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Dilute Acid Extraction is a useful Indicator of the Supply of Slowly Available Phosphorus in Vertisols
Author(s) -
McLaren Timothy I.,
Guppy Christopher N.,
Tighe Matthew K.,
Moody Phil,
Bell Mike
Publication year - 2014
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2013.05.0188
Subject(s) - vertisol , bicarbonate , chemistry , soil water , phosphorus , environmental chemistry , solubility , zoology , agronomy , environmental science , soil science , biology , organic chemistry
Long‐term studies suggest readily available P, measured using a bicarbonate extractant, can be replenished by slowly available inorganic P pools. The aim of this study was to estimate the supply of slowly available P to the soil solution. Readily and slowly available P pools were measured using two agronomic soil P tests (the bicarbonate (Colwell) and dilute acid (Bureau of Sugar Experiment Stations; BSES) extractants, respectively) in vertisol soils of the northern grains region (NGR) of eastern Australia. The amount of P supplied to the soil solution was estimated by the iron oxide sink method accumulated over 96 h (FeOt‐P). The readily available P pool (i.e., Colwell‐P) was strongly correlated with FeOt‐P, and this pool was likely to be replenished by the slowly available P pool (i.e., BSES‐P) when BSES‐P concentrations were >61 mg P kg −1 . The slowly available P pool did not supply the readily available P pool when the Ca (mg kg −1 )/P (mg kg −1 ) ratio in the BSES extract was >74:1, suggesting the presence of Ca phosphates of low solubility affected potential buffering. Using a multiple linear regression, approximately 75% of the variability in the ability of the slowly available P pool to supply soil solution P could be explained by the quantity of BSES‐P and the ratio of Ca/P in the BSES extract.