• ISSN 1008-505X
  • CN 11-3996/S
MO Gui-mei, ZHANG Ze-kun, HE Lu-lu, JIN Qian-wei, DU Yi-chun, HE Hong-hua. Regulatory effects of fulvic acid on soil phosphorus availability, maize growth, and phosphorus uptake under different phosphorus levels and water conditions in arid regionsJ. Journal of Plant Nutrition and Fertilizers, 2025, 31(7): 1366-1377. DOI: 10.11674/zwyf.2024569
Citation: MO Gui-mei, ZHANG Ze-kun, HE Lu-lu, JIN Qian-wei, DU Yi-chun, HE Hong-hua. Regulatory effects of fulvic acid on soil phosphorus availability, maize growth, and phosphorus uptake under different phosphorus levels and water conditions in arid regionsJ. Journal of Plant Nutrition and Fertilizers, 2025, 31(7): 1366-1377. DOI: 10.11674/zwyf.2024569

Regulatory effects of fulvic acid on soil phosphorus availability, maize growth, and phosphorus uptake under different phosphorus levels and water conditions in arid regions

  • Objectives Drought and phosphorus (P) deficiency seriously affect soil P availability and restrict crop growth. This study aimed to reveal the effects of fulvic acid (FA) on soil P availability, maize growth and P uptake under drought stress with different P levels, in order to provide a theoretical basis for P-utilization efficiency and agricultural development in arid regions.
    Methods A pot experiment with three factor-three level design was conducted using maize in a loess soil. The low, medium, and high P levels were 30 (P30), 60 (P60), and 120 mg/kg (P120); the normal (W1), mild drought (W2), and moderate drought (W3) water conditions were 75%, 60%, 45% of field capacity, respectively; and the three application rates of FA were 0 (FA0), 50 (FA1), and 100 mg/kg (FA2), respectively. The maize was harvested after 60 days of growth for measurement of plant height, biomass and P concentration. At the same time, soil pH, Olsen-P, P fraction concentration, alkaline phosphatase activity and organic acid in rhizosphere were determined.
    Results FA enhanced soil P availability under drought conditions, and its effect was related to P application and water conditions. At P60W2 and P120W2, FA1 and FA2 treatments significantly reduced soil pH by 0.14−0.21 units through acidification effects, resulting in 15%−19% and 44%−47% increases in soil Olsen-P and labile P concentration, respectively. At P60W3, FA2 treatment increased tartrate and Olsen-P concentration. Moreover, there was a positive (P<0.05) correlation between tartrate and Olsen-P concentration, indicating that fulvic acid could improve soil P availability by promoting the secretion of organic acid in rhizosphere. Under drought conditions at any P treatment level, FA had no significant effect on soil alkaline phosphatase activity. At P30W2, FA1 and FA2 treatments reduced various parts of maize biomass (35%−39%) and plant P accumulation (20%−38%). However, at P60W2 and P120W2, FA promoted maize growth and P uptake. At P60W2, applying FA2 increased P-uptake efficiency by 38%. At P120W2, applying FA1 increased maize plant height by 10%, and applying FA2 increased root P concent by 12%.
    Conclusions Under drought and medium to high soil P conditions, the application of fulvic acid can drive the transformation of soil P forms through acidification effects and the regulation of organic acid in rhizosphere, increasing soil Olsen-P and labile P concentration, and thus improving soil P availability. However, only under mild drought conditions can the application of fulvic acid promote maize growth and P uptake.
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