Abstract
On soils of low P supply organic P (Po) makes up a similar or even larger part in soil solution than inorganic P (Pi). The ability of wheat (Triticum aestivum L., cv. Star) plants to hydrolyze and absorb this Po in comparison to similar concentrations of Pi was studied. Four concentration levels of Pi and Po were obtained by extracting two soils with deionized water in a ratio of 1:1 and concentrating the resulting filtrate by freeze drying to different degrees. The concentration of Pi varied between 5 and 36 μM and Po between 3 and 22 μM. Wheat seedlings were grown in these solutions for 12 and 24 h and acid and alkaline phosphatase activity determined. The reduction of Po concentration in solution expressed on a root length basis gave the rate of Po hydrolysis and the reduction in concentration of Pi and Po gave the P inflow into the roots. No alkaline phosphatase activity was detected. The activity of wheat root acid phosphatase increased with Po concentration in solution. Phosphorus uptake was 2 to 6 fold higher from Pi than from Po at similar concentrations of both. The rate of uptake from Pi, the inflow, as well as the rate of hydrolysis of Po increased linearly with concentration but at similar concentration the inflow was 2 to 4 times higher than the rate of Po hydrolysis. Results suggest that plants can utilize Po after hydrolysis by phosphatase, but Pi is more important and preferentially used by plants; Po may be essential for plant nutrition especially in high P-fixing soils.
Published Version
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