• ISSN 1008-505X
  • CN 11-3996/S

局部供磷主要改变根−土互作磷吸收过程而非叶磷组分分配促进玉米生长

Localized phosphorus application promotes maize growth more through modified root-soil interactions conducive to phosphorus uptake than leaf phosphorus allocation patterns

  • 摘要:
    目的 土壤养分分布呈异质性,本研究通过不同磷肥局部供应模拟土壤磷不均匀分布的环境,探究玉米地下部根−土互作过程中根系磷高效吸收机制,并系统地关联地上部叶磷组分及其分配模式变化中磷高效利用过程的响应规律,为玉米生产磷肥合理施用及磷资源可持续利用提供依据。
    方法 以郑单958玉米(Zea mays L. cv. ZD958)为供试材料,在钙质土壤中进行了盆栽试验。设置磷肥均匀供应和局部供应两种供应方式,每个模式下分别施用磷酸一铵(MAP)、磷酸二铵(DAP)和磷酸二氢钾(PK)三种磷源肥料。测定了玉米地上部生物量和磷浓度,分析了上位叶、中位叶和下位叶中的主要有机磷组分(包括代谢磷、核酸磷、脂质磷和残渣磷);测定玉米根系形态(总根长、根表面积、侧根长度及其密度等)和生理特征(根际pH、有机酸浓度和酸性磷酸酶活性)。
    结果 相较于均匀供磷,局部供磷显著提高了玉米地上部生物量(20.0%)和磷积累量(39.1%),其中磷酸二铵效果最佳。局部供磷显著优化了玉米根系形态特征,总根长、一级侧根长度及密度增加,根表面积扩大,根际酸化加剧,有机酸分泌量与酸性磷酸酶活性提升。此外,局部供磷提高了玉米中位叶和下位叶的代谢磷浓度以及上位叶的核酸磷浓度,而其它叶片磷组分未改变,且各叶位磷组分下位叶向上位叶的再转移效率保持不变。磷肥供应方式和种类对玉米各叶位磷组分浓度及其分配模式的影响相对有限。结构方程模型进一步分析表明,磷肥供应方式与种类显著改变玉米根系形态(路径系数分别为0.87和0.64)和生理特征(路径系数分别为0.80和0.49),二者与地上部生长显著正相关(P<0.05),是促进玉米地上部生长的主要因素,而非直接作用于叶磷组分及其分配模式。
    结论 在钙质土壤中,局部供磷有效提升玉米根系对磷的利用能力,主要通过促进根系伸长、增加侧根密度与细根比例,并降低根际pH、增强有机酸分泌和酸性磷酸酶活性;而非通过改变玉米叶磷的组成及再分配。这一结果凸显了根−土互作在玉米磷高效利用中的核心地位。

     

    Abstract:
    Objectives Considering the heterogeneous distribution of soil nutrients, this study simulated a soil environment with uneven phosphorus (P) availability through localized P fertilizer application to investigate the mechanisms underlying efficient P acquisition of maize roots during the root-soil interaction process. It systematically correlated the response patterns of high P utilization efficiency with changes in maize leaf P fractions and their allocation. This research provides a basis for rational P fertilizer application and sustainable P resource use in maize production.
    Methods A pot experiment was conducted using Zea mays L. cv. ZD958 as the experimental material in calcareous soils. Two P fertilizer application ways (uniform and localized application) were set up, and each combined with three types of P fertilizers: monoammonium phosphate (MAP), diammonium phosphate (DAP), and potassium dihydrogen phosphate (KP). Aboveground biomass and P concentration were analyzed, and the main organic P fractions (metabolic P, nucleic acid P, lipid P, and residual P) in the upper, middle, and lower leaves were measured. The root morphological traits (total root length, root surface area, lateral root length and density, etc.) and the physiological traits (rhizosphere pH, carboxylate concentration, and acid phosphatase activity) were also assessed.
    Results Compared to uniform P fertilizer application, localized P fertilizer application significantly increased maize shoot biomass by 20.0% and P accumulation by 39.1%, with DAP exhibiting the highest beneficial effect. Localized P application demonstrated promotion effect on root morphological traits: increased total root length, 1st-order lateral root length and density, and root surface area, and on the physiological traits: intensified rhizosphere acidification, increased carboxylate concentration and acid phosphatase activity. Localized P application increased metabolic P concentrations in middle and lower leaves and nucleic acid P concentrations in upper leaves, while other fractions and their remobilization characteristics from lower to upper leaves remained unchanged. The effects of application way and P fertilizer types on leaf P fractions and their allocation were relatively limited. Partial least squares path modelling analysis showed that the P fertilizer application way and type significantly altered morphological (path coefficients of 0.87 and 0.64, respectively) and physiological traits (path coefficients of 0.80 and 0.49, respectively) of maize roots. Notably, the root morphological and physiological traits exhibit a significant positive correlation with maize aboveground growth (P<0.05), rather than directly affecting leaf P fractions and their allocation.
    Conclusions In calcareous soils, localized P application effectively enhances the P utilization capacity of maize roots primarily by promoting root elongation, increasing the density of lateral root branching and the proportion of fine roots, lowering rhizosphere pH, and boosting organic acid secretion and acid phosphatase activity, rather than through influencing the composition and redistribution of P in maize leaves. This highlights the central role of root-soil interactions in the efficient P utilization of maize.

     

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