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Phosphorus availability for plant uptake in a phosphorus-enriched noncalcareous sandy soil
G F Koopmans1, W J Chardon, P A I Ehlert
1Wageningen University and Research Centre (WUR), P.O. Box 47, 6700 AA, Wageningen, The Netherlands. gerwin.koopmans@wur.nl
Journal of Environmental Quality
|July 1, 2004
Summary
Mining soil phosphorus by growing crops can effectively reduce phosphorus in P-enriched soils. This strategy lowers phosphorus in soil solution, decreasing the risk of phosphorus leaching into the environment.
Area of Science:
- Soil Science
- Environmental Chemistry
- Agronomy
Background:
- Phosphorus (P)-enriched soils pose a risk of P leaching.
- Mining soil phosphorus, through crop uptake without external P addition, is a proposed management strategy.
- Understanding long-term soil P availability is crucial for effective management.
Purpose of the Study:
- To evaluate the effectiveness of mining soil phosphorus in reducing P in different soil pools.
- To determine the long-term availability of soil phosphorus in P-enriched sandy soil.
- To assess the impact of soil layer thickness on P mining efficiency.
Main Methods:
- A 978-day greenhouse pot experiment with grass grown on P-enriched soil at zero P application.
- Analysis of soil phosphorus in solution (0.01 M CaCl2 extracts) and sorbed P (P(ox)).
- Construction of desorption isotherms using the Langmuir equation to model P availability.
Main Results:
- Plant uptake can remove up to 65% of the total acid ammonium oxalate-extractable phosphorus (P(ox)) over the long term.
- The Langmuir equation accurately described the P desorption isotherm, indicating P(ox) is largely plant-available.
- Mining soil phosphorus significantly decreased P concentration in soil solution, reducing leaching risk.
Conclusions:
- Mining soil phosphorus is an effective strategy for reducing P concentration in soil solution in P-enriched soils.
- Long-term plant uptake can deplete a substantial portion of soil P, mitigating leaching risks.
- The strong nonlinearity of the desorption isotherm explains the greater relative decrease in soil solution P compared to P(ox).