、N135和N180处理小麦产量的平均值依次为1.2、2.4、2.9、3.2和3.4 t/hm2;N0处理的小麦产量随试验年限而降低,年降低幅度达67 kg/hm2（P0.001）;但增施氮肥后降低趋势得到显著控制,当施氮水平提高到N 90 kg/hm2时,产量随年限呈现出缓慢升高的趋势。随着施氮水平的提高,地上部氮肥利用率由40%（N45处理）降低到28%（N180）。不同施氮水平条件下,SOC含量随年限呈缓慢升高趋势。23年后（2007年）,N0、N45、N90、N135和N180处理下,0—20 cm土层SOC储量依次为16.9、18.2、18.7、19.0和19.1 t/hm2;TSN储量依次为2.03、2.16 、2.24 、2.34和2.37 t/hm2。施氮水平与产量呈显著的抛物线关系（R2＝0.993）。产量与SOC存在着极显著的线性相关关系（R2=0.997）。增施N 1 kg/hm2,小麦产量可提高29 kg/hm2,SOC提高1.2 kg/hm2,TSN提高0.13 kg/hm2。根茬还田量的增加是导致黄土旱塬区SOC和TSN提高的主要因素。     

Soil and Rice Responses to Phosphate Fertilizer in Two Contrasting Seasons on Acid Sulfate Soil

Acid sulfate soils (ASS) are characterized by low pH, aluminum (Al), and iron (Fe) toxicity and are typically deficient in phosphate (PO₄). The application of phosphorus (P) fertilizer could help reduce the level of exchangeable Al and Fe, thereby improving the rice growth and yield. Five levels of P (0, 20, 40, 60 and 80 kg phosphorus pentoxide (P₂O₅)/ha) were tested with rice varieties MTL560 in the wet season and MTL480 in the dry season. The optimum rate of P was 60 kg P₂O₅/ha for rice in the dry season and 80 kg P₂O₅/ha in the wet season. Soil testing showed at the start of the season that there was sufficient P in the soil. At the end of the season there was a reduction in soil Al and Fe in plots that had P rates above 40 kg P₂O₅/ha. It is therefore likely that P application reduced Al and Fe toxicity through precipitation and formation of Al-P and Fe-P compounds, which boasted yield, rather amending a soil P deficiency.     

NITROGEN FERTILIZER MANAGEMENT FOR IMPROVED GRAIN QUALITY AND YIELD IN WINTER WHEAT IN OKLAHOMA

From 2002 to date, a long-term field experiment has been conducted at Lake Carl Blackwell, Oklahoma, with different rates and times of nitrogen (N) fertilizer application to determine their effect on grain yield, protein and N uptake of winter wheat. Trend analysis for N rates (0, 50, 100, 150 and 200 kg N ha^?1) and orthogonal contrasts for different application times (pre-plant, top-dressed in February and March) were performed. With increasing fertilizer N, wheat grain yield and protein content increased from 2110 kg ha^?1 to 6783 kg ha^?1 and from 8.96 to 17.19%, respectively. For grain yield, protein, and N use efficiency, split applications of N fertilizer were much more efficient than applying all N pre-plant. Large differences in grain yields were noted for different years at the same N rate (range exceeded 5.0 Mg ha^?1) and that illustrated the need for making within-year-specific N rate recommendations.     

高肥力土壤冬小麦生长季肥料氮的去向研究 Ⅰ.冬小麦生长季肥料氮的去向

用15N示踪微区试验研究了常规灌溉和磷钾供应充足的条件下 ,冬小麦生育期肥料氮的去向。结果表明 ,冬小麦对肥料氮的吸收随施氮量的增加而显著增加 ,收获期冬小麦吸收肥料氮占总吸氮量的比例 45% ,吸收土壤氮占 55%。氮肥在整个作物 土壤体系中的回收率随施氮量的增加而显著减少 ,损失量增加。施氮量为 1 2 0kgN hm2 时 ,氮肥的损失率只有 9% ,在作物中的回收率为 45% ,在 0～ 1 0 0cm土壤中的残留率为 45% ;施氮量为 3 60kgN hm2 时 ,氮肥的损失率为 55% ,在作物中的回收率为2 3 % ,在 0～ 1 0 0cm土壤中的回收率为 2 1 %。残留肥料氮以NH4 N存在的数量很少 ,以NO3 N存在的数量随施氮量的增加而显著升高 ,低量施氮时以有机结合态存在的数量远远高于前两种形态 ,但在高量施氮条件下 ,以有机结合态存在的比例与NO3 N相当。肥料氮在 0～ 1 0 0cm土壤各层次中均有残留 ,随着深度的增加 ,残留量减少。从整体上看 ,肥料氮在收获时往下移动超出 1 0 0cm土体。