Abstract

To evaluate phosphorus (P) availability and the role of microorganisms in P dynamics in the barley rhizosphere, we constructed a rhizobox using two arable Andosols under different fertilization management regimens and cultivated barley (Hordeum vulgare L. cv. Minorimugi) for 5 weeks. The phosphatase-labile pool of organic phosphorus (Po) was assessed using a phosphatase-addition approach in combination with chemical extraction of Po from soils. A considerable amount of inorganic P (Pi) in the NaHCO3 fraction was taken up by barley roots in a soil with high Pi availability, whereas Po, primarily phytate-like P in the NaHCO3 fraction, was hydrolyzed and then taken up by barley roots in a soil with low Pi availability. No significant utilization of either NaOH-Pi or NaOH-Po was observed for both soils during the 5-week cultivation. In the soil with low Pi availability, elevated acid phosphomonoesterase and phosphodiesterase activities, and greater utilization of Po substrates by bacteria in the Biolog ECO plate, were observed in the rhizosphere when compared with those in the bulk soil. This suggested enhanced Po hydrolysis by increased phosphatase activities to meet the P demand, making the Po an important P source for barley in the soil.

Highlights

  • Organic phosphorus (Po) comprises a considerable portion of phosphorus (P) in arableAndosols [1,2]

  • Because Po contributes to crop plant nutrition after its mineralization to inorganic P (Pi) [3], evaluating the lability of soil Po to phosphatase hydrolysis is indispensable for assessing P availability for crop plants in arable soils, in particular

  • Because of the remarkably high activity of phosphatase in the rhizosphere, which is produced by both plant roots and microorganisms [5,6], Po seems to be actively mineralized in the rhizosphere

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Summary

Introduction

Organic phosphorus (Po) comprises a considerable portion of phosphorus (P) in arableAndosols [1,2]. The spatial distribution of phosphatase activity in the rhizosphere was revealed using soil zymography [7] and many studies have suggested the utilization of Po in the rhizosphere by comparing the amount of Po between the rhizosphere and bulk soils [8,9,10], to our knowledge, no studies have assessed the availability of Po by examining phosphatase-hydrolyzable Po extracted from rhizosphere soils with millimeter order distances from plant roots. We assessed Po availability by phosphatase addition to extracts from the rhizosphere of barley cultivated in Andosols using the rhizobox system, which allowed a spatial resolution of 1 mm. Activities of acid phosphomonoesterase and phosphodiesterase and substrate utilization profiles in Biolog plates were determined to investigate the underlying basis of the P dynamics in the rhizosphere

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