中国农业科学 ›› 2006, Vol. 39 ›› Issue (12): 2449-2458 .

• 耕作栽培·生理生态 • 上一篇    下一篇

冬小麦产量与籽粒蛋白质含量协同变化特点及水肥调控

张玉峰,杨武德,白晶晶,王大成,牛 波,冯美臣   

  1. 山西农业大学文理学院数学系
  • 收稿日期:2005-11-11 修回日期:2006-09-04 出版日期:2006-12-10 发布日期:2006-12-10
  • 通讯作者: 杨武德

Coordinated Variation Law of Yield and Grain Protein Content in Winter Wheat and Strategies of Irriagation and Fertilization

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  1. 山西农业大学文理学院数学系
  • Received:2005-11-11 Revised:2006-09-04 Online:2006-12-10 Published:2006-12-10

摘要: 【目的】揭示冬小麦产量与籽粒蛋白质含量协同变化特点,为小麦高产优质栽培决策提供依据。【方法】根据盆栽水肥和田间肥料试验数据建立冬小麦产量和籽粒蛋白质含量关于土壤水分含量及氮磷肥的单因素和两因素效应函数,通过对函数曲线变化状态及其特点的分析,揭示小麦产量和蛋白质含量在不同水肥条件下的协同变化特点及其条件,并据此确定各种条件下高产优质的水肥管理方案。【结果】低肥和中肥(或土壤水分含量为田间最大持水量的50%和60%)条件下,产量和籽粒蛋白质含量随土壤水分含量(或施氮量)增加的曲线分别为凸型和凹型。蛋白质含量最低值和产量最高值之间对应的施氮量为产量和蛋白质含量在土壤水分含量为田间最大持水量的50%和60%条件下协同变化的施氮量区间。在高肥和土壤水分含量为田间最大持水量的70%和80%条件下,产量和蛋白质含量曲线均为凸型,蛋白质含量达到最大值之前对应的土壤水分含量为高肥条件下产量和蛋白质含量协同变化区间;产量达到最大值之前对应的施氮量为土壤水分含量为田间最大持水量的70%和80%条件下产量和蛋白质含量协同变化区间。【结论】在一定的水肥条件下,小麦产量和蛋白质含量协同变化是可能的。用极差变换将产量和蛋白质含量理论值标准化,其标准值曲线的交点即为二者的最佳结合点。用等值线图描述产量和蛋白质含量的水氮和氮磷两因素效应,分析产量和蛋白质含量变化规律及其关系,确定实现一定生产目标的水肥管理方案。这为小麦高产优质水肥调控提供了一种行之有效的方法。

关键词: 冬小麦, 籽粒蛋白质含量, 协同变化规律, 水肥调控

Abstract: Abstract Based on the pot cultivation and the field experiments, the effect functions of winter wheat yield and grain protein content were established, in which the soil water content and nitrogen and P2O5 were taked as the effect factors. The function curves reveal the coordinated variation law of yield and grain protein content with increase of soil water content (or nitrogen) at different nitrogen dose (or soil water content). The results indicated that the variation curves of yield and grain protein content with soil water content (or nitrogen) are convex and concave respectively in lower fertility and mean fertility (or 50% and 60% of soil water content), and that means the negative correlation of yield and grain protein content. But the yield and grain protein content are all increasing with soil water content increasing between minimum protein content and maximum yield in mean fertility. So the soil water content between minimum protein content and maximum yield are the soil water content of coordinated variation of yield and grain protein content (Fig.1 and Fig.2). The variation curves of yield and grain protein content with soil water content (or nitrogen) are convex in high fertility (or 70% and 80% of soil water content), and the soil water content (or nitrogen dose) before maximum protein content (or maximum yield) are the soil water content (or nitrogen dose) of coordinated variation of yield and grain protein content (Fig. 1 and Fig.2). The simulated value of yield and grain protein content were standardized using polar difference variant, and the intersection point of curves of the standardized variables is the best combination of yield and grain protein content(Fig.3 and Fig.4). We can make the irrigation and fertilization management plan according to the intersection points and the variation state of the curves. The effect of yield and grain protein content with soil water content and nitrogen (or nitrogen and P2O5 ) was described by isopleth (Fig.5 and Fig.6). On the basis of the isogram, we can analyse the variation law of single factor or two factors in yield and grain protein content with soil water content, nitrogen and P2O5, and make management plans of high yield and high quality.

Key words: winter wheat, grain protein content, coordinated variation law, strategy of irrigation and fertilization