Abstract

Rhizosphere processes play a critical role in phosphorus (P) acquisition by plants and microbes, especially under P-limited conditions. Here, we investigated the impacts of nutrient addition and plant species on plant growth, rhizosphere processes, and soil P dynamics. In a glasshouse experiment, blue lupin (Lupinus angustifolius), white clover (Trifolium repens L.), perennial ryegrass (Lolium perenne L.), and wheat (Triticum aestivum L.) were grown in a low-P pasture soil for 8 weeks with and without the single and combined addition of P (33 mg kg−1) and nitrogen (200 mg kg−1). Phosphorus addition increased plant biomass and total P content across plant species, as well as microbial biomass P in white clover and ryegrass. Alkaline phosphatase activity was higher for blue lupin. Legumes showed higher concentrations of organic anions compared to grasses. After P addition, the concentrations of organic anions increased by 11-,10-, 5-, and 2-fold in the rhizospheres of blue lupin, white clover, wheat, and ryegrass, respectively. Despite the differences in their chemical availability (as assessed by P fractionation), moderately labile inorganic P and stable organic P were the most depleted fractions by the four plant species. Inorganic P fractions were depleted similarly between the four plant species, while blue lupin exhibited a strong depletion of stable organic P. Our findings suggest that organic anions were not related to the acquisition of inorganic P for legumes and grasses. At the same time, alkaline phosphatase activity was associated with the mobilization of stable organic P for blue lupin.

Highlights

  • From gene duplication to root system development and photosynthesis, phosphorus (P) is involved in a plethora of biological and biochemical mechanisms that are critical to crop production [1,2]

  • In terms of the total plant biomass, plant species reacted to P addition as follows: white clover > ryegrass > wheat > blue lupin

  • Total P content was enhanced by 5.3, 3.7, 1.5, and 0.4-fold after P addition in white clover, ryegrass, wheat, and blue lupin, respectively; whereas in the NP

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Summary

Introduction

From gene duplication to root system development and photosynthesis, phosphorus (P) is involved in a plethora of biological and biochemical mechanisms that are critical to crop production [1,2]. The total amount of P in soils may exceed plant requirements; only a small amount is available for plant uptake [3]. Soil P is present in inorganic and organic forms [4]. Inorganic P is subject to adsorption and precipitation with iron (Fe), aluminum (Al), and calcium (Ca) cations, as well as with positively charged soil particles [5,6], whereas organic P represents up to 65% of total P and requires a mineralization step to become available for plant uptake [7,8,9,10,11]. The exudation of protons from plant roots is used by P-deficient plants to acidify the soil and solubilize inorganic

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