Nutrient management in a <i>Pinus</i><i>radiata</i> plantation after thinning: the effect of nitrogen fertilizer on soil nitrogen fluxes and tree growth

J. C. Carlyle

Canadian Journal of Forest Research · 1995 · 33 citations · 0 references

Concepts

Abstract

The influence of N fertilizer on soil mineral N fluxes, canopy development, and tree growth was studied in a thinned 11-year-old Pinusradiata D. Don plantation. Ammonium sulphate and single superphosphate were applied in an incomplete factorial design, but only the main effects of N application at 0 (control) or 200 kg N•ha −1 are considered here. Spring application of fertilizer increased the quantity of mineral N in the forest floor plus surface soil (0–0.30 m) from 1.2 to 194 kg•ha −1 . Within 51 weeks this had fallen to 8.3 kg•ha −1 , and after 89 weeks had returned to prefertilizer levels. In the unfertilized soil, rates of net mineralization were low with little seasonal variation. Nitrogen fertilizer increased N mineralization; over the 2 years of measurement fertilized and unfertilized soils mineralized 155 and 77 kg N•ha −1 , respectively. There was no net immobilization of fertilizer N. There was no leaching of mineral N from the unfertilized soil whereas 149 kg N•ha −1 was leached below 0.30 m during the 2 years after fertilizer application. Nitrogen uptake increased from 71 kg•ha −1 in the control to 203 kg•ha −1 in the fertilized treatment. Fifty-one percent (103 kg•ha −1 ) of N uptake by trees in the fertilized treatment occurred within 20 weeks of fertilizer application. Fertilized trees took up 58% of the available N (N added as fertilizer plus N mineralized), while 42% was leached. Ammonium dominated the soil mineral N pool and mineral N fluxes, with nitrate generally accounting for less than 10% of mineral N in both fertilized and unfertilized soils. Leaching of mineral N from the fertilized soil (N leach , kg•ha −1 •week −1 ) was highly correlated (r 2 = 0.92) with soil mineral N content (N start , kg•ha −1 ) and effective rainfall (rainfall minus evaporation, R eff , mm•week −1 ) according to the relationship N leach = aN start + bR eff , while N uptake (kg•ha −1 •week −1 ) was highly correlated (r 2 = 0.91) with soil mineral N content and N mineralization (N min , kg•ha −1 •week −1 ) according to the relationship N uptake = aN start + bN min . Fertilizer increased needle N concentrations and content by 52 and 87%, respectively, after 58 weeks, and resulted in a 17% increase in leaf area index after 71 weeks. These differences were reflected by an increase in basal area increment of 23% during the 2 years since fertilizer application. The rapid uptake of N fertilizer was associated with storage in existing biomass. Uptake of fertilizer N should, therefore, increase with plantation biomass. Consequently, it should be possible to increase the uptake of N fertilizer, and minimize leaching, by applying fertilizer before, rather than after, thinning. Such a strategy may be particularly appropriate for soils that have a low capacity to retain applied N.