A simple diffusion test for soil phosphorus availability

The availability of phosphorus to plants was estimated by a new method based on the diffusion of P from a thin layer of water-saturated stationary soil to a disc of iron oxide coated filter paper. Twenty-one acid Finnish soil samples were tested using four modifications of the method which differed in the duration of the diffusion time and in the thickness of the soil layer. The new diffusion tests were compared with other soil P testing methods and evaluated as indicators of the availability of P to pot-grown barley and oats. Close linear correlations were found between the initial (18 or 42 h) P diffusion rate and the water extractable P contents determined at the extraction ratios of 1:10 and 1:60, respectively (r=0.97–0.99). The amounts of P obtained by the new method were small when the diffusion time was short, but after prolonged diffusion (1 week) the test values were close to the amounts of P taken up by plants. The relationships of plant yield and P uptake with soil P test values were affected by soil acidity. Although the original soil P test values were significantly correlated, the accuracy of all methods drastically improved when the interfering effect of soil acidity was taken into account using a simple pH-correction model. The correlation coefficients (r) between the test values of diffusible P in soil and the uptake of P by plants increased up to 0.97.