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首页> 外文期刊>Field Crops Research >Warming and nitrogen fertilization effects on winter wheat yields in northern China varied between four years
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Warming and nitrogen fertilization effects on winter wheat yields in northern China varied between four years

机译:北方地区增温和氮肥对冬小麦产量的影响在四年之间有所不同

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摘要

Global warming is expected to affect wheat productivity significantly, but with large regional differences depending on current climatic conditions. We conducted a study that aimed to investigate how wheat growth and development as well as yield and yield components respond to warming combined with nitrogen fertilization. Infrared heaters were applied above the crop and soil to provide a warming of around 2 degrees C at 5 cm soil depth during the whole winter wheat growing season from 2008 to 2012 at a site near Shijiazhuang in the North China Plain. Two temperature levels (warming and ambient) for winter wheat were compared in a factorial combination with (N2, 240 kg N ha(-1) y(-1)) and without nitrogen fertilizer (N1) in a field experiment. Measurements showed that the infrared heater increased soil temperature by 1.6 to 2.2 degrees C in N2 and by 1.3 to 2.0 degrees C in N1 depending on soil depth (0.05 to 0.40 m). The volumetric water content decreased significantly before heading by 9.3, 3.9, 2.4 and 1.2 vol% in the soil depth of 0.10, 0.20, 0.40, 0.60m in N2 and by 5.9, 1.4, 1.3 and 1.2 vol% in N1 from heating compared with no heating. The duration of the entire growth period was shortened by on average 7 days in the warming compared with control treatment. The early growth stages before re-greening in spring were shortened by 12 to 18 days, whereas the later stages were prolonged by up to 6 days. Warming reduced grain yield by 36%, 39% (P < 0.05) and 12% for N2 and 33%, 7% and 10% for N1 in 2009, 2011 and 2012, respectively, which can be considered years with normal winter weather. However, warming increased grain yield by 1% and 31% (P < 0.05) in N1 and N2, respectively, in a year with unusually cold and snowy winter conditions (2010). Warming increased plant height and 1000-grain weight, but reduced spike number per m(2). This suggests that the wheat yield loss may be related to reduction of spike number, which was affected by decreased soil water content under warming. Warming tended to give larger yield reductions at higher nitrogen fertilizer rates, and this may be related to larger water consumption with both higher nitrogen and temperature leading to water shortages. These effects indicate that wheat yield loss from warming was primarily associated with more severe water shortage from greater evapotranspiration under warming. The large crop canopy in the fertilized plot may further have enhanced evapotranspiration and thus severity of the drought leading to larger yield reduction in fertilized plots. Yield increased under warming when water was not a limited factor in a year with unusual cold and wet winter
机译:预计全球变暖将对小麦生产力产生重大影响,但根据当前气候条件,区域差异会很​​大。我们进行了一项研究,旨在研究小麦的生长发育以及产量和产量成分如何响应变暖与氮肥的关系。在华北平原石家庄附近的一个地点,从2008年至2012年整个冬小麦生长季节,在作物和土壤上方安装了红外加热器,以在5厘米土壤深度提供约2摄氏度的升温。在田间试验中,比较了有(N2,240 kg N ha(-1)y(-1))和不含氮肥(N1)的析因组合下冬小麦的两个温度水平(变暖和环境温度)。测量结果表明,根据土壤深度(0.05至0.40 m),红外加热器在N2中将土壤温度升高1.6至2.2摄氏度,在N1中将土壤温度升高1.3至2.0摄氏度。与加热相比,N2的土壤深度为0.10、0.20、0.40、0.60m时,去向前的体积水含量显着下降了9.3、3.9、2.4和1.2vol%,与加热相比,N1的下降了5.9、1.4、1.3和1.2vol%。没有暖气。与对照处理相比,在升温过程中,整个生长期平均缩短了7天。春季重新绿化之前的早期生长阶段缩短了12至18天,而后期则延长了长达6天。变暖使2009年,2011年和2012年的N2分别降低了36%,39%(P <0.05)和12%,N1分别降低了33%,7%和10%,这可以认为是冬季天气正常的年份。然而,在异常寒冷和多雪的冬季条件下,一年的变暖使N1和N2的谷物单产分别提高了1%和31%(P <0.05)(2010)。变暖增加了株高和1000粒重,但减少了每m(2)的穗数。这表明小麦产量损失可能与穗数减少有关,穗数减少受增温条件下土壤含水量减少的影响。在较高的氮肥施用量下,变暖往往会导致较大的减产,这可能与较高的氮和温度导致更大的耗水量有关,导致缺水。这些影响表明,变暖导致的小麦单产下降主要与变暖下更大的蒸散作用导致的更为严重的水资源短缺有关。施肥区的大作物冠层可能进一步具有蒸散作用,因此干旱的严重性导致施肥区更大的减产。在异常寒冷和潮湿的一年中,当水不受限制时,在变暖下单产增加

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