• ISSN 1008-505X
  • CN 11-3996/S

控制排水调控土壤水、磷动态及大豆磷素吸收利用

Controlled drainage regulates soil water-phosphorus dynamics and soybean phosphorus uptake

  • 摘要:
    目的 针对淮北平原砂质壤土区旱涝频发现状,探讨控制排水对土壤水分、不同形态磷含量动态变化及大豆磷素吸收利用的影响,分析控制排水提升磷素利用效率的机制,为该区域土壤水肥高效利用和排水调控提供理论依据。
    方法 试验在安徽省水利厅新马桥灌溉试验中心站开展,以大豆为供试作物进行测坑受渍试验,设置3个排水控制深度:距地表50 cm (WT50)、100 cm (WT100)和20~30 cm (WTvar),以及全生育期地下水埋深固定为50 cm的非受渍条件作为对照(CK)。监测受渍排水期、间歇期和全生育期土壤含水率、不同形态磷含量及生育期末大豆各器官干物质积累量、磷含量、磷素积累量,分析各时段始末的土壤含水率及磷含量变化以探究土壤水磷的时段变幅。结合相关分析、随机森林模型和结构方程模型解析控制排水对磷肥利用效率的影响机制。
    结果 受渍显著降低叶片磷素积累量20.2%~34.1%和叶片磷含量16.5%~22.3%,而WT50处理整株、地上部、叶、籽粒及荚的磷素积累量降幅均最小。受渍显著降低了WTvar和WT100处理的磷肥偏生产力,而WT50处理降幅不显著。受渍排水期,WT50处理0—20 cm土壤水溶性磷含量增幅比WTvar处理显著减小22.6%,而WT100处理降幅较大且与前两者差异显著,WTvar和WT50处理0—20 cm土壤全磷含量降幅均显著小于WT100处理。间歇期,WT50处理40—60 cm土壤有效磷含量降幅显著大于WTvar和WT100处理,WT50处理0—20 cm土壤水溶性磷含量降幅比WTvar显著减小40.5%,而WT100处理增幅较大且与前两者差异显著。全生育期内,WT50处理20—40 cm土壤全磷含量降幅显著大于WT100处理,同时30—40 cm土壤含水率增幅显著高于WT100处理。Pearson相关分析表明,磷肥吸收效率和磷肥偏生产力均与整株、地上部、籽粒和荚的干物质积累量,及整株、地上部、籽粒的磷素积累量显著正相关;磷肥偏生产力还与荚磷素积累量、叶磷含量显著正相关,与地下水埋深超标准累积值(SEW50)显著负相关。随机森林模型和结构方程模型进一步表明,控制排水通过改变SEW50,直接影响大豆籽粒和荚的干物质积累量和土壤有效磷、全磷残留量,并间接影响籽粒磷素积累,从而调控磷肥利用效率。
    结论 淮北平原砂质壤土区,50 cm排水控制深度可显著改善耕层水分状况,提升土壤磷素有效性,进而提高大豆磷肥利用效率。

     

    Abstract:
    Objectives In response to the frequent alternation of drought and waterlogging in sandy loam soils of the Huaibei Plain, this study investigated the effects of controlled drainage on the dynamic of soil moisture and phosphorus fractions, as well as on phosphorus uptake and utilization in soybean. The aim was to elucidate the mechanisms by which controlled drainage enhances phosphorus use efficiency and to provide a scientific basis for drainage regulation for the efficient use of soil water and nutrients.
    Methods The experiment was conducted at the Xinmaqiao Irrigation Experimental Center of the Anhui Provincial Department of Water Resources. A soybean waterlogging experiments were conducted. Three controlled drainage depths were set: 50 cm (WT50), 100 cm (WT100), and a variable depth of 20−30 cm (WTvar) below the surface. A non-waterlogged condition with the groundwater table depth fixed at 50 cm throughout the entire growth period was used as the control (CK). Soil water content, groundwater table depth, soil phosphorus fractions, soybean dry matter accumulation, soybean P content, and total P accumulation in various soybean organs were measured during the waterlogging-drainage stage, intermittent stage, and the whole growth period. Analyze the changes in soil water content and phosphorus content at the beginning and end of each time period to investigate the temporal variation amplitudes of soil water and phosphorus. Correlation analysis, random forest model, and structural equation model were employed to analyze the regulatory pathways of controlled drainage on phosphorus fertilizer use efficiency.
    Results Waterlogging significantly reduced leaf P accumulation and content by 20.2%−34.1% and 16.5%−22.3%, respectively, whereas WT50 showed the smallest reductions in P accumulation in the whole plant, aboveground parts, leaves, seeds, and pods. Waterlogging significantly decreased the partial factor productivity of P fertilizer under WTvar and WT100, while WT50 was less affected. During the waterlogging-drainage stage, the increase in water-soluble P in the 0−20 cm soil layer under WT50 was 22.6% lower than that under WTvar, while WT100 showed a larger decrease with significant differences from both. The reduction in total P in the 0−20 cm soil layer under WTvar and WT50 was significantly smaller than that under WT100. During the intermittent stage, the decrease in available P in the 40−60 cm layer under WT50 was significantly larger than that under WTvar and WT100. The decrease in water-soluble P in the 0−20 cm layer under WT50 was 40.5% smaller than that under WTvar, whereas WT100 exhibited a marked increase. In the whole growth period, the reduction in total P in the 20−40 cm layer under WT50 was significantly greater than that under WT100. The increase in soil water content at the 30-40 cm depth under WT50 treatment was significantly higher than that under WT100 treatment. Pearson correlation analysis showed that phosphorus uptake efficiency and partial factor productivity were significantly and positively correlated with dry matter accumulation of the whole plant, aboveground parts, grains, and pods, as well as with phosphorus accumulation in the whole plant, aboveground parts, and grains. In addition, partial factor productivity of P fertilizer was significantly positively correlated with phosphorus accumulation in pods and leaf phosphorus concentration, but significantly negatively correlated with the cumulative value of groundwater table depth exceeding the threshold (SEW50). Random forest and structural equation models further indicated that controlled drainage affected soybean seed and pod dry matter accumulation as well as soil available and total P retention by altering SEW50, thereby indirectly influencing seed P accumulation and regulating P fertilizer use efficiency.
    Conclusions A controlled drainage depth of 50 cm in sandy loam soils of the Huaibei Plain significantly improved soil moisture conditions in the plough layer and enhanced soil phosphorus availability, thereby increasing phosphorus fertilizer use efficiency in soybean.

     

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