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The fate of freshly added phosphorus in representative agricultural soils
Author(s) -
Assimakopoulos J.,
Bovis C.,
Kosmas C.,
Nychas A.
Publication year - 1998
Publication title -
zeitschrift für pflanzenernährung und bodenkunde
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 0044-3263
DOI - 10.1002/jpln.1998.3581610313
Subject(s) - entisol , vertisol , chemistry , soil water , carbonate , alfisol , sorption , fractionation , mineralogy , phosphorus , nuclear chemistry , environmental chemistry , chromatography , geology , soil science , adsorption , organic chemistry
Surface and subsurface samples from 26 representative agricultural soils (13 Entisols, 9 Alfisols and 4 Vertisols) from Central and South Western Greece were equilibrated for a week with P solutions ranging from zero to 800 mg P kg −1 soil. The Freundlich and in the cases of high fine carbonate content (> 6%) the linear equations described the sorption isotherms in a satisfactory way. Sequential fractionation indicated that a 0.1 M NaOH plus 1 M NaCl + 0.3 M Na‐citrate + 1 M NaHCO 3 (buffer) solution extracted more than 60% of the P retained by Entisols containing low to medium fine carbonates and by Vertisols, and less than 60% by Entisols with a high fine carbonate content. In all Entisols, this percentage decreased significantly at P additions higher than 150 mg kg −1 . The opposite was observed in Vertisols, in which this fraction was the most important part of the retained P up to the maximum P addition. In contrast, in Alfisols this fraction reached 100%, but in the case of high Bray‐P (> 50 ppm) it was more than 100% of the retained P. The second fraction extracted with the 0.3 M Na‐citrate + 1 M NaHCO 3 buffer plus Na‐dithionite was found to be much smaller than the first fraction, increasing with P additions in absolute amounts but remaining constant as a percentage of the retained P, ranging from 15–35% among the studied samples. The third fraction obtained with 1 M HCl solution showed a peculiar behaviour. It was close to zero of the retained P in samples containing carbonates (Entisols and Vertisols) at P additions up to 300 mg kg −1 soil, but increased significantly at higher P additions and almost doubled in Entisols. Finally, the P fraction obtained after seven successive extractions with 0.01 M CaCl 2 , correlated well by a polynomial of 2nd degree equation with NaOH+CB‐P and linearly with Olsen‐P and Bray‐P.