首页> 外文期刊>Australian Journal of Crop Science >The effects of irrigation and nitrogen application rates on yield of spring wheat (longfu-920), and water use efficiency and nitrate nitrogen accumulation in soil
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The effects of irrigation and nitrogen application rates on yield of spring wheat (longfu-920), and water use efficiency and nitrate nitrogen accumulation in soil

机译:灌溉和施氮量对春小麦(longfu-920)产量,水分利用效率和土壤硝态氮累积的影响

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In the middle reaches of Heihe River Basin, the environmental deterioration caused by excessive nitrogen (N) and irrigation application in agricultural ecosystems has received much attention in recent years. A combination of careful irrigation and N management is needed to improve N uptake efficiency and to minimize potential nitrate (NO -3 -N) leaching. A field experiment was designed to investigate the effects of different irrigation and N application rates on grain yield, water use efficiency (WUE) and soil nitrate-N (NO -3 -N) accumulation on a recently reclaimed sandy farmland at the margin of the Gobi Desert in 2006 and 2007. The experiment followed a completely randomized split-plot design, taking the various irrigation treatments (0.6, 0.8 and 1.0 of the estimated evapotranspiration-ET) in the main-plots and N supply treatments as split-plot (with five levels of 0, 79, 140, 221 and 300 kg N ha-1). The results indicated a wide annual variability in grain yield, kernel numbers and straw yield, mainly due to greater rainfall and irrigation rates in the second year. A significant irrigation effect was observed on grain yield, kernel numbers and straw yield. The highest levels were achieved with a high irrigation supply, although WUE generally decreased linearly with increasing seasonal irrigation rates in 2 years. The low irrigation treatment (0.6 ET) produced significantly lower grain yield (20.7 %), kernels number (9.3 %) and straw yield (12.2 %) than high irrigation treatment (1.0 ET). The low irrigation treatment had a higher WUE (4.25 kg ha-1 mm-1) than that of 3.25 kg ha-1 mm-1 with high irrigation over the 2 years. On contrary to the irrigation, the N application rate of 221 kg ha-1 had the highest values of grain yield, kernel numbers, straw yield and WUE under the 3 irrigation regimes. The average grain yield of 221 kg N ha-1 were found to be 99.1, 45.1, 20.0 and 7.4 % higher than those of 0, 79, 140 and 300 kg N ha-1, respectively over the 2 years. The 221 kg N ha -1 had the highest WUE (4.75 kg ha-1 mm-) among all N treatments. No more NO -3 -N accumulation was found in the 200 cm soil profiles under the medium (0.8 ET) and low irrigation, when the N application was below 221 kg ha-1, at harvesting stage and there was a little potential for NO -3 -N leaching. High irrigation led to a high NO - 3 -N leaching and a high plant N-uptake, resulting in lower NO -3 -N accumulation at the harvest stage compare to the sowing or soil preparation stage. This was within the 200 cm soil profiles and over the 2 wheat growing seasons. The N application rate of 221 kg N ha-1 produced a high grain yield of spring wheat, but the N application rate was lower than that of 221 kg N ha-1 as concerned NO -3 -N accumulation at harvesting stage under deficit irrigation. The optimum economic N rates ranged from 174 to 226 kg ha-1.
机译:在黑河流域中游,近年来由于氮(N)过多和农业生态系统中灌溉技术的应用而引起的环境恶化受到了广泛关注。需要仔细灌溉和氮素管理相结合,以提高氮素吸收效率并最大程度地减少潜在的硝酸盐(NO -3 -N)淋溶。设计了一个田间试验,以调查不同灌溉和施氮量对黄土高原边缘最近复垦的沙质农田的粮食产量,水分利用效率(WUE)和土壤硝态氮(NO -3 -N)积累的影响。 2006年和2007年的戈壁沙漠。该实验遵循完全随机的分割图设计,将主要地段的各种灌溉处理(估计的蒸散量-ET的0.6、0.8和1.0)和氮供应处理作为分割图(的水平分别为0、79、140、221和300 kg N ha-1)。结果表明,谷物产量,籽粒数量和稻草产量的年度变化很大,这主要是由于第二年降雨和灌溉率增加所致。观察到灌溉对谷物产量,籽粒数量和秸秆产量的显着影响。较高的灌溉量可以达到最高水平,尽管WUE通常在2年内随着季节性灌溉率的增加而线性下降。与高灌溉处理(1.0 ET)相比,低灌溉处理(0.6 ET)产生的谷物产量(20.7%),谷粒数(9.3%)和秸秆产量(12.2%)显着较低。在两年内,低灌溉处理的WUE(4.25 kg ha-1 mm-1)高于3.25 kg ha-1 mm-1的WUE。与灌溉相反,在3种灌溉方式下,221 kg ha-1的氮肥施用量具有最高的籽粒产量,籽粒数,秸秆产量和WUE值。两年中平均221 kg N ha-1的平均单产分别比0、79、140和300 kg N ha-1高99.1%,45.1、20.0和7.4%。在所有N种处理中,221 kg N ha -1的WUE最高(4.75 kg ha-1 mm-)。在中等水平(0.8 ET)和低灌溉条件下,当氮素施用量低于221 kg ha-1时,在收获阶段,在200 cm的土壤剖面中没有发现更多的NO -3 -N积累,并且潜在的NO可能性很小。 -3 -N浸出。较高的灌溉量导致较高的NO-3 -N淋溶和较高的植物氮素吸收,与播种或整地相比,收获期的NO -3 -N积累量较低。这在200厘米的土壤剖面内,并且在两个小麦生长季节内。施氮量为221 kg N ha-1时,春小麦的籽粒产量较高,但考虑到亏缺灌溉条件下收获期NO -3 -N的积累,施氮量低于221 kg N ha-1。 。最佳经济氮肥浓度范围为174至226 kg ha-1。

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