Legume introduction enhances rhizosphere phosphorus availability through organic acid-induced dissolution and microbial transformation: Insights from an 11-year field experiment in grassland

• Legume increase available P via increasing organic acid and genes for P activation • P addition reduces microbial P transformation • N addition accelerates depletion of available P While chemical fertilization offers a direct solution to restore soil fertility in degraded ecosystem, revegetation through legume introduction represents a more sustainable management strategy. However, the mechanisms by which legume introduction influence soil phosphorus (P) transformation, and how these processes respond to nutrient fertilization, remain poorly understood. Using one-time sampling from an 11-year field experiment, we investigated how the introduction of a legume ( Medicago falcata L.) influenced rhizosphere soil P fractions, both alone and in combination with nitrogen (N; 5 g m −2 yr −1 ) and P (3.2 g m −2 yr −1 ) fertilization. Our findings reveal that legume introduction stimulated the mobilization of soil P by increasing organic acid concentrations and microbial P demand, as indicated by the microbial biomass N:P ratio. This resulted in significant changes in P pools, marked by a 97.4% increase in labile inorganic P, a 22.9% decrease in moderately labile inorganic P, a 9.6% decrease in moderately labile organic P, and a 3.7% decrease in non-labile P pool. In contrast, while N fertilization promoted the solubilization of moderately labile inorganic P and the dissolution of the non-labile P pool by lowering soil pH and enhancing the abundance of genes for inorganic P solubilization, it ultimately led to a 10.6% depletion of the labile P pool. Phosphorus fertilization increased labile inorganic P, moderately labile inorganic P, and non-labile P, yet it inhibited microbial P transformation processes. Importantly, legume introduction mitigated the negative impacts of N fertilization on bioavailable P and the negative effects of P fertilization on microbial P mineralization genes. These findings suggest that legume introduction is a sustainable practice to stimulate P cycling in natural grassland, highlighting the importance of activating microbial functions in grassland management and restoration.

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Publication Details

Journal
Journal of Integrative Agriculture
Published
2025-12-01
DOI
https://doi.org/10.1016/j.jia.2025.12.003
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
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article

Legume introduction enhances rhizosphere phosphorus availability through organic acid-induced dissolution and microbial transformation: Insights from an 11-year field experiment in grassland

Chuan Fei Guo, Tongtian Guo, Jiqiong Zhou, Yingjun Zhang et al.
Journal of Integrative Agriculture
Soil Carbon and Nitrogen Dynamics
article

Legume introduction enhances rhizosphere phosphorus availability through organic acid-induced dissolution and microbial transformation: Insights from an 11-year field experiment in grassland

Chuan Fei Guo, Tongtian Guo, Jiqiong Zhou, Yingjun Zhang, Gaowen Yang, Meiqi Guo
article en

Abstract

• Legume increase available P via increasing organic acid and genes for P activation • P addition reduces microbial P transformation • N addition accelerates depletion of available P While chemical fertilization offers a direct solution to restore soil fertility in degraded ecosystem, revegetation through legume introduction represents a more sustainable management strategy. However, the mechanisms by which legume introduction influence soil phosphorus (P) transformation, and how these processes respond to nutrient fertilization, remain poorly understood. Using one-time sampling from an 11-year field experiment, we investigated how the introduction of a legume ( Medicago falcata L.) influenced rhizosphere soil P fractions, both alone and in combination with nitrogen (N; 5 g m −2 yr −1 ) and P (3.2 g m −2 yr −1 ) fertilization. Our findings reveal that legume introduction stimulated the mobilization of soil P by increasing organic acid concentrations and microbial P demand, as indicated by the microbial biomass N:P ratio. This resulted in significant changes in P pools, marked by a 97.4% increase in labile inorganic P, a 22.9% decrease in moderately labile inorganic P, a 9.6% decrease in moderately labile organic P, and a 3.7% decrease in non-labile P pool. In contrast, while N fertilization promoted the solubilization of moderately labile inorganic P and the dissolution of the non-labile P pool by lowering soil pH and enhancing the abundance of genes for inorganic P solubilization, it ultimately led to a 10.6% depletion of the labile P pool. Phosphorus fertilization increased labile inorganic P, moderately labile inorganic P, and non-labile P, yet it inhibited microbial P transformation processes. Importantly, legume introduction mitigated the negative impacts of N fertilization on bioavailable P and the negative effects of P fertilization on microbial P mineralization genes. These findings suggest that legume introduction is a sustainable practice to stimulate P cycling in natural grassland, highlighting the importance of activating microbial functions in grassland management and restoration.

Journal of Integrative Agriculture
Openalex Percentile: Top 53%
Soil Carbon and Nitrogen Dynamics
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