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Effect of irrigation amount and water salinity on water consumption and water productivity of spring wheat in Northwest China.

机译:灌溉量和水盐度对西北地区春小麦耗水量和水分生产率的影响。

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摘要

Sustainable development of agriculture is restricted by fresh water shortage and water quality deterioration in some arid and semi-arid areas. Therefore, deficit irrigation and saline water irrigation have to be applied for sustaining crop yield. In order to determine the rational irrigation management practice in an arid region of Northwest China, field experiments were conducted in 2008, 2009 and 2010 to study the effects of irrigation amount and water salinity on water consumption and water productivity of spring wheat. Altogether nine irrigation treatments including three levels of irrigation water amount with 375, 300, and 225 mm (w1, w2 and w3) and three levels of irrigation water salinity with 0.65, 3.2, and 6.1 dS m-1 (s1, s2 and s3) were arranged in a randomized split-plot design with three replications for each treatment. In 2008, yield increased with increasing irrigation amount under both fresh and saline water irrigation. However, in 2009 and 2010, the highest yield at the same salinity level under saline water irrigation was obtained by w2. Actual evapotranspiration (ETa) decreased with decreasing irrigation amount. Therefore, w2 got higher water use efficiency (WUE) (1.25-1.63 kg m-3) and irrigation water use efficiency (IWUE) (2.11-2.36 kg m-3) than w1, which indicated that irrigation amount 300 mm is beneficial to yield and water use efficiency at water salinity 3.2 and 6.1 dS m-1. Thus, for the purpose of highest yield and WUE, irrigation amount should be controlled at appropriate level under saline water irrigation. The effect of irrigation water salinity on ETa was significant in 2009 and 2010, while the effect on yield, WUE and IWUE was only significant in 2010. However, the differences of yield, ETa, WUE and IWUE between s2 and s1 were statistically insignificant in the 3 years. It can be concluded that irrigation water salinity 3.2 dS m-1 has no significant effect on wheat yield and water productivity. The interaction effects of irrigation amount and water salinity on yield, ETa and WUE were statistically insignificant in the experiments.
机译:在某些干旱和半干旱地区,淡水短缺和水质恶化限制了农业的可持续发展。因此,必须采用亏缺灌溉和盐水灌溉来维持作物的产量。为了确定西北干旱地区合理的灌溉管理方式,分别于2008年,2009年和2010年进行了田间试验,研究了灌溉量和水盐度对春小麦耗水量和水分生产率的影响。总共进行了9种灌溉处理,包括375、300和225 mm(w1,w2和w3)的三个水平的灌溉水量和0.65、3.2和6.1 dS m -1 (s1,s2和s3)按随机分割图设计,每种处理重复3次。 2008年,在淡水和盐水灌溉下,产量都随着灌溉量的增加而增加。然而,在2009年和2010年,通过咸水灌溉,在相同盐度水平下获得了最高产量。实际蒸散量(ET a )随着灌溉量的减少而降低。因此,w2的水分利用效率(WUE)(1.25-1.63 kg m -3 )和灌溉水利用效率(IWUE)(2.11-2.36 kg m -3 )较高。 )比w1高,说明在盐分3.2和6.1 dS m -1 时,灌溉量300 mm有利于产量和水分利用效率。因此,为达到最高产量和WUE的目的,应在盐水灌溉下将灌溉量控制在适当的水平。灌溉水盐度对ET a 的影响在2009年和2010年显着,而对产量,WUE和IWUE的影响仅在2010年显着。但是,产量差异ET a ,s2和s1之间的WUE和IWUE在3年内无统计学意义。可以得出结论,灌溉水盐度为3.2 dS m -1 对小麦的产量和水分生产率没有显着影响。在试验中,灌溉量和水盐度对产量,ET a 和WUE的相互作用影响均无统计学意义。

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