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1.
不同氮肥用量下冬小麦土壤剖面累积硝态氮及其与氮素表观盈亏的关系 总被引：7，自引：2，他引：5
以在陕西关中地区户县、周至两县连续2年的20余个3414肥料田间试验为研究对象,研究了不同施氮量下冬小麦收获后土壤2 m剖面硝态氮的分布、累积及其与土壤氮素表观盈亏量间的关系。结果表明:随着氮肥用量的提高,土壤剖面硝态氮累积量明显增加,其向土壤下层淋溶的程度也越严重;当施氮量为180～240 kg/hm2时,一些试验点的土壤氮素已经表现出盈余;当施氮量达到270～360 kg/hm2,所有试验点土壤氮素均明显盈余。不同施氮量时土壤表观氮素平衡值（施氮量与氮素携出量的差值）与土壤02 m剖面硝态氮累积量之间呈极显著正相关,说明土壤表观氮素平衡和盈亏决定了土壤剖面硝酸盐的累积状况;土壤氮素表观盈余值每增加100 kg/hm2,02 m土壤剖面硝态氮累积量增加约62.5 kg/hm2。 相似文献
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施氮量对冀西北春玉米氮肥利用率和土壤硝态氮时空分布的影响 总被引：13，自引：1，他引：12
在田间条件下研究了施氮量对春玉米产量、氮肥利用率和土壤硝态氮时空分布的影响,旨在为冀西北春玉米氮肥优化管理提供理论依据。研究结果表明,春玉米产量随施氮量的增加而提高,当施氮量高于225 kg/hm2时,春玉米产量和氮肥利用率显著降低。从春玉米播种前到收获后,不施氮处理0-90 cm各土层硝态氮含量不断降低,施氮处理0-30 cm和30-60 cm土层硝态氮含量呈先上升后迅速下降并保持稳定的趋势,而60-90 cm土层硝态氮在春玉米生长后期有增加的趋势;春玉米收获后随着土层深度的增加,硝态氮呈波浪式下降,施氮量300,375 kg/hm2处理60-90,120-150,150-180 cm土层硝态氮含量显著高于其它处理。随着施氮量的增加,春玉米0-90,90-180,0-180 cm土层硝态氮累积量均呈增加趋势,高施氮量土层累积的硝态氮存在着更大的淋溶风险。因此,综合分析氮肥用量对春玉米产量、氮肥利用率的影响,并考虑土壤硝态氮时空分布下的环境风险,合理的施氮量应控制在195~225 kg/hm2之间。 相似文献
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施氮和豌豆/玉米间作对土壤无机氮时空分布的影响 总被引：3，自引：1，他引：3
为探明甘肃河西走廊绿洲灌区豌豆/玉米间作体系土壤无机氮时空分布现状和过量施用氮肥对环境的影响,2011年在田间试验条件下,采用土钻法采集土壤剖面样品,采用Ca Cl2溶液浸提、流动分析仪测定土壤无机氮含量的方法,研究了不同氮水平[0 kg(N)·hm?2、75 kg(N)·hm?2、150 kg(N)·hm?2、300 kg(N)·hm?2、450 kg(N)·hm?2]下豌豆/玉米间作体系土壤无机氮时空分布规律。结果表明:作物整个生育期内,灌漠土无机氮以硝态氮为主,其含量是铵态氮的7.55倍。在玉米整个生育期内,与不施氮相比,75 kg(N)·hm?2、150 kg(N)·hm?2、300 kg(N)·hm?2和450 kg(N)·hm?2处理的土壤硝态氮含量分别增加29.7%、67.5%、88.2%和134.3%。与豌豆收获期相比,在玉米收获时土壤硝态氮含量平均降低44.2%。间作豌豆和间作玉米分别比对应的单作在0~120 cm土层硝态氮含量降低6.1%和5.1%。豌豆/玉米间作体系土壤无机氮累积量在不同施氮量和不同生育时期都是表层(0~20 cm)最高。豌豆收获后,0~60 cm土层土壤无机氮累积量间作豌豆和间作玉米分别比相应单作降低4.9%和1.9%,60~120 cm土层降低10.8%和9.2%;玉米收获后0~60 cm土层平均降低28.2%和9.4%,60~120 cm土层平均降低23.5%和12.5%。土壤无机氮残留量间作豌豆比单作豌豆在0~60 cm土层降低4.9%,60~120 cm降低10.9%。因此,施用氮肥显著增加了土壤无机氮含量和累积量,且主要影响土壤硝态氮。过量的氮肥投入会因作物不能及时全部吸收而被大水漫灌和降雨等途径淋洗到土壤深层,造成氮肥损失和农田环境污染。间作能显著降低土壤无机氮浓度和累积量,特别在作物生长后期对土壤无机氮累积的降低作用更加明显。 相似文献
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渭北旱塬小麦不同栽培模式对土壤硝态氮残留的影响 总被引：10，自引：0，他引：10
在陕西渭北旱塬进行了4年田间小麦试验,研究了旱地不同栽培模式、施氮量和种植密度对土壤硝态氮残留累积的影响。结果表明,种植小麦4年后,0-200 cm土壤剖面中残留硝态氮为29.87~462.59 kg/hm2,且主要积累在80-160 cm土层,土壤氮库不仅明显,且残留比前3年土壤剖面显著下移(前3年主要累积在100 cm),差异达显著和极显著水平;不同栽培模式和种植密度0-200 cm土层硝态氮残留累积规律及其小麦籽粒吸氮量基本相似,排序均为:地膜覆盖>常规种植>秸秆覆盖>垄沟种植;随施氮量的增加土壤硝态氮残留量也相应增加,N0处理0-200 cm土壤平均硝态氮残留量为57.69 kg/hm2,N120处理平均为97.04 kg/hm2,虽然高于无氮处理,但两者差异未达到显著水平,N240处理平均为355.43 kg/hm2,比前者增加的幅度更大,其差异达到极显著水平。因施氮肥而增加的土壤硝态氮残留量为14.9~401.18 kg/hm2,平均占4年施氮量的19.59%,其中地膜覆盖占26.07%,常规种植占20.98%,秸秆覆盖占17.46%,垄沟种植种植占13.87%。 相似文献
5.
施氮对春玉米氮素利用及农田氮素平衡的影响 总被引：25，自引：8，他引：17
田间试验研究了玉米对不同土壤氮素供应水平下作物氮素吸收利用、土壤氮素供应以及农田氮素平衡的影响。结果表明,玉米产量随施氮量的增加而显著提高,当施氮量高于N 240 kg/hm2时,产量有减少趋势;氮素当季利用率随施氮量的增加逐渐降低。土壤中硝态氮含量在玉米整个生育时期呈现先迅速下降后缓慢升高的趋势;玉米成熟期,施氮处理的各层土壤中硝态氮含量显著高于不施氮处理,各层硝态氮含量基本随施氮量的增加而升高。适量施氮促进玉米对氮素的吸收和利用,进而提高玉米生物量和产量;过量施氮导致硝态氮在土壤中大量累积,提高了硝态氮淋溶风险。施氮处理显著提高了收获后土壤中残留无机氮(Nmin),土壤残留Nmin随施氮量的增加而增加;当施氮量高于N 240 kg/hm2时,残留Nmin有下降趋势。氮素表观损失随施氮量的增加而增加。在本试验条件下,综合产量、氮肥利用率和土壤硝态氮累积情况考虑,合理施氮量应控制在N 1802~40 kg/hm2左右。 相似文献
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养分专家系统推荐施肥对甜瓜产量品质和土壤氮素淋失的影响 总被引：1，自引：1，他引：0
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水氮耦合对绿洲灌区土壤硝态氮运移及甜瓜氮素吸收的影响 总被引：7，自引：2，他引：5
在地处沙漠绿洲的甜瓜种植区,研究不同水、 氮输入量对土壤氮素平衡和运移的影响,为当地甜瓜生产的水肥管理提供科学依据。通过2009、 2010连续两年田间裂区试验,研究了不同灌水量（1500、 2100、 2700、 3300 m3/hm2,以W1500、 W2100、 W2700和W3300表示）和施氮量（N 0、 120、 240、 360 kg/hm2,以N0、 N120、 N240和N360表示）对土壤硝态氮分布、 累积和甜瓜的水、 氮吸收以及产量的影响。结果表明,甜瓜收获后各处理土壤硝态氮含量在040 cm土层最高, 0200 cm土层呈现先减少后增加再减少的变化趋势,且施氮量越大,硝态氮在80120 cm土层大量累积的趋势越明显。土壤硝态氮累积量随施氮量的增加而增加,随灌水量的增加而减少,灌水量超过2700 m3/hm2 时,仅有不到53%的硝态氮留存在0100 cm土层。甜瓜产量和果实氮素吸收量随灌水量和施氮量的增加而提高,但在W3300N360处理略有下降。氮素回收率随施氮量的增加持续降低,氮收获指数以处理W2700N240最大,水分利用效率以W1500N240处理最大。W2700N240处理能够兼顾甜瓜产量,平衡氮素吸收运移与土壤中硝态氮的留存空间3个方面,是绿洲灌区甜瓜种植的高产高效的水氮输入模式。 相似文献
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施氮量对冬小麦产量的影响及土壤硝态氮运转特性 总被引：17，自引：2，他引：15
以冬小麦“西农9814”为材料进行大田试验,研究施氮量对小麦产量构成因素、土壤中硝态氮变化的影响。结果表明,适宜施氮量（N 276 kg/hm2）可以显著提高小麦的穗重、穗粒数、千粒重等产量构成因素,比对照增产24.6%。产量构成因素中以穗粒数与产量的相关性最强,达极显著水平,千粒重次之。土壤耕层硝态氮主要集中在0—40 cm土层,且含量随着施氮量的增加而增加。随着小麦生育期的推移,耕层中硝态氮呈下降趋势,0—40 cm耕层变化显著,到成熟期各土层硝态氮含量基本趋于一致。施氮量在N 0～207 kg/hm2范围内,硝态氮积累的增加量变化不显著,但当施氮量高于N 207 kg/hm2时,土壤中硝态氮的积累量随施氮量增加而显著增加,增加了硝态氮的冗余和向下淋溶的可能。 相似文献
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《Communications in Soil Science and Plant Analysis》2012,43(7):878-886
Reliable and quick methods for measuring nitrogen (N)–supplying capacities of soils (NSC) are a prerequisite for using N fertilizers. This study was conducted to develop a routine method for estimation of mineralizable N in two calcareous soils (sandy loam and clay soils) treated with municipal waste compost or sheep manure. The methods used were anaerobic biological N mineralization, mineral N released by 2 M potassium chloride (KCl), ammonium (NH4 +) N extracted by 1 N sulfuric acid (H2SO4), NH4 +-N extracted by acid potassium permanganate (KMnO4), and NH4 +-N released by oxidation of soil organic matter using acidified potassium permanganate. The results showed that oxidizable N extracted by acid permanganate, a simple and rapid measure of soil N availability, was correlated with results of the anaerobic method. Oxidative 0.05 N KMnO4 was the best method, accounting for 78.4% of variation in NSC. Also, the amount of mineralized N increased with increasing level of organic materials and was greater in clay soil than sandy loam soil. 相似文献
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不同供N水平对花生硝酸盐累积与分布的影响 总被引：1，自引：0，他引：1
采用盆栽试验,研究了不同供氮水平对花生植株硝酸盐累积、分布及产量的影响。结果表明,花生荚果产量随施氮量的增加呈二次曲线变化趋势,当施用量为N.150.9.kg/hm2时产量最高;植株硝酸盐含量、累积量和累积速率基本随施氮量的增加而提高。同一氮素水平,不同器官的硝酸盐含量因生育期不同存在较大差异,幼苗和花针期茎中的含量最高,饱果成熟期地下器官的含量明显高于地上器官;全生育期叶片和茎中的硝酸盐含量随生育进程逐步降低,而子仁和果壳中含量逐步增加;收获时硝酸盐在茎中的分配比例随施氮量的增加而提高,在根中的分配比例下降。在一定的氮素水平内(N135.kg/hm2),硝酸盐在子仁中的分配比例与供氮水平一致,但过量施氮会导致在营养体中的比例上升,子仁中的比例下降,其它器官规律不明显。在本试验范围内,子仁及其它器官中的硝酸盐含量均未超出WHO和FAO制定的标准,未造成硝酸盐污染;但过量施氮能够显著提高花生荚果和耕层土壤硝酸盐含量。因此,综合考虑花生品质、单位肥料的增产量以及生态效应,花生适宜的施氮量为N.90.kg/hm2。 相似文献
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《Communications in Soil Science and Plant Analysis》2012,43(3):507-518
Studies have reported significant differences in nitrate accumulation among genotypes within a crop species, but the reason for these differences is not clear. This study investigated nitrate (NO3) efflux from roots of two oilseed rape cultivars (Brassica napus L. cvs. ZY821 and D89) and the relationship between nitrate efflux and plant nitrate accumulation. Nitrate efflux was estimated by measuring nitrate released from roots into nitrate-free nutrient solutions 58 days after sowing. The solutions were buffered with either 2.0 mM (n-morpholino) ethanesulfonic acid (MES) or 0.05 mM phosphate. Whole-plant and petiole nitrate accumulations were significantly greater for ZY821 compared to D89. Nitrate efflux varied diurnally, and the difference between cultivars was greater in the morning than in the afternoon. Data suggested that the relatively high pH of the phosphate-buffered solutions increased nitrate efflux rates from oilseed rape plants; therefore phosphate buffer should not be used when making direct determinations of nitrate efflux. Maximum cumulative nitrate efflux was 0.97 μmol g?1 fresh-weight (FW) root for ZY821 and 1.9 μmol g?1 FW root for D89. Maximum nitrate efflux rate was 0.084 μmol g?1 FW min?1 for ZY821 and 0.097 μmol g?1 FW min?1 for D89. These results indicated that between the two cultivars, ZY821 had the greatest petiole nitrate nitrogen concentration and the lowest total nitrate efflux. We suggest that cultivars with low nitrate efflux rates are able to translocate and store greater amounts of nitrate in aboveground plant organs, especially in petioles. 相似文献
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《Communications in Soil Science and Plant Analysis》2012,43(3):571-588
Extraction of soil nitrate nitrogen (NO3 ?-N) and ammonium nitrogen (NH4 +-N) by chemical reagents and their determinations by continuous flow analysis were used to ascertain factors affecting analysis of soil mineral N. In this study, six factors affecting extraction of soil NO3 ?-N and NH4 +-N were investigated in 10 soils sampled from five arable fields in autumn and spring in northwestern China, with three replications for each soil sample. The six factors were air drying, sieve size (1, 3, and 5 mm), extracting solution [0.01 mol L?1 calcium chloride (CaCl2), 1 mol L?1 potassium chloride (KCl), and 0.5 mol L?1 potassium sulfate (K2SO4)] and concentration (0.5, 1, and 2 mol L?1 KCl), solution-to-soil ratio (5:1, 10:1, and 20:1), shaking time (30, 60, and 120 min), storage time (2, 4, and 6 weeks), and storage temperature (?18 oC, 4 oC, and 25 oC) of extracted solution. The recovery of soil NO3 ?-N and NH4 +-N was also measured to compare the differences of three extracting reagents (CaCl2, KCl, and K2SO4) for NO3 ?-N and NH4 +-N extraction. Air drying decreased NO3 ?-N but increased NH4 +-N concentration in soil. Soil passed through a 3-mm sieve and shaken for 60 min yielded greater NO3 ?-N and NH4 +-N concentrations compared to other treatments. The concentrations of extracted NO3 ?-N and NH4 +-N in soil were significantly (P < 0.05) affected by extracting reagents. KCl was found to be most suitable for NO3 ?-N and NH4 +-N extraction, as it had better recovery for soil mineral N extraction, which averaged 113.3% for NO3 ?-N and 94.9% for NH4 +-N. K2SO4 was not found suitable for NO3 ?-N extraction in soil, with an average recovery as high as 137.0%, and the average recovery of CaCl2 was only 57.3% for NH4 +-N. For KCl, the concentration of extracting solution played an important role, and 0.5 mol L?1 KCl could fully extract NO3 ?-N. A ratio of 10:1 of solution to soil was adequate for NO3 ?-N extraction, whereas the NH4 +-N concentration was almost doubled when the solution-to-soil ratio was increased from 5:1 to 20:1. Storage of extracted solution at ?18 °C, 4 °C, and 25 °C had no significant effect (P < 0.05) on NO3 ?-N concentration, whereas the NH4 +-N concentration varied greatly with storage temperature. Storing the extracted solution at ?18 oC obtained significantly (P < 0.05) similar results with that determined immediately for both NO3 ?-N and NH4 +-N concentrations. Compared with the immediate extraction, the averaged NO3 ?-N concentration significantly (P < 0.05) increased after storing 2, 4, and 6 weeks, respectively, whereas NH4 +-N varied in the two seasons. In conclusion, using fresh soil passed through a 3-mm sieve and extracted by 0.5 mol L?1 KCl at a solution-to-soil ratio of 10:1 was suitable for extracting NO3 ?-N, whereas the concentration of extracted NH4 +-N varied with KCl concentration and increased with increasing solution-to-soil ratio. The findings also suggest that shaking for 60 min and immediate determination or storage of soil extract at ?18 oC could improve the reliability of NO3 ?-N and NH4 +-N results. 相似文献
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氮肥形态和用量对蔬菜生长与硝态氮累积的影响 总被引：31，自引：0，他引：31
Experiments were carried out on a vegetable field with Peking cabbage (Bvassica pekinensis (Lour.) Rupr.), cabbage (Bvassica chinensis var. oleifera Makino and nemoto), green cabbage (Brassica chinensis L.), spinach (Spinacia oleracea L.) and rape (Brassica campestris L.) to study the effects of N forms and N rates on their growth and nitrate accumulation. The results indicated that application of ammonium chloride, ammonium nitrate, sodium nitrate and urea significantly increased the yields and nitrate concentrations of Peking cabbage and spinach. Although no significant difference was found in the yields after application of the 4 N forms, nitrate N increased nitrate accumulation in vegetables much more than ammonium N. The vegetable yields were not increased continuously with N rate increase, and oversupply of N reduced the plant growth, leading to a yield decline. This trend was also true for nitrate concentrations in some vegetables and at some sampling times. However, as a whole, the nitrate concentrations in vegetables were positively correlated with N rates. Thus, addition of N fertilizer to soil was the major cause for increases in nitrate concentrations in vegetables. Nitrate concentrations were much higher in roots, stems and petioles than in blades at any N rate. 相似文献
16.
【目的】探究油菜NO3-的吸收、分配和对低氮胁迫的响应及其氮利用效率,为理解油菜在不同低氮胁迫下相关生理变化及其氮素利用效率提供科学依据。【方法】以常规油菜品种814为研究材料,采用砂培试验,在正常供氮水平（10 mmol/L）和低氮胁迫水平（3 mmol/L、1 mmol/L）下,研究油菜的根系特性、蒸腾作用对低氮胁迫的响应及其氮素吸收效率,并研究油菜NO3-的运输分配与同化对低氮胁迫的响应及其氮素利用效率。【结果】与正常供氮处理（10 mmol/L）相比,低氮胁迫处理（3 mmol/L、1 mmol/L）的油菜NO3-含量、全氮含量均显著下降,但（NO3-）叶/根、（全氮（%））叶/根显著升高,植株根系干物质重、根系吸收面积均显著下降,但根冠比显著升高。油菜植株在低氮胁迫下气孔导度和蒸腾速率显著增加,一方面促进植株对NO3-的捕获,另一方面也促使更大比例的NO3-分配在植物的地上部分,但植株的水分散失加剧,水分利用效率显著下降。低氮胁迫处理油菜根和叶中NR、GS活性与正常供氮处理之间的差异不显著或有增加,其叶绿素含量、光合速率均显著下降,但光合氮素利用率显著升高。【结论】在低氮胁迫条件下,油菜植株的氮素和干物质累积均显著下降,但NO3-在植株的地上部分分配比例的增加以及光合氮素利用率的升高促使植株的氮素利用效率显著提高。 相似文献
17.
Jessey George Luke Holtham Kasra Sabermanesh Sigrid Heuer Mark Tester Darren Plett Trevor Garnett 《植物养料与土壤学杂志》2016,179(6):717-725
Nitrate (NO$ _3^ - $ ) and ammonium (NH$ _4^+ $ ) are the predominant forms of nitrogen (N) available to plants in agricultural soils. Nitrate concentrations are generally ten times higher than those of NH$ _4^+ $ and this ratio is consistent across a wide range of soil types. The possible contribution of these small concentrations of NH$ _4^+ $ to the overall N budget of crop plants is often overlooked. In this study the importance of this for the growth and nitrogen budget of maize (Zea mays L.) was investigated, using agriculturally relevant concentrations of NH$ _4^+ $ . Maize inbred line B73 was grown hydroponically for 30 d at low (0.5 mM) and sufficient (2.5 mM) levels of NO$ _3^ - $ . Ammonium was added at 0.05 mM and 0.25 mM to both levels of NO$ _3^ - $ . At low NO$ _3^ - $ levels, addition of NH$ _4^+ $ was found to improve the growth of maize plants. This increased plant growth was accompanied by an increase in total N uptake, as well as total phosphorus, sulphur and other micronutrients in the shoot. Ammonium influx was higher than NO$ _3^ - $ influx for all the plants and decreased as the total N in the nutrient medium increased. This study shows that agriculturally relevant proportions of NH$ _4^+ $ supplied in addition to NO$ _3^ - $ can increase growth of maize. 相似文献
18.
不同施氮水平对春玉米氮素利用及土壤硝态氮残留的影响 总被引：1，自引：0，他引：1
过量施用氮肥造成的环境问题日益严重,氮肥合理使用成为了人们研究的热点。通过研究不同施氮水平对春玉米氮素利用及土壤硝态氮残留的影响,为氮肥的合理利用提供依据。通过在北京市通州区农业技术推广站进行田间小区试验,研究了不同施氮量（0、50、100、200和300kg·hm^-2）对春玉米产量及氮素利用效率、氮平衡和土壤硝态氮累积量的影响。结果表明：（1）春玉米在施氮量为200kg·hm^-2时达到最高产量,为9006．4kg．hm^-2,不同氮肥水平的氮肥利用率在19．7％-25．8％之间,在100kg·hm^-2时的利用效率最高,达到25．8％。（2）作物吸氮量随输入量的增加而增加,氮盈余主要以土壤残留为主,表观损失在氮盈余中的比例虽小,但随施氮量的增加而增加的趋势更加明显。（3）硝态氮在180cm土层中的累积量随氮素输入量的增加而显著增加,在300kg·hm^-2时达到最高值,为195kg·hm^-2,在施氮水平为100kg·hm^-2时作物生长的需要就基本上能够得到满足,而在高施氮水平下（200和300kg·hm^-2）时土壤中的硝态氮出现富集现象,对环境形成一定的威胁。 相似文献
19.
Zhi-ping Yang Yong-liang Wang Cai-xia Guo Jun-ling Guo Xiu-fu Shuai Russell Yost 《Journal of plant nutrition》2017,40(17):2373-2381
Excessive nitrogen application has caused serious environmental pollution under high-yield maize system in China. Our objective was to evaluate critical stalk nitrate (NO3?) levels that support high yield (>13 Mgha?1), but are not in excess. Optimal stalk NO3? concentration was determined by conducting seven nitrogen levels experiments in two high yield maize regions: Dongyang County (DY) and Wenshui County (WS). Optimal stalk NO3? concentration category range to obtain maximum yield in DY (sandy loam, higher accumulated temperature and solar radiation compared with WS) was 0.44–1.19, which similar to the criteria of US (0.70–2.0 g kg?1). While for WS (loam soil, lower accumulated temperature and solar radiation compared with DY), optimal stalk NO3? concentration category range to obtain maximum yield was 1.95–4.15, greatly higher than the US criteria. These results suggested thatit is necessary to establish matching optimal stalk NO3? category ranges for different ecological regions in China. 相似文献
20.
针对黄土高原旱作区糜子生产中氮肥种类单一、肥料利用效率低的问题,本试验以当地习惯施氮尿素N 120kg/hm2(TN)为对照,设置控释氮肥N 120kg/hm2(T1)、108kg/hm2(T2)、96kg/hm2(T3)、84kg/hm2(T4)、72kg/hm2(T5)和不施肥(T0)七个处理,探究不同控释氮肥处理下土壤全氮、微生物量氮、硝态氮和铵态氮含量的变化规律,分析糜子成熟期氮素积累分配、氮素利用效率及产量对控释氮肥的响应,以期为建立旱地糜子控释氮肥一次性基施轻简栽培技术提供支撑。结果表明：与施用尿素相比,等量控释氮肥可以提高糜子抽穗期和成熟期土壤全氮、微生物量氮、硝态氮和铵态氮含量分别达0.38%~5.51%、1.76%~7.63%、5.41%~11.80%和4.04%~14.77%,其中硝态氮和铵态氮含量两年均显著高于TN,随着控释氮肥减量糜子田各形态氮素均呈降低趋势,减氮量达20%以上时土壤硝态氮和铵态氮含量均显著低于TN处理。施用控释氮肥可以提高糜子成熟期氮素积累量1.97%~3.21%,增加糜子氮素向籽粒中的分配比例0.55%~1.18%,控释氮肥减量20%以上时糜子氮素积累量显著低于尿素全量基施处理。与普通尿素相比,控释氮肥提高了糜子氮肥表观利用率、氮肥偏生产力及氮肥农学利用率,增幅分别为3.29%~4.59%、3.88%~4.14%和5.01%~7.63%,其中氮肥偏生产力处理间差异达显著水平,随着控释氮肥减量糜子氮肥表观利用率、氮肥偏生产力及氮肥农学利用率均呈上升趋势。施用控释氮肥通过增加单位面积穗数和穗重显著提高了糜子产量两年分别达3.88%和4.47%,控释氮肥减量20%以下时糜子产量与尿素差异不显著。相关性分析结果表明,糜子氮素积累量与产量呈极显著正相关,氮素利用效率指标与土壤硝态氮含量相关性最强。综上所述,施用控释氮肥较尿素可显著提高糜子生育中后期土壤供氮能力,促进糜子对氮素的吸收利用进而增加产量,且在适量减氮20%时并未显著降低糜子产量,因此控释氮肥在糜子生产中有较大的应用前景及减氮潜力。 相似文献