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ABSTRACT
Four experiments were run to evaluate the resin and 32P methods as valid laboratory methods in a calcareous soil. Recovery of four levels of added KH2PO4, after several cycles of wetting, drying, and mixing was evaluated. Total-exchangeable P (TEP24) was determined by the carrier-free method, and resinextractable P by equilibrating 1 g soil sample with 2 g resin overnight. Equilibrium of 31P and 32P on the soil-solid phase was evaluated by measuring specific activities with time. Different soil-solution ratios, using water and 0.01M CaCl2 as extractants, were evaluated to determine their effects on the total exchangeable P. Water and four different salts at three different molarities were used as extractants with 1 and 2 g resin to determine total released P in solution and on the resin.
The recovery experiment showed a high correlation between added and recovered P, using both TEP24 and resin methods; the time-equilibration study indicated a lack of complete equilibrium between 31P and 32P after 2 hours shaking, and a near complete or complete equilibrium at 24 hours; different soil-solution ratios did not affect total exchangeable P, and water extracted the most resin-P and 0.01M CaSO4 the least (roughly one-half of pure water):
1 Contribution from the USDA, Science and Education Administration in cooperation with the Colorado State Univ. Experiment Station. Scientific Series No. 2253.
2 Soil Scientists, USDA-SEA, Agron. Dept., Colorado State Univ., Fort Collins, CO 80523.
Received for publication October 25, 1977. Accepted for publication August 31, 1978.
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