基于地下水埋深的江汉平原冬小麦防涝渍排水指标确定

    Determination of groundwater depth-based drainage index against waterlogging and submergence for winter wheat in Jianghan Plain

    • 摘要: :2014-2015年在测坑(筒)分别开展孕穗期、灌浆期冬小麦遭受浅地下水埋深和先涝后渍胁迫试验,研究江汉平原冬小麦关键生育期适宜的地下水埋深。同时,构建不同排水标准计算方法,量化作物相对产量,提出先涝后渍胁迫下的排水指标。结果表明,孕穗期0、20和40 cm地下水位(持续受渍18 d)分别使小麦减产44.78%、17.31%和10.44%,而灌浆期相应减产67.72%、33.70%和10.34%。导致小麦减产的主要原因可能是穗粒数减少和千粒质量降低,建议江汉平原小麦田孕穗期和灌浆期地下水位维持在50 cm左右。先涝后渍过程中涝害使小麦减产幅度大于渍害,可以考虑以受涝历时和降渍历时为控制指标的排水模型、按时间划分涝害和渍害的排水模型,以及涝渍综合水深指标作为江汉平原小麦花后排除涝渍的排水模型。若允许小麦减产15%(即相对产量为85%)作为排水控制标准,建议小麦花后涝渍综合水深指标控制在275.6~283.6 cm·d。

       

      Abstract: Abstract: Jianghanplain area is characterized by plenty of rainfall in spring, which results in frequent occurrence of waterlogging of wheat field. Subsurface waterlogging is often found in these fields. It is necessary to investigate the influence of shallow groundwater table and waterlogging followed by submergence on the growth and yield and develop a suitable groundwater depth drainage index for the waterlogged fields. In order to achieve the objectives, tube-shaped concrete facilities were used for the irrigation and drainage adjustment experiment in 2014 and 2015. Wheat was planted in the facility. The treatment of shallow groundwater table at 0, 20, 40 and 60 cm sustained 18 d and different degrees of waterlogging followed by submergence were designed. The treatments were conducted in the booting and filling stages of wheat. The flooding depth in the waterlogging treatment was kept at 5 cm. Meanwhile, the facility for wheat cultivation in soil with moisture kept at 70%-80% of water holding capacity was used as a control. The results showed when the 0-cm groundwater table sustaining 18 d at booting and filling stage could reduce wheat yield by 44.78% and 67.72%, the 20-cm groundwater table sustaining 18 d could reduce the yield by 17.31% and 33.70%, the 40-cm groundwater table sustaining 18 d decreased the yield by 10.44% and 10.34% and the 60-cm groundwater table sustaining 18 d could had higher yield than the that under 100 cm, suggesting that the groundwater table kept at 50 cm at booting and filling stage of winter wheat was suitable. The yield reduction might be due to the decrease of kernels per and thousand seed weight. The regression showed that the yield could reach 95.1%-99.8% and 89.8%-96.9% of the control when the underground water depth was 40- 50 cm, it could reach 100% of the control when the underground water depth was 50.7 and 57.1 cm and it may slightly increase when the underground water depth was 60-80 cm. The wheat suffering from the damage of waterlogging followed by submergence after anthesis caused a severe reduction in wheat yield, and the surface waterlogging had the larger influence than subsurface waterlogging on yield of winter wheat. Different types of drainage indexes including surface and subsurface waterlogging duration days, sum of waterlogging or water table within 50 cm of soil surface, sum of both flood depth and water table within 50 cm of soil surface under surface waterlogging, sum of water table within 50 cm of soil surface after draining surface water logging, and comprehensive water depth of waterlogging were evaluated. The regression between relative yield and these indexes showed that the indexes with surface and subsurface waterlogging duration days, drainage model based on time classification and comprehensive water depth of waterlogging were reliable. If the wheat yield decrease by 15% was allowed, the comprehensive water depth of waterlogging should be 275.6-283.6 cm·d after anthesis. The research may provide support for wheat drainage management in booting and filling stage in the middle and lower reaches of the Yangtze River.

       

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