Phosphorus dynamics in Swedish agricultural soils as influenced by fertilization and mineralogical properties: Insights gained from batch experiments and XANES spectroscopy
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文摘

The dominant role of Al and Fe(hydr)oxides for accumulating added P was confirmed.

Neoformation of Ca phosphate occurred in 2 of 6 soils after long-term fertilization.

The P K-edge fluorescence intensity was strongly correlated with HCl-digestible P.

In unfertilized, non-calcareous soils, phosphate had a minimum solubility at pH 6–7.

Soil test P (P-AL) was related to the initial adsorbed P calculated from isotherms.

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