Agricultural systems that receive high amounts of inorganic nitrogen (N) fertilizer in the form of either ammonium (NH
4+), nitrate (NO
3−) or a combination thereof are expected to differ in soil N transformation rates and fates of NH
4+ and NO
3−. Using
15N tracer techniques this study examines how crop plants and soil microbes vary in their ability to take up and compete for fertilizer N on a short time scale (hours to days). Single plants of barley (
Hordeum vulgare L. cv.
Morex) were grown on two agricultural soils in microcosms which received either NH
4+, NO
3− or NH
4NO
3. Within each fertilizer treatment traces of
15NH
4+ and
15NO
3− were added separately. During 8 days of fertilization the fate of fertilizer
15N into plants, microbial biomass and inorganic soil N pools as well as changes in gross N transformation rates were investigated. One week after fertilization 45-80% of initially applied
15N was recovered in crop plants compared to only 1-10% in soil microbes, proving that plants were the strongest competitors for fertilizer N. In terms of N uptake soil microbes out-competed plants only during the first 4 h of N application independent of soil and fertilizer N form. Within one day microbial N uptake declined substantially, probably due to carbon limitation. In both soils, plants and soil microbes took up more NO
3− than NH
4+ independent of initially applied N form. Surprisingly, no inhibitory effect of NH
4+ on the uptake and assimilation of nitrate in both, plants and microbes, was observed, probably because fast nitrification rates led to a swift depletion of the ammonium pool. Compared to plant and microbial NH
4+ uptake rates, gross nitrification rates were 3-75-fold higher, indicating that nitrifiers were the strongest competitors for NH
4+ in both soils. The rapid conversion of NH
4+ to NO
3− and preferential use of NO
3− by soil microbes suggest that in agricultural systems with high inorganic N fertilizer inputs the soil microbial community could adapt to high concentrations of NO
3− and shift towards enhanced reliance on NO
3− for their N supply.
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