Abstract

The microbial immobilization of ammonium and nitrate was measured by 13N organic measurements after the application of labelled urea, (NH 4) 2SO 4, KNO 3 (KN) or NH 4NO 3 with or without glucose in four different soils. In the soils incubated without glucose, the microbial immobilization of the added ammonium varied between 1.5 and 4 mg N kg −1 soil. No immobilization occurred at the expense of NO 3 when KN was applied. When glucose was added at the rate 500 mg C kg −1 soil, the immobilization was very active between the first and the third day, at 10°C. The maximal amounts of 13N immobilized were much higher for the [ 15N]urea, 15(NH 4) 2SO 4, 15NH 4NO 3 and 15NO 3K. treatments than for the NH 4 15NO 3 application. This preferential immobilization of NH 4 was also observed in pure cultures of bacteria isolated from one of the soils and attributed to the inhibition of nitrate uptake by ammonium. The immobilization ratio, immobilized N: decomposed C, was calculated for glucose, accounting for pool substitution effects and immobilization due to native C. It was independent of the form of N applied and similar between soils, c 45–48 mg N g −1 C.

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